Powered by Deep Web Technologies
Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


1

Watershed characteristics contributing to the 1983-84 debris flows in the Wasatch Range, Davis County, Utah  

E-Print Network [OSTI]

and Centerville watersheds 65 Properties of soils in the Morgan Area, Utah Soil Survey that are comparable to soils in the study area (USDA, 1980) 73 LIST OF FIGURES Figure Page 1 Contour trenches in the Ford watershed as they appeared in 1988 2 Damage.... Much more sediment and debris were produced from canyon mouths than originally were mobilized from landslide material (Santi, 1988). Damage to residences in the paths of debris flows along the base of the Wasatch Range was extensive (Figure 2...

Coleman, William Kevin

2012-06-07T23:59:59.000Z

2

Analysis of the 1 December 2011 Wasatch downslope windstorm  

Science Journals Connector (OSTI)

A downslope windstorm on 1 December 2011 led to considerable damage along a narrow 50-km swath at the western base of the Wasatch Mountains in northern Utah. The strongest surface winds began suddenly at 0900 UTC, primarily in the southern portion ...

John Lawson; John Horel

3

Wasatch County, Utah: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Wasatch County, Utah: Energy Resources Wasatch County, Utah: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 40.3629418°, -110.9983515° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.3629418,"lon":-110.9983515,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

4

Hot Canyon  

ScienceCinema (OSTI)

This historical film footage, originally produced in the early 1950s as part of a series by WOI-TV, shows atomic research at Ames Laboratory. The work was conducted in a special area of the Laboratory known as the "Hot Canyon."

None

2013-03-01T23:59:59.000Z

5

La Jolla Canyon and Scripps Canyon Bibliography  

E-Print Network [OSTI]

said the cable was called Beal's Cable when he arrived atthe cable pre-dates 1951. Alan Beal worked for/with Francisunderwater canyons was done. Beal's Cable was laid by E.R. (

Brueggeman, Peter

2009-01-01T23:59:59.000Z

6

FINAL REPORT CANYON AND SLOPE  

E-Print Network [OSTI]

and the influence of canyons on slope cur- rents ; f) identification of communities which may be affected by oil#12;FINAL REPORT CANYON AND SLOPE PROCESSES STUDY VOLUME I EXECUTIVE S(2@lARY Prepared for United and provides diverse habi- tats for biological communities. In the Mid- and North Atlantic Region, canyons have

Mathis, Wayne N.

7

Camp Pendleton Kings Canyon  

E-Print Network [OSTI]

Camp Pendleton Marine Corps Base Kings Canyon National Park China Lake Naval Weapons Center Edwards Valley National Park Fort Irwin Mojave National Preserve Mono County Fresno County Inyo County Tulare County San Bernardino County Kern County Ventura County Los Angeles County Riverside County Orange County

8

Upper Los Alamos Canyon Cleanup  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Upper Los Alamos Canyon Cleanup Upper Los Alamos Canyon Cleanup Upper Los Alamos Canyon Cleanup The Upper Los Alamos Canyon Project involves cleaning up hazardous materials left over from some of the Laboratory's earliest activities. Contact Environmental Communication & Public Involvement P.O. Box 1663 MS M996 Los Alamos, NM 87545 (505) 667-0216 Email Located along Los Alamos Canyon from 7th Street to the Pajarito Ski Hill, the Upper Los Alamos Canyon Project involves examining sites in present and former Laboratory technical areas to see if any further environmental cleanup actions are needed. If not, the Laboratory can apply to have these sites removed permanently from LANL's Hazardous Waste Permit, meaning that no further actions are needed at those sites. Among the 115 sites included in the Upper LA Canyon Project, 54 have been

9

California Nuclear Profile - Diablo Canyon  

U.S. Energy Information Administration (EIA) Indexed Site

Diablo Canyon" "Unit","Summer capacity (mw)","Net generation (thousand mwh)","Summer capacity factor (percent)","Type","Commercial operation date","License expiration date"...

10

Upper Los Alamos Canyon Cleanup  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

septic tanks, sanitary and industrial waste lines, storm drains, incinerators, transformer sites, and areas in which soil has been contaminated. The Upper Los Alamos Canyon...

11

Prehistoric deforestation at Chaco Canyon?  

Science Journals Connector (OSTI)

...human-caused deforestation. Fuel use frequently is invoked...forced residents to seek fuel outside the canyon and prevented...of grayware cooking vessels (utility wares) were...by factors other than fuel availability and that...anything reliable about fuel consumption in the canyon during...

W. H. Wills; Brandon L. Drake; Wetherbee B. Dorshow

2014-01-01T23:59:59.000Z

12

Hudson Canyon | Open Energy Information  

Open Energy Info (EERE)

Canyon Canyon Jump to: navigation, search Name Hudson Canyon Facility Hudson Canyon Sector Wind energy Facility Type Offshore Wind Facility Status Proposed Owner Deepwater Wind Long Island Developer Deepwater Wind Location Atlantic Ocean NY Coordinates 40.151°, -73.53° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.151,"lon":-73.53,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

13

Juniper Canyon | Open Energy Information  

Open Energy Info (EERE)

Juniper Canyon Juniper Canyon Jump to: navigation, search Name Juniper Canyon Facility Juniper Canyon Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Iberdrola Developer Iberdrola Energy Purchaser Merchant Location In Klickitat County 4.6 miles Southeast of Goldendale Coordinates 45.910223°, -120.224317° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.910223,"lon":-120.224317,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

14

Texas-Louisiana- Mississippi Salt Basin Greater Green River Basin  

U.S. Energy Information Administration (EIA) Indexed Site

Texas-Louisiana- Texas-Louisiana- Mississippi Salt Basin Greater Green River Basin W. Gulf Coast Basin Appalachian Basin Wind River Basin Eastern Shelf NW Shelf Abo Sussex-Shannon Muddy J Mesaverde- Lance-Lewis Medina/Clinton-Tuscarora Bradford-Venango-Elk Berea-Murrysville Piceance Basin Bossier Williston Basin Ft Worth Basin Davis Bighorn Basin Judith River- Eagle Permian Basin Anadarko Basin Denver Basin San Juan Basin North-Central Montana Area Uinta Basin Austin Chalk Codell-Niobrara Penn-Perm Carbonate Niobrara Chalk Dakota Morrow Mesaverde Thirty- One Cleveland Ozona Canyon Wasatch- Mesaverde Red Fork Mesaverde Granite Wash Stuart City-Edwards Bowdoin- Greenhorn Travis Peak Olmos Cotton Valley Vicksburg Wilcox Lobo Pictured Cliffs Cretaceous Cretaceous-Lower Tertiary Mancos- Dakota Gilmer Lime Major Tight Gas Plays, Lower 48 States

15

Mineral resources of the Desolation Canyon, Turtle Canyon, and Floy Canyon Wilderness Study Areas, Carbon Emery, and Grand counties, Utah  

SciTech Connect (OSTI)

This paper reports on the Desolation Canyon, Turtle Canyon, and Floy Canyon Wilderness Study Areas which include 242,000 acres, 33,690 acres, and 23,140 acres. Coal deposits underlie all three study areas. Coal zones in the Blackhawk and Nelsen formations have identified bituminous coal resources of 22 million short tons in the Desolation Canyon Study Area, 6.3 million short tons in the Turtle Canyon Study Area, and 45 million short tons in the Floy Canyon Study Area. In-place inferred oil shale resources are estimated to contain 60 million barrels in the northern part of the Desolation Canyon area. Minor occurrences of uranium have been found in the southeastern part of the Desolation Canyon area and in the western part of the Floy Canyon area. Mineral resource potential for the study areas is estimated to be for coal, high for all areas, for oil and gas, high for the northern tract of the Desolation Canyon area and moderate for all other tracts, for bituminous sandstone, high for the northern part of the Desolation Canyon area, and low for all other tracts, for oil shale, low in all areas, for uranium, moderate for the Floy Canyon area and the southeastern part of the Desolation Canyon area and low for the remainder of the areas, for metals other than uranium, bentonite, zeolites, and geothermal energy, low in all areas, and for coal-bed methane unknown in all three areas.

Cashion, W.B.; Kilburn, J.E.; Barton, H.N.; Kelley, K.D.; Kulik, D.M. (US Geological Survey (US)); McDonnell, J.R. (Bureau of Mines (US))

1990-09-01T23:59:59.000Z

16

Internal Tides in Monterey Submarine Canyon  

Science Journals Connector (OSTI)

The M2 internal tide in Monterey Submarine Canyon is simulated using a modified version of the Princeton Ocean Model. Most of the internal tide energy entering the canyon is generated to the south, on Sur Slope and at the head of Carmel Canyon. ...

Rob A. Hall; Glenn S. Carter

2011-01-01T23:59:59.000Z

17

Bear Canyon Geothermal Facility | Open Energy Information  

Open Energy Info (EERE)

Canyon Geothermal Facility Canyon Geothermal Facility Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Bear Canyon Geothermal Facility General Information Name Bear Canyon Geothermal Facility Facility Bear Canyon Sector Geothermal energy Location Information Location Clear Lake, California, Coordinates 38.762851116528°, -122.69217967987° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":38.762851116528,"lon":-122.69217967987,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

18

Spring Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Spring Canyon Wind Farm Spring Canyon Wind Farm Jump to: navigation, search Name Spring Canyon Wind Farm Facility Spring Canyon Wind Farm Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Invenergy Developer Invenergy Energy Purchaser Xcel Energy Location Near Peetz CO Coordinates 40.95366°, -103.166993° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.95366,"lon":-103.166993,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

19

Threemile Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Threemile Canyon Wind Farm Threemile Canyon Wind Farm Jump to: navigation, search Name Threemile Canyon Wind Farm Facility Threemile Canyon Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner John Deere Wind Developer John Deere Wind Energy Purchaser PacifiCorp Location Morrow County OR Coordinates 45.837861°, -119.701286° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.837861,"lon":-119.701286,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

20

Three Mile Canyon | Open Energy Information  

Open Energy Info (EERE)

Mile Canyon Mile Canyon Jump to: navigation, search Name Three Mile Canyon Facility Three Mile Canyon Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner John Deere Wind Developer Momentum RE Energy Purchaser PacifiCorp Location Morrow County OR Coordinates 45.717419°, -119.502258° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.717419,"lon":-119.502258,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


21

Hay Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Hay Canyon Wind Farm Hay Canyon Wind Farm Jump to: navigation, search Name Hay Canyon Wind Farm Facility Hay Canyon Wind Farm Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Iberdrola Renewables Developer Iberdrola Renewables Energy Purchaser Snohomish Public Utility District Location Near Moro OR Coordinates 45.479548°, -120.741491° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.479548,"lon":-120.741491,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

22

EIS-0219: F-Canyon Plutonium Solutions  

Broader source: Energy.gov [DOE]

This EIS evaluates the potential environmental impacts of processingthe plutonium solutions to metal form using the F-Canyon and FB-Line facilities at the Savannah River Site.

23

Geological control of springs and seeps in the Farmington Canyon Complex, Davis County, Utah  

E-Print Network [OSTI]

METHODOLOGY Selection of Canyons This study concentrates on two canyons in Davis County, Utah. The location and distribution of springs was documented in Lightning and Steed Canyons. These canyons were the site of documented debris flows that occurred... METHODOLOGY Selection of Canyons This study concentrates on two canyons in Davis County, Utah. The location and distribution of springs was documented in Lightning and Steed Canyons. These canyons were the site of documented debris flows that occurred...

Skelton, Robyn Kaye

2012-06-07T23:59:59.000Z

24

Devil's Canyon Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Devil's Canyon Geothermal Project Devil's Canyon Geothermal Project Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Devil's Canyon Geothermal Project Project Location Information Coordinates 40.938333333333°, -117.53916666667° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.938333333333,"lon":-117.53916666667,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

25

Coyote Canyon Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Coyote Canyon Geothermal Project Coyote Canyon Geothermal Project Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Coyote Canyon Geothermal Project Project Location Information Coordinates 39.723055555556°, -118.08027777778° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":39.723055555556,"lon":-118.08027777778,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

26

Red Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Red Canyon Wind Farm Red Canyon Wind Farm Facility Red Canyon Wind Farm Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner NextEra Energy Resources Developer Florida Power & Light Co. Location Borden TX Coordinates 32.95326011°, -101.215539° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":32.95326011,"lon":-101.215539,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

27

Biglow Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Biglow Canyon Wind Farm Biglow Canyon Wind Farm Facility Biglow Canyon Wind Farm Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Portland General Electric Developer Orion/Portland General Electric Energy Purchaser Portland General Electric Location Sherman County OR Coordinates 45.629003°, -120.605607° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.629003,"lon":-120.605607,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

28

Microsoft Word - Badger Canyon CXWEB.doc  

Broader source: Energy.gov (indexed) [DOE]

KEC-4 KEC-4 SUBJECT: Environmental Clearance Memorandum David Tripp Project Manager - TEP-CSB-1 Proposed Action: Badger Canyon Substation Radio Communication Tower Project Budget Information: Work Order 00253262 Task 03 Categorical Exclusions Applied (from Subpart D, 10 C.F.R. Part 1021: B1.7 "Acquisition, installation, operation, and removal of communication systems..." B1.19 "Siting, construction, and operation of microwave and radio communication towers and associated facilities..." Location: Badger Canyon Substation, Benton County, Washington - Township 8 North, Range 28 East, Section 1 Proposed by: Bonneville Power Administration (BPA) Description of the Proposed Action: BPA proposes to replace a 40-foot monopole communication

29

Coyote Canyon Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Coyote Canyon Geothermal Area Coyote Canyon Geothermal Area (Redirected from Coyote Canyon Geothermal Resource Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Coyote Canyon Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (6) 9 Exploration Activities (0) 10 References Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":6,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"500px","height":"300px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":39.927105,"lon":-117.927225,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

30

Big Canyon Creek Ecological Restoration Strategy.  

SciTech Connect (OSTI)

He-yey, Nez Perce for steelhead or rainbow trout (Oncorhynchus mykiss), are a culturally and ecologically significant resource within the Big Canyon Creek watershed; they are also part of the federally listed Snake River Basin Steelhead DPS. The majority of the Big Canyon Creek drainage is considered critical habitat for that DPS as well as for the federally listed Snake River fall chinook (Oncorhynchus tshawytscha) ESU. The Nez Perce Soil and Water Conservation District (District) and the Nez Perce Tribe Department of Fisheries Resources Management-Watershed (Tribe), in an effort to support the continued existence of these and other aquatic species, have developed this document to direct funding toward priority restoration projects in priority areas for the Big Canyon Creek watershed. In order to achieve this, the District and the Tribe: (1) Developed a working group and technical team composed of managers from a variety of stakeholders within the basin; (2) Established geographically distinct sub-watershed areas called Assessment Units (AUs); (3) Created a prioritization framework for the AUs and prioritized them; and (4) Developed treatment strategies to utilize within the prioritized AUs. Assessment Units were delineated by significant shifts in sampled juvenile O. mykiss (steelhead/rainbow trout) densities, which were found to fall at fish passage barriers. The prioritization framework considered four aspects critical to determining the relative importance of performing restoration in a certain area: density of critical fish species, physical condition of the AU, water quantity, and water quality. It was established, through vigorous data analysis within these four areas, that the geographic priority areas for restoration within the Big Canyon Creek watershed are Big Canyon Creek from stream km 45.5 to the headwaters, Little Canyon from km 15 to 30, the mainstem corridors of Big Canyon (mouth to 7km) and Little Canyon (mouth to 7km). The District and the Tribe then used data collected from the District's stream assessment and inventory, utilizing the Stream Visual Assessment Protocol (SVAP), to determine treatment necessary to bring 90% of reaches ranked Poor or Fair through the SVAP up to good or excellent. In 10 year's time, all reaches that were previously evaluated with SVAP will be reevaluated to determine progress and to adapt methods for continued success. Over 400 miles of stream need treatment in order to meet identified restoration goals. Treatments include practices which result in riparian habitat improvements, nutrient reductions, channel condition improvements, fish habitat improvements, invasive species control, water withdrawal reductions, improved hydrologic alterations, upland sediment reductions, and passage barrier removal. The Nez Perce Soil and Water Conservation District (District) and the Nez Perce Tribe Department of Fisheries Resource Management Watershed Division (Tribe) developed this document to guide restoration activities within the Big Canyon Creek watershed for the period of 2008-2018. This plan was created to demonstrate the ongoing need and potential for anadromous fish habitat restoration within the watershed and to ensure continued implementation of restoration actions and activities. It was developed not only to guide the District and the Tribe, but also to encourage cooperation among all stakeholders, including landowners, government agencies, private organizations, tribal governments, and elected officials. Through sharing information, skills, and resources in an active, cooperative relationships, all concerned parties will have the opportunity to join together to strengthen and maintain a sustainable natural resource base for present and future generations within the watershed. The primary goal of the strategy is to address aquatic habitat restoration needs on a watershed level for resident and anadromous fish species, promoting quality habitat within a self-sustaining watershed. Seven objectives have been developed to support this goal: (1) Identify factors limiting quality

Rasmussen, Lynn; Richardson, Shannon

2007-10-01T23:59:59.000Z

31

Trail Canyon Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Trail Canyon Geothermal Project Trail Canyon Geothermal Project Project Location Information Coordinates 38.325555555556°, -114.29388888889° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":38.325555555556,"lon":-114.29388888889,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

32

Panther Canyon Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Panther Canyon Geothermal Project Panther Canyon Geothermal Project Project Location Information Coordinates 40.549444444444°, -117.57666666667° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.549444444444,"lon":-117.57666666667,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

33

Blue Canyon VI | Open Energy Information  

Open Energy Info (EERE)

VI VI Jump to: navigation, search Name Blue Canyon VI Facility Blue Canyon VI Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner EDP Renewables North America LLC Developer EDP Renewables North America LLC Energy Purchaser Merchant Location Lawton OK Coordinates 34.8582°, -98.54752° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.8582,"lon":-98.54752,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

34

DOE - Office of Legacy Management -- Acid Pueblo Canyon - NM 03  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Acid Pueblo Canyon - NM 03 Acid Pueblo Canyon - NM 03 FUSRAP Considered Sites Acid/Pueblo Canyon, NM Alternate Name(s): Radioactive Liquid Waste Treatment Plant (TA-45) Acid/Pueblo and Los Alamos Canyon NM.03-3 Location: Canyons in the Pajarito Plateau Region in Los Alamos County, Los Alamos, NM NM.03-3 Historical Operations: Late 1943 or early 1944, head of the south fork of Acid Canyon received untreated liquid waste containing tritium and isotopes of strontium, cesium, uranium, plutonium, and americium discharged from main acid sewer lines and subsequently from the TA-3 plutonium treatment plant. NM.03-3 Eligibility Determination: Radiological Survey(s): Verification Surveys NM.03-5 NM.03-6 Site Status: Certified- Certification Basis and Federal Register Notice NM.03-2

35

Coyote Canyon Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Coyote Canyon Geothermal Area Coyote Canyon Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Coyote Canyon Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (6) 9 Exploration Activities (0) 10 References Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"TERRAIN","zoom":6,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"500px","height":"300px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":39.927105,"lon":-117.927225,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

36

Internal tides in canyons and their effect on acoustics  

Science Journals Connector (OSTI)

Internal gravity waves of tidal frequency are generated as the ocean tides push water upward onto the continental shelf. Such waves also arrive at the continental slope from deep water and are heavily modified by the change in water depth. The wave generation and wave shoaling effects have an additional level of complexity where a canyon is sliced into the continental slope. Recently steps have been taken to simulate internal tides in canyons to understand the physical processes of internal tides in canyons and also to compute the ramifications on sound propagation in and near the canyons. Internal tides generated in canyons can exhibit directionality with the directionality being consistent with an interesting multiple-scattering effect. The directionality imparts a pattern to the sound-speed anomaly field affecting propagation. The directionality also means that short nonlinear internal waves which have specific strong effects on sound can have interesting patterns near the canyons. In addition to the directionality of internal tides radiated from canyons the internal tide energy within the canyons can be patchy and may unevenly affect sound.

2014-01-01T23:59:59.000Z

37

20140430_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 April to 30 April 2014.

Thibedeau, Joe

2014-05-05T23:59:59.000Z

38

Green Machine Florida Canyon Hourly Data 20130731  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 7/1/13 to 7/31/13.

Vanderhoff, Alex

2013-08-30T23:59:59.000Z

39

20130416_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 4/16/13.

Vanderhoff, Alex

2013-04-24T23:59:59.000Z

40

Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 6/1/13 to 6/30/13

Vanderhoff, Alex

2013-07-15T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


41

Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 6/1/13 to 6/30/13

Vanderhoff, Alex

42

20130416_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 4/16/13.

Vanderhoff, Alex

43

20140430_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 April to 30 April 2014.

Thibedeau, Joe

44

Green Machine Florida Canyon Hourly Data 20130731  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 7/1/13 to 7/31/13.

Vanderhoff, Alex

45

EIS-0427: Grapevine Canyon Wind Project, Coconino County, Arizona |  

Broader source: Energy.gov (indexed) [DOE]

27: Grapevine Canyon Wind Project, Coconino County, Arizona 27: Grapevine Canyon Wind Project, Coconino County, Arizona EIS-0427: Grapevine Canyon Wind Project, Coconino County, Arizona Summary This EIS evaluates the environmental impacts of a proposed wind energy generation project in Coconino County, Arizona, on privately owned ranch lands and trust lands administered by the Arizona State Land Department. The proposed project includes a new transmission tie-line that would cross lands administered by Coconino National Forest and interconnect with DOE's Western Area Power Administration's existing Glen Canyon-Pinnacle Peak transmission lines. Public Comment Opportunities No public comment opportunities available at this time. Documents Available for Download September 11, 2012 EIS-0427: Record of Decision Interconnection of the Grapevine Canyon Wind Project, Coconino County,

46

Klondike III / Biglow Canyon Wind Integration Project  

Broader source: Energy.gov (indexed) [DOE]

Proposed Action and Alternatives 2-3 Proposed Action and Alternatives 2-3 Figure 1 Proposed 230-kV Towers and Rights-of-Way Klondike III/Biglow Canyon Wind Integration Project Bonneville Power Administration Proposed Action and Alternatives 2-4 Figure 1, continued CUMULATIVE IMPACTS ANALYSIS, PROPOSED WIND PROJECTS, SHERMAN COUNTY, WASHINGTON March 2006 WEST, Inc. 32 Figure 1. Region map of wind projects proposed for Sherman County. D e s c h u t e s Ri ver C a n y o n C o l u m b ia R i v e r Hwy 19 H w y 2 0 6 H w y 9 7 I 8 4 Grass Valley Moro Wasco Biggs Arlington Condon Fourmile Canyon McDonald Ferry Biggs Junction Deschutes River Crossing The Dalles Complex RM 15.9-16.8 RM 40 Sherman Co Wasco Co G i l l i a m C o Gilliam Co Morrow Co Rowena Plateau Historic Columbia River Highway John D a y R i v e r C a n y o n P:\B\BPAX00000324\0600INFO\GS\arcmap\figures\visiblity_tech_report\fig2_visual_resources_or.mxd January 9, 2006

47

Nine Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Wind Farm Wind Farm Facility Nine Canyon Wind Farm Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Energy Northwest Developer Energy Northwest Energy Purchaser Energy Northwest Location Benton County Coordinates 46.286065°, -119.425532° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":46.286065,"lon":-119.425532,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

48

Blue Canyon Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Wind Farm Wind Farm Facility Blue Canyon Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Babcock & Brown/Horizon Developer Zilkha Renewable/Kirmart Corp. Energy Purchaser Western Farmers' Electric Cooperative Location North of Lawton OK Coordinates 34.852678°, -98.551807° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.852678,"lon":-98.551807,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

49

Beneficial Reuse at Bodo Canyon Site | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

Services » Environmental Justice » Beneficial Reuse at Bodo Services » Environmental Justice » Beneficial Reuse at Bodo Canyon Site Beneficial Reuse at Bodo Canyon Site The George Washington University Environmental Resource Policy Graduate Program Capstone Project Beneficial Reuse at Bodo Canyon Site Feasibility and Community Support for Photovoltaic Array May 2012 The George Washington University Environmental Resource Policy Graduate Program Capstone Project was an analysis of LM's efforts to support the installation of a commercial solar photovoltaic system at the former uranium mill site near Durango, Colorado. Beneficial Reuse at Bodo Canyon Site More Documents & Publications EA-1770: Final Environmental Assessment Performance of a Permeable Reactive Barrier Using Granular Zero-Valent Iron: FY 2004 Annual Report Durango, Colorado, Disposal Site

50

Olowalu-Ukumehame Canyon Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Olowalu-Ukumehame Canyon Geothermal Area Olowalu-Ukumehame Canyon Geothermal Area (Redirected from Olowalu-Ukumehame Canyon Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Olowalu-Ukumehame Canyon Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (4) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0

51

Canyon Bloomers, Inc Greenhouse Low Temperature Geothermal Facility | Open  

Open Energy Info (EERE)

Canyon Bloomers, Inc Greenhouse Low Temperature Geothermal Facility Canyon Bloomers, Inc Greenhouse Low Temperature Geothermal Facility Jump to: navigation, search Name Canyon Bloomers, Inc Greenhouse Low Temperature Geothermal Facility Facility Canyon Bloomers, Inc Sector Geothermal energy Type Greenhouse Location Buhl, Idaho Coordinates 42.5990714°, -114.7594946° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[]}

52

The Role of Convective Outflow in the Waldo Canyon Fire  

Science Journals Connector (OSTI)

The meteorological conditions associated with the rapid intensification and spread of the catastrophic Waldo Canyon fire on 26 June 2012 are studied. The fire caused two fatalities, destroyed 347 homes in Colorado Springs, and resulted in ...

Richard H. Johnson; Russ S. Schumacher; James H. Ruppert Jr.; Daniel T. Lindsey; Julia E. Ruthford; Lisa Kriederman

2014-09-01T23:59:59.000Z

53

Copper Canyon, Texas: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Display map This article is a stub. You can help OpenEI by expanding it. Copper Canyon is a town in Denton County, Texas. It falls under Texas's 26th congressional...

54

Safety Evaluation for Packaging (onsite) T Plant Canyon Items  

SciTech Connect (OSTI)

This safety evaluation for packaging (SEP) evaluates and documents the ability to safely ship mostly unique inventories of miscellaneous T Plant canyon waste items (T-P Items) encountered during the canyon deck clean off campaign. In addition, this SEP addresses contaminated items and material that may be shipped in a strong tight package (STP). The shipments meet the criteria for onsite shipments as specified by Fluor Hanford in HNF-PRO-154, Responsibilities and Procedures for all Hazardous Material Shipments.

OBRIEN, J.H.

2000-07-14T23:59:59.000Z

55

Nonassociated gas resources in low-permeability sandstone reservoirs, lower tertiary Wasatch Formation, and upper Cretaceous Mesaverde Group, Uinta Basin, Utah  

SciTech Connect (OSTI)

The US Geological Survey recognizes six major plays for nonassociated gas in Tertiary and Upper Cretaceous low-permeability strata of the Uinta Basin, Utah. For purposes of this study, plays without gas/water contacts are separated from those with such contacts. Continuous-saturation accumulations are essentially single fields, so large in areal extent and so heterogeneous that their development cannot be properly modeled as field growth. Fields developed in gas-saturated plays are not restricted to structural or stratigraphic traps and they are developed in any structural position where permeability conduits occur such as that provided by natural open fractures. Other fields in the basin have gas/water contacts and the rocks are water-bearing away from structural culmination`s. The plays can be assigned to two groups. Group 1 plays are those in which gas/water contacts are rare to absent and the strata are gas saturated. Group 2 plays contain reservoirs in which both gas-saturated strata and rocks with gas/water contacts seem to coexist. Most units in the basin that have received a Federal Energy Regulatory Commission (FERC) designation as tight are in the main producing areas and are within Group 1 plays. Some rocks in Group 2 plays may not meet FERC requirements as tight reservoirs. However, we suggest that in the Uinta Basin that the extent of low-permeability rocks, and therefore resources, extends well beyond the limits of current FERC designated boundaries for tight reservoirs. Potential additions to gas reserves from gas-saturated tight reservoirs in the Tertiary Wasatch Formation and Cretaceous Mesaverde Group in the Uinta Basin, Utah is 10 TCF. If the potential additions to reserves in strata in which both gas-saturated and free water-bearing rocks exist are added to those of Group 1 plays, the volume is 13 TCF.

Fouch, T.D.; Schmoker, J.W.; Boone, L.E.; Wandrey, C.J.; Crovelli, R.A.; Butler, W.C.

1994-08-01T23:59:59.000Z

56

Patterns in biodiversity and distribution of benthic Polychaeta in the Mississippi Canyon, Northern Gulf of Mexico  

E-Print Network [OSTI]

) and deep (> 1500 m). Results of statistical analyses revealed that depth was the most important determinant in organizing polychaete assemblages in the study area. The Mississippi Canyon and the Central Transect (a non-canyon area) were found...

Wang, Yuning

2006-04-12T23:59:59.000Z

57

Sediment transport in the Mississippi Canyon: the role of currents and storm events on optical variability  

E-Print Network [OSTI]

Two modes of sediment transport were found to exist in the Mississippi Canyon: the offshelf transport of material in intermediate nepheloid layers originating at depths of 50-175 m and the resuspension and transport of material within the canyon...

Burden, Cheryl A

1999-01-01T23:59:59.000Z

58

Olowalu-Ukumehame Canyon Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Olowalu-Ukumehame Canyon Geothermal Area Olowalu-Ukumehame Canyon Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Olowalu-Ukumehame Canyon Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (0) 9 Exploration Activities (4) 10 References Area Overview Geothermal Area Profile Location: Hawaii Exploration Region: Hawaii Geothermal Region GEA Development Phase: 2008 USGS Resource Estimate Mean Reservoir Temp: Estimated Reservoir Volume: Mean Capacity: Click "Edit With Form" above to add content History and Infrastructure Operating Power Plants: 0 No geothermal plants listed. Add a new Operating Power Plant

59

Microsoft Word - Final_NineCanyon_CommunicationTowerInstall_CX  

Broader source: Energy.gov (indexed) [DOE]

1, 2013 1, 2013 REPLY TO ATTN OF: KEC-4 SUBJECT: Environmental Clearance Memorandum Kelly Gardner, PMP Project Manager, TEP-TPP-1 Proposed Action: Nine Canyon Substation Communication Tower Addition: 331800 McNary Sub Bus Tie Relay Replacements and 310427 McNary-Badger Canyon Transfer Trip Install Categorical Exclusion Applied (from Subpart D, 10 C.F.R. Part 1021): B4.6 - Additions and modifications to transmission facilities Location: Kennewick, Benton County, Washington Proposed by: Bonneville Power Administration (BPA) Description of the Proposed Action: BPA proposes to install a 60-foot communications tower and associated communication equipment at the Benton County Public Utility District's Nine Canyon Substation in Benton County, Washington. The upgrade would involve replacing the

60

Nine Canyon III Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Nine Canyon III Wind Farm Nine Canyon III Wind Farm Facility Nine Canyon III Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Energy Northwest Developer Energy Northwest/RES Americas Energy Purchaser Energy Northwest Coordinates 46.286065°, -119.425532° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":46.286065,"lon":-119.425532,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


61

Peak discharge of a Pleistocene lava-dam outburst flood in Grand Canyon, Arizona, USA  

E-Print Network [OSTI]

produced the largest known flood on the Colorado River in Grand Canyon. The Hyaloclastite Dam was up to 366 Canyon; Colorado river; Pleistocene floods; Lava dams; Hydraulic modeling; Paleoflood indicators; DamPeak discharge of a Pleistocene lava-dam outburst flood in Grand Canyon, Arizona, USA Cassandra R

62

New insights on the runout of large landslides in the Valles-Marineris canyons, Mars  

E-Print Network [OSTI]

New insights on the runout of large landslides in the Valles-Marineris canyons, Mars E. Lajeunesse-Marineris canyons, Mars, Geophys. Res. Lett., 33, L04403, doi:10.1029/ 2005GL025168. 1. Introduction [2] Since the first pictures returned from Viking Orbiters, the numerous landslides identified along the canyons

Lajeunesse, Eric

63

Engineering Geologic Assessment of Risk to Visitors: Canyon Lake Gorge, Texas  

E-Print Network [OSTI]

Presented here are the results of a study of geological hazards conducted in Canyon Lake Gorge of Central Texas. Canyon Lake Gorge formed in 2002 when the emergency spillway of Canyon Lake was overtopped. Since that time, the gorge has been opened...

Kolkmeier, Benjamin D.

2010-07-14T23:59:59.000Z

64

Biglow Canyon Phase III Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Biglow Canyon Phase III Wind Farm Biglow Canyon Phase III Wind Farm Jump to: navigation, search Name Biglow Canyon Phase III Wind Farm Facility Biglow Canyon Phase III Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Portland General Electric Developer Orion Energy Group Energy Purchaser Portland General Electric Location Sherman County OR Coordinates 45.6375°, -120.605278° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.6375,"lon":-120.605278,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

65

Blue Canyon II Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Blue Canyon II Wind Farm Blue Canyon II Wind Farm Jump to: navigation, search Name Blue Canyon II Wind Farm Facility Blue Canyon II Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Horizon Wind Energy Developer Horizon Wind Energy Energy Purchaser American Electric Power Location North of Lawton OK Coordinates 34.8582°, -98.54752° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.8582,"lon":-98.54752,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

66

Glen Canyon Dam Long-Term Experimental and Management Plan EIS  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Glen Canyon LTEMP EIS Glen Canyon LTEMP EIS Glen Canyon Dam, a 1,300-MW water-storage and hydroelectric facility is located on the Colorado River upstream of the Grand Canyon. EVS is evaluating the effects of dam operations on the Colorado River. A comprehensive evaluation of Glen Canyon Dam operations and their effects on the Colorado River through the Grand Canyon is being conducted by the Department of the Interior with EVS assistance. The Long-Term Experimental and Management Plan (LTEMP) Environmental Impact Statement (EIS) - the first such evaluation in over 15 years - will examine flow regimes to meet the goals of supplying water for communities, agriculture, and industry and will protect the resources of the Grand Canyon, while providing clean hydropower. The LTEMP EIS, which is expected to be completed by the end of 2013, will

67

Small Mammal Sampling in Mortandad and Los Alamos Canyons, 2005  

SciTech Connect (OSTI)

As part of an ongoing ecological field investigation at Los Alamos National Laboratory, a study was conducted that compared measured contaminant concentrations in sediment to population parameters for small mammals in the Mortandad Canyon watershed. Mortandad Canyon and its tributary canyons have received contaminants from multiple solid waste management units and areas of concern since establishment of the Laboratory in the 1940s. The study included three reaches within Effluent and Mortandad canyons (E-1W, M-2W, and M-3) that had a spread in the concentrations of metals and radionuclides and included locations where polychlorinated biphenyls and perchlorate had been detected. A reference location, reach LA-BKG in upper Los Alamos Canyon, was also included in the study for comparison purposes. A small mammal study was initiated to assess whether potential adverse effects were evident in Mortandad Canyon due to the presence of contaminants, designated as contaminants of potential ecological concern, in the terrestrial media. Study sites, including the reference site, were sampled in late July/early August. Species diversity and the mean daily capture rate were the highest for E-1W reach and the lowest for the reference site. Species composition among the three reaches in Mortandad was similar with very little overlap with the reference canyon. Differences in species composition and diversity were most likely due to differences in habitat. Sex ratios, body weights, and reproductive status of small mammals were also evaluated. However, small sample sizes of some species within some sites affected the analysis. Ratios of males to females by species of each site (n = 5) were tested using a Chi-square analysis. No differences were detected. Where there was sufficient sample size, body weights of adult small mammals were compared between sites. No differences in body weights were found. Reproductive status of species appears to be similar across sites. However, sample size prevents a detailed examination of reproduction composition. Because of small sample size of some species and differences that might occur on a seasonal basis, additional sampling would need to be conducted to further evaluate sex ratios, body weights, and reproductive characteristics.

Kathy Bennett, Sherri Sherwood, and Rhonda Robinson

2006-08-15T23:59:59.000Z

68

Environmental analysis of Lower Pueblo/Lower Los Alamos Canyon, Los Alamos, New Mexico  

SciTech Connect (OSTI)

The radiological survey of the former radioactive waste treatment plant site (TA-45), Acid Canyon, Pueblo Canyon, and Los Alamos Canyon found residual contamination at the site itself and in the channel and banks of Acid, Pueblo, and lower Los Alamos Canyons all the way to the Rio Grande. The largest reservoir of residual radioactivity is in lower Pueblo Canyon, which is on DOE property. However, residual radioactivity does not exceed proposed cleanup criteria in either lower Pueblo or lower Los Alamos Canyons. The three alternatives proposed are (1) to take no action, (2) to construct a sediment trap in lower Pueblo Canyon to prevent further transport of residual radioactivity onto San Ildefonso Indian Pueblo land, and (3) to clean the residual radioactivity from the canyon system. Alternative 2, to cleanup the canyon system, is rejected as a viable alternative. Thousands of truckloads of sediment would have to be removed and disposed of, and this effort is unwarranted by the low levels of contamination present. Residual radioactivity levels, under either present conditions or projected future conditions, will not result in significant radiation doses to persons exposed. Modeling efforts show that future transport activity will not result in any residual radioactivity concentrations higher than those already existing. Thus, although construction of a sediment trap in lower Pueblo Canyon is a viable alternative, this effort also is unwarranted, and the no-action alternative is the preferred alternative.

Ferenbaugh, R.W.; Buhl, T.E.; Stoker, A.K.; Becker, N.M.; Rodgers, J.C.; Hansen, W.R.

1994-12-01T23:59:59.000Z

69

Coyote Canyon Steam Plant Biomass Facility | Open Energy Information  

Open Energy Info (EERE)

Steam Plant Biomass Facility Steam Plant Biomass Facility Jump to: navigation, search Name Coyote Canyon Steam Plant Biomass Facility Facility Coyote Canyon Steam Plant Sector Biomass Facility Type Landfill Gas Location Orange County, California Coordinates 33.7174708°, -117.8311428° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":33.7174708,"lon":-117.8311428,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

70

New York Canyon Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

New York Canyon Geothermal Project New York Canyon Geothermal Project Project Location Information Coordinates 40.056111111111°, -118.01083333333° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":40.056111111111,"lon":-118.01083333333,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

71

Blue Canyon V Wind Farm | Open Energy Information  

Open Energy Info (EERE)

V Wind Farm V Wind Farm Jump to: navigation, search Name Blue Canyon V Wind Farm Facility Blue Canyon V Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Horizon-EDPR Developer Horizon-EDPR Energy Purchaser Public Service of Oklahoma Location Caddo & Comanche Counties OK Coordinates 34.8582°, -98.54752° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.8582,"lon":-98.54752,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

72

New York Canyon Stimulation Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Stimulation Geothermal Project Stimulation Geothermal Project Jump to: navigation, search Last modified on July 22, 2011. Project Title New York Canyon Stimulation Project Type / Topic 1 Recovery Act: Enhanced Geothermal System Demonstrations Project Type / Topic 2 EGS Demonstration Project Description The projects expected outcomes and benefits are; - Demonstrated commercial viability of the EGS-stimulated reservoir by generating electricity using fluids produced from the reservoir at economic costs. - Significant job creation and preservation and economic development in support of the Recovery Act of 2009. State Nevada Objectives Demonstrate the commercial application of EGS techniques at the New York Canyon (NYC) site in a way that minimizes cost and maximizes opportunities for repeat applications elsewhere.

73

Box Canyon Motel Space Heating Low Temperature Geothermal Facility | Open  

Open Energy Info (EERE)

Motel Space Heating Low Temperature Geothermal Facility Motel Space Heating Low Temperature Geothermal Facility Jump to: navigation, search Name Box Canyon Motel Space Heating Low Temperature Geothermal Facility Facility Box Canyon Motel Sector Geothermal energy Type Space Heating Location Ouray, Colorado Coordinates 38.0227716°, -107.6714487° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[]}

74

Harbison Canyon, California: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Harbison Canyon, California: Energy Resources Harbison Canyon, California: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 32.8203296°, -116.8300236° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":32.8203296,"lon":-116.8300236,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

75

New York Canyon Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

form form View source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit with form History Facebook icon Twitter icon » New York Canyon Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: New York Canyon Geothermal Area Contents 1 Area Overview 2 History and Infrastructure 3 Regulatory and Environmental Issues 4 Exploration History 5 Well Field Description 6 Geology of the Area 7 Geofluid Geochemistry 8 NEPA-Related Analyses (6) 9 Exploration Activities (1) 10 References Area Overview Geothermal Area Profile Location: Lovelock, NV Exploration Region: Central Nevada Seismic Zone Geothermal Region GEA Development Phase: None"None" is not in the list of possible values (Phase I - Resource Procurement and Identification, Phase II - Resource Exploration and Confirmation, Phase III - Permitting and Initial Development, Phase IV - Resource Production and Power Plant Construction) for this property.

76

American Canyon Power Plant Biomass Facility | Open Energy Information  

Open Energy Info (EERE)

Biomass Facility Biomass Facility Jump to: navigation, search Name American Canyon Power Plant Biomass Facility Facility American Canyon Power Plant Sector Biomass Facility Type Landfill Gas Location Napa County, California Coordinates 38.5024689°, -122.2653887° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":38.5024689,"lon":-122.2653887,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

77

DOE - Office of Legacy Management -- Bayo Canyon NM Site - NM 01  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Bayo Canyon NM Site - NM 01 Bayo Canyon NM Site - NM 01 FUSRAP Considered Sites Bayo Canyon, NM Alternate Name(s): Bayo Canyon Area Bayo Canyon (TA-10) Site NM.01-2 Location: Canyon in the Pajarito Plateau Region in Los Alamos County, Los Alamos, NM NM.01-3 Historical Operations: Used in 1944-1961 by the MED and later AEC at Los Alamos National Laboratory as a firing site for conventional and high-explosives experiments involving natural and depleted uranium, strontium, and lanthanum as a radiation source for blast diagnosis. NM.01-3 NM.01-5 Eligibility Determination: Eligible NM.01-1 Radiological Survey(s): Assessment Survey NM.01-3 Site Status: Certified- Certification Basis NM.01-5 NM.01-6 Long-term Care Requirements: Long-Term Surveillance and Maintenance Requirements for Remediated FUSRAP Sites S07566_FUSRAP

78

Aquatic macroinvertebrates and water quality in Sandia Canyon  

SciTech Connect (OSTI)

In 1990, field studies of water quality and stream macroinvertebrate communities were initiated in Sandia Canyon at Los Alamos National Laboratory. The studies were designed to establish baseline data and to determine the effects of routine discharges of industrial and sanitary waste. Water quality measurements were taken and aquatic macroinvertebrates sampled at three permanent stations within the canyon. Two of the three sample stations are located where the stream regularly receives industrial and sanitary waste effluents. These stations exhibited a low diversity of macroinvertebrates and slightly degraded water quality. The last sample station, located approximately 0.4 km (0.25 mi) downstream from the nearest wastewater outfall, appears to be in a zone of recovery where water quality parameters more closely resemble those found in natural streams in the Los Alamos area. A large increase in macroinvertebrate diversity was also observed at the third station. These results indicate that effluents discharged into Sandia Canyon have a marked effect on water quality and aquatic macroinvertebrate communities.

Bennett, K.

1994-05-01T23:59:59.000Z

79

Landslide assessment of Newell Creek Canyon, Oregon City, Oregon  

SciTech Connect (OSTI)

A study has been conducted in Newell Creek Canyon near Oregon City, Oregon, T3S, T2S, R2E. A landslide inventory has located 53 landslides in the 2.8 km[sup 2] area. The landslides range in area from approximately 15,000m[sup 2] to 10m[sup 2]. Past slides cover an approximate 7% of the canyon area. Landslide processes include: slump, slump-translational, slump-earthflow and earthflow. Hard, impermeable clay-rich layers in the Troutdale Formation form the failure planes for most of the slides. Slopes composed of Troutdale material may seem to be stable, but when cuts and fills are produced, slope failure is common because of the perched water tables and impermeable failure planes. Good examples of cut and fill failures are present on Highway 213 which passes through Newell Creek Canyon. Almost every cut and fill has failed since the road construction began. The latest failure is in the fill located at mile-post 2.1. From data gathered, a slope stability risk map was generated. Stability risk ratings are divided into three groups: high, moderate and low. High risk of slope instability is designated to all landslides mapped in the slide inventory. Moderate risk is designated to slopes in the Troutdale Formation greater than 8[degree]. Low risk is designated to slopes in the Troutdale Formation less than 8[degree].

Growney, L.; Burris, L.; Garletts, D.; Walsh, K. (Portland State Univ., OR (United States). Dept. of Geology)

1993-04-01T23:59:59.000Z

80

Nine Canyon Wind Farm Phase II | Open Energy Information  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Nine Canyon Wind Farm Phase II Jump to: navigation, search Name Nine Canyon Wind Farm Phase II Facility Nine Canyon Wind Farm Phase II Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Energy Northwest Developer Energy Northwest Energy Purchaser Energy Northwest Location Benton County Coordinates 46.286065°, -119.425532° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":46.286065,"lon":-119.425532,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


81

DE-AI26-06NT42878 - Alaminos Canyon Task | netl.doe.gov  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Enhanced Oil Recovery Deepwater Tech Methane Hydrate Geochemical Evaluation of Deep Sediment Hydrate Deposits in Alaminos Canyon, Block 818, Texas-Louisiana Shelf...

82

Study of bacterial activity and ecology of Bingham Canyon mine dumps;.  

E-Print Network [OSTI]

??There were at least two types of chemoautotrophic thiobacilli found in the leaching streams of Bingham Canyon min dump. One of these organisms oxidizes free (more)

Chen, Young-Chang

1968-01-01T23:59:59.000Z

83

EA-1980: Spar Canyon-Round Valley Access Road System Improvements...  

Energy Savers [EERE]

proposed improvements to the access road system for its existing Spar Canyon-Round Valley Transmission Line located on BLM land in Custer County, Idaho. Additional information is...

84

DOE/EA-1521; Environmental Assessment for Spring Canyon Wind Project, Logan County, Colorado  

Broader source: Energy.gov (indexed) [DOE]

EA, Spring Canyon Wind Project ix EA, Spring Canyon Wind Project ix TABLE OF CONTENTS Page 1.0 PURPOSE AND NEED......................................................................................................... 1 1.1 INTRODUCTION ..................................................................................................... 1 1.2 PURPOSE AND NEED............................................................................................. 3 1.2.1 Federal Agency Action ............................................................................... 3 1.2.2 Applicant's Purpose and Need .................................................................... 3 1.3 SCOPING .................................................................................................................. 3

85

ORIGINAL RESEARCH PAPER Canyon-infilling and gas hydrate occurrences in the frontal fold  

E-Print Network [OSTI]

ORIGINAL RESEARCH PAPER Canyon-infilling and gas hydrate occurrences in the frontal fold to infer the canyon-infilling, fold uplift, and gas hydrate occurrences beneath the frontal fold at the toe simu- lating reflector (BSR) on seismic sections indicates the base of gas hydrate stability zone

Lin, Andrew Tien-Shun

86

Green Canyon Hot Springs Greenhouse Low Temperature Geothermal Facility |  

Open Energy Info (EERE)

Greenhouse Low Temperature Geothermal Facility Greenhouse Low Temperature Geothermal Facility Facility Green Canyon Hot Springs Sector Geothermal energy Type Greenhouse Location Newdale, Idaho Coordinates 43.8832463°, -111.6063483° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[]}

87

20140301-0331_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Mar to 31 Mar 2014.

Thibedeau, Joe

2014-04-07T23:59:59.000Z

88

20140601-0630_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 June to 30 June 2014.

Thibedeau, Joe

2014-06-30T23:59:59.000Z

89

20140701-0731_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 July to 31 July 2014.

Thibedeau, Joe

2014-07-31T23:59:59.000Z

90

20131201-1231_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Dec to 31 Dec 2013.

Thibedeau, Joe

2014-01-08T23:59:59.000Z

91

20140201-0228_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Feb to 28 Feb 2014.

Thibedeau, Joe

2014-03-03T23:59:59.000Z

92

20140501-0531_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 May to 31 May 2014.

Thibedeau, Joe

2014-06-02T23:59:59.000Z

93

20131101-1130_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Nov to 30 Nov 2013.

Thibedeau, Joe

2013-12-02T23:59:59.000Z

94

20130801-0831_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 8/1/13 to 8/31/13.

Vanderhoff, Alex

2013-09-10T23:59:59.000Z

95

20130901-0930_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 1 September 2013 to 30 September 2013.

Thibedeau, Joe

2013-10-25T23:59:59.000Z

96

20131001-1031_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 1 Oct 2013 to 31 Oct 2013.

Thibedeau, Joe

2013-11-05T23:59:59.000Z

97

20140101-0131_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Jan to 31 Jan 2014.

Thibedeau, Joe

2014-02-03T23:59:59.000Z

98

20130501-20130531_Green Machine Florida Canyon Hourly Data  

SciTech Connect (OSTI)

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from May 2013

Vanderhoff, Alex

2013-06-18T23:59:59.000Z

99

20140201-0228_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Feb to 28 Feb 2014.

Thibedeau, Joe

100

20131101-1130_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Nov to 30 Nov 2013.

Thibedeau, Joe

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


101

20140301-0331_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Mar to 31 Mar 2014.

Thibedeau, Joe

102

20131001-1031_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 1 Oct 2013 to 31 Oct 2013.

Thibedeau, Joe

103

20140601-0630_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 June to 30 June 2014.

Thibedeau, Joe

104

20131201-1231_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Dec to 31 Dec 2013.

Thibedeau, Joe

105

20130801-0831_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 8/1/13 to 8/31/13.

Vanderhoff, Alex

106

20130501-20130531_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from May 2013

Vanderhoff, Alex

107

20140701-0731_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 July to 31 July 2014.

Thibedeau, Joe

108

20140101-0131_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 Jan to 31 Jan 2014.

Thibedeau, Joe

109

20140501-0531_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 01 May to 31 May 2014.

Thibedeau, Joe

110

20130901-0930_Green Machine Florida Canyon Hourly Data  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Employing innovative product developments to demonstrate financial and technical viability of producing electricity from low temperature geothermal fluids, coproduced in a mining operation, by employing ElectraTherm's modular and mobile heat-to-power "micro geothermal" power plant with output capacity expected in the 30-70kWe range. The Green Machine is an Organic Rankine Cycle power plant. The Florida Canyon machine is powered by geothermal brine with air cooled condensing. The data provided is an hourly summary from 1 September 2013 to 30 September 2013.

Thibedeau, Joe

111

Gas Flux Sampling At Olowalu-Ukumehame Canyon Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Gas Flux Sampling At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Gas Flux Sampling At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Exploration Activity Details Location Olowalu-Ukumehame Canyon Area Exploration Technique Gas Flux Sampling Activity Date Usefulness could be useful with more improvements DOE-funding Unknown Notes Soil mercury concentration and radon emanometry surveys were conducted along the stream beds in both Olowalu and Ukumehame Canyons and on the coastal alluvial fans (Cox and Cuff, 1981a). The results of these surveys indicated that a few minor -nomalies might be present. However, the extreme topographic relief in the area did not permit sufficient coverage of the

112

Biglow Canyon Phase II Wind Farm | Open Energy Information  

Open Energy Info (EERE)

Phase II Wind Farm Phase II Wind Farm Jump to: navigation, search Name Biglow Canyon Phase II Wind Farm Facility Biglow Canyon Phase II Sector Wind energy Facility Type Commercial Scale Wind Facility Status In Service Owner Portland General Electric Developer Orion Energy Group Energy Purchaser Portland General Electric Location Sherman County OR Coordinates 45.6375°, -120.605278° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":45.6375,"lon":-120.605278,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

113

Depositional environment and reservoir morphology of Canyon sandstones, Central Midland Basin, Texas  

E-Print Network [OSTI]

channels are thinner, have lim1ted lateral extent compared to upper- and m1ddle-fan channels, and consist of bet- ter developed Bouma sequences. Few sequences exceed thicknesses of 1 foot in distal channels. Canyon sandstones are fine grained (0. 14... divisions. Texture Canyon sandstones 1n Lucky Canyon and Jameson field exh1b1t sim- ilar textural characteristics (Table 3). Mean size of monocrystalline quartz is f1ne to very fine grained. Sort1ng, as measured by standard deviations in each sample...

Jones, James Winston

2012-06-07T23:59:59.000Z

114

Microsoft Word - canyon disposition rpt 2 01 05.doc  

Broader source: Energy.gov (indexed) [DOE]

Department of Energy Efforts to Department of Energy Efforts to Dispose of Hanford's Chemical Separation Facilities DOE/IG-0672 February 2005 -2- benefits of using the facility as a disposal site. Instead, the study focused on characterizing and performing technical analysis on the structural integrity of the facility. In studying the merits of the Initiative, the Department did not ensure that the cost study was sufficient in scope, and once completed, never reviewed the study to determine whether it was accurate and complete or adequately supported the preferred alternative. As a result of not thoroughly evaluating the feasibility of using canyon facilities for waste disposal, the Department may not realize savings ranging up to $500 million. This report highlights the importance of the Department's oversight of its contractors' activities to

115

Mercury Vapor At Olowalu-Ukumehame Canyon Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

source source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit History Facebook icon Twitter icon » Mercury Vapor At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Exploration Activity Details Location Olowalu-Ukumehame Canyon Area Exploration Technique Mercury Vapor Activity Date Usefulness could be useful with more improvements DOE-funding Unknown Notes Soil mercury concentration and radon emanometry surveys were conducted along the stream beds in both Olowalu and Ukumehame Canyons and on the coastal alluvial fans (Cox and Cuff, 1981a). The results of these surveys

116

Field Mapping At Olowalu-Ukumehame Canyon Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

source source History View New Pages Recent Changes All Special Pages Semantic Search/Querying Get Involved Help Apps Datasets Community Login | Sign Up Search Page Edit History Facebook icon Twitter icon » Field Mapping At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Field Mapping At Olowalu-Ukumehame Canyon Area (Thomas, 1986) Exploration Activity Details Location Olowalu-Ukumehame Canyon Area Exploration Technique Field Mapping Activity Date Usefulness not useful DOE-funding Unknown Notes Geologic mapping (Diller, 1982) in this area has identified several trachitic and alkalic dikes, plugs, and vents within the area bounded by the canyons (Fig. 21). The frequency distribution of those dikes in the two

117

EA-1863: Vegetation Management on the Glen Canyon-Pinnacle Peak  

Broader source: Energy.gov (indexed) [DOE]

63: Vegetation Management on the Glen Canyon-Pinnacle Peak 63: Vegetation Management on the Glen Canyon-Pinnacle Peak Transmission Lines Spanning the Coconino National Forest, Coconino County, Arizona EA-1863: Vegetation Management on the Glen Canyon-Pinnacle Peak Transmission Lines Spanning the Coconino National Forest, Coconino County, Arizona Summary DOE's Western Area Power Administration is preparing this EA to evaluate the environmental impacts of updating the vegetation management and right-of-way maintenance program for Western's Glen Canyon to Pinnacle Peak 345-kV transmission lines, which cross the Coconino National Forest, Coconino County, Arizona. For more information on this EA, contact: Ms. Linette King at: lking@wapa.gov. Public Comment Opportunities No public comment opportunities available at this time.

118

Savannah River Site's H Canyon Begins 2012 with New and Continuing  

Broader source: Energy.gov (indexed) [DOE]

Site's H Canyon Begins 2012 with New and Site's H Canyon Begins 2012 with New and Continuing Missions - Transuranic waste remediation, new mission work are the focus of the nation's only active nuclear chemical separations facility in 2012 Savannah River Site's H Canyon Begins 2012 with New and Continuing Missions - Transuranic waste remediation, new mission work are the focus of the nation's only active nuclear chemical separations facility in 2012 January 1, 2012 - 12:00pm Addthis H Canyon, above, and HB-Line are scheduled to soon begin dissolving and purifying plutonium currently stored at the Savannah River Site to demonstrate the capability to produce oxide material that meets the Mixed Oxide Facility (MOX) feedstock specifications. The production process at MOX, which is now under construction, will eventually create fuel pellets for U.S. commercial reactor fuel assemblies.

119

EA-1863: Vegetation Management on the Glen Canyon-Pinnacle Peak  

Broader source: Energy.gov (indexed) [DOE]

3: Vegetation Management on the Glen Canyon-Pinnacle Peak 3: Vegetation Management on the Glen Canyon-Pinnacle Peak Transmission Lines Spanning the Coconino National Forest, Coconino County, Arizona EA-1863: Vegetation Management on the Glen Canyon-Pinnacle Peak Transmission Lines Spanning the Coconino National Forest, Coconino County, Arizona Summary DOE's Western Area Power Administration is preparing this EA to evaluate the environmental impacts of updating the vegetation management and right-of-way maintenance program for Western's Glen Canyon to Pinnacle Peak 345-kV transmission lines, which cross the Coconino National Forest, Coconino County, Arizona. For more information on this EA, contact: Ms. Linette King at: lking@wapa.gov. Public Comment Opportunities No public comment opportunities available at this time.

120

Micro-Earthquake At New York Canyon Geothermal Area (2011) | Open Energy  

Open Energy Info (EERE)

York Canyon Geothermal Area (2011) York Canyon Geothermal Area (2011) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Micro-Earthquake At New York Canyon Geothermal Area (2011) Exploration Activity Details Location New York Canyon Geothermal Area Exploration Technique Micro-Earthquake Activity Date 2011 Usefulness not indicated DOE-funding Unknown Exploration Basis Determine seismicity before and after reservoir stimulation for EGS Notes The overall goal is to gather high resolution seismicity data before, during and after stimulation activities at the EGS projects. This will include both surface and borehole deployments (as necessary in available boreholes) to provide high quality seismic data for improved processing and interpretation methodologies. This will allow the development and testing

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


121

Record of Decision - Klondike III/ Biglow Canyon Wind Integration Project - 10-25-06  

Broader source: Energy.gov (indexed) [DOE]

Klondike III/Biglow Canyon Wind Integration Project Klondike III/Biglow Canyon Wind Integration Project DECISION The Bonneville Power Administration (BPA) has decided to implement the Proposed Action identified in the Klondike III/Biglow Canyon Wind Integration Project Final Environmental Impact Statement (FEIS) (DOE/EIS-0374, September 2006). Under the Proposed Action, BPA will offer PPM Energy, Inc. (PPM) contract terms for interconnection of the proposed Klondike III Wind Project, located in Sherman County, Oregon, with the Federal Columbia River Transmission System (FCRTS). BPA will also offer Portland General Electric (PGE) 1 contract terms for interconnection of its proposed Biglow Canyon Wind Farm, also located in Sherman County, Oregon, with the FCRTS, as proposed in the FEIS. To interconnect these wind projects,

122

Recovery Act Begins Box Remediation Operations at F Canyon | Department of  

Broader source: Energy.gov (indexed) [DOE]

Recovery Act Begins Box Remediation Operations at F Canyon Recovery Act Begins Box Remediation Operations at F Canyon Recovery Act Begins Box Remediation Operations at F Canyon May 17, 2011 - 12:00pm Addthis Media Contacts Jim Giusti, DOE (803) 952-7697 james-r.giusti@srs.gov Paivi Nettamo, SRNS (803) 646-6075 paivi.nettamo@srs.gov AIKEN, S.C. - The F Canyon box remediation program, an American Recovery and Reinvestment Act project at Savannah River Site (SRS), has come online to process legacy transuranic (TRU) waste for off-site shipment and permanent disposal at the Waste Isolation Pilot Plant (WIPP), a geological repository in New Mexico. The $40-million facility will process approximately 330 boxes containing TRU waste with a radiological risk higher than seen in the rest of the Site's original 5,000-cubic-meter

123

Integrated Project Management Planning for the Deactivation of the Savannah River Site F-Canyon Complex  

SciTech Connect (OSTI)

This paper explains the planning process that is being utilized by the Westinghouse Savannah River Company to take the F-Canyon Complex facilities from operations to a deactivated condition awaiting final decommissioning.

Clark, T.G.

2000-12-01T23:59:59.000Z

124

Strontium isotopes reveal distant sources of architectural timber in Chaco Canyon, New Mexico  

E-Print Network [OSTI]

Strontium isotopes reveal distant sources of architectural timber in Chaco Canyon, New Mexico-carried from isolated mountaintops 75­100 km away. Because strontium from local dust, water, and underlying

125

Large-Eddy Simulation of Flow and Pollutant Transport in Urban Street Canyons with Ground Heating  

E-Print Network [OSTI]

Our study employed large-eddy simulation (LES) based on a one-equation subgrid-scale model to investigate the flow field and pollutant dispersion characteristics inside urban street canyons. Unstable thermal stratification ...

Li, Xian-Xiang

126

Evolution of depositional and slope instability processes on Bryant Canyon area, Northwest Gulf of Mexico  

E-Print Network [OSTI]

Bryant and Eastern Canyon systems are located on the northwest Gulf of Mexico, and they are characterized by a very complex sedimentological history related to glacioeustatic cycles, river discharges, and interactions of depositional and halokinetic...

Tripsanas, Efthymios

2005-02-17T23:59:59.000Z

127

Seismic stratigraphy and salt tectonics of the Alaminos Canyon area, Gulf of Mexico.  

E-Print Network [OSTI]

morphology, salt structure, and suprasalt sediments indicate the majority of the slope is covered by a shallow salt canopy. The salt structure map indicates that the Alaminos Canyon study area represents a transition from a semi-continuous salt sheet...

Mechler, Suzanne Marie

2012-06-07T23:59:59.000Z

128

Early Channel Evolution in the Middle Permian Brushy Canyon Formation, West Texas, USA  

E-Print Network [OSTI]

measured at both locations. A total of 16 samples were collected for petrographic analysis and X-ray fluorescence (XRF) imaging. Spectacular outcrop quality makes the Middle Permian Brushy Canyon Formation in Guadalupe Mountains National Park an ideal...

Gunderson, Spencer

2011-10-21T23:59:59.000Z

129

Savannah River Sites H Canyon Work Ensures Future Missions for Facility  

Broader source: Energy.gov [DOE]

EM and its primary contractor at the Savannah River Site (SRS) safely completed 16 facility modifications three months ahead of schedule in support of the continued operation and sustainability of the H Canyon facility.

130

Fire modeling for Building 221-T - T Plant Canyon Deck and Railroad Tunnel  

SciTech Connect (OSTI)

This report was prepared by Hughes Associates, Inc. to document the results of fire models for building 221-T Canyon Deck and Railroad Tunnel. Backup data is contained in document No. WHC-SD-CP-ANAL-010, Rev. 0.

Oar, D.L.

1994-09-29T23:59:59.000Z

131

Explaining the relationship between prehistoric agriculture and environment at Chaco Canyon, New Mexico  

E-Print Network [OSTI]

5000 feet and reaches elevations up to 11, 000 feet. The physical landscape consists of steepwalled sandstone mesa, deep canyons with many drainage resources, volcanic mountains, sand desert, and shale desert (Hunt 1974:6, 426) Most..., in the early A. D. 1200s the Chacoan culture collapsed altogather and the canyon was abandoned. Chaco Chronology and Regional System The San Juan Basin can be divide into three subareas: the Interior Lowland, the Encircling Upland, and Puerco-Red Mesa...

Gang, G-Young

2012-06-07T23:59:59.000Z

132

Canyon and channel networks of Peru-Chile fore arc at Arica Bight  

SciTech Connect (OSTI)

Canyons and channels of the Peru-Chile fore arc between 17{degree}30'S to 19{degree}30'S form a complex, integrated network revealed in SeaMARC II side-scan mosaics. The largest canyon, incised 200-600 m, is bordered by a series of sidewall slumps, producing a sinuosity that mimics subaerial meanders. The canyon courses across the Arequipa fore-arc basin floor, across a structural high and onto the middle trench slope to about 4,000 m where it disappears into a background of complex small-scale structures, From 500-2,500 m depth the canyon strikes north-south oblique to the regional slope. At 2,500 m, it abruptly turns to the southwest toward the trench axis. At this elbow, a second canyon heads on the midslope and also trends north-south until 3,500 m, where it too abruptly changes to a southwest course. A history of stream piracy analogous to subaerial systems is implied in this geometry. Tributaries join this main canyon from the landward side, forming a dendritic pattern. These channels have levees which are linked by submarine crevasse splays to sediment waves on the Arequipa basin floor. The orientation of the waves is reminiscent of bow waves from a passing ship, oblique to channel and pointing downslope, and may provide an indication of the vertical extent of passing turbidity currents. Sediments are dominantly olive gray, hemipelagic silts with sands present only immediately adjacent to the canyons. Boulders of mudstone line portions of the canyon floor. Sands are absent from the lowermost slope and trench axis, as are any indications of submarine fans. Sands may be rare in this system, with those that are present kneaded into the active margin system along the lower trench slope.

Coulbourn, W.T. (Hawaii Institute of Geophysics, Honolulu (USA))

1990-05-01T23:59:59.000Z

133

EIS-0480: Long-Term Experimental and Management Plan for the Operation of Glen Canyon Dam  

Broader source: Energy.gov [DOE]

Two agencies of the Department of the Interior, Bureau of Reclamation and National Park Service, are jointly preparing a Long-Term Experimental and Management Plan for the Glen Canyon Dam and an EIS for adoption of the Plan. The Glen Canyon Dam, on the Colorado River in northern, Arizona, generates hydroelectric power that is marketed by DOE's Western Area Power Administration, a cooperating agency.

134

Amphipods of the deep Mississippi Canyon, northern Gulf of Mexico: ecology and bioaccumulation of organic contaminants  

E-Print Network [OSTI]

AMPHIPODS OF THE DEEP MISSISSIPPI CANYON, NORTHERN GULF OF MEXICO: ECOLOGY AND BIOACCUMULATION OF ORGANIC CONTAMINANTS A Dissertation by YOUSRIA S. SOLIMAN Submitted to the Office of Graduate Studies of Texas A&M University... in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY May 2007 Major Subject: Oceanography AMPHIPODS OF THE DEEP MISSISSIPPI CANYON, NORTHERN GULF OF MEXICO: ECOLOGY AND BIOACCUMULATION...

Soliman, Yousria Soliman

2009-05-15T23:59:59.000Z

135

Hydropower and the environment: A case study at Glen Canyon Dam  

SciTech Connect (OSTI)

The management of hydroelectric resources in the Colorado River requires a balancing of hydrologic, social, natural and cultural resources. The resulting management often has to deal with inherently conflicting objectives, short and long-term goals, time frames and operational flexibility. Glen Canyon Dam, AZ, on the Colorado River, controls the release of water into the Grand Canyon. The dam has been under intense public scrutiny since it was completed in 1963. An Environmental Impact Statement evaluating the future operations and options for Glen Canyon Dam was initiated by the Department of the Interior in 1989 and completed in 1995. An Adaptive Management approach to future operational management has been developed as part of the Glen Canyon Dam Environmental Impact Statement process. Future operations at Glen Canyon Dam will take into consideration the need to balance water movement and hydroelectricity development with natural, recreation, Native American and cultural needs. Future management of rivers requires acknowledgement of the dynamic nature of ecosystems and the need to link scientific information into the decision-making process. Lessons learned and programs developed at Glen Canyon Dam may be applied to other river systems.

Wegner, D.L. [Denver Technical Service Center, Flagstaff, AZ (United States)

1995-12-31T23:59:59.000Z

136

RESEARCH AND DEVELOPMENT ACTIVITIES AT SAVANNAH RIVER SITE'S H CANYON FACILITY  

SciTech Connect (OSTI)

The Savannah River Site's (SRS) H Canyon Facility is the only large scale, heavily shielded, nuclear chemical separations plant still in operation in the U.S. The facility's operations historically recovered uranium-235 (U-235) and neptunium-237 (Np-237) from aluminum-clad, enriched-uranium fuel tubes from Site nuclear reactors and other domestic and foreign research reactors. Today the facility, in conjunction with HB Line, is working to provide the initial feed material to the Mixed Oxide Facility also located on SRS. Many additional campaigns are also in the planning process. Furthermore, the facility has started to integrate collaborative research and development (R&D) projects into its schedule. H Canyon can serve as the appropriate testing location for many technologies focused on monitoring the back end of the fuel cycle, due to the nature of the facility and continued operation. H Canyon, in collaboration with the Savannah River National Laboratory (SRNL), has been working with several groups in the DOE complex to conduct testing demonstrations of novel technologies at the facility. The purpose of conducting these demonstrations at H Canyon will be to demonstrate the capabilities of the emerging technologies in an operational environment. This paper will summarize R&D testing activities currently taking place in H Canyon and discuss the possibilities for future collaborations.

Sexton, L.; Fuller, Kenneth

2013-07-09T23:59:59.000Z

137

The Impact of the Medieval Climatic Anomaly in Prehistoric California: A Case Study from Canyon Oaks, CA-ALA-613/H  

E-Print Network [OSTI]

Burial Removal, and Monitoring at Ca-Ala-613/H, Pleasanton,Case Study From Canyon Oaks, CA-ALA-613/H | Pilloud ViolentCase Study From Canyon Oaks, CA-ALA-613/H | Pilloud McGuhe,

Pilloud, Marin A

2006-01-01T23:59:59.000Z

138

Colorado's perfect firestorm Conflagrations such as the Waldo Canyon fire may make climate change skeptics easier to  

E-Print Network [OSTI]

Op-Ed Colorado's perfect firestorm Conflagrations such as the Waldo Canyon fire may make climate their belongings and flee as the Waldo Canyon fire barreled toward their house in Colorado Springs. They were among. Colorado this year has been far drier than normal and has seen record-high temperatures. Streams

California at Davis, University of

139

PUBLISHED ONLINE: 20 JUNE 2010 | DOI: 10.1038/NGEO894 Rapid formation of a modern bedrock canyon by a  

E-Print Network [OSTI]

and sediment-transport modelling to show that the flood moved metre-sized boulders, excavated 7 m of limestone canyon by a single flood event Michael P. Lamb1 * and Mark A. Fonstad2 Deep river canyons are thought carved rapidly during ancient megaflood events4­12 . Quantification of the flood discharge, duration

140

Role of oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinatubo, Bingham Canyon and El Teniente  

E-Print Network [OSTI]

dacitic magma chamber (~ 800/C), then acid-sulphatehydrothermal fluids. At Bingham Canyon, UtahRole of oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinatubo, Bingham Canyon and El Teniente Hattori, K.H. and De Hoog, J.C.M., Earth Sciences, Univ. Ottawa, Ottawa, K1N 6N5

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


141

Microsoft Word - CX-BadgerCanyon-RichlandNo1_WoodPoles_FY13.docx  

Broader source: Energy.gov (indexed) [DOE]

7, 2013 7, 2013 REPLY TO ATTN OF: KEPR/Pasco SUBJECT: Environmental Clearance Memorandum Walker Miller Electrical Engineer - TPCF-W RICHLAND Proposed Action: Wood pole replacements on the Badger Canyon-Richland #1 transmission line PP&A Project No.: 2670 Categorical Exclusion Applied (from Subpart D, 10 C.F.R. Part 1021): B1.3 Routine maintenance activities. Location: City of Richland, Benton County, WA Transmission Line/ROW Structure # Township Range Section County, State Badger Canyon-Richland #1 4/9 and 4/10 9N 28E 26 Benton, WA Proposed by: Bonneville Power Administration (BPA) Description of the Proposed Action: BPA, at the expense of the City of Richland, proposes to raise structures 4/9 and 4/10 of the Badger Canyon-Richland #1 115-kilovolt transmission line to

142

Green Canyon Hot Springs Pool & Spa Low Temperature Geothermal Facility |  

Open Energy Info (EERE)

Green Canyon Hot Springs Pool & Spa Low Temperature Geothermal Facility Green Canyon Hot Springs Pool & Spa Low Temperature Geothermal Facility Facility Green Canyon Hot Springs Sector Geothermal energy Type Pool and Spa Location Newdale, Idaho Coordinates 43.8832463°, -111.6063483° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[]}

143

DOE - Office of Legacy Management -- White Canyon AEC Ore Buying Station -  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

White Canyon AEC Ore Buying Station White Canyon AEC Ore Buying Station - UT 04 FUSRAP Considered Sites Site: White Canyon AEC Ore Buying Station (UT.04) Designated Name: Alternate Name: Location: Evaluation Year: Site Operations: Site Disposition: Radioactive Materials Handled: Primary Radioactive Materials Handled: Radiological Survey(s): Site Status: The history of domestic uranium procurement under U.S. Atomic Energy Commission (AEC) contracts identifies a number of ore buying stations (sampling and storage sites) that were operated during the period late-1949 through the mid-1960s. During this period the AEC established ore-buying stations in new uranium producing areas where it appeared that ore production would be sufficient to support a uranium milling operation. The

144

Cosmogenic-nuclide burial ages for Pleistocene sedimentary fill in Unaweep Canyon, Colorado, USA  

Science Journals Connector (OSTI)

We applied both single-sample and isochron methods of cosmogenic-nuclide burial dating to determine the age of the sedimentary fill in Unaweep Canyon, western Colorado, USA. This stratigraphic sequence is of interest because it documents capture and diversion of the ancestral Gunnison River by the Colorado River during late Cenozoic incision of the Colorado Plateau. Seven 26Al10Be burial ages from sedimentary infill penetrated by a borehole in central Unaweep Canyon, as well as a 26Al10Be burial isochron age formed by multiple clasts and grain-size separates in a sample from the stratigraphically lower Gateway gravels, indicate that canyon blockage, initiation of lacustrine sediment accumulation, and presumed river capture, took place 1.410.19Ma. Lacustrine sedimentation ceased 1.340.13Ma.

Greg Balco; Gerilyn S. Soreghan; Dustin E. Sweet; Kristen R. Marra; Paul R. Bierman

2013-01-01T23:59:59.000Z

145

Structural character of the northern segment of the Paintbrush Canyon fault, Yucca Mountain, Nevada  

SciTech Connect (OSTI)

Detailed mapping of exposed features along the northern part of the Paintbrush Canyon fault was initiated to aid in construction of the computer-assisted three-dimensional lithostratigraphic model of Yucca Mountain, to contribute to kinematic reconstruction of the tectonic history of the Paintbrush Canyon fault, and to assist in the interpretation of geophysical data from Midway Valley. Yucca Mountain is segmented into relatively intact blocks of east-dipping Miocene volcanic strata, bounded by north-striking, west-dipping high-angle normal faults. The Paintbrush Canyon fault, representing the easternmost block-bounding normal fault, separates Fran Ridge from Midway Valley and continues northward across Yucca Wash to at least the southern margin of the Timber Mountain Caldera complex. South of Yucca Wash, the Paintbrush Canyon Fault is largely concealed beneath thick Quaternary deposits. Bedrock exposures to the north reveal a complex fault, zone, displaying local north- and west-trending grabens, and rhombic pull-apart features. The fault scarp, discontinuously exposed along a mapped length of 8 km north of Yucca Wash, dips westward by 41{degrees} to 74{degrees}. Maximum vertical offset of the Rhyolite of Comb Peak along the fault measures about 210 m in Paintbrush Canyon and, on the basis of drill hole information, vertical offset of the Topopoah Spring Tuff is about 360 m near the northern part of Fran Ridge. Observed displacement along the fault in Paintbrush Canyon is down to the west with a component of left-lateral oblique slip. Unlike previously proposed tectonic models, strata adjacent to the fault dip to the east. Quaternary deposits do not appear displaced along the fault scarp north of Yucca Wash, but are displaced in trenches south of Yucca Wash.

Dickerson, R.P. [Science Applications International Corp., Golden, CO (United States); Spengler, R.W. [Geological Survey, Denver, CO (United States)

1994-12-31T23:59:59.000Z

146

Architecture of gas-hydrate-bearing sands from Walker Ridge 313, Green Canyon 955, and Alaminos Canyon 21: Northern deepwater Gulf of Mexico  

Science Journals Connector (OSTI)

Logging-while-drilling data acquired during the 2009 Gulf of Mexico (GoM) Gas Hydrate Joint Industry Project Leg II program combined with features observed in seismic data allow assessment of the depositional environment, geometry, and internal architecture of gas-hydrate-bearing sand reservoirs from three sites in the northern Gulf of Mexico (GoM): Walker Ridge 313, Alaminos Canyon 21, and Green Canyon 955. The site descriptions assist in the understanding of the geological development of gas-hydrate-bearing sands and in the assessment of their energy production potential. Three sand-rich units are described from the Walker Ridge site, including multiple ponded sand-bodies representing turbidite channel and associated levee and terminal lobe environments within the Terrebonne basin on the lower slope of the GoM. Older units display fewer but greater-reservoir-quality channel and proximal levee facies as compared to thinner, more continuous, and unconfined sheet-like sands that characterize the younger units, suggesting a decrease in depositional gradient with time in the basin. The three wells in the Green Canyon 955 site penetrated proximal levee sands within a previously recognized Late Pleistocene basin floor turbidite-channel-levee complex. Reservoirs encountered in GC955 exhibit thin-bedded internal structure and complex fault compartmentalization. Two wells drilled in the Alaminos Canyon 21 site tested a large, shallow, sand unit within the Diana mini-basin that exhibits steep lateral margins, non-sinuous elongate form, and flat base with hummocky upper surface. These features suggest deposition as a mass-transport deposit consisting of remobilized sand-rich turbidites or as a large basin-floor fan that was potentially eroded and buried by later-stage, mud-prone, mass-transport deposits.

Ray Boswell; Matthew Frye; Dianna Shelander; William Shedd; Daniel R. McConnell; Ann Cook

2012-01-01T23:59:59.000Z

147

Final Technical Report - Modernization of the Boulder Canyon Hydroelectric Project  

SciTech Connect (OSTI)

The Boulder Canyon Hydroelectric Project (BCH) was purchased by the City of Boulder, CO (the city) in 2001. Project facilities were originally constructed in 1910 and upgraded in the 1930s and 1940s. By 2009, the two 10 MW turbine/generators had reached or were nearing the end of their useful lives. One generator had grounded out and was beyond repair, reducing plant capacity to 10 MW. The remaining 10 MW unit was expected to fail at any time. When the BCH power plant was originally constructed, a sizeable water supply was available for the sole purpose of hydroelectric power generation. Between 1950 and 2001, that water supply had gradually been converted to municipal water supply by the city. By 2001, the water available for hydroelectric power generation at BCH could not support even one 10 MW unit. Boulder lacked the financial resources to modernize the facilities, and Boulder anticipated that when the single, operational historical unit failed, the project would cease operation. In 2009, the City of Boulder applied for and received a U.S. Department of Energy (DOE) grant for $1.18 million toward a total estimated project cost of $5.155 million to modernize BCH. The federal funding allowed Boulder to move forward with plant modifications that would ensure BCH would continue operation. Federal funding was made available through the American Recovery and Reinvestment Act (ARRA) of 2009. Boulder determined that a single 5 MW turbine/generator would be the most appropriate capacity, given the reduced water supply to the plant. Average annual BCH generation with the old 10 MW unit had been about 8,500 MW-hr, whereas annual generation with a new, efficient turbine could average 11,000 to 12,000 MW-hr. The incremental change in annual generation represents a 30% increase in generation over pre-project conditions. The old turbine/generator was a single nozzle Pelton turbine with a 5-to-1 flow turndown and a maximum turbine/generator efficiency of 82%. The new unit is a double nozzle Pelton turbine with a 10-to-1 flow turndown and a maximum turbine/generator efficiency of 88%. This alone represents a 6% increase in overall efficiency. The old turbine operated at low efficiencies due to age and non-optimal sizing of the turbine for the water flow available to the unit. It was shut down whenever water flow dropped to less than 4-5 cfs, and at that flow, efficiency was 55 to 60%. The new turbine will operate in the range of 70 to 88% efficiency through a large portion of the existing flow range and would only have to be shut down at flow rates less than 3.7 cfs. Efficiency is expected to increase by 15-30%, depending on flow. In addition to the installation of new equipment, other goals for the project included: ?¢???¢ Increasing safety at Boulder Canyon Hydro ?¢???¢ Increasing protection of the Boulder Creek environment ?¢???¢ Modernizing and integrating control equipment into Boulder?¢????s municipal water supply system, and ?¢???¢ Preserving significant historical engineering information prior to power plant modernization. From January 1, 2010 through December 31, 2012, combined consultant and contractor personnel hours paid for by both the city and the federal government have totaled approximately 40,000. This equates roughly to seven people working full time on the project from January 2010 through December 2012. This project also involved considerable material expense (steel pipe, a variety of valves, electrical equipment, and the various components of the turbine and generator), which were not accounted for in terms of hours spent on the project. However, the material expense related to this project did help to create or preserve manufacturing/industrial jobs throughout the United States. As required by ARRA, the various components of the hydroelectric project were manufactured or substantially transformed in the U.S. BCH is eligible for nomination to

Joe Taddeucci, P E

2013-03-29T23:59:59.000Z

148

Abandonment of the name Elephant Canyon Formation in southeastern Utah: Physical and temporal implications  

SciTech Connect (OSTI)

At its type locality near the confluence of the Green and Colorado rivers, the Elephant Canyon Formation consists of about 1,000 ft (310 m) of cyclically interbedded sandstones, limestones, and shales. The base of the formation was previously interpreted as an angular unconformity, with Wolfcampian (Lower Permian) strata resting directly on a Missourian (lower Upper Pennsylvanian) sequence composed of similar-appearing strata called the Honaker Trail Formation. The authors however, have traced individual strata within the lower Elephant Canyon and upper Honaker Trail and have found no evidence of the angular unconformity that supposedly defines their contact. After recollecting the type section of the Elephant Canyon, they found faunal evidence indicating that the lower 450 ft (138 m) of the formation is uppermost Pennsylvanian (Virgilian) in age rather than Permian (Wolfcampian). Owing to the illusory nature of the angular unconformity and the lack of biostratigraphic evidence for a major stratigraphic break at the base of the type section, they are here abandoning Elephant Canyon Formation and reinstating the pre-1962, lithostratigraphically-based terminology. Until better physical correlations between the type locality of the Rico Formation and the Canyonlands area are available, they recommend the informal term lower Cutler beds rather than Rico Formation for the rocks below the Cedar Mesa Sandstone and above the upper member of the Hermosa Formation. In addition, interpretations of the origin and history of the Meander Anticline based on the existence of an angular unconformity within the upper Paleozoic strata of the study area must be modified.

Loope, D.B. (Univ. of Nebraska, Lincoln (USA)); Sanderson, G.A. (Amoco Production Co., Tulsa, OK (USA)); Verville, G.J.

1990-10-01T23:59:59.000Z

149

Measurements of net radiation, ground heat flux and surface temperature in an urban canyon  

SciTech Connect (OSTI)

The Joint Urban 2003 (JU2003) field study was conducted in Oklahoma City in July 2003 to collect data to increase our knowledge of dispersion in urban areas. Air motions in and around urban areas are very complicated due to the influence of urban structures on both mechanical and thermal forcing. During JU2003, meteorological instruments were deployed at various locations throughout the urban area to characterize the processes that influence dispersion. Some of the instruments were deployed to characterize urban phenomena, such as boundary layer development. In addition, particular sites were chosen for more concentrated measurements to investigate physical processes in more detail. One such site was an urban street canyon on Park Avenue between Broadway and Robinson Avenues in downtown Oklahoma City. The urban canyon study was designed to examine the processes that control dispersion within, into and out of the urban canyon. Several towers were deployed in the Park Avenue block, with multiple levels on each tower for observing the wind using sonic anemometers. Infrared thermometers, net radiometers and ground heat flux plates were deployed on two of the towers midway in the canyon to study the thermodynamic effects and to estimate the surface energy balance. We present results from the surface energy balance observations.

Gouveia, F J; Leach, M J; Shinn, J H

2003-11-06T23:59:59.000Z

150

Submarine canyons: hotspots of benthic biomass and productivity in the deep sea  

Science Journals Connector (OSTI)

...benthic invertebrate biomass and the estimated productivity...deposited onto flat, low-energy areas of the Kaikoura...the highest megabenthic biomass previously recorded at...export. The overall biomass and organic loading patterns...Kaikoura Canyon is a low-energy depocentre for POM derived...

2010-01-01T23:59:59.000Z

151

The Influence of Canyon Winds on Flow Fields near Colorado's Front Range  

Science Journals Connector (OSTI)

A network of sodars was operated in the late summer and fall of 1993 to monitor the occurrence of nocturnal winds from a canyon in Colorado's Front Range near the Rocky Flats Plant and to determine the influence of those winds on the flow fields ...

J. C. Doran

1996-04-01T23:59:59.000Z

152

EA-1980: Spar Canyon-Round Valley Access Road System Improvements, Custer County, Idaho  

Broader source: Energy.gov [DOE]

Bonneville Power Administration is preparing an EA to assess potential environmental impacts of proposed improvements to the access road system for its existing Spar Canyon-Round Valley Transmission Line located on Bureau of Land Management land in Custer County, Idaho.

153

Geology and Production Characteristics of Fractured Reservoirs in the Miocene Monterey Formation, West Cat Canyon Oilfield, Santa Maria Valley, California  

Science Journals Connector (OSTI)

West Cat Canyon Field is a faulted anticlinal ... of central coastal California known as Santa Maria Valley (Figs. 33-1, 33-2). ... fields), Lompoc, Jesus Maria, Santa Maria Valley, Casmalia, and Orcutt.

Perry O. Roehl; R. M. Weinbrandt

1985-01-01T23:59:59.000Z

154

Cap de Creus canyon: a link between shelf and slope sediment dispersal systems in the western Gulf of Lions, France  

E-Print Network [OSTI]

river, ~160 km to the NE). It is hypothesized that the westernmost Cap de Creus canyon is intercepting the regional sediment-transport pathway and directing it offshore, allowing significant sediment export through this area. The overall goal...

DeGeest, Amy Louise

2006-04-12T23:59:59.000Z

155

Capability to Recover Plutonium-238 in H-Canyon/HB-Line - 13248  

SciTech Connect (OSTI)

Plutonium-238 is used in Radioisotope Thermoelectric Generators (RTGs) to generate electrical power and in Radioisotope Heater Units (RHUs) to produce heat for electronics and environmental control for deep space missions. The domestic supply of Pu-238 consists of scrap material from previous mission production or material purchased from Russia. Currently, the United States has no significant production scale operational capability to produce and separate new Pu-238 from irradiated neptunium-237 targets. The Department of Energy - Nuclear Energy is currently evaluating and developing plans to reconstitute the United States capability to produce Pu-238 from irradiated Np-237 targets. The Savannah River Site had previously produced and/or processed all the Pu-238 utilized in Radioisotope Thermoelectric Generators (RTGs) for deep space missions up to and including the majority of the plutonium for the Cassini Mission. The previous full production cycle capabilities included: Np- 237 target fabrication, target irradiation, target dissolution and Np-237 and Pu-238 separation and purification, conversion of Np-237 and Pu-238 to oxide, scrap recovery, and Pu-238 encapsulation. The capability and equipment still exist and could be revitalized or put back into service to recover and purify Pu-238/Np-237 or broken General Purpose Heat Source (GPHS) pellets utilizing existing process equipment in HB-Line Scrap Recovery, and H-Canyon Frame Waste Recovery processes. The conversion of Np-237 and Pu-238 to oxide can be performed in the existing HB-Line Phase-2 and Phase- 3 Processes. Dissolution of irradiated Np-237 target material, and separation and purification of Np-237 and Pu-238 product streams would be possible at production rates of ?2 kg/month of Pu-238 if the existing H-Canyon Frames Process spare equipment were re-installed. Previously, the primary H-Canyon Frames equipment was removed to be replaced: however, the replacement project was stopped. The spare equipment is stored and still available for installation. Out of specification Pu-238 scrap material can be purified and recovered by utilizing the HB-Line Phase- 1 Scrap Recovery Line and the Phase-3 Pu-238 Oxide Conversion Line along with H-Canyon Frame Waste Recovery process. In addition, it also covers and describes utilizing the Phase-2 Np-237 Oxide Conversion Line, in conjunction with the H-Canyon Frames Process to restore the H-Canyon capability to process and recover Np-237 and Pu-238 from irradiated Np-237 targets and address potential synergies with other programs like recovery of Pu-244 and heavy isotopes of curium from other target material. (authors)

Fuller, Kenneth S. Jr.; Smith, Robert H. Jr.; Goergen, Charles R. [Savannah River Nuclear Solutions, LLC, Savannah River Site, Aiken, SC 29802 (United States)] [Savannah River Nuclear Solutions, LLC, Savannah River Site, Aiken, SC 29802 (United States)

2013-07-01T23:59:59.000Z

156

Depositional environment and reservoir morphology of Guadalupian Bell Canyon sandstones, Scott field, Ward and Reeves counties, Texas  

E-Print Network [OSTI]

DEPOSITIONAL ENVIRONMENT AND RESERVOIR MORPHOLOGY OF GUADALUPIAN BELL CANYON SANDSTONES, SCOTT FIELD. WARD AND REEVES COUNTIES, TEXAS A Thesis by GERARD PAUL KASHATUS Submitted to the Graduate College of Texas ASM University in partial... fulfillment of the requirement for the degree of MASTER OF SCIENCE May 1986 Major Subject: Geology DEPOSITIONAL ENVIRONMENT AND RESERVOIR MORPHOLOGY OF GUADALUPIAN BELL CANYON SANDSTONES, SCOTT FIELD, WARD AND REEVES COUNTIES, TEXAS A Thesis by GERARD...

Kashatus, Gerard Paul

2012-06-07T23:59:59.000Z

157

Microsoft Word - CX-Franklin-BadgerCanyonGrandview-RedMtnsDisconnectSwitch_WEB.docx  

Broader source: Energy.gov (indexed) [DOE]

8, 2012 8, 2012 REPLY TO ATTN OF: KEPR-4 SUBJECT: Environmental Clearance Memorandum Richard Heredia Project Manager - TEP-TPP-1 Proposed Action: Franklin-Badger Canyon and Grandview-Red Mountain switch replacements PP&A Project No.: 2,349 / 2,350 Categorical Exclusion Applied (from Subpart D, 10 C.F.R. Part 1021): B1.3 Routine maintenance Location: Benton County, Washington Proposed by: Bonneville Power Administration (BPA) Description of the Proposed Action: BPA proposes to replace disconnect switches and related equipment on the Franklin-Badger Canyon No.2 and Grandview-Red Mountain No.1 115- kilovolt transmission lines. The switch stands will be replaced in the same locations as the existing structures, and related load break equipment will be upgraded in-kind to existing. Both

158

Klondike III/Biglow Canyon Wind Integration Project; Record of Decision, October 25, 2006.  

SciTech Connect (OSTI)

The Bonneville Power Administration (BPA) has decided to implement the Proposed Action identified in the Klondike III/Biglow Canyon Wind Integration Project Final Environmental Impact Statement (FEIS) (DOE/EIS-0374, September 2006). Under the Proposed Action, BPA will offer PPM Energy, Inc. (PPM) contract terms for interconnection of the proposed Klondike III Wind Project, located in Sherman County, Oregon, with the Federal Columbia River Transmission System (FCRTS). BPA will also offer Portland General Electric (PGE)1 contract terms for interconnection of its proposed Biglow Canyon Wind Farm, also located in Sherman County, Oregon, with the FCRTS, as proposed in the FEIS. To interconnect these wind projects, BPA will build and operate a 12-mile long, 230-kilovolt (kV) double-circuit transmission line between the wind projects and BPA's new 230-kV John Day Substation in Sherman County, Oregon. BPA will also expand its existing 500-kV John Day Substation.

United States. Bonneville Power Administration

2006-10-25T23:59:59.000Z

159

Large-eddy simulation of flows over two-dimensional idealised street canyons with height variation  

Science Journals Connector (OSTI)

A series of large-eddy simulation (LES) models consisting of two-dimensional (2D) idealised street canyons with building height variability (BHV) are examined. Building blocks with two different heights are placed alternately in the computational domains, constructing repeated street canyons of building-height-to-street-width (aspect) ratio (AR) = 1, 0.5, 0.25 and 0.125 together with BHV = 0.2, 0.4 and 0.6. LES results show that the air exchange rate (ACH) increases with increasing aerodynamic resistance. Apart from AR, BHV is another factor affecting the aerodynamic resistance and thus the ACH. The (vertical) dispersion coefficient ?z of plume transport is also closely related to the aerodynamic resistance, suggesting that introducing BHV in urban areas could help improve the air quality.

Colman C.C. Wong; Chun-Ho Liu

2014-01-01T23:59:59.000Z

160

Upper Mission Canyon coated-grain producing facies in Williston basin  

SciTech Connect (OSTI)

The upper Mission Canyon formation, along the northeastern flank of the Williston basin, is a regressive carbonate and evaporite sequence, which has been informally divided into log-defined intervals. Oil production locally occurs at the transition from anhydrite to carbonate for each of the regressive intervals. These carbonate shoreline reservoirs are limestones dominated by coated grains. Porosity is intergranular and vuggy, and production from these reservoirs locally exceeds 400,000 bbl of oil/well. Upper Mission Canyon beds are also productive in island-shoal reservoirs, which developed basinward of of shorelines. These limestone reservoirs are also dominated by coated grains and porosity is intergranular and vuggy. Oil production from these reservoirs is variable, but wells within the Sherwood field along the US-Canadian border have produced over 2.0 MMbbl of oil/well.

Hendricks, M.L. (Hendricks and Associates, Inc., Denver, CO (USA))

1989-08-01T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


161

Draft Environmental Impact Statement Klondike III/Biglow Canyon Wind Integration Project  

Broader source: Energy.gov (indexed) [DOE]

Summary S-1 Summary S-1 Summary In this Summary: * Purpose and Need for Action * Alternatives * Affected Environment * Impacts This summary covers the major points of the draft Environmental Impact Statement (EIS) prepared for the Klondike III/Biglow Canyon Wind Integration Project proposed by the Bonneville Power Administration (BPA). The project includes constructing a new double-circuit 230-kilovolt (kV) transmission line in northern Sherman County, Oregon. The new line would connect the Klondike III Wind Project and the Biglow Canyon Wind Farm to BPA's existing John Day 500-kV Substation. The project would also require expansion of BPA's existing John Day 500-kV Substation and a new 230-kV substation to integrate the two wind projects. As a federal agency, BPA is required by the National Environmental Policy Act

162

Depositional environment and facies relationships of the Canyon sandstone, Val Verde Basin, Texas  

E-Print Network [OSTI]

and generous wi. th their time were Mr. Jim Patterson, Mr. Andy McDade, Mr. Buddy Reily, and Mr. Gary Swindell. Mr. Jim Hayes, Hayes Oil Company, Midland, Texas, provided the Shanklin 1-10 core. The interest and help of Mr. Hayes and Mr. Wayne Piette... Model . Transport Mechanism. Depositional History RESERVOIR CHARACTERISTICS OF THE CANYON SANDSTONE CONCI USIONS. . . . ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ REFERENCES CITED. . . . . . . . . . . ~ . ~ ~ ~ ~ APPENDIX, . . . . . . ~ ~ ~ ~, ~ ~ ~ ~ ~ ~ Osborn-Hayes-Shanklin...

Mitchell, Michael Harold

2012-06-07T23:59:59.000Z

163

Annotated bibliography for the humpback chub (Gila cypha) with emphasis on the Grand Canyon population.  

SciTech Connect (OSTI)

Glen Canyon Dam is a hydroelectric facility located on the Colorado River in Arizona that is operated by the U.S. Bureau of Reclamation (Reclamation) for multiple purposes including water storage, flood control, power generation, recreation, and enhancement of fish and wildlife. Glen Canyon Dam operations have been managed for the last several years to improve conditions for the humpback chub (Gila cypha) and other ecosystem components. An extensive amount of literature has been produced on the humpback chub. We developed this annotated bibliography to assist managers and researchers in the Grand Canyon as they perform assessments, refine management strategies, and develop new studies to examine the factors affecting humpback chub. The U.S. Geological Survey recently created a multispecies bibliography (including references on the humpback chub) entitled Bibliography of Native Colorado River Big Fishes (available at www.fort.usgs.gov/Products/data/COFishBib). That bibliography, while quite extensive and broader in scope than ours, is not annotated, and, therefore, does not provide any of the information in the original literature. In developing this annotated bibliography, we have attempted to assemble abstracts from relevant published literature. We present here abstracts taken unmodified from individual reports and articles except where noted. The bibliography spans references from 1976 to 2009 and is organized in five broad topical areas, including: (1) biology, (2) ecology, (3) impacts of dam operations, (4) other impacts, and (5) conservation and management, and includes twenty subcategories. Within each subcategory, we present abstracts alphabetically by author and chronologically by year. We present relevant articles not specific to either the humpback chub or Glen Canyon Dam, but cited in other included reports, under the Supporting Articles subcategory. We provide all citations in alphabetical order in Section 7.

Goulet, C. T.; LaGory, K. E.; Environmental Science Division

2009-10-05T23:59:59.000Z

164

CAPABILITY TO RECOVER PLUTONIUM-238 IN H-CANYON/HB-LINE  

SciTech Connect (OSTI)

Plutonium-238 is used in Radioisotope Thermoelectric Generators (RTGs) to generate electrical power and in Radioisotope Heater Units (RHUs) to produce heat for electronics and environmental control for deep space missions. The domestic supply of Pu-238 consists of scrap material from previous mission production or material purchased from Russia. Currently, the United States has no significant production scale operational capability to produce and separate new Pu-238 from irradiated neptunium-237 targets. The Department of Energy - Nuclear Energy is currently evaluating and developing plans to reconstitute the United States capability to produce Pu-238 from irradiated Np-237 targets. The Savannah River Site had previously produced and/or processed all the Pu-238 utilized in Radioisotope Thermoelectric Generators (RTGs) for deep space missions up to and including the majority of the plutonium for the Cassini Mission. The previous full production cycle capabilities included: Np-237 target fabrication, target irradiation, target dissolution and Np-237 and Pu-238 separation and purification, conversion of Np-237 and Pu-238 to oxide, scrap recovery, and Pu-238 encapsulation. The capability and equipment still exist and could be revitalized or put back into service to recover and purify Pu-238/Np-237 or broken General Purpose Heat Source (GPHS) pellets utilizing existing process equipment in HB-Line Scrap Recovery, and H-anyon Frame Waste Recovery processes. The conversion of Np-237 and Pu-238 to oxide can be performed in the existing HB-Line Phase-2 and Phase-3 Processes. Dissolution of irradiated Np-237 target material, and separation and purification of Np-237 and Pu-238 product streams would be possible at production rates of ~ 2 kg/month of Pu-238 if the existing H-Canyon Frames Process spare equipment were re-installed. Previously, the primary H-Canyon Frames equipment was removed to be replaced: however, the replacement project was stopped. The spare equipment is stored and still available for installation. Out of specification Pu-238 scrap material can be purified and recovered by utilizing the HB-Line Phase-1 Scrap Recovery Line and the Phase-3 Pu-238 Oxide Conversion Line along with H-Canyon Frame Waste Recovery process. In addition, it also covers and describes utilizing the Phase-2 Np-237 Oxide Conversion Line, in conjunction with the H-Canyon Frames Process to restore the H-Canyon capability to process and recover Np-237 and Pu-238 from irradiated Np-237 targets and address potential synergies with other programs like recovery of Pu-244 and heavy isotopes of curium from other target material.

Fuller, K.; Smith, Robert H. Jr.; Goergen, Charles R.

2013-01-09T23:59:59.000Z

165

The influence of controlled floods on fine sediment storage in debris fan-affected canyons of the Colorado River basin  

Science Journals Connector (OSTI)

Abstract Prior to the construction of large dams on the Green and Colorado Rivers, annual floods aggraded sandbars in lateral flow-recirculation eddies with fine sediment scoured from the bed and delivered from upstream. Flows greater than normal dam operations may be used to mimic this process in an attempt to increase time-averaged sandbar size. These controlled floods may rebuild sandbars, but sediment deficit conditions downstream from the dams restrict the frequency that controlled floods produce beneficial results. Here, we integrate complimentary, long-term monitoring data sets from the Colorado River in Marble and Grand Canyons downstream from Glen Canyon dam and the Green River in the Canyon of Lodore downstream from Flaming Gorge dam. Since the mid-1990s, several controlled floods have occurred in these canyon rivers. These controlled floods scour fine sediment from the bed and build sandbars in eddies, thus increasing channel relief. These changes are short-lived, however, as interflood dam operations erode sandbars within several months to years. Controlled flood response and interflood changes in bed elevation are more variable in Marble Canyon and Grand Canyon, likely reflecting more variable fine sediment supply and stronger transience in channel bed sediment storage. Despite these differences, neither system shows a trend in fine-sediment storage during the period in which controlled floods were monitored. These results demonstrate that controlled floods build eddy sandbars and increase channel relief for short interflood periods, and this response may be typical in other dam-influenced canyon rivers. The degree to which these features persist depends on the frequency of controlled floods, but careful consideration of sediment supply is necessary to avoid increasing the long-term sediment deficit.

Erich R. Mueller; Paul E. Grams; John C. Schmidt; Joseph E. Hazel Jr.; Jason S. Alexander; Matt Kaplinski

2014-01-01T23:59:59.000Z

166

Marble Canyon 1/sup 0/ x 2/sup 0/ NTMS area Arizona: data report  

SciTech Connect (OSTI)

Results of ground water and stream/surface sediment reconnaissance (HSSR) in the National Topographic Map Series (NTMS) Marble Canyon 1/sup 0/ x 2/sup 0/ quadrangle are presented. The target sampling density for all media collected was one site per 12 square kilometers. This resulted in 884 sediment samples being collected; however, dry conditions and sparse population resulted in the collection of only 2 ground water samples. Grand Canyon National Park, Glen Canyon National Recreation Area, and much Indian tribal land in the southern half of the quadrangle were not sampled. Neutron activation analysis (NAA) results are given for uranium and 16 other elements in sediments, and for uranium and 9 other elements in ground water. Mass spectrometry results are given for helium in ground water. Field measurements for sediment samples are presented in tables and maps. Statistical summaries of data and a brief description of results are given. A generalized geologic map and a summary of the geology of the area are included. Data from ground water include: water chemistry measurements (pH, conductivity, and alkalinity); physical measurements (water temperature, and scintillometer readings); and elemental analyses (U, Al, Br, Cl, Dy, F, He, Mg, Mn, Na, and V). Data from sediment sites include: water chemistry measurements (where available) for pH, conductivity, and alkalinity; and elemental analyses(U, Th, Hf, Al, Ce, Dy, Eu, Fe, La, Lu, Mn, Sc, Sm, Na, Ti, V, and Yb). Sample site descriptors (stream characteristics, vegetation, etc.) are also tabulated. Histograms, cumulative frequency, and areal distribution plots for most elements; Log U/Th, Log U/Hf, and Log U/(Th + Hf) ratios; and scintillometer readings are included.

Heffner, J.D.

1980-07-01T23:59:59.000Z

167

Numerical simulation and wind tunnel studies of pollution dispersion in an isolated street canyon  

Science Journals Connector (OSTI)

A three dimensional numerical modelling study of an urban isolated street canyon are done using Computational Fluid Dynamics (CFD) software FLUENT. The concentration predictions of FLUENT are compared with the Environmental Wind Tunnel (EWT) test results conducted at Indian Institute of Technology, Delhi for the Aspect Ratio (AR) of 1 and 1.5 at perpendicular wind direction. In FLUENT, three different k??? turbulence models, i.e., standard, Renormalisation Group (RNG) and realisable, are used. RNG model has been found to be best matched with the wind tunnel results (d = 0.80) for AR = 1, showing that for separated flows, it works best.

Seema Awasthi; K.K. Chaudhry

2009-01-01T23:59:59.000Z

168

221-U Facility concrete and reinforcing steel evaluations specification for the canyon disposition initiative (CDI)  

SciTech Connect (OSTI)

This describes a test program to establish the in-situ material properties of the reinforced concrete in Building 221-U for comparison to the original design specifications. Field sampling and laboratory testing of concrete and reinforcing steel structural materials in Building 221-U for design verification will be undertaken. Forty seven samples are to be taken from radiologically clean exterior walls of the canyon. Laboratory testing program includes unconfined compressive strength of concrete cores, tensile strength of reinforcing steel, and petrographic examinations of concrete cores taken from walls below existing grade.

Baxter, J.T.

1998-05-28T23:59:59.000Z

169

Seismic stratigraphy and salt tectonics along the Sigsbee Escarpment, southeastern Green Canyon region  

E-Print Network [OSTI]

for the degree of MASTER OF SCIENCE December 1986 Major Subject: Geophysics SEISItllC STRATIGHAPHY AND SALT TECTONICS ALONG THE 'ilGSHEL' L'SCARPMENT. SOI. THEASTERX GREEN CANYON RFGION A Thesis ALAN MARK SWIERCZ Approved as to style and content by: Earl... R. Hoskins (Chairman of Committee) Robert J. McCabe (Member) Gr M. arberg (Member) AVilliam R. Bryant ('Member) j~/ Earl R. Hoskins (Head of Department) December 1986 ABSTRAC'T Seismic Stratigraphy and Salt Tectonics along the Sigsbee...

Swiercz, Alan Mark

2012-06-07T23:59:59.000Z

170

Deformation of a basement corner, Crazy Woman Canyon, northeastern Bighorn Mountains, Wyoming  

E-Print Network [OSTI]

to differential uplift and rotation of basement blocks. The objectives of the pmject are as follows: 1. To study how the crystalline basement deforms and how it interacts with the sedimentary cover rocks, 2. To produce a detailed geologic map of the area... mapping at a scale of 1:12, 000, clay models, and geologic cross sections suggest two possible interpretations of how the uplifted and rotated basement blocks in the Crazy Woman Canyon area are related to the regional geometry of the eastern Bighorn...

Smith, Gretchen Louise

2012-06-07T23:59:59.000Z

171

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM  

SciTech Connect (OSTI)

Advanced reservoir characterization techniques are being used at the Nash Draw Brushy Canyon Pool project to develop reservoir management strategies for optimizing oil recovery from this Delaware reservoir. The reservoir characterization, geologic modeling, 3-D seismic interpretation, and simulation studies have provided a detailed model of the Brushy Canyon zones. This model was used to predict the success of different reservoir management scenarios and to aid in determining the most favorable combination of targeted drilling, pressure maintenance, well stimulation, and well spacing to improve recovery from this reservoir.

Murphy, M.B.

1999-02-01T23:59:59.000Z

172

A review on the flow structure and pollutant dispersion in urban street canyons for urban planning strategies  

Science Journals Connector (OSTI)

As a result of rapid urbanization in numerous cities around the world, the demand for transportation has increased rapidly, resulting in emission of high levels of exhaust pollutants into the atmosphere. This is a major cause of deterioration in the ... Keywords: Urban street canyon, air quality, flow structure, pollutant dispersion

Afiq Witri Muhammad Yazid, Nor Azwadi Che Sidik, Salim Mohamed Salim, Khalid M Saqr

2014-08-01T23:59:59.000Z

173

Basin configuration and depositional trends in the Mission Canyon and Ratcliffe beds, U.S. portion of the Williston basin  

SciTech Connect (OSTI)

Construction of Mission Canyon and Ratcliffe depositional trends utilizing shoreline models and anhydrite edge maps shows a significant change in basin configuration associated with regional sea level changes. Sea level highstand, which began during deposition of the Scallion member of the Lodgepole Formation, was punctuated by two lowstand events. The first occurred during deposition of the MC-2 anhydrite (Tilston). During this lowstand event, the width of the carbonate basin decreased significantly. With sea level rise, a broad basin formed with carbonate and evaporate ramp deposition (Lands, Wayne, Glenburn and Mohall members). The top of the Mohall contains evidence of the second lowstand event. This event introduced quartz sand detritus into the basin (Kisbey Sandstone). Because of sea level lowstand, Sherwood and younger Mission Canyon beds were deposited during highstand in a narrower carbonate basin. Funneling of marine currents and tides in this basin created higher energy shoreline and shoal deposits than those commonly found in older Mission Canyon sediments. The top of the Mission Canyon (Rival) was capped by a deepening event or transgression which enlarged the basin and created broad Ratcliffe ramp systems similar to those that existed during Glenburn and Mohall deposition. By utilizing sequence stratigraphy and mapping shoreline trends and basin configuration, reservoir and trap geometries are identified, and exploration success is improved.

Hendricks, M.L. [Hendricks and Associates, Inc., Englewood, CO (United States)

1996-06-01T23:59:59.000Z

174

Age of Barrier Canyon-style rock art constrained by cross-cutting relations and luminescence dating techniques  

Science Journals Connector (OSTI)

...Rock Art of the Colorado Plateau and Four...Johnson Books , Boulder, CO ). 21 Schaafsma...in canyons of the Colorado Plateau . Geol Soc Am Bull...record of extreme floods and climate change...drought in the upper Colorado River Basin . Geophys...Study of Rock Art (Boulder, CO). The authors...

Joel L. Pederson; Melissa S. Chapot; Steven R. Simms; Reza Sohbati; Tammy M. Rittenour; Andrew S. Murray; Gary Cox

2014-01-01T23:59:59.000Z

175

Age of Barrier Canyon-style rock art constrained by cross-cutting relations and luminescence dating techniques  

Science Journals Connector (OSTI)

...coincident with the top of former T1 flood deposits providing a platform...sediment storage in canyons of the Colorado Plateau . Geol Soc Am Bull 99 ( 2...5000-year record of extreme floods and climate change in the southwestern...Medieval drought in the upper Colorado River Basin . Geophys Res Lett...

Joel L. Pederson; Melissa S. Chapot; Steven R. Simms; Reza Sohbati; Tammy M. Rittenour; Andrew S. Murray; Gary Cox

2014-01-01T23:59:59.000Z

176

Multiple fluvial processes detected by riverside seismic and infrasound monitoring of a controlled flood in the Grand Canyon  

E-Print Network [OSTI]

experiment (CFE) in the Grand Canyon to show that three types of fluvial processes can be monitored from as the dominant seismic source between 15 and 45 Hz. Two lower-frequency seismic bands also excited by the CFE and infrasound responses to the CFE. Citation: Schmandt, B., R. C. Aster, D. Scherler, V. C. Tsai, and K

Tsai, Victor C.

177

Fall Chinook Acclimation Project; Pittsburg Landing, Captain John Rapids, and Big Canyon, Annual Report 2003.  

SciTech Connect (OSTI)

Fisheries co-managers of U.S. v Oregon supported and directed the construction and operation of acclimation and release facilities for Snake River fall Chinook from Lyons Ferry Hatchery at three sites above Lower Granite Dam. In 1996, Congress instructed the U.S. Army Corps of Engineers (USCOE) to construct, under the Lower Snake River Compensation Plan (LSRCP), final rearing and acclimation facilities for fall Chinook in the Snake River basin to complement their activities and efforts in compensating for fish lost due to construction of the lower Snake River dams. The Nez Perce Tribe (NPT) played a key role in securing funding and selecting acclimation sites, then assumed responsibility for operation and maintenance of the facilities. In 1997, Bonneville Power Administrative (BPA) was directed to fund operations and maintenance (O&M) for the facilities. Two acclimation facilities, Captain John Rapids and Pittsburg Landing, were located on the Snake River between Asotin, WA and Hells Canyon Dam and one facility, Big Canyon, was located on the Clearwater River at Peck. The Capt. John Rapids facility is a single pond while the Pittsburg Landing and Big Canyon sites consist of portable fish rearing tanks assembled and disassembled each year. Acclimation of 450,000 yearling smolts (150,000 each facility) begins in March and ends 6 weeks later. When available, an additional 2,400,000 fall Chinook sub-yearlings may be acclimated for 6 weeks, following the smolt release. The project goal is to increase the naturally spawning population of Snake River fall Chinook salmon upstream of Lower Granite Dam. This is a supplementation project; in that hatchery produced fish are acclimated and released into the natural spawning habitat for the purpose of returning a greater number of spawners to increase natural production. Only Snake River stock is used and production of juveniles occurs at Lyons Ferry Hatchery. This is a long-term project, targeted to work towards achieving delisting goals established by National Marine Fisheries Service (NMFS or NOAA Fisheries) and ultimately to provide fall Chinook adults through the Lower Snake River Compensation Plan program as mitigation for construction and operation of the four lower Snake River dams. Complete adult returns (all age classes) for all three acclimation facilities occurred in the year 2002. Progeny (which would then be natural origin fish) would be counted towards achieving Endangered Species Act delisting criteria. In 2003, a total of 2,138,391 fish weighing 66,201 pounds were released from the three acclimation facilities. The total includes 437,633 yearling fish weighing 44,330 pounds and 1,700,758 sub-yearling fish weighing 21,871 pounds.

McLeod, Bruce

2004-01-01T23:59:59.000Z

178

Preliminary Thermal Modeling of HI-STORM 100 Storage Modules at Diablo Canyon Power Plant ISFSI  

SciTech Connect (OSTI)

Thermal analysis is being undertaken at Pacific Northwest National Laboratory (PNNL) in support of inspections of selected storage modules at various locations around the United States, as part of the Used Fuel Disposition Campaign of the U.S. Department of Energy, Office of Nuclear Energy (DOE-NE) Fuel Cycle Research and Development. This report documents pre-inspection predictions of temperatures for two modules at the Diablo Canyon Power Plant ISFSI identified as candidates for inspection. These are HI-STORM 100 modules of a site-specific design for storing PWR 17x17 fuel in MPC-32 canisters. The temperature predictions reported in this document were obtained with detailed COBRA-SFS models of these storage systems, with the following boundary conditions and assumptions. storage module overpack configuration based on FSAR documentation of HI-STORM100S-218, Version B; due to unavailability of site-specific design data for Diablo Canyon ISFSI modules Individual assembly and total decay heat loadings for each canister, based on at-loading values provided by PG&E, aged to time of inspection using ORIGEN modeling o Special Note: there is an inherent conservatism of unquantified magnitude informally estimated as up to approximately 20% -- in the utility-supplied values for at-loading assembly decay heat values Axial decay heat distributions based on a bounding generic profile for PWR fuel. Axial location of beginning of fuel assumed same as WE 17x17 OFA fuel, due to unavailability of specific data for WE17x17 STD and WE 17x17 Vantage 5 fuel designs Ambient conditions of still air at 50F (10C) assumed for base-case evaluations o Wind conditions at the Diablo Canyon site are unquantified, due to unavailability of site meteorological data o additional still-air evaluations performed at 70F (21C), 60F (16C), and 40F (4C), to cover a range of possible conditions at the time of the inspection. (Calculations were also performed at 80F (27C), for comparison with design basis assumptions.) All calculations are for steady-state conditions, on the assumption that the surfaces of the module that are accessible for temperature measurements during the inspection will tend to follow ambient temperature changes relatively closely. Comparisons to the results of the inspections, and post-inspection evaluations of temperature measurements obtained in the specific modules, will be documented in a separate follow-on report, to be issued in a timely manner after the inspection has been performed.

Cuta, Judith M.; Adkins, Harold E.

2014-04-17T23:59:59.000Z

179

Fall Chinook Aclimation Project; Pittsburg Landing, Captain John Rapids, and Big Canyon, Annual Report 2001.  

SciTech Connect (OSTI)

Fisheries co-managers of U.S. v Oregon supported and directed the construction and operation of acclimation and release facilities for Snake River fall Chinook from Lyons Ferry Hatchery at three sites above Lower Granite Dam. In 1996, Congress instructed the U.S. Army Corps of Engineers (USCOE) to construct, under the Lower Snake River Compensation Plan (LSRCP), final rearing and acclimation facilities for fall Chinook in the Snake River basin to complement their activities and efforts in compensating for fish lost due to construction of the lower Snake River dams. The Nez Perce Tribe (NPT) played a key role in securing funding and selecting acclimation sites, then assumed responsibility for operation and maintenance of the facilities. In 1997, Bonneville Power Administrative (BPA) was directed to fund operations and maintenance (O&M) for the facilities. Two acclimation facilities, Captain John Rapids and Pittsburg Landing, are located on the Snake River between Asotin, WA and Hells Canyon Dam and one facility, Big Canyon, is located on the Clearwater River at Peck. The Capt. John Rapids facility is a single pond while the Pittsburg Landing and Big Canyon sites consist of portable fish rearing tanks assembled and disassembled each year. Acclimation of 450,000 yearling smolts (150,000 each facility) begins in March and ends 6 weeks later. When available, an additional 2,400,000 fall Chinook sub-yearlings may be acclimated for 6 weeks, following the smolt release. The project goal is to increase the naturally spawning population of Snake River fall Chinook salmon upstream of Lower Granite Dam. This is a supplementation project; in that hatchery produced fish are acclimated and released into the natural spawning habitat for the purpose of returning a greater number of spawners to increase natural production. Only Snake River stock is used and production of juveniles occurs at Lyons Ferry Hatchery. This is a long-term project, and will ultimately work towards achieving delisting goals established by National Marine Fisheries Service (NMFS). Complete returns for all three acclimation facilities will not occur until the year 2002. Progeny (which would then be natural origin fish protected under the Endangered Species Act) from those returns will be returning for the next five years. In 2001, a total of 2,051,099 fish weighing 59,647 pounds were released from the three acclimation facilities. The total includes 318,932 yearling fish weighing 31,128 pounds and 1,732,167 sub-yearling fish weighing 28,519 pounds. Yearling fish numbers were reduced by Bacterial Kidney Disease (BKD) and sub-yearling acclimation time was limited by record low river water flows.

McLeod, Bruce

2004-01-01T23:59:59.000Z

180

Draft Environmental Impact Statement Klondike III/Biglow Canyon Wind Integration Project  

Broader source: Energy.gov (indexed) [DOE]

generated from the proposed Klondike III Wind Project to the Federal Columbia River Transmission System. Orion Energy LLC has also asked BPA to interconnect 400 MW of electricity from its proposed Biglow Canyon Wind Farm, located north and east of the proposed Klondike III Wind Project. To interconnect these projects, BPA would need to build and operate a 230-kV double-circuit transmission line about 12 miles long, expand one substation and build one new substation. The wind projects would require wind turbines, substation(s), access roads, and other facilities. Two routes for the transmission line are being considered. Both begin at PPM's Klondike Schoolhouse Substation then travel north (Proposed Action) or north and westerly (Middle Alternative) to a new BPA

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


181

Long-term surveillance plan for the Bodo Canyon Disposal Site, Durango, Colorado  

SciTech Connect (OSTI)

This long-term surveillance plan (LTSP) for the Durango, Colorado, Uranium Mill Tailings Remedial Action (UMTRA) Project disposal site describes the surveillance activities for the Durango (Bodo Canyon) disposal site, which will be referred to as the disposal site throughout this document. The US Department of Energy (DOE) will carry out these activities to ensure that the disposal site continues to function as designed. This LTSP was prepared as a requirement for acceptance under the US Nuclear Regulatory Commission (NRC) general license for custody and long-term care of residual radioactive materials (RRM). RRMs include tailings and other uranium ore processing wastes still at the site, which the DOE determines to be radioactive. This LTSP is based on the DOE`s Guidance for Implementing the UMTRA Project Long-term Surveillance Program (DOE, 1992).

Not Available

1994-03-01T23:59:59.000Z

182

Integrated study of Mediterranean deep canyons: Novel results and future challenges  

Science Journals Connector (OSTI)

Abstract This volume compiles a number of scientific papers resulting from a sustained multidisciplinary research effort of the deep-sea ecosystem in the Mediterranean Sea. This started 20 years ago and peaked over the last few years thanks to a number of Spanish and European projects such as PROMETEO, DOS MARES, REDECO, GRACCIE, HERMES, HERMIONE and PERSEUS, amongst others. The geographic focus of most papers is on the NW Mediterranean Sea including the Western Gulf of Lion and the North Catalan margin, with a special attention to submarine canyons, in particular the Blanes and Cap de Creus canyons. This introductory article to the Progress in Oceanography special issue on Mediterranean deep canyons provides background information needed to better understand the individual papers forming the volume, comments previous reference papers related to the main topics here addressed, and finally highlights the existing relationships between atmospheric forcing, oceanographic processes, seafloor physiography, ecosystem response, and litter and chemical pollution. This article also aims at constituting a sort of glue, in terms of existing knowledge and concepts and novel findings, linking together the other twenty papers in the volume, also including some illustrative figures. The main driving ideas behind this special issue, particularly fitting to the study area of the NW Mediterranean Sea, could be summarized as follows: (i) the atmosphere and the deep-sea ecosystem are connected through oceanographic processes originating in the coastal area and the ocean surface, which get activated at the occasion of high-energy events leading to fast transfers of matter and energy to the deep; (ii) shelf indented submarine canyons play a pivotal role in such transfers, which involve dense water, sedimentary particles, organic matter, litter and chemical pollutants; (iii) lateral inputs (advection) from the upper continental margin contributes significantly to the formation of intermediate and deep-water masses, and the associated fluxes of matter and energy are a main driver of deep-sea ecosystems; (iv) deep-sea organisms are highly sensitive to the arrival of external inputs, starting from the lowest food web levels and propagating upwards as time passes, which also relies upon the biology, nutritional needs and life expectancy of each individual species; and (v) innovative knowledge gained through such multidisciplinary research is of the utmost significance for an improved management of deep-sea living resources, such as the highly priced red shrimp Aristeus antennatus, for which a pilot management plan largely based in the findings described here and in related articles has been recently published (BOE, 2013). The researchers involved in such challenging endeavour have learnt tremendously from the results obtained so far and from each other, but are fully aware that there are still many unsolved questions. That is why this introductory article also includes Future challenges both in the title and as an individual section at the end, to express that there is still a long way to go.

M. Canals; J.B. Company; D. Martn; A. Snchez-Vidal; E. Ramrez-Llodr

2013-01-01T23:59:59.000Z

183

Dynamic modelling of transient emissions and concentrations from traffic in street canyons  

Science Journals Connector (OSTI)

In the EU 5th framework project DECADE (2001??2003), a new methodology has been developed to calculate in detail the engine power required to drive a given vehicle over any particular route. It includes the rapidly changing (transient) demands placed on the engine, an area that has proved an obstacle to accurate simulations in the past. Together with the associated speed profiles, the actual power demands allow a detailed calculation of emissions and ambient air concentrations in street canyons. This makes the methodology a valuable tool for detailed assessments of the ambient air quality impact of e.g., street design (traffic lights, road bumps, busy crossings), driving patterns, driving behaviour and fleet composition.

Clemens Mensink; Guido Cosemans; Luc Pelkmans

2005-01-01T23:59:59.000Z

184

Process centrifuge operating problems and equipment failures in canyon reprocessing facilities at the Savannah River Site  

SciTech Connect (OSTI)

The Savannah River Laboratory (SRL) maintains a compilation of operating problems and equipment failures that have occurred in the fuel reprocessing areas of the Savannah River Site (SRS). At present, the data bank contains more than 230,000 entries ranging from minor equipment malfunctions to incidents with the potential for injury or contamination of personnel, or for economic loss. The data bank has been used extensively for a wide variety of purposes, such as failure analyses, trend analyses, and preparation of safety analyses. Typical of the data are problems associated with the canyon process centrifuges. This report contains a compilation of the centrifuge operating problems and equipment failures primarily as an aid to organizations with related equipment. Publication of these data was prompted by a number of requests for this information by other Department of Energy (DOE) sites. 11 refs., 2 figs., 4 tabs.

Durant, W.S.; Baughman, D.F.

1990-03-01T23:59:59.000Z

185

Hydrodynamic effects on Mission Canyon (Mississippian) oil accumulations, Billings Nose area, North Dakota  

SciTech Connect (OSTI)

Mission Canyon oil production on the south flank of the Williston basin provides an example of an area in the mature stage of exploration that shows significant hydrodynamic effects on oil accumulations related to stratigraphic traps. The effects are illustrated by the Billings Nose fields and the Elkhorn Ranch field. The reservoirs have low hydraulic gradients of about 2 m/km (10 ft/mi), tilted oil-water contacts with gradients of 5 m/km (25 ft/mi), and variable formation-water salinities that range from brackish to highly saline. Oil accumulations in some zones are displayed off structure and downdip to the northeast, parallel to porosity pinch-outs. Other zones are pure hydrodynamic closure. Future success in exploration and development in the play will depend on recognizing the hydrodynamic effects and predicting oil displacement. 34 refs., 15 figs., 1 tab.

Berg, R.R. (Texas A M Univ., College Station, TX (United States)); DeMis, W.D. (Marathon Oil Co., Houston, TX (United States)); Mitsdarffer, A.R. (Dupont Environmental Remediation Services, Houston, TX (United States))

1994-04-01T23:59:59.000Z

186

Occurrence of gas hydrate in Oligocene Frio sand: Alaminos Canyon Block 818: Northern Gulf of Mexico  

SciTech Connect (OSTI)

A unique set of high-quality downhole shallow subsurface well log data combined with industry standard 3D seismic data from the Alaminos Canyon area has enabled the first detailed description of a concentrated gas hydrate accumulation within sand in the Gulf of Mexico. The gas hydrate occurs within very fine grained, immature volcaniclastic sands of the Oligocene Frio sand. Analysis of well data acquired from the Alaminos Canyon Block 818 No.1 ('Tigershark') well shows a total gas hydrate occurrence 13 m thick, with inferred gas hydrate saturation as high as 80% of sediment pore space. Average porosity in the reservoir is estimated from log data at approximately 42%. Permeability in the absence of gas hydrates, as revealed from the analysis of core samples retrieved from the well, ranges from 600 to 1500 millidarcies. The 3-D seismic data reveals a strong reflector consistent with significant increase in acoustic velocities that correlates with the top of the gas-hydrate-bearing sand. This reflector extends across an area of approximately 0.8 km{sup 2} and delineates the minimal probable extent of the gas hydrate accumulation. The base of the inferred gas-hydrate zone also correlates well with a very strong seismic reflector that indicates transition into units of significantly reduced acoustic velocity. Seismic inversion analyses indicate uniformly high gas-hydrate saturations throughout the region where the Frio sand exists within the gas hydrate stability zone. Numerical modeling of the potential production of natural gas from the interpreted accumulation indicates serious challenges for depressurization-based production in settings with strong potential pressure support from extensive underlying aquifers.

Boswell, R.D.; Shelander, D.; Lee, M.; Latham, T.; Collett, T.; Guerin, G.; Moridis, G.; Reagan, M.; Goldberg, D.

2009-07-15T23:59:59.000Z

187

Paleoseismic investigations of the Paintbrush Canyon fault in southern Midway Valley, Yucca Mountain, Nevada: Preliminary results  

SciTech Connect (OSTI)

Trench mapping in southern Midway Valley provides evidence of multiple surface-faulting events on a western splay of the Paintbrush Canyon fault during the middle to late Pleistocene. The 6-m-wide fault zone exposed in the trench strikes N30-45E and dips steeply ([approximately]78[degree]) to the west, although some shears within the zone dip to the east. Tertiary volcanic bedrock is exposed only on the footwall block within the trench. Unconsolidated colluvial and eolian deposits are present in the hanging-wall block and above bedrock in the footwall block. These deposits tentatively are assigned, respectively, mid Pleistocene and late Pleistocene ages based on correlations with surficial map units in Midway Valley. Three to five displacement events are inferred based on faulted colluvial and eolian deposits, and scarp-derived colluvial wedges. Total cumulative dip-slip displacement of the oldest middle Pleistocene subunit is estimated to be about 170 to 270 cm. The dip-slip displacement associated with the youngest event is about 15 cm. The earlier displacements are estimated to have produced between 40 and 85 cm of dip-slip displacement per event. The most recent event occurred after deposition of late Pleistocene colluvium deposited against the fault scarp but before deposition of an overlying hillslope-derived colluvium of probable late pleistocene age. Based on the preliminary results of the authors study, the middle to late Quaternary rate of dip-slip displacement is approximately 0.01 m/kyr or less. Ongoing work, including soil-stratigraphic studies and numerical dating of deposits, should better constrain the timing and a rate of faulting along this western splay of the Paintbrush Canyon fault.

Swan, F.H.; Wesling, J.R.; Thomas, A.P. (Geomatrix Consultants, San Francisco, CA (United States))

1993-04-01T23:59:59.000Z

188

Ex post power economic analysis of record of decision operational restrictions at Glen Canyon Dam.  

SciTech Connect (OSTI)

On October 9, 1996, Bruce Babbitt, then-Secretary of the U.S. Department of the Interior signed the Record of Decision (ROD) on operating criteria for the Glen Canyon Dam (GCD). Criteria selected were based on the Modified Low Fluctuating Flow (MLFF) Alternative as described in the Operation of Glen Canyon Dam, Colorado River Storage Project, Arizona, Final Environmental Impact Statement (EIS) (Reclamation 1995). These restrictions reduced the operating flexibility of the hydroelectric power plant and therefore its economic value. The EIS provided impact information to support the ROD, including an analysis of operating criteria alternatives on power system economics. This ex post study reevaluates ROD power economic impacts and compares these results to the economic analysis performed prior (ex ante) to the ROD for the MLFF Alternative. On the basis of the methodology used in the ex ante analysis, anticipated annual economic impacts of the ROD were estimated to range from approximately $15.1 million to $44.2 million in terms of 1991 dollars ($1991). This ex post analysis incorporates historical events that took place between 1997 and 2005, including the evolution of power markets in the Western Electricity Coordinating Council as reflected in market prices for capacity and energy. Prompted by ROD operational restrictions, this analysis also incorporates a decision made by the Western Area Power Administration to modify commitments that it made to its customers. Simulated operations of GCD were based on the premise that hourly production patterns would maximize the economic value of the hydropower resource. On the basis of this assumption, it was estimated that economic impacts were on average $26.3 million in $1991, or $39 million in $2009.

Veselka, T. D.; Poch, L. A.; Palmer, C. S.; Loftin, S.; Osiek, B; Decision and Information Sciences; Western Area Power Administration

2010-07-31T23:59:59.000Z

189

Tectonostratigraphic reconstruction and lithofacies distribution of tertiary slope sedimentary rocks in the Western Mississippi Canyon area  

SciTech Connect (OSTI)

The distribution of upper Tertiary, sandstone-prone, deep-water sedimentary rocks from the vicinity of Cognac field, Mississippi Canyon (MC) 194, south of Mars field (MC763) is presented based on an integrated sequence stratigraphic analysis of seismic, well log, and biostratigraphic data. Paleo-salt distributions were reconstructed by plotting the changing positions of depocenters on five isopach maps generated from six key sequence boundaries. Depositional trends, projected under allochthonous salt sheets, indicated subsalt prospectivity. Sixteen sequences were interpreted and subdivided into three lowstand depositional units (basin-floor fan, slope fan, and prograding wedge). Thirty isochron/seismic facies maps were made to reveal the stratigraphic pattern through the late Tertiary. During the early Miocene, a salt-rimmed syncline centered north of Mars field in MC455 accumulated sediments. The salt rim collapsed, creating a middle Miocene turtle structure. Middle-late Miocene sand-rich turbidites bypassed this structure and were deposited to the south around Mars field and beyond. At the same time, another depotrough 30 mi east of Mars field channeled deep-water sands to the MC730 area. A late Miocene-early Pliocene counterregional fault striking parallel to the shelf edge formed as salt evacuated the area on the south side of the Cognac (MC194) and Lena (MC280) fields. This fault trapped the Pliocene reservoir sandstones that produce in these fields. Sedimentation during the late Pliocene-early Pleistocene was very slow (0.2m/1,000 yr) and characterized by thin, stacked, condensed sections of hemipelagic shale. Since the mid-Pleistocene, the Mississippi River has supplied sediments to the Mississippi Canyon area that have induced salt deformation that has in turn affected recent sedimentation.

Hannan, A.E.; Risch, D.L.; Chowdhury, A.N. [Geco-Prakla, Inc., Houston, TX (United States)

1994-12-31T23:59:59.000Z

190

P-Wave Residual Differences and Inferences on an Upper Mantle Source for the Silent Canyon Volcanic Centre, Southern Great Basin, Nevada  

Science Journals Connector (OSTI)

......Canyon volcanic centre of the Nevada Test Site have been reduced by corresponding...1968. Geologic setting of Nevada Test Site and Neliis Air Force Range...comparison of the Lake Superior and Nevada Test Site source regions, Seism. Data......

William Spence

1974-09-01T23:59:59.000Z

191

AVTA Federal Fleet PEV Readiness Data Logging and Characterization Study for the National Park Service: Grand Canyon National Park  

SciTech Connect (OSTI)

This report focuses on the Grand Canyon National Park (GCNP) fleet to identify daily operational characteristics of select vehicles and report findings on vehicle and mission characterizations to support the successful introduction of PEVs into the agencies fleets. Individual observations of these selected vehicles provide the basis for recommendations related to electric vehicle adoption and whether a battery electric vehicle or plug-in hybrid electric vehicle (collectively PEVs) can fulfill the mission requirements.

Stephen Schey; Jim Francfort; Ian Nienhueser

2014-08-01T23:59:59.000Z

192

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM  

SciTech Connect (OSTI)

The Nash Draw Brushy Canyon Pool in Eddy County New Mexico is a cost-shared field demonstration project in the US Department of Energy Class II Program. A major goal of the Class III Program is to stimulate the use of advanced technologies to increase ultimate recovery from slope-basin clastic reservoirs. Advanced characterization techniques are being used at the Nash Draw project to develop reservoir management strategies for optimizing oil recovery from this Delaware reservoir. Analysis, interpretation, and integration of recently acquired geologic, geophysical, and engineering data revealed that the initial reservoir characterization was too simplistic to capture the critical features of this complex formation. Contrary to the initial characterization, a new reservoir description evolved that provided sufficient detail regarding the complexity of the Brushy Canyon interval at Nash Draw. This new reservoir description is being used as a risk reduction tool to identify ''sweet spots'' for a development drilling program as well as to evaluate pressure maintenance strategies. The reservoir characterization, geological modeling, 3-D seismic interpretation, and simulation studies have provided a detailed model of the Brushy Canyon zones. This model was used to predict the success of different reservoir management scenarios and to aid in determining the most favorable combination of targeted drilling, pressure maintenance, well simulation, and well spacing to improve recovery from this reservoir.

Murphy, Mark B.

1999-02-24T23:59:59.000Z

193

Klondike III/Biglow Canyon Wind Integration Project; Final Environmental Impact Statement, September 2006.  

SciTech Connect (OSTI)

BPA has been asked by PPM Energy, Inc. to interconnect 300 megawatts (MW) of electricity generated from the proposed Klondike III Wind Project to the Federal Columbia River Transmission System. Orion Energy LLC has also asked BPA to interconnect 400 MW of electricity from its proposed Biglow Canyon Wind Farm, located north and east of the proposed Klondike III Wind Project. (Portland General Electric recently bought the rights to develop the proposed Biglow Canyon Wind Farm from Orion Energy, LLC.) Both wind projects received Site Certificates from the Oregon Energy Facility Siting Council on June 30, 2006. To interconnect these projects, BPA would need to build and operate a 230-kV double-circuit transmission line about 12 miles long, expand one substation and build one new substation. The wind projects would require wind turbines, substation(s), access roads, and other facilities. Two routes for the transmission line are being considered. Both begin at PPM's Klondike Schoolhouse Substation then travel north (Proposed Action) or north and westerly (Middle Alternative) to a new BPA 230-kV substation next to BPA's existing John Day 500-kV Substation. BPA is also considering a No Action Alternative in which BPA would not build the transmission line and would not interconnect the wind projects. The proposed BPA and wind projects would be located on private land, mainly used for agriculture. If BPA decides to interconnect the wind projects, construction of the BPA transmission line and substation(s) could commence as early as the winter of 2006-07. Both wind projects would operate for much of each year for at least 20 years. The proposed projects would generally create no or low impacts. Wildlife resources and local visual resources are the only resources to receive an impact rating other than ''none'' or ''low''. The low to moderate impacts to wildlife are from the expected bird and bat mortality and the cumulative impact of this project on wildlife when combined with other proposed wind projects in the region. The low to high impacts to visual resources reflect the effect that the transmission line and the turbine strings from both wind projects would have on viewers in the local area, but this impact diminishes with distance from the project.

United States. Bonneville Power Administration

2006-09-01T23:59:59.000Z

194

Flowsheet modifications for dissolution of sand, slag, and crucible residues in the F-canyon dissolvers  

SciTech Connect (OSTI)

An initial flowsheet for the dissolution of sand, slag, and crucible (SS{ampersand}C) was developed for the F- Canyon dissolvers as an alternative to dissolution in FB-Line. In that flowsheet, the sand fines were separated from the slag chunks and crucible fragments. Those two SS{ampersand}C streams were packaged separately in mild-steel cans for dissolution in the 6.4D dissolver. Nuclear safety constraints limited the dissolver charge to approximately 350 grams of plutonium in two of the three wells of the dissolver insert and required 0.23M (molar) boron as a soluble neutron poison in the 9.3M nitric acid/0.013M fluoride dissolver solution. During the first dissolution of SS{ampersand}C fines, it became apparent that a significant amount of the plutonium charged to the 6.4D dissolver did not dissolve in the time predicted by previous laboratory experiments. The extended dissolution time was attributed to fluoride complexation by boron. An extensive research and development (R{ampersand}D) program was initiated to investigate the dissolution chemistry and the physical configuration of the dissolver insert to understand what flowsheet modifications were needed to achieve a viable dissolution process.

Rudisill, T.S.; Karraker, D.G.; Graham, F.R.

1997-12-01T23:59:59.000Z

195

Behavioral and phylogenetic differentiation in a potential cryptic species complex, the canyon treefrog  

Science Journals Connector (OSTI)

Detection of genetic and behavioral diversity within morphologically similar species has led to the discovery of cryptic species complexes. We tested the hypothesis that the canyon treefrog (Hyla arenicolor) may consist of cryptic species by examining mate-attraction signals among highly divergent lineages defined by mitochondrial DNA (mtDNA). Unexpectedly calls exhibited little variation among the three U.S. lineages despite large mtDNA sequence divergences. We re-analyzed intraspecific and interspecific phylogenetic relationships by sequencing both mitochondrial and nuclear genetic markers among populations and a closely related but morphologically and behaviorally different species the Arizona treefrog (H. wrightorum). Discordance between mitochondrial and nuclear datasets suggests multiple instances of introgression of H. wrightorum's mitochondrial genome into populations of H. arenicolor. Furthermore intraspecific population structure based on nuclear markers shows better congruence with patterns of call variation than population structure based on the mitochondrial dataset. Although the U.S. lineages do not appear to represent cryptic species Mexican lineages do show biologically relevant call differences as assessed through female preference tests. Our results suggest that call variation can indicate genetic structure of populations; however a multilocus approach should be used in defining genetic structure as using only mtDNA may lead to erroneous conclusions.

2014-01-01T23:59:59.000Z

196

MOBILIZATION, POISONING, AND FILTRATION OF F-CANYON TANK 804 SLUDGE  

SciTech Connect (OSTI)

The Savannah River Site (SRS) Deactivation and Decommissioning (SDD) Organization is evaluating options to disposition the F-Canyon 800 series underground tanks (including removal of the sludge heels from these tanks) and requested assistance from Savannah River National Laboratory (SRNL) personnel to develop methods to effectively mobilize the sludge from these tanks (i.e., Tanks 804, 808, and 809). Because of the high plutonium content in Tank 804 (estimated to be as much as 1500 g), SDD needs to add a neutron poison to the sludge. They considered manganese and boron as potential poisons. Because of the large amount of manganese needed and the very slow filtration rate of the sludge/manganese slurry, SDD requested that SRNL investigate the impact of using boron rather than manganese as the poison. SRNL performed a series of experiments to help determine the disposal pathway of the material currently located in Tank 804. The objectives of this work are: (1) Determine the mobility of Tank 804 sludge when mixed with 10-15 parts sodium hydroxide as a function of pH between 10 and 14. (2) Determine the solubility of boron in sodium hydroxide solution with a free hydroxide concentration between 1 x 10{sup -4} and 2.0 M. (3) Recommend a filter pore size for SDD such that the filtrate contains no visible solids. (4) Determine whether a precipitate forms when the filtrate pH is adjusted to 12, 7, or 2 with nitric acid.

Poirier, M; Thomas Peters, T; Samuel Fink, S

2006-05-04T23:59:59.000Z

197

EXPLORING FOR SUBTLE MISSION CANYON STRATIGRAPHIC TRAPS WITH ELASTIC WAVEFIELD SEISMIC TECHNOLOGY  

SciTech Connect (OSTI)

A source-receiver geometry was designed for a 9C3D seismic survey in Montrail County, North Dakota, that will involve the largest number of active 3-component stations (1,800 to 2,100) ever attempted in an onshore U.S. multicomponent seismic survey. To achieve the data-acquisition objectives, 3-component geophone strings will be provided by the Bureau of Economic Geology, Dawson Geophysical, and Vecta Technology. Data acquisition will commence in late October 2003. The general objective of this study is to demonstrate the value of multicomponent seismic technology for exploring for subtle oolitic-bank reservoirs in the Mission Canyon Formation of the Williston Basin. The work tasks done during this report period concentrated on developing an optimal design for the seismic survey. This first semiannual report defines the geographical location and geometrical shape of the survey and documents the key acquisition parameters that will be implemented to yield high-fold, high-resolution 9-component seismic data.

John Beecherl

2003-10-01T23:59:59.000Z

198

Long-term surveillance plan for the Bodo Canyon Disposal Site, Durango, Colorado. Revision 1  

SciTech Connect (OSTI)

This long-term surveillance plan (LTSP) for the Uranium Mill Tailings Remedial Act on (UMTRA) Project Bodo Canyon disposal site at Durango, Colorado, describes the surveillance activities for the disposal site. The US Department of Energy (DOE) will carry out these activities to ensure that the disposal call continues to function as designed This LTSP was prepared as a requirement for DOE acceptance under the US Nuclear Regulatory Commission (NRC) general license for custody and long-term care of residual radioactive materials (RRM) from processing uranium ore. This LTSP documents that the land and interests are owned by the United States and details how long-term care of the disposal site will be carried out. It is based on the DOE`s Guidance for Implementing the UMTRA Project Long-term Surveillance Program (DOE, 1992a). Following the introduction, contents of this report include the following: site final condition; site drawings and photographs; permanent site surveillance features; ground water monitoring; annual site inspections; unscheduled inspections; custodial maintenance; corrective action; record keeping and reporting requirements; emergency notification and reporting; quality assurance; personal health and safety; list of contributions; and references.

NONE

1995-11-01T23:59:59.000Z

199

Installation of the Monitoring Site at the Los Alamos Canyon Low-Head Weir  

SciTech Connect (OSTI)

The Cerro Grande fire of 2000 had an enormously adverse impact on and around Los Alamos National Laboratory (LANL). Immediately there were concerns about the potential for enhanced runoff/offsite transport of contaminant-laden sediments because of watershed damage. In response to this concern, the U.S. Army Corps of Engineers installed a low-head weir in Los Alamos Canyon near the White Rock ''Y.'' However, the occurrence of fractured basalt at the surface and ponding of runoff behind the weir enhance the possibility of downward migration of contaminants. Therefore, three boreholes were drilled on the south bank of the channel by LANL to provide a means of monitoring the impact of the Cerro Grande fire and of the weir on water quality beneath the canyon. The boreholes and associated instrumentation are referred to as the Los Alamos Weir Site (LAWS). The three boreholes include a vertical hole and two angled holes (one at approximately 45{sup o} and one at approximately 30{sup o}). Since the basalt is highly fractured, the holes would not stay open. Plans called for inserting flexible liners into all holes. However, using liners in such unstable ground was problematic and, in the angled holes, required deployment through scalloped or perforated polyvinyl chloride (PVC) shield. The vertical hole (LAWS-01), drilled to a total depth of 281.5 ft below ground surface (bgs), was completed as a 278-ft deep monitoring well with four screens: one targeting shallow perched water encountered at 80 ft, two in what may correspond to the upper perched zone at regional groundwater characterization well R-9i (1/4 mi. to the west), and one in what may correspond to the lower perched zone at R-9i. A Water FLUTe{trademark} system deployed in the well isolates the screened intervals; associated transducers and sampling ports permit monitoring head and water quality in the screened intervals. The second hole (LAWS-02), drilled at an angle of 43{sup o} from horizontal, is 156 ft long and bottoms at a depth of 106 ft bgs. The shallow perched water seen at LAWS-01 (at 80 ft) was not encountered. A scalloped PVC shield was installed to keep the hole open while permitting flexible liners to contact the borehole wall. It was initially instrumented with a color-reactive liner to locate water-producing fractures. That was later replaced by an absorbent liner to collect water from the vadose zone. The third hole (LAWS-03), drilled at an angle of 34{sup o} from horizontal, initially had a length of 136 ft and bottomed at a depth of 76 ft bgs. However, the PVC shield rotated during installation such that scallops were at the top and rock debris repeatedly fell in, preventing liner insertion. While pulling the scalloped PVC to replace it with a perforated PVC shield that did not require orientation, the scalloped PVC broke and only 85 ft was recovered. The hole was blocked at that position and could not be drilled out with the equipment available. Thus, LAWS-03 was completed at a length of 85 ft and a depth of 40 ft bgs. An absorbent liner was installed at the outset in preparation for the 2002 summer monsoon season. The entire monitoring site is enclosed inside a locked, 8-ft-high chainlink fence for security. The liners used in the angled boreholes carry electrical wire pairs to detect soil-moisture changes. Surface-water data are provided by stream gages above and below the weir site. Depth of ponding behind the weir is provided by a gage installed just behind the structure.

W.J.Stone; D.L.Newell

2002-08-01T23:59:59.000Z

200

Williams Holding Lease steamflood demonstration project, Cat Canyon Field. Final report  

SciTech Connect (OSTI)

The objective of this pilot program was to evaluate the efficiency and economics of the steam displacement process for future full-scale development of the Cat Canyon S1-B reservoir and in similar heavy crude oil reservoirs. Acivities prior to the initiation of displacement steam injection in April, 1977 included cyclic steam stimulations of the production wells, acquisition of steam generator permits, and the drilling of pilot injection wells. Initial displacement operations were hampered by packer failures and the loss of sand control in the injection wells. Steamflood response occurred over a ten-month period beginning in October, 1977 in four of the nine pilot producers. Subsequent attempts to divert steam to the non-responding producers failed. Poor oil production and high water/oil ratios characterized steamflood performance. Computer thermal simulation studies identified steam channeling, over-injection of steam, and poor quality steam at the sand face as causes of the adverse response. This led to a decision to temporarily suspend steamflood injection from February, 1980 to December, 1981. Improvement in oil production and a decrease in the water/oil ratio resulted during this dewatering period. Displacement injection was resumed in January, 1982 through insulated tubulars and at lower injection rates. Although steamflood response has occurred in three of the nine producers to date, total pilot production has declined steadily since January, 1982. The non-responding producers have been responsible for the majority of this decline. Additionally, the wells that have responded have not met performance expectations. For these reasons, displacement injection was permanently halted on December 15, 1982. Getty Oil Company is presently operating a third generation pilot using knowledge and experience gained from the Williams Holding DOE pilot and a previous pilot. 21 figures, 3 tables.

Bardet, C.K.

1983-07-01T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


201

Auxiliary feedwater system risk-based inspection guide for the Diablo Canyon Unit 1 Nuclear Power Plant  

SciTech Connect (OSTI)

This document presents a compilation of auxiliary feedwater (AFW) system failure information which has been screened for risk significance in terms of failure frequency and degradation of system performance. It is a risk-prioritized listing of failure events and their causes that are significant enough to warrant consideration in inspection planning at Diablo Canyon. This information is presented to provide inspectors with increased resources for inspection planning at Diablo Canyon. The risk importance of various component failure modes was identified by analysis of the results of probabilistic risk assessments (PRAs) for many pressurized water reactors (PWRs). However, the component failure categories identified in PRAs are rather broad, because the failure data used in the PRAs is an aggregate of many individual failures having a variety of root causes. In order to help inspectors to focus on specific aspects of component operation, maintenance and design which might cause these failures, an extensive review of component failure information was performed to identify and rank the root causes of these component failures. Both Diablo Canyon and industry-wide failure information was analyzed. Failure causes were sorted on the basis of frequency of occurrence and seriousness of consequence, and categorized as common cause failures, human errors, design problems, or component failures. This information permits an inspector to concentrate on components important to the prevention of core damage. Other components which perform essential functions, but which are not included because of high reliability or redundancy, must also be addressed to ensure that degradation does not increase their failure probabilities, and hence their risk importances. 23 refs., 1 fig., 1 tab.

Gore, B.F.; Vo, T.V.; Harrison, D.G.

1990-08-01T23:59:59.000Z

202

Big Stick/Four Eyes fields: structural, stratigraphic, and hydrodynamic trapping within Mission Canyon Formation, Williston basin  

SciTech Connect (OSTI)

The Mississippian Mission Canyon formation of the Williston basin is the region's most prolific oil producing horizon. Big Stick/Four Eyes is among the most prolific of the Mission Canyon fields. Primary production from 87 wells is projected to reach 47 million bbl of oil. An additional 10-20 million bbl may be recovered through waterflooding. The complex was discovered in 1977 by the Tenneco 1-29 BN, a wildcat with primary objectives in the Devonian Duperow and Ordovician Red River Formations. A series of Mission Canyon discoveries followed in the Big Stick, Treetop, T-R, and Mystery Creek fields. Early pressure studies showed that these fields were part of an extensive common reservoir covering 44.75 mi/sup 2/ (115.91 km/sup 2/). The reservoir matrix is formed from restricted marine dolostones deposited on a low-relief ramp. Landward are algal-laminated peritidal limestones and saline and supratidal evaporites of a sabkhalike shoreline system. Open-marine limestones, rich in crinoids, brachiopods, and corals, mark the seaward limit of reservoir facies. Regressive deposition placed a blanket of anhydrite over the carbonate sequence providing a seal for the reservoir. Lateral trapping is accomplished through a combination of processes. Upper reservoir zones form belts of porosity that parallel the northeasterly trending shoreline. The trend is cut by the northward plunging Billings anticline, which provides structural closure to the north. Facies changes pinch out porosity to the south and east. Trapping along depositional strike to the southwest is only partially controlled by stratigraphic or structural factors. A gentle tilt of 25 ft per mi (5 m per km) occurs in the oil-water contact to the east-northeast, due to freshwater influx from Mississippian outcrop on the southern and southwestern basin margins.

Breig, J.J.

1988-07-01T23:59:59.000Z

203

Thermal and daylighting evaluation of the effect of varying aspect ratios in urban canyons in Curitiba, Brazil  

Science Journals Connector (OSTI)

Urbanization is commonly associated with densification which may lead to vertical growth or urban consolidation. The present study evaluates the daylighting potential as a function of urban morphology for the city of Curitiba ( 25 2 5 ? 5 0 ? ? S 46 1 6 ? 1 5 ? ? W ). It also presents a thermal analysis for a representative street axis orientation in this location showing indoor conditions within a test office for different aspect ratios. In Curitiba certain street axes were designated to allow densification (in the so-called structural sector of the city). As a consequence there is a great risk of urban canyons being formed as local legislation does not impose height restrictions to adjacent buildings. Daylight analysis was based on software simulations with LUZ DO SOL DLN ECOTECT and RADIANCE. Thermal analysis was carried out by means of computer simulations with the IDA ICEsoftware. It was verified that diagonal axial orientations relative to the north (rotated in 45) provide higher daylighting potentials to buildings located in urban canyons. With regard to the thermal effect of varying the aspect ratio in an east-west street axis results confirm daylighting simulations showing the interrelation between both comfort parameters.

Eduardo Krger; Mauro Suga

2009-01-01T23:59:59.000Z

204

Historical macrobenthic community assemblages in the Avils Canyon, N Iberian Shelf: Baseline biodiversity information for a marine protected area  

Science Journals Connector (OSTI)

Deep-sea ecosystems are highly diverse, and European countries seek to protect these environments by identifying conservation targets. One of these is the Avils Canyon, southern Bay of Biscay, NE Atlantic, Spain. We present the first analysis of historical benthic communities (19871988) of this canyon ecosystem, which is a valuable source of biodiversity baseline information. We found 810 taxa divided in five main macrobenthic assemblages, showing a highly diverse benthic community. Bathymetry was the major structuring agent of benthic community, separating shallow (assemblages I and II, 31 to 307m depth) from deep stations (assemblages III, IV and V, 198 to 1400m depth). Especially diverse was assemblage IV, located at the easternmost part of the continental slope (3781100m depth) where we found reef-forming corals Lophelia pertusa and Madrepora oculata. These and other communities (sea-pens [Order Pennatulacea, Phylum Cnidaria] and burrowing macrofauna) represent key habitats in NE Atlantic continental slopes, which are currently threatened. The present dataset has produced the most comprehensive assessment of diversity in this area to date, focusing on the taxonomic groups which may best reflect the health of the marine ecosystem and supporting previous studies which indicate that the continental slope of the southern Bay of Biscay hosts key benthic habitats.

Maite Louzao; Nuria Anadn; Julio Arrontes; Consuelo lvarez-Claudio; Dulce Mara Fuente; Francisco Ocharan; Araceli Anadn; Jos Luis Acua

2010-01-01T23:59:59.000Z

205

The stratigraphy of selected Mission Canyon wireline log markers, US portion of the Williston basin, North Dakota  

SciTech Connect (OSTI)

The Mission Canyon Formation along the northeast flank of the US Williston basin has been informally subdivided into intervals (members) based on wireline log markers. Wireline log responses of the markers are produced by both lithologic changes and radioactive elements present within these thin stratigraphic intervals. The wireline markers were originally described as transgressive events. Detailed stratigraphic analyses of the Sherwood and State A markers indicate they were deposited during progradation and sea level stillstand. A typical facies tract from east to west within the Sherwood marker contains anhydrites and anhydritic dolomites deposited in sabkha environments; patterned dolomudstones along shoreline trends (the Sherwood argillaceous marker); and limestones in shoaling environments along the Mission Canyon shelf (Sherwood gamma marker). During stillstand, brines produced in sabkha environments (east of the Sherwood shoreline) were enriched in magnesium and potassium. These brines migrated basinward first, dolomitizing mudstones. These brines were magnesium depleted by the time they reached shoals along the shelf. Potassium, however, remained in the system and is present within the marker along the shelf, as shown by a slight increase in API units on Spectrologs.

Hendricks, M.L. (Hendricks and Associates, Inc., Denver, CO (United States))

1991-06-01T23:59:59.000Z

206

Effects of hydropower operations on recreational use and nonuse values at Glen Canyon and Flaming Gorge Dams  

SciTech Connect (OSTI)

Increases in streamflows are generally positively related to the use values of angling and white-water boating, and constant flows tend to increase the use values more than fluctuating flows. In most instances, however, increases in streamflows beyond some threshold level cause the use values to decrease. Expenditures related to angling and white-water boating account for about $24 million of activity in the local economy around Glen Canyon Dam and $24.8 million in the local economy around flaming Gorge Dam. The range of operational scenarios being considered in the Western Area Power Administration`s Electric Power Marketing Environmental Impact Statement, when use rates are held constant, could change the combined use value of angling and white-water boating below Glen Canyon Dam, increasing it by as much as 50%, depending on prevailing hydrological conditions. Changes in the combined use value below Flaming Gorge Dam could range from a decrease of 9% to an increase of 26%. Nonuse values, such as existence and bequest values, could also make a significant contribution to the total value of each site included in this study; however, methodological and data limitations prevented estimating how each operational scenario could change nonuse values.

Carlson, J.L.

1995-03-01T23:59:59.000Z

207

The Role of Convective Outflow in the Waldo Canyon Fire* RICHARD H. JOHNSON, RUSS S. SCHUMACHER, AND JAMES H. RUPPERT JR.  

E-Print Network [OSTI]

The Role of Convective Outflow in the Waldo Canyon Fire* RICHARD H. JOHNSON, RUSS S. SCHUMACHER-00361.s1. Corresponding author address: Richard H. Johnson, Dept. of Atmospheric Science, Colorado State University, 200 West Lake Street, 1371 Campus Delivery, Fort Collins, CO 80523-1371. E-mail: johnson

Johnson, Richard H.

208

Upper Plio-Pleistocene salt tectonics and seismic stratigraphy on the lower continental slope, Mississippi Canyon OCS Area, Gulf of Mexico  

E-Print Network [OSTI]

of sequence E, which represents the late Wisconsinan glacial. Salt generally occurs as tongues or sheets, and forms continuous masses in the basinward part of the canyon at water depths of about 1300 m (4300 ft). Areas without salt are near the "spur...

Liu, Jia-Yuh

2012-06-07T23:59:59.000Z

209

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM  

SciTech Connect (OSTI)

The Nash Draw Brushy Canyon Pool in Eddy County New Mexico was a cost-shared field demonstration project in the U.S. Department of Energy Class III Program. A major goal of the Class III Program was to stimulate the use of advanced technologies to increase ultimate recovery from slope-basin clastic reservoirs. Advanced characterization techniques were used at the Nash Draw Pool (NDP) project to develop reservoir management strategies for optimizing oil recovery from this Delaware reservoir. The objective of the project was to demonstrate that a development program, which was based on advanced reservoir management methods, could significantly improve oil recovery at the NDP. Initial goals were (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to other oil and gas producers. Analysis, interpretation, and integration of recently acquired geological, geophysical, and engineering data revealed that the initial reservoir characterization was too simplistic to capture the critical features of this complex formation. Contrary to the initial characterization, a new reservoir description evolved that provided sufficient detail regarding the complexity of the Brushy Canyon interval at Nash Draw. This new reservoir description was used as a risk reduction tool to identify 'sweet spots' for a development drilling program as well as to evaluate pressure maintenance strategies. The reservoir characterization, geological modeling, 3-D seismic interpretation, and simulation studies have provided a detailed model of the Brushy Canyon zones. This model was used to predict the success of different reservoir management scenarios and to aid in determining the most favorable combination of targeted drilling, pressure maintenance, well stimulation, and well spacing to improve recovery from this reservoir. An Advanced Log Analysis technique developed from the NDP project has proven useful in defining additional productive zones and refining completion techniques. This program proved to be especially helpful in locating and evaluating potential recompletion intervals, which has resulted in low development costs with only small incremental increases in lifting costs. To develop additional reserves at lower costs, zones behind pipe in existing wells were evaluated using techniques developed for the Brushy Canyon interval. These techniques were used to complete uphole zones in thirteen of the NDP wells. A total of 14 recompletions were done: four during 1999, four during 2000, two during 2001, and four during 2002-2003. These workovers added reserves of 332,304 barrels of oil (BO) and 640,363 MCFG (thousand cubic feet of gas) at an overall weighted average development cost of $1.87 per BOE (barrel of oil equivalent). A pressure maintenance pilot project in a developed area of the field was not conducted because the pilot area was pressure depleted, and the reservoir in that area was found to be compartmentalized and discontinuous. Economic analyses and simulation studies indicated that immiscible injection of lean hydrocarbon gas for pressure maintenance was not warranted at the NDP and would need to be considered for implementation in similar fields very soon after production has started. Simulation studies suggested that the injection of miscible carbon dioxide (CO{sub 2}) could recover significant quantities of oil at the NDP, but a source of low-cost CO{sub 2} was not available in the area. Results from the project indicated that further development will be under playa lakes and potash areas that were beyond the regions covered by well control and are not accessible with vertical wells. These areas, covered by 3-D seismic surveys that were obtained as part of the project, were accessed with combinations of deviated/horizontal wells. Three directional/horizontal wells have been drilled and completed to develop reserves under surface-restricted areas and potash mines. The third

Mark B. Murphy

2005-09-30T23:59:59.000Z

210

Demonstration of shield-type longwall supports at York Canyon Mine of Kaiser Steel Corporation. Final technical report A  

SciTech Connect (OSTI)

This report represents work on a program that was originated by the USBM of the Department of the Interior and was transferred to the Department of Energy on October 1, 1977. A demonstration with the Government funded Hemscheidt 320 HSL caliper type shield supports was conducted at three longwall panels of Kaiser Steel Corporation's York Canyon Mine. The purpose of this longwall demonstration was to provide the US coal industry with information on all aspects of shield longwall mining in high seams. The demonstration provided a working model for the coal industry and during the project, 350 people from the industry, schools, and government agencies visited the demonstration. They were provided with a first hand knowledge of a working shield longwall. The demonstration showed that the control of large coal lumps may be a problem in the mining of coal seam thicker than 8 feet. Mining with shield type supports provided good working conditions and a safe working environment. The shield requires very little maintenance and has a high mechanical availability.

Lawrence, R.G.; King, R.

1980-04-01T23:59:59.000Z

211

La Jolla Canyon and Scripps Canyon Bibliography  

E-Print Network [OSTI]

Henry, M.J. (1976). The unconsolidated sediment distributionfan valley cut into unconsolidated sediment is encountered.water saturated and unconsolidated) surficial deposits on

Brueggeman, Peter

2009-01-01T23:59:59.000Z

212

Stratigraphic and structural configuration of the Navajo (Jurassic) through Ouray (Mississippian-Devonian) formations in the vicinity of Davis and Lavender Canyons, southeastern Utah  

SciTech Connect (OSTI)

This study developed a three-dimensional computer model of stratigraphic and structural relationships within a 3497-km/sup 2/ (1350-mi/sup 2/) study area centered on the proposed site for a high-level nuclear waste repository in southeastern Utah. The model consists of a sequence of internally reconciled isopach and structure contour maps horizontally registered and stored in stratigraphic order. This model can be used to display cross sections, perspective block diagrams, or fence diagrams at any orientation; estimate depth of formation contacts and thicknesses for any new stratigraphic or hydrologic boreholes; facilitate ground-water modeling studies; and evaluate the structural and stratigraphic evolution of the study area. This study also includes limited evaluations of aquifer continuity in the Elephant Canyon and Honaker Trail Formations, and of salt dissolution and flowage features as interpreted from geophysical logs. The study identified a long history of movement in the fault system in the north-central part of the study area and a major salt flowage feature in the northeastern part. It describes the Elephant Canyon Formation aquifer as laterally limited, the Honaker Trail Formation aquifer as fairly continuous over the area, and Beef Basin in the southern part of the area as a probable dissolution feature. It also concludes that the Shay-Bridger Jack-Salt Creek Graben system is apparently a vertically continuous feature between the basement and ground surface. No stratigraphic or structural discontinuities were detected in the vicinity of Davis Canyon that appear to be detrimental to the siting of a waste repository.

McCleary, J.R.; Romie, J.E.

1986-04-01T23:59:59.000Z

213

Generating Economic Development from a Wind Power Plant in Spanish Fork Canyon, Utah: A Case Study and Analysis of State-Level Economic Impacts  

Wind Powering America (EERE)

Generating Economic Development from a Wind Power Generating Economic Development from a Wind Power Project in Spanish Fork Canyon, Utah: A Case Study and Analysis of State-Level Economic Impacts Sandra Reategui Edwin R. Stafford, Ph.D. Cathy L. Hartman, Ph.D. Center for the Market Diffusion of Renewable Energy and Clean Technology Jon M. Huntsman School of Business Utah State University 3560 Old Main Hill Logan, Utah 84322-3560 January 2009 DOE/GO-102009-2760 Acknowledgements ....................................................................................................................... 1 Introduction ................................................................................................................................... 2 Report Overview ......................................................................................................................... 2

214

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico, Class III  

SciTech Connect (OSTI)

The Nash Draw Brushy Canyon Pool (NDP) is southeast New Mexico is one of the nine projects selected in 1995 by the U.S. Department of Energy (DOE) for participation in the Class III Reservoir Field Demonstration Program. The goals of the DOE cost-shared Class Program are to: (1) extend economic production, (2) increase ultimate recovery, and (3) broaden information exchange and technology application. Reservoirs in the Class III Program are focused on slope-basin and deep-basin clastic depositional types.

Murphy, Mark B.

2000-10-25T23:59:59.000Z

215

Stratigraphic and diagenetic controls on the occurrence of porosity in the Mississippian Mission Canyon Formation in the Billings Nose Area, North Dakota  

E-Print Network [OSTI]

). The south-plunging OOOO SASKATCHEWAN MONTANA POPLAR -4000 0 0 0 CEDAR CREEK ANTICLINE CQ i(r NESSON ~ ANTICLINE 0 A I. 'v, ??. . . qO 0 "'OS J PRYGURG 0 0 I MANITOBA NORTH DAKOTA Y I EDGE OF M I SS ION CANYON I I I I NORTH... in the Williston Basin in 1936 on the Cedar Creek anticline in Montana (Gerhard et al, 1982a). The discovery was uneconomical and was not developed. Despite this poor start, the Williston Basin has become a major producer of oil and gas on the North American...

Beaber, Daniel Edward

1989-01-01T23:59:59.000Z

216

Crime Alert: Theft of Cell Phone near Campus On November 8th, at about 4:00 pm, a student was walking on Blaine St, near Canyon Crest Drive  

E-Print Network [OSTI]

Crime Alert: Theft of Cell Phone near Campus On November 8th, at about 4:00 pm, a student was walking on Blaine St, near Canyon Crest Drive listening to his iPhone on a pair of headphones. A subject approached him, asked to use his iPhone and when the victim refused, the suspect grabbed the phone and ran

217

The Grand (Canyon) Experiment  

Science Journals Connector (OSTI)

...was bad. Water was viewed as a...power at the peak consumption times. Today, the...billion cubic meters of water must pass through...during the day and reduce that flow to as little...few years, just to make up for the erosion that occurs...Sediments Rivers Snails Water Movements georef...

Elizabeth Pennisi

2004-12-10T23:59:59.000Z

218

Boulder Canyon Project  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

November 2015 * All work is contingent on outage availability Hoover Instrument Transformer Replacement * 6 out the 12 have been replaced * 3 of the remaining will be done in...

219

Environmental Assessment and Finding of No Significant Impact: Curecanti-Lost Canyon 230-kV Transmission Line Reroute Project, Montrose County, Colorado  

SciTech Connect (OSTI)

The Department of Energy (DOE), Western Area Power Administration (Western) is proposing to reroute a section of the Curecanti-Lost Canyon 230-kilovolt (kV) transmission line, in Montrose County, Colorado. A portion of the transmission line, situated 11 miles southeast of Montrose, Colorado, crosses Waterdog Peak, an area of significant geologic surface activity, which is causing the transmission line's lattice steel towers to shift. This increases stress to structure hardware and conductors, and poses a threat to the integrity of the transmission system. Western proposes to relocate the lattice steel towers and line to a more geologically stable area. The existing section of transmission line and the proposed relocation route cross Bureau of Land Management and private land holdings.

N /A

2000-03-20T23:59:59.000Z

220

Southwestern Regional Partnership For Carbon Sequestration (Phase 2) Pump Canyon CO2- ECBM/Sequestration Demonstration, San Juan Basin, New Mexico  

SciTech Connect (OSTI)

Within the Southwest Regional Partnership on Carbon Sequestration (SWP), three demonstrations of geologic CO{sub 2} sequestration are being performed -- one in an oilfield (the SACROC Unit in the Permian basin of west Texas), one in a deep, unmineable coalbed (the Pump Canyon site in the San Juan basin of northern New Mexico), and one in a deep, saline reservoir (underlying the Aneth oilfield in the Paradox basin of southeast Utah). The Pump Canyon CO{sub 2}-enhanced coalbed methane (CO{sub 2}/ECBM) sequestration demonstration project plans to demonstrate the effectiveness of CO{sub 2} sequestration in deep, unmineable coal seams via a small-scale geologic sequestration project. The site is located in San Juan County, northern New Mexico, just within the limits of the high-permeability fairway of prolific coalbed methane production. The study area for the SWP project consists of 31 coalbed methane production wells located in a nine section area. CO{sub 2} was injected continuously for a year and different monitoring, verification and accounting (MVA) techniques were implemented to track the CO{sub 2} movement inside and outside the reservoir. Some of the MVA methods include continuous measurement of injection volumes, pressures and temperatures within the injection well, coalbed methane production rates, pressures and gas compositions collected at the offset production wells, and tracers in the injected CO{sub 2}. In addition, time-lapse vertical seismic profiling (VSP), surface tiltmeter arrays, a series of shallow monitoring wells with a regular fluid sampling program, surface measurements of soil composition, CO{sub 2} fluxes, and tracers were used to help in tracking the injected CO{sub 2}. Finally, a detailed reservoir model was constructed to help reproduce and understand the behavior of the reservoir under production and injection operation. This report summarizes the different phases of the project, from permitting through site closure, and gives the results of the different MVA techniques.

Advanced Resources International

2010-01-31T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


221

Post-1935 changes in forest vegetation of Grand Canyon National Park, Arizona, USA: Part 2Mixed conifer, spruce-fir, and quaking aspen forests  

Science Journals Connector (OSTI)

This study examined changes in never-harvested mixed conifer (MCF), spruce-fir (SFF), and quaking aspen forests (QAF) in Grand Canyon National Park (GCNP), Arizona, USA based on repeat sampling of two sets of vegetation study plots, one originally sampled in 1935 and the other in 1984. The 1935 plots are the earliest-known, sample-intensive, quantitative documentation of forest vegetation over a Southwest USA landscape. Findings documented that previously described increases in densities and basal areas attributed to fire exclusion were followed by decreases in 19352004 and 19842005. Decreases in MCF were attributable primarily to quaking aspen (Populus tremuloides) and white fir (Abies concolor), but there were differences between dry-mesic and moist-mesic MCF subtypes. Decreases in SFF were attributable to quaking aspen, spruce (Picea engelmannii+Picea pungens), and subalpine fir (Abies lasiocarpa). Decreases in QAF resulted from the loss of quaking aspen during succession. Changes in ponderosa pine forest (PPF) are described in a parallel paper (Vankat, J.L., 2011. Post-1935 changes in forest vegetation of Grand Canyon National Park, Arizona, USA: part 1 ponderosa pine forest. Forest Ecology and Management 261, 309325). Graphical synthesis of historical and modern MCF data sets for GCNP indicated tree densities and basal areas increased from the late 19th to the mid 20th century and then decreased to the 21st century. Changes began earlier, occurred more rapidly, and/or were larger at higher elevation. Plot data showed that basal area decreased earlier and/or more rapidly than density and that decreases from 1935 to 2004 resulted in convergence among MCF, SFF, and PPF. If GCNP coniferous forests are trending toward conditions present before fire exclusion, this implies density and basal area were more similar among these forests in the late 19th century than in 1935. Changes in MCF and SFF can be placed in a general framework of forest accretion, inflection, and recession in which increases in tree density and basal area are followed by an inflection point and decreases. Accretion was triggered by the exogenous factor of fire exclusion, and inflection and recession apparently were driven by the endogenous factor of density-dependent mortality combined with exogenous factors such as climate. Although the decreases in density and basal area could be unique to GCNP, it is likely that the historical study plots provided a unique opportunity to quantitatively determine forest trends since 1935. This documentation of post-1935 decreases in MCF and SFF densities and basal areas indicates a shift in perspective on Southwestern forests is needed.

John L. Vankat

2011-01-01T23:59:59.000Z

222

CORROSION OF ALUMINUM CLAD SPENT NUCLEAR FUEL IN THE 70 TON CASK DURING TRANSFER FROM L AREA TO H-CANYON  

SciTech Connect (OSTI)

Aluminum-clad spent nuclear fuel will be transported for processing in the 70-ton nuclear fuel element cask from L Basin to H-canyon. During transport these fuels would be expected to experience high temperature aqueous corrosion from the residual L Basin water that will be present in the cask. Cladding corrosion losses during transport were calculated for material test reactor (MTR) and high flux isotope reactors (HFIR) fuels using literature and site information on aqueous corrosion at a range of time/temperature conditions. Calculations of the cladding corrosion loss were based on Arrhenius relationships developed for aluminum alloys typical of cladding material with the primary assumption that an adherent passive film does not form to retard the initial corrosion rate. For MTR fuels a cladding thickness loss of 33 % was found after 1 year in the cask with a maximum temperature of 260 {degrees}C. HFIR fuels showed a thickness loss of only 6% after 1 year at a maximum temperature of 180 {degrees}C. These losses are not expected to impact the overall confinement function of the aluminum cladding.

Mickalonis, J.

2014-06-01T23:59:59.000Z

223

Tracing dust provenance, cycling, and history in the Wasatch Mountains using strontium isotopes and tree rings.  

E-Print Network [OSTI]

??To further our understanding of dust cycling from the Great Basin to the Rocky Mountains, this study uses strontium concentrations and isotopes (87Sr/86Sr) to investigate (more)

Miller, Olivia Leigh

2013-01-01T23:59:59.000Z

224

Spatial patch patterns and altered forest structure in middle elevation versus upper ecotonal mixed-conifer forests, Grand Canyon National Park, Arizona, USA  

Science Journals Connector (OSTI)

In the American Southwest, mixed-conifer forest experienced altered disturbance regimes with the exclusion of fire since the early 1900s. This research analyzes patch development and tree spatial patterns in the middle versus upper mixed-conifer forests at Grand Canyon National Park in Arizona (USA). The methods used include: (1) sizestructure analyses, to compare species patch development; (2) dendrochronological dating of tree establishment and fire history; (3) tree ring master chronology, to determine periods of suppressed growth, compared to a palmer drought severity index; (4) spatial analyses by size and age, with univariate and bivariate analyses of spatial association as well as spatial autocorrelation. Results show that unlike the lower ecotone of the mixed-conifer zone, both the middle elevation and upper ecotone were mixed-conifer forests before Euro-American settlement. At the upper ecotone, two decades (1870s and 1880s) had no successful conifer establishment but instead aspen cohorts, corresponding to the fire history of synchronized fires. Overall, the upper ecotone has shifted in composition in the absence of surface fires from mixed conifer to encroachment of subalpine species, particularly Engelmann spruce. Spatial patterns of tree sizes and tree ages imply development of a size hierarchy in an aging patch. In addition, shifts in species composition from ponderosa pine and white fir overstory to Engelmann spruce and Douglas-fir understory affected within-patch spatial patterns. These results provide quantitative evidence of past and present forest conditions for the development of restoration strategies for Southwestern mixed-conifer forests.

Joy Nystrom Mast; Joy J. Wolf

2006-01-01T23:59:59.000Z

225

Evaluate Potential Means of Rebuilding Sturgeon Populations in the Snake River between Lower Granite and Hells Canyon Dams, 1997 Annual Report.  

SciTech Connect (OSTI)

During 1997 the first phase of the Nez Perce Tribe White Sturgeon Project was completed and the second phase was initiated. During Phase I the ''Upper Snake River White Sturgeon Biological Assessment'' was completed, successfully: (1) compiling regional white sturgeon management objectives, and (2) identifying potential mitigation actions needed to rebuild the white sturgeon population in the Snake River between Hells Canyon and Lower Granite dams. Risks and uncertainties associated with implementation of these potential mitigative actions could not be fully assessed because critical information concerning the status of the population and their habitat requirements were unknown. The biological risk assessment identified the fundamental information concerning the white sturgeon population that is needed to fully evaluate the effectiveness of alternative mitigative strategies. Accordingly, a multi-year research plan was developed to collect specific biological and environmental data needed to assess the health and status of the population and characterize habitat used for spawning and rearing. In addition, in 1997 Phase II of the project was initiated. White sturgeon were captured, marked, and population data were collected between Lower Granite Dam and the mouth of the Salmon River. During 1997, 316 white sturgeon were captured in the Snake River. Of these, 298 were marked. Differences in the fork length frequency distributions of the white sturgeon were not affected by collection method. No significant differences in length frequency distributions of sturgeon captured in Lower Granite Reservoir and the mid- and upper free-flowing reaches of the Snake River were detected. The length frequency distribution indicated that white sturgeon between 92 and 183 cm are prevalent in the reaches of the Snake River that were sampled. However, white sturgeon >183 have not changed markedly since 1970. I would speculate that some factor other than past over-fishing practices is limiting the recruitment of white sturgeon into larger size classes (>183 cm). Habitat, food resources, and migration have been severely altered by the impoundment of the Snake River and it appears that the recruitment of young may not be severely affected as recruitment of fish into size classes > 183 cm.

Hoefs, Nancy (Nez Perce Tribe, Department of Fisheries Resource Management, Lapwai, ID)

2004-02-01T23:59:59.000Z

226

White Sturgeon Management Plan in the Snake River between Lower Granite and Hells Canyon Dams; Nez Perce Tribe, 1997-2005 Final Report.  

SciTech Connect (OSTI)

White sturgeon in the Hells Canyon reach (HCR) of the Snake River are of cultural importance to the Nez Perce Tribe. However, subsistence and ceremonial fishing opportunities have been severely limited as a result of low numbers of white sturgeon in the HCR. Hydrosystem development in the Columbia River Basin has depressed numbers and productivity of white sturgeon in the HCR by isolating fish in impounded reaches of the basin, restricting access to optimal rearing habitats, reducing the anadromous forage base, and modifying early life-history habitats. Consequently, a proactive management plan is needed to mitigate for the loss of white sturgeon production in the HCR, and to identify and implement feasible measures that will restore and rebuild the white sturgeon population to a level that sustains viability and can support an annual harvest. This comprehensive and adaptive management plan describes the goals, objectives, strategies, actions, and expected evaluative timeframes for restoring the white sturgeon population in the HCR. The goal of this plan, which is to maintain a viable, persistent population that can support a sustainable fishery, is supported by the following objectives: (1) a natural, stable age structure comprising both juveniles and a broad spectrum of spawning age-classes; (2) stable or increasing numbers of both juveniles and adults; (3) consistent levels of average recruitment to ensure future contribution to reproductive potential; (4) stable genetic diversity comparable to current levels; (5) a minimum level of abundance of 2,500 adults to minimize extinction risk; and (6) provision of an annual sustainable harvest of 5 kg/ha. To achieve management objectives, potential mitigative actions were developed by a Biological Risk Assessment Team (BRAT). Identified strategies and actions included enhancing growth and survival rates by restoring anadromous fish runs and increasing passage opportunities for white sturgeon, reducing mortality rates of early life stages by modifying flows in the HCR, reducing mortality imposed by the catch and release fishery, augmenting natural production through translocation or hatchery releases, and assessing detrimental effects of contaminants on reproductive potential. These proposed actions were evaluated by assessing their relative potential to affect population growth rate and by determining the feasibility of their execution, including a realistic timeframe (short-term, mid-term, long-term) for their implementation and evaluation. A multi-pronged approach for management was decided upon whereby various actions will be implemented and evaluated under different timeframes. Priority management actions include: Action I- Produce juvenile white sturgeon in a hatchery and release into the management area; Action G- Collect juvenile white sturgeon from other populations in the Snake or Columbia rivers and release them into the management area; and Action D- Restore white sturgeon passage upriver and downriver at Lower Snake and Idaho Power dams. An integral part of this approach is the continual monitoring of performance measures to assess the progressive response of the population to implemented actions, to evaluate the actions efficacy toward achieving objectives, and to refine and redirect strategies if warranted.

Nez Perce Tribe Resources Management Staff, (Nez Perce Tribe, Department of Fisheries Resource Management, Lapwai, ID)

2005-09-01T23:59:59.000Z

227

First-time remote sensing of NO2 vertical distributions in an urban street canyon using Topographic Target Light scattering Differential Optical Absorption Spectroscopy (ToTaL-DOAS)  

Science Journals Connector (OSTI)

Topographic Target Light scattering Differential Optical Absorption Spectroscopy (ToTaL-DOAS) measurements were performed in a street canyon in Gwangju, Korea (3510?51.43?N, 12652?53.74?E) during a period of 10 days in October 2010. NO2 slant volume mixing ratios (VMRs) at the lowest elevation angle (EL) of 1, as obtained from ToTaL-DOAS measurements, were validated via comparisons with collocated in situ ground data, showing good agreement within a scatter range of 20% during the entire measurement period, and within a scatter range of 15% when cloudy days were excluded. For the first time, based on inversion calculations using ToTaL-DOAS data, we retrieved NO2 vertical distributions that consist of five layers (from 6 to 118m) for three measurement days. We obtained generally decreasing NO2 \\{VMRs\\} with altitude, whereas increased NO2 \\{VMRs\\} at two elevated layers (619m and 1933m) were observed on 26 and 27 October. We obtained a coefficient of determination (R2) of 0.87 (0.61) between slant \\{VMRs\\} at 1 EL (retrieved NO2 \\{VMRs\\} in the layer from 6m to 19m) and in situ data, with the scatter of the correlation being within the 15% (10%) range. The relation between retrieved NO2 \\{VMRs\\} at 619m and slant \\{VMRs\\} at 1 EL yielded an R2 value of 0.97, with the scatter of the correlation being within the 5% range. The results demonstrate that the ToTaL-DOAS technique is a useful tool in identifying the temporal and vertical characteristics of NO2 \\{VMRs\\} in an urban street canyon with a complex geometry.

Hanlim Lee; Myojeong Gu; Young J. Kim; Jungbae Hwang; Ukkyo Jung

2012-01-01T23:59:59.000Z

228

Anisotropic models to account for large borehole washouts to estimate gas hydrate saturations in the Gulf of Mexico Gas Hydrate Joint Industry Project Leg II Alaminos Canyon 21B well  

Science Journals Connector (OSTI)

Through the use of 3-D seismic amplitude mapping, several gas hydrate prospects were identified in the Alaminos Canyon (AC) area of the Gulf of Mexico. Two locations were drilled as part of the Gulf of Mexico Gas Hydrate Joint Industry Project Leg II (JIP Leg II) in May of 2009 and a comprehensive set of logging-while-drilling (LWD) logs were acquired at each well site. LWD logs indicated that resistivity in the range of ?2ohm-m and P-wave velocity in the range of ?1.9km/s were measured in the target sand interval between 515 and 645 feet below sea floor. These values were slightly elevated relative to those measured in the sediment above and below the target sand. However, the initial well log analysis was inconclusive regarding the presence of gas hydrate in the logged sand interval, mainly because large washouts caused by drilling in the target interval degraded confidence in the well log measurements. To assess gas hydrate saturations in the sedimentary section drilled in the Alaminos Canyon 21 B (AC21-B) well, a method of compensating for the effect of washouts on the resistivity and acoustic velocities was developed. The proposed method models the washed-out portion of the borehole as a vertical layer filled with sea water (drilling fluid) and the apparent anisotropic resistivity and velocities caused by a vertical layer are used to correct the measured log values. By incorporating the conventional marine seismic data into the well log analysis, the average gas hydrate saturation in the target sand section in the AC21-B well can be constrained to the range of 828%, with 20% being our best estimate.

M.W. Lee; T.S. Collett; K.A. Lewis

2012-01-01T23:59:59.000Z

229

Mio-Pliocene erosional exhumation of the central Colorado Plateau, eastern Utah: New insights from apatite (U-Th)/He thermochronometry  

E-Print Network [OSTI]

majority of the cores collected are from the Book Cliffs, especially the eastern Book Cliffs near Hay Canyon, an intensely explored region with many old oil exploration wells. Cores from wells GC-1 (GC-1), 2 Book Cliffs (2BC-), 3 Book Cliffs (3BC-), 4... the Mesaverde Group and the Wasatch Formation were collected from 2BC and GC-1, which had 200?300 m of core available. Wells 3BC and 4BC had less than 100 m of core to sample, so only 1?3 very fine-grained Mesaverde sandstone samples were collected from each...

Hoffman, Markella

2009-08-20T23:59:59.000Z

230

O F F I C E O F A D M I S S I O N S 2 0 1 S . 1 4 6 0 E . R M . 2 5 0 S S A L T L A K E C I T Y , U T 8 4 1 1 2 8 0 1 -5 8 1 -7 2 8 1 w w w . a d m i s s i o n s . u t a h . e d u a d m i s s i o n s @ u t a h . e d u f a c e b o o k . c o m / U t a  

E-Print Network [OSTI]

; Wasatch Drive is two lights past 1300 East) · At Wasatch Drive turn left (north) · Continue on Wasatch Drive, past one stoplight and the Legacy Bridge · Hugging the right side of the street as it forks, take South; Wasatch Drive is two lights past 1300 South) · At Wasatch Drive turn left (north) · Continue

Tipple, Brett

231

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico. Annual report, September 25, 1995--September 24, 1996  

SciTech Connect (OSTI)

The basic driver for this project is the low recovery observed in Delaware reservoirs, such as the Nash Draw Pool (NDP). This low recovery is caused by low reservoir energy, less than optimum permeabilities and porosities, and inadequate reservoir characterization and reservoir management strategies which are typical of projects operated by independent producers. Rapid oil decline rates and high gas/oil ratios are typically observed in the first year of primary production. Based on the production characteristics that have been observed in similar Delaware fields, pressure maintenance is a likely requirement at the Nash Pool. Three basic constraints to producing the Nash Draw Brushy Canyon Reservoir are: (1) limited areal and interwell geologic knowledge, (2) lack of an engineering tool to evaluate the various producing strategies, and (3) limited surface access prohibiting development with conventional drilling. The limited surface access is caused by the proximity of underground potash mining and surface playa lakes. The objectives of this project are: (1) to demonstrate that a development drilling program and pressure maintenance program, based on advanced reservoir management methods, can significantly improve oil recovery compared with existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers, especially in the Permian Basin.

Murphy, M.B.

1997-08-01T23:59:59.000Z

232

Canyon, Texas: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

9803342°, -101.9188024° 9803342°, -101.9188024° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.9803342,"lon":-101.9188024,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

233

Klondike III / Biglow Canyon Wind Integration Project  

Broader source: Energy.gov (indexed) [DOE]

Cumulative Impacts Analysis For Avian Cumulative Impacts Analysis For Avian Resources From Proposed Wind Projects In Sherman County, Washington CUMULATIVE IMPACTS ANALYSIS FOR AVIAN RESOURCES FROM PROPOSED WIND PROJECTS IN SHERMAN COUNTY, WASHINGTON FINAL REPORT March 2006 Prepared For: Bonneville Power Administration 905 NE 11th Avenue Portland, Oregon, 97232 Prepared By: David Young, Kimberly Bay, & Victoria Poulton Western EcoSystems Technology, Inc. 2003 Central Avenue Cheyenne, Wyoming 82001 CUMULATIVE IMPACTS ANALYSIS, PROPOSED WIND PROJECTS, SHERMAN COUNTY, WASHINGTON March 2006 WEST, Inc. i TABLE OF CONTENTS 1.0 INTRODUCTION AND BACKGROUND ............................................................................. 1 2.0 METHODS ...............................................................................................................................

234

Mission Canyon, California: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

4508303°, -119.7129141° 4508303°, -119.7129141° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.4508303,"lon":-119.7129141,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

235

Grand Canyon Village, Arizona: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

463718°, -112.1540586° 463718°, -112.1540586° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":36.0463718,"lon":-112.1540586,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

236

Canyon County, Idaho: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

6779581°, -116.6865435° 6779581°, -116.6865435° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":43.6779581,"lon":-116.6865435,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

237

Geology of the Florida Canyon gold deposit, Pershing County,...  

Open Energy Info (EERE)

Nevada, in: Gold and Silver Deposits of Western Nevada Authors Hastings, J.S., Burkhart, T.H., and Richardson and R.E. Published Geological Society of Nevada 1993 fall field trip...

238

DOE - Office of Legacy Management -- Burro Canyon Disposal Cell...  

Office of Legacy Management (LM)

materials from the Slick RockOld North Continent site and the Slick RockUnion Carbide site were disposed of in this dedicated disposal cell. The Department of Energys...

239

Overview of ''Red Oil'' Frequency Analyses for F-Canyon  

SciTech Connect (OSTI)

A very small potential exists in the Savannah River Site (SRS) separations operations for an uncontrolled reaction between tri-n-butyl phosphate (TBP) and nitric acid that could result in unacceptable damage to separations facilities and a significant release of radioactive materials. The recent ''red oil'' (TBP and nitric acid) accident in Tomsk, Russia, resulted in considerable damage and radioactive release. Explosions have also occurred at SRS during the early years of operations. While the SRS separations facilities have operated without incident for many years, it is prudent to revisit the SRS defense-in-depth approach to preventing such an accident and to upgrade preventive procedures and hardware as appropriate.

Lux, C.R.

2000-07-19T23:59:59.000Z

240

Mississippi Canyon 252 Incident NRDA Tier 1 for Deepwater Communities  

E-Print Network [OSTI]

, and are visible on Google Earth. With 3D seismic data obtained by the oil and gas industry for geophysical invertebrates, and very small abundant planktivorous fishes in the mesophotic habitats. Oil fouling and death

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


241

White Creek and Nine Canyon wind farms Fact Sheet  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

(MW) of wind storage and shaping service to help integrate power from the proposed White Creek Wind Project in Klickitat Co., Wash., into the Northwest power system. BPA also...

242

The kinematics of debris flow transport down a canyon  

E-Print Network [OSTI]

of the channel colluvium and maximize the effects of the debris-induced stresses. First, the slope of the channel must fall within critical limits. As Campbell (1975) generalizes, slopes of less than about 15' are relatively stable, and slopes of more than 45... be divided into normal (o) and shear (s) components. (b) When loaded with debris. shear stress increases accordingly, and effective normal stress (o') remains the same as pore pressure (u) increases. 30 rained 20 ndrained (kPa) 10 0 0 10 20 30 40 50...

Santi, Paul M.

2012-06-07T23:59:59.000Z

243

Geology of the Big Brushy canyon area, Brewster County, Texas  

E-Print Network [OSTI]

e p. Pe 1eoypoda Ezo~grro olartpi { Stattuoh) Homoagra SuuEzensis (Uhitney) Ostrea spn ~an ~nne en e (88 7880'ill sp n %Flneoe p. Gastropoda Turritella sp, ~os%orna sp, Cspbakepoda . =Rugaiosras mssioanum:$8ose... e p. Pe 1eoypoda Ezo~grro olartpi { Stattuoh) Homoagra SuuEzensis (Uhitney) Ostrea spn ~an ~nne en e (88 7880'ill sp n %Flneoe p. Gastropoda Turritella sp, ~os%orna sp, Cspbakepoda . =Rugaiosras mssioanum:$8ose...

Howle, Arlen Guy

2012-06-07T23:59:59.000Z

244

The Copper Creek Clovis Point from Hells Canyon, Northeastern Oregon  

E-Print Network [OSTI]

No. 1 (2008) | pp. 75-84 The Copper Creek Clovis Point fromside of the Snake River to the Copper Creek point discovery1 (2008) 5 cm Figure 4. The Copper Creek Clovis point (tick

Reid, Kenneth C.; Root, Matthew J.; Hughes, Richard E.

2008-01-01T23:59:59.000Z

245

Paleofluvial Mega-Canyon Beneath the Central Greenland Ice Sheet  

Science Journals Connector (OSTI)

...m km ?1 , which is similar to the southern 500 km of the Colorado River and around three times larger than the average for the Mississippi...Fowler A. C. Clark C. D. Hulton N. R. J. , Subglacial floods beneath ice sheets . Phil. Trans. R. Soc. A 364 , 1769...

Jonathan L. Bamber; Martin J. Siegert; Jennifer A. Griggs; Shawn J. Marshall; Giorgio Spada

2013-08-30T23:59:59.000Z

246

EIS-0374: Klondike III/ Bigelow Canyon Wind Integration Project, OR  

Broader source: Energy.gov [DOE]

This EIS analyzes BPA's decision to approve an interconnection requested by PPM Energy, Inc. (PPM) to integrate electrical power from their proposed Klondike III Wind roject (Wind Project) into the Federal Columbia River Transmission System (FCRTS).

247

Reclaiming Altered Landscapes: The Bingham Canyon Mine Memorial.  

E-Print Network [OSTI]

??Open-Pit mining in America has created landscape alterations that are vast and permanent. These landscapes have created and erased entire communities in order to extract (more)

Haddadin, Dafer S.

2013-01-01T23:59:59.000Z

248

Black Canyon City, Arizona: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

City, Arizona: Energy Resources City, Arizona: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 34.0708665°, -112.1507149° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":34.0708665,"lon":-112.1507149,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

249

Sampling and Analysis Plan for PUREX canyon vessel flushing  

SciTech Connect (OSTI)

A sampling and analysis plan is necessary to provide direction for the sampling and analytical activities determined by the data quality objectives. This document defines the sampling and analysis necessary to support the deactivation of the Plutonium-Uranium Extraction (PUREX) facility vessels that are regulated pursuant to Washington Administrative Code 173-303.

Villalobos, C.N.

1995-03-01T23:59:59.000Z

250

Authigenic clay minerals in sandstones of the Delaware Mountain Group: Bell Canyon and Cherry Canyon Formations, Waha Field, West Texas  

E-Print Network [OSTI]

feldspars dominate over the plagioclases. Calcite is the dominant cementing mineral, though sulfate and halite cements have been observed. Hays (1992) showed that a diverse suite of authigenic minerals occurs in these sandstones, including silicate...

Walling, Suzette Denise

2012-06-07T23:59:59.000Z

251

ewly discovered at the bottom of the Hudson Canyon, the largest submarine canyon off the eastern United States, is  

E-Print Network [OSTI]

ocean's surface currents," explains Hugh Roarty, research project manager at the Coastal OceanEducationConservation Milestone in Ocean Exploration The first-ever ocean crossing by an underwater glider was hailed on both oceanmatters "Partnering with IMCS, a world leader in coastal ocean observation, gives OPT a significant

Garfunkel, Eric

252

Geomorphic response of submarine canyons to tectonic activity: Insights from the Cook Strait canyon system, New Zealand  

Science Journals Connector (OSTI)

...that a knickpoint degrades and reforms as it encounters regions of...CS is indicative of a low-energy setting because of a decrease...the tip of Baja California, Mexico: Geological Society of America...Divett, T., 2012, Tidal energy resource complexity in a large...

Aaron Micallef; Joshu J. Mountjoy; Philip M. Barnes; Miquel Canals; Galderic Lastras

253

u42501.PDF  

Office of Legacy Management (LM)

Younger sedimentary rocks overlying the Wasatch Formation are the Tertiary sandstone, oil shale, and marlstone beds of the Green River Formation which crop out almost continuously...

254

A N A S S E S S M E N T O F HONORS THINK TANK REPORT MAY 2013  

E-Print Network [OSTI]

A N A S S E S S M E N T O F HONORS THINK TANK REPORT MAY 2013 Awareness, Use, EducationUstAinAbility At the University of UtAh Wasatch Waters Think Tank Honors College May 2013 #12;Please cite this report as follows: Wasatch Waters Think Tank. 2013. An assessment of water: awareness, use, education, and sustainability

Feschotte, Cedric

255

Some Economic Effects of Drouth on Ranch Resources.  

E-Print Network [OSTI]

Some EconomiG Eflpcts of Drouth .. . . . TEXAS AGRICULTURAL EXPERIMENT STATION R. D. LEWIS. DIRECTOR. COLLEGE STATION. TEXAS \\ ., 1 - SUMMARY Most of the 162 ranches on which data were obtained for this study are on the Edwards Plateau within... 100 miles south and west of San Angelo. Data on ranch operations were obtained from the Texas Production Credit Association and the Farmers Home Administration at San Angelo, and from the Ozona National Bank. The current drout'h over most of West...

Ward, J. M.; Bonnen, C. A.

1955-01-01T23:59:59.000Z

256

Implementing the Pecos River Watershed Protection Plan through a Heliborne Electromagnetic (EM) Survey: Final Report  

E-Print Network [OSTI]

for the hydrological assessment. ..................................... 9 Figure 3: Distribution of TDS of the groundwater in the Pecos Valley Aquifer. ........................... 11 List of Acronyms BRACS Brackish Resources Aquifer Characterization System Database... June 45, 2013, in Pecos, Imperial, Iraan and Ozona. Throughout these public meetings, this project (TSSWCB 12-11) was discussed. [6] During the meeting in Imperial on June 4, landowners voiced concerns over the planned HEM survey methodology...

Gregory, L.; Sheng, Z.; Hassan, A.; McDonald, A.; Porter, A.

2014-01-01T23:59:59.000Z

257

Impact of Local Morphology on Sedimentation in a Submarine Canyon, ROV Studies in Eel Canyon, Northern California, U.S.A.  

Science Journals Connector (OSTI)

...disaggregated using a sonic bath and sodium metaphosphate as a dispersant solution. Sand and mud fractions were separated through wet...activity. 137Cs has been present in the marine environment since nuclear bomb testing started in ~ 1953, and the depth of 137Cs penetration...

Tina M. Drexler; Charles A. Nittrouer; Beth L. Mullenbach

258

Integrated reservoir study of the 8 reservoir of the Green Canyon 18 field  

E-Print Network [OSTI]

The move into deeper waters in the Gulf of Mexico has produced new opportunities for petroleum production, but it also has produced new challenges as different reservoir problems are encountered. This integrated reservoir characterization effort has...

Aniekwena, Anthony Udegbunam

2004-11-15T23:59:59.000Z

259

Simulation of wind-driven dispersion of fire pollutants in a street canyon using FDS  

Science Journals Connector (OSTI)

Air quality in urban areas attracts great attention due to increasing pollutant emissions and their negative effects on human health and environment. Numerous studies, such as those by Mouilleau and Champassith (...

Dusica J. Pesic; Milan DJ. Blagojevic

2014-01-01T23:59:59.000Z

260

Rock-water interactions of the Madison Aquifer, Mission Canyon Formation, Williston Basin, North Dakota  

E-Print Network [OSTI]

system. Results (i.e., degree of saturation with respect to calcite, dolomite, halite, gypsum, and anhydrite) were integrated with a graphical matrix analysis program to produce color-coded maps that depict potential precipitation-dissolution boundaries...

Spicer, James Frank

2012-06-07T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


261

Hydrodynamics of the Mission Canyon Formation in the Billings Nose area, North Dakota  

E-Print Network [OSTI]

of salinities to pressure gradients. . . . . . . -. . Values used in correction of potentiometric maps Conversion of water resistivities to salinities. 83 Calculation of time-temperature index (TTI) for burial history of Bakken Shale in Figure 35 96 Summary... shouting gently north~ard plunging anticlinal structure. Contour interval 50 ft (15 m). Modified from Walen (pers. comm. , 1983). 32 R 101 W R 1OOW T 143 N o 66S 0 0 4 P4 4 o 4 0 ~ q ~ 0 ~ T 142 N 0 & o )60 ~ ~ 0 ~ ~ 0 6600 4...

Mitsdarffer, Alan Ray

2012-06-07T23:59:59.000Z

262

Occurrence of gas hydrate in Oligocene Frio sand: Alaminos Canyon Block 818: Northern Gulf of Mexico  

E-Print Network [OSTI]

a suspected hazard to oil and gas drilling operations, andregional oil and gas reservoir) and the BGHS. Drilling

Boswell, R.D.

2010-01-01T23:59:59.000Z

263

STRATAL PATTERNS OF THE WILLIAMS FORK (HUNTER CANYON) FORMATION, PICEANCE BASIN, COLORADO  

E-Print Network [OSTI]

in the style of accommodation. The Williams Fork Formation contains stratal packages and was chosen for detailed study because of extensive exposures and a noticeable vertical change in lithology and sandstone-to-shale (net-to-gross) ratios. Ages... by Hancock (1925) and then eventually traced from the Grand Hogback to the Colorado-Utah state line by Fisher et al. (1960) and Collins (1976). The Williams Fork Formation is a gas producing formation (Cumella and Ostby, 2003), and previous study has...

Ost, Rebekah Corrie

2010-12-31T23:59:59.000Z

264

2006Volume78number3 131 chenbach Canyon is an easily  

E-Print Network [OSTI]

. This is both a short drive, just east of the city in the Organ Mountains, and a short hike, which even after (Cane Cholla), Fouquieria splendens (Ocotillo), Dasylirion wheeleri (Sotol), Yucca baccata (Banana Yucca

Gorelick, Root

265

Assessment of Native Salmonids Above Hells Canyon Dam, Idaho, 2002-2003 Annual Report.  

SciTech Connect (OSTI)

We assessed the relationships between specific stream attributes and Yellowstone cutthroat trout Oncorhynchus clarki bouvieri distribution and biomass at 773 stream reaches (averaging 100 m in length) throughout the Upper Snake River Basin in Idaho, in an effort to identify possible limiting factors. Because limiting factors were expected to vary across the range of cutthroat trout distribution in Idaho, separate logistic and multiple regression models were developed for each of the nine major river drainages to relate stream conditions to occurrence and biomass of cutthroat trout. Adequate stream flow to measure fish and habitat existed at 566 sites, and of those, Yellowstone cutthroat trout were present at 322 sites, while rainbow trout O. mykiss (or rainbow x cutthroat hybrids) and brook trout Salvelinus fontinalis occurred at 108 and 181 sites, respectively. In general, cutthroat trout presence at a specific site within a drainage was associated with a higher percentage of public property, higher elevation, more gravel and less fine substrate, and more upright riparian vegetation. However, there was much variation between drainages in the direction and magnitude of the relationships between stream characteristics and Yellowstone cutthroat trout occurrence and biomass, and in model strength. This was especially true for biomass models, in which we were able to develop models for only five drainages that explained more than 50% of the variation in cutthroat trout biomass. Sample size appeared to affect the strength of the biomass models, with a higher explanation of biomass variation in drainages with lower sample sizes. The occurrence of nonnative salmonids was not strongly related to cutthroat trout occurrence, but their widespread distribution and apparent ability to displace native cutthroat trout suggest they may nevertheless pose the largest threat to long-term cutthroat trout persistence in the Upper Snake River Basin.

Meyer, Kevin A.; Lamansky, Jr., James A. (Idaho Department of Fish and Game, Boise, ID)

2004-03-01T23:59:59.000Z

266

Glen Canyon Dam, Fluctuating Water Levels, and Riparian Breeding Birds: The Need for Management Compromise  

E-Print Network [OSTI]

of the lake coincided WtI 1Paper presented at the North American several years of above average snowfall

267

Recreational water quality analyses of the Colorado River corridor in Grand Canyon.  

Science Journals Connector (OSTI)

...Article Recreational water quality analyses of the Colorado River...J. F. Nix. 1977. Water quality loadings during thirteen storms...American Society Agricultural Engineers Meeting, paper no. 77-2529...watershed on bacteri- al water quality. J. Environ. Qual. 3...

B Tunnicliff; S K Brickler

1984-11-01T23:59:59.000Z

268

CARBON AND OXYGEN ISOTOPIC ANALYSIS: BUG, CHEROKEE, AND PATTERSON CANYON FIELDS, SAN JUAN COUNTY, UTAH  

SciTech Connect (OSTI)

Over 400 million barrels (64 million m{sup 3}) of oil have been produced from the shallow-shelf carbonate reservoirs in the Pennsylvanian (Desmoinesian) Paradox Formation in the Paradox Basin, Utah and Colorado. With the exception of the giant Greater Aneth field, the other 100 plus oil fields in the basin typically contain 2 to 10 million barrels (0.3-1.6 million m{sup 3}) of original oil in place. Most of these fields are characterized by high initial production rates followed by a very short productive life (primary), and hence premature abandonment. Only 15 to 25 percent of the original oil in place is recoverable during primary production from conventional vertical wells. An extensive and successful horizontal drilling program has been conducted in the giant Greater Aneth field. However, to date, only two horizontal wells have been drilled in small Ismay and Desert Creek fields. The results from these wells were disappointing due to poor understanding of the carbonate facies and diagenetic fabrics that create reservoir heterogeneity. These small fields, and similar fields in the basin, are at high risk of premature abandonment. At least 200 million barrels (31.8 million m{sup 3}) of oil will be left behind in these small fields because current development practices leave compartments of the heterogeneous reservoirs undrained. Through proper geological evaluation of the reservoirs, production may be increased by 20 to 50 percent through the drilling of low-cost single or multilateral horizontal legs from existing vertical development wells. In addition, horizontal drilling from existing wells minimizes surface disturbances and costs for field development, particularly in the environmentally sensitive areas of southeastern Utah and southwestern Colorado.

David E. Eby; Thomas C. Chidsey Jr; Kevin McClure; Craig D. Morgan; Stephen T. Nelson

2003-12-01T23:59:59.000Z

269

REDUCTIONS WITHOUT REGRET: DETAILS - AVOIDING BOX CANYONS, ROACH MOTELS, AND WRONG TURNS  

SciTech Connect (OSTI)

The United States is concurrently pursuing the goals of reducing the size of its nuclear weapons force strategic and non-strategic, deployed and non-deployed and of modernizing the weapons it continues to possess. Many of the existing systems were deployed 30 to 50 years ago, and the modernization process can be expected to extend over the next decade or more. Given the impossibility of predicting the future over the lifetime of systems that could extend to the end of this century, it is essential that dead ends in force development be avoided, and the flexibility and availability of options be retained that allow for Scalability downward in the event that further reductions are agreed upon; Reposturing to respond to changes in threat levels and to new nuclear actors; and Breakout response in the event that a competitor significantly increases its force size or force capability, In this paper, we examine the current motivations for reductions and modernization; review a number of historical systems and the attendant capabilities that have been eliminated in recent decades; discuss the current path forward for the U.S. nuclear force; provide a view of the evolving deterrence situation and our assessment of the uncertainties involved; and present examples of possibly problematic directions in force development. We close with our thoughts on how to maintain flexibility and the availability of options for which a need might recur in the future.

Swegle, John A.; Tincher, Douglas J.

2013-08-09T23:59:59.000Z

270

Occurrence of gas hydrate in Oligocene Frio sand: Alaminos Canyon Block 818: Northern Gulf of Mexico  

E-Print Network [OSTI]

Documented Example of Gas Hydrate Saturated Sand in the Gulfthat observed for gas hydrate-bearing sand sediments in thethan those for the gas hydrate-bearing sand formations in

Boswell, R.D.

2010-01-01T23:59:59.000Z

271

Assessment of Native Salmonids Above Hells Canyon Dam, Idaho; 1998 Annual Report.  

SciTech Connect (OSTI)

Native resident salmonids in the western United States are in decline throughout much of their range. The purpose of the multi-phased project is to restore native salmonids in the upper Snake River basin to self-sustaining, harvestable levels.

Meyer, Kevin A. (Idaho Department of Fish and Game, Boise, ID)

1999-03-01T23:59:59.000Z

272

Williams Holding lease steamflood demonstration project, Cat Canyon Field. Fourth progress report, December 1979-April 1981  

SciTech Connect (OSTI)

Activities prior to the initiation of displacement steam injection in April 1977 included cyclic steam stimulations of the production wells, acquisition of steam generator permits, and the drilling of pilot injection wells. Steamflood response occurred over a ten-month period beginning in October 1977 in four of the nine pilot producers. Subsequent attempts to divert steam to the non-responding producers failed. Poor oil production and high water-oil ratios characterized steamflood performance. Computer thermal simulation studies identified steam channeling, over-injection of steam, and poor quality steam at the sand face as causes of the adverse response. This led to a decision to temporarily suspend steamflood injection in February 1980. Improvement in oil production and a decrease in the water-oil ratio resulted during the following months.

Loftus, S.R.

1981-10-01T23:59:59.000Z

273

Assessment of Native Salmonids Above Hells Canyon Dam, Idaho, 2004-2005 Annual Report.  

SciTech Connect (OSTI)

In the western United States, exotic brook trout Salvelinus fontinalis frequently have a deleterious effect on native salmonids, and biologists often attempt to remove brook trout in streams using electrofishing. Although the success of electrofishing removal projects typically is low, few studies have assessed the underlying mechanisms of failure, especially in terms of compensatory responses. We evaluated the effectiveness of a three-year removal project in reducing brook trout and enhancing native salmonids in 7.8 km of an Idaho stream and looked for brook trout compensatory responses such as decreased natural mortality, increased growth, increased fecundity at length, or earlier maturation. Due to underestimates of the distribution of brook trout in the first year and personnel shortages in the third year, the multiagency watershed advisory group that performed the project fully treated the stream (i.e. multipass removals over the entire stream) in only one year. In 1998, 1999, and 2000, a total of 1,401, 1,241, and 890 brook trout were removed, respectively. For 1999 and 2000, an estimated 88 and 79% of the total number of brook trout in the stream were removed. For the section of stream that was treated in all years, the abundance of age-1 and older brook trout decreased by 85% from 1998 to 2003. In the same area, the abundance of age-0 brook trout decreased 86% from 1998 to 1999 but by 2003 had rebounded to near the original abundance. Abundance of native redband trout Oncorhynchus mykiss decreased for age-1 and older fish but did not change significantly for age-0 fish. Despite high rates of removal, total annual survival rate for brook trout increased from 0.08 {+-} 0.02 in 1998 to 0.20 {+-} 0.04 in 1999 and 0.21 {+-} 0.04 in 2000. Growth of age-0 brook trout was significantly higher in 2000 (the year after their abundance was lowest) compared to other years, and growth of age-1 and age-2 brook trout was significantly lower following the initial removal years but recovered by 2003. Few other brook trout demographic parameters changed appreciably over the course of the project. Electrofishing removals required 210 person-days of effort. Despite experiencing slight changes in abundance, growth, and survival, brook trout in Pikes Fork appeared little affected by three years of intensive removal efforts, most likely because mortality within the population was high prior to initiation of the project such that the removal efforts merely replaced natural mortality with exploitation.

Meyer, Kevin A.; Lamansky, Jr., James A. (Idaho Department of Fish and Game, Boise, ID)

2005-08-01T23:59:59.000Z

274

THE OPTICAL GREEN VALLEY VERSUS MID-INFRARED CANYON IN COMPACT GROUPS  

SciTech Connect (OSTI)

Compact groups of galaxies provide conditions similar to those experienced by galaxies in the earlier universe. Recent work on compact groups has led to the discovery of a dearth of mid-infrared transition galaxies (MIRTGs) in Infrared Array Camera (3.6-8.0 ?m) color space as well as at intermediate specific star formation rates. However, we find that in compact groups these MIRTGs have already transitioned to the optical ([gr]) red sequence. We investigate the optical color-magnitude diagram (CMD) of 99 compact groups containing 348 galaxies and compare the optical CMD with mid-infrared (mid-IR) color space for compact group galaxies. Utilizing redshifts available from Sloan Digital Sky Survey, we identified new galaxy members for four groups. By combining optical and mid-IR data, we obtain information on both the dust and the stellar populations in compact group galaxies. We also compare with more isolated galaxies and galaxies in the Coma Cluster, which reveals that, similar to clusters, compact groups are dominated by optically red galaxies. While we find that compact group transition galaxies lie on the optical red sequence, LVL+SINGS mid-IR transition galaxies span the range of optical colors. The dearth of mid-IR transition galaxies in compact groups may be due to a lack of moderately star-forming low mass galaxies; the relative lack of these galaxies could be due to their relatively small gravitational potential wells. This makes them more susceptible to this dynamic environment, thus causing them to more easily lose gas or be accreted by larger members.

Walker, Lisa May; Butterfield, Natalie; Johnson, Kelsey; Zucker, Catherine [Astronomy Department, University of Virginia, Charlottesville, VA 22904 (United States); Gallagher, Sarah [Department of Physics and Astronomy, University of Western Ontario, London, ON N6A 3K7 (Canada); Konstantopoulos, Iraklis [Australian Astronomical Observatory, North Ryde, NSW 1670 (Australia); Zabludoff, Ann [Steward Observatory, University of Arizona, Tucson, AZ 85721 (United States); Hornschemeier, Ann E.; Tzanavaris, Panayiotis [Laboratory for X-Ray Astrophysics, NASA Goddard Space Flight Center, Greenbelt, MD 20771 (United States); Charlton, Jane C. [Department of Astronomy and Astrophysics, Pennsylvania State University, University Park, PA 16802 (United States)

2013-10-01T23:59:59.000Z

275

The effect of prescribed fire on sugar pine mortality in Sequoia and Kings Canyon National Parks  

E-Print Network [OSTI]

for Sierran mixed-conifer forests. PSW-GTR-220, US Forestfires in a mixed conifer forest. Canadian Journal of Forestin a Sierra Nevada mixed-conifer forest. Forest Ecology and

Nesmith, Jonny CB

2011-01-01T23:59:59.000Z

276

Experiments on Hydraulic Jumps in Turbidity Currents Near a Canyon-Fan Transition  

Science Journals Connector (OSTI)

...attention. Recently Parker, Fukushima, and Pantin (11) have...sediment by-passing put forward by Mutti (19). The...11. G. Parker, Y. Fukushima, H. Pantin, ibid. 171, 145 (1986). 12. Y. Fukushima, G. Parker, H. Pantin...

MARCELO GARCIA; GARY PARKER

1989-07-28T23:59:59.000Z

277

Ice Climbing in Clear Creek Canyon A climbing trip report by Glenn Murray  

E-Print Network [OSTI]

metal thingies?' Sean pulls on his boots. He has great boots, massive leather Kastingers with wooden

278

Structural fabric of the Palisades Monocline: a study of positive inversion, Grand Canyon, Arizona  

E-Print Network [OSTI]

. During inversion, contraction induced reverse reactivation of existing hanging wall faults, footwall folding and footwall thrust-faulting. Precambrian normal slip along the master normal fault and subsequent Laramide reverse slip along the new footwall...

Orofino, James Cory

2005-08-29T23:59:59.000Z

279

Geologic versus wildfire controls on hillslope processes and debris flow initiation in the Green River canyons  

E-Print Network [OSTI]

Geologic versus wildfire controls on hillslope processes and debris flow initiation in the Green are unknown. A recent episode of enhanced debris-flow and wildfire activity provided an opportunity to examine with recent debris flows to determine how surficial geology, wildfire, topography, bedrock strength

Pederson, Joel L.

280

Geometry and styles of displacement transfer, eastern Sun River Canyon Area, Sawtooth Range, Montana  

E-Print Network [OSTI]

) ~Kk CRETACEOUS (Kootenoi Fm) ~J JURASS IC ~Mm MISS I SS I PP I AN ~D DEVON I AN 50 STRIKE AND DIP THRUST FAULT PE R I 0 D CON TACT TOPOGRAPHIC CONTOUR o o lO LIJ O 'z ~oo, Mm Alorrh 4600~ RIVER (PI. ';. I , " I ))U" &~71 30 8 O... are absent in northwest Montana but are present in clastic wedges adjacent to well known uplifts of crystal- line basement blocks in Wyoming and Colorado. Price attributes fragments of Proterozoic and Paleozoic age rock in Cretaceous and Late Jurassic...

Goldburg, Barbara Louise

2012-06-07T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


281

Dwelling in the canyons: Dwelling detection in Urban Environments Using GPS, Wi-Fi, and Geolocation  

E-Print Network [OSTI]

. Most of our significant places are indoors, which hampers the detection us- ing GPS. In this work, we-Fi and geolocation. Our study is based on data collected on mobile phones in cities of various sizes in four European such as traffic prediction, city planning, and for deter- mining social interactions. Therefore human mobility has

Langendoen, Koen

282

Ecology and Management of Canyon Flies (Fannia benjamini complex) in California  

E-Print Network [OSTI]

M. W. 1976. Mosquito Ecology: Field sampling methods. Newin southern Israel. J. Vector Ecology. 36(1): S212-S218.control from chemical ecology. Agriculture, Ecosystems &

Ekanayake, Panchali Kumari

2012-01-01T23:59:59.000Z

283

Depositional environment of Canyon (Cisco) sandstones, North Jameson field Mitchell County, Texas  

E-Print Network [OSTI]

-fill turbidites. Cores from the field exhibit the characteristics of classic sedimentary structures, compositional trends, upward fining texture, and absence of biogenic structures that are indicat1ve of turbidites. Channel-fill deposits are dominated by "AE... The average grain size of the sandstones ranges between 0. 16 and 0. 19 mm (fine grained. ). Average composition consists of 49 to 52 percent quartz, 15 to 27 percent, feldspar, 13 to 20 percent rock fragments and 8 to 12 percent matrix. Cement ranges...

Dally, David Jesse

2012-06-07T23:59:59.000Z

284

Detection of Gas Hydrates in Garden Banks and Keathley Canyon from Seismic Data  

E-Print Network [OSTI]

, where the sub-seafloor is a complex structure of shallow salt diapirs and sheets underlying heavily deformed shallow sediments and surrounding diverse minibasins. Here, we consider the effect these structural factors have on gas hydrate occurrence...

Murad, Idris

2011-08-08T23:59:59.000Z

285

Rock-water interactions of the Madison Aquifer, Mission Canyon Formation, Williston Basin, North Dakota.  

E-Print Network [OSTI]

??The Williston Basin is located in the northern Great Plains of the United States. This area includes eastern Montana, northwestern South Dakota, and western North (more)

Spicer, James Frank

2012-01-01T23:59:59.000Z

286

EXPLORING FOR SUBTLE MISSION CANYON STRATIGRAPHIC TRAPS WITH ELASTIC WAVEFIELD SEISMIC TECHNOLOGY  

SciTech Connect (OSTI)

The 9C3D seismic data that will form the principal data base needed for this research program have been successfully acquired. The seismic field data exhibit a good signal-to-noise (S/N) ratio for all elastic-wave modes. Thus the major hurdle of acquiring optimal-quality 9-C seismic data has been cleared. The stratigraphic oil-reservoir target that will be the imaging objective of the seismic data-processing effort is described in this report to indicate the challenge that now confronts the data-processing phase of the project.

John Beecherl

2004-02-01T23:59:59.000Z

287

Simulation of Nocturnal Drainage Flows Enhanced by Deep Canyons: The Rocky Flats Case  

Science Journals Connector (OSTI)

The DELTAADREA (discretization with elements of triangle approachatmospheric dispersion of pollutants over irregular terrain) numerical prediction model, developed at the National Center for Scientific Research Demokritos, is specifically ...

Melpomeni Varvayanni; John G. Bartzis; Nicolas Catsaros; Panagiotis Deligiannis; Chuck E. Elderkin

1997-06-01T23:59:59.000Z

288

Experiments on Hydraulic Jumps in Turbidity Currents Near a Canyon-Fan Transition  

Science Journals Connector (OSTI)

...cathodoluminescence ex-periments. Many useful comments on our manu-script were made by K. Kash, J. M. Worlock, and M. Saifi. We are especially gratefill to D. E. Aspnes for making concrete suggestions for the improvement ofour report. 8 May 1989...

MARCELO GARCIA; GARY PARKER

1989-07-28T23:59:59.000Z

289

Long-Term Surveillance Plan for the Burro Canyon Disposal Cell...  

Office of Legacy Management (LM)

developed regulations for the issuance of a general license for the custody and long-term care of UMTRA Project disposal sites in 1 0 CFR Part 40. The purpose of this general...

290

Amphitheater-headed canyons formed by megaflooding at Malad Gorge, Idaho  

Science Journals Connector (OSTI)

...counts) and of a boulder bar upstream of...2B) showing the flood depth calculated to...also inferred from boulder bars (median grain...2B) where the flood was largely unconfined...of the Bonneville Flood (Geol Soc Am, Boulder, CO), 90 pp . 31...

Michael P. Lamb; Benjamin H. Mackey; Kenneth A. Farley

2014-01-01T23:59:59.000Z

291

Amphitheater-headed canyons formed by megaflooding at Malad Gorge, Idaho  

Science Journals Connector (OSTI)

...inferred from boulder bars (median...where the flood was largely...features of the Colorado Plateau: A comparative...Pleistocene Bonneville Flood in the Snake...Geol Soc Am , Boulder, CO ), Vol K-2...the Bonneville Flood (Geol Soc Am, Boulder, CO), 90 pp...

Michael P. Lamb; Benjamin H. Mackey; Kenneth A. Farley

2014-01-01T23:59:59.000Z

292

Amphitheater-headed canyons formed by megaflooding at Malad Gorge, Idaho  

Science Journals Connector (OSTI)

...likely carved by a large-scale flood event that occurred ?45 ka...formed during the Bonneville Flood [?1822 ka (27, 28...1988 ) Sapping features of the Colorado Plateau: A comparative planetary geology...Late Pleistocene Bonneville Flood in the Snake River Plain, Idaho...

Michael P. Lamb; Benjamin H. Mackey; Kenneth A. Farley

2014-01-01T23:59:59.000Z

293

Constructing the aesthetic sense : traversing scales of habitation in the Bingham Canyon Mine  

E-Print Network [OSTI]

The activities of mining and mine reclamation in the American West raise questions of how we perceive, value, and differentiate between 'natural' and man-made landscapes, as they produce radical alterations of the land on ...

Pierce, Matthew W., 1973-

2004-01-01T23:59:59.000Z

294

Constructing the aesthetic sense : traversing scales of habitation in the Bingham Canyon Mine .  

E-Print Network [OSTI]

??The activities of mining and mine reclamation in the American West raise questions of how we perceive, value, and differentiate between 'natural' and man-made landscapes, (more)

Pierce, Matthew W., 1973-

2004-01-01T23:59:59.000Z

295

Predicting velocities and turbulent exchange in isolated street canyons and at a neighborhood scale  

E-Print Network [OSTI]

Urban planners need a fast, simple model to assess the impact of early design phase iterations of neighborhood layout on the microclimate. Specifically, this model should be able to predict the expected urban heat island ...

Hall, Terianne C

2010-01-01T23:59:59.000Z

296

Debris flow deposition and reworking by the Colorado River in Grand Canyon, Arizona  

E-Print Network [OSTI]

], thereby disrupting any steady or quasi-steady state that the fluvial system may have had above maximum dam releases, and surface shape shifted from concave to convex. Dam releases above power influences on the system, which may be much more significant in terms of rate of change. Construction

297

The ecological distribution of vertebrates and flowering plants in Capote Canyon, Presidio County, Texas  

E-Print Network [OSTI]

(Continued) Ze na id u ra. macroura RN A A A A C C A A S TR IGIDAE Bubo virginianus pallescens R I APODIDAE I I Aeronautes saxa- talis S C A C A C A C A PICIDAE Dendrocopos s ca la r is ca cto- philus TYRANNIDAE RN U U Sayornis nigricsns... (Continued) Ze na id u ra. macroura RN A A A A C C A A S TR IGIDAE Bubo virginianus pallescens R I APODIDAE I I Aeronautes saxa- talis S C A C A C A C A PICIDAE Dendrocopos s ca la r is ca cto- philus TYRANNIDAE RN U U Sayornis nigricsns...

Ohlendorf, Harry Max

2012-06-07T23:59:59.000Z

298

W00604050033 W00604040011  

E-Print Network [OSTI]

-Site Canyon Area A Canyon Fish Ladder Canyon HE K-SITE 340 430 BURNING GROUND 410 V-SITE 360 BUNKER 411

299

HYDRAULIC CALCULATIONS FOR A MODIFIED IN-SITU RETORT  

E-Print Network [OSTI]

D. C. , 1974), 2. Oil Shale Tract C-b: Materials (AshlandRiver, containing the oil shale; and the Wasatch foundationof dolomitic marlstone (oil shale) and soluble materials.

Hall, W.G.

2012-01-01T23:59:59.000Z

300

A new interpretation of deformation rates in the Snake River Plain and adjacent basin and range regions based on GPS measurements  

Science Journals Connector (OSTI)

......from continuous sites and other campaigns...velocity field to test previous hypotheses...Oregon and northern Nevada areas beginning...structure between the Nevada Test Site and Boise, Idaho...zone in southern Nevada linking the Wasatch......

S.J. Payne; R. McCaffrey; R.W. King; S.A. Kattenhorn

2012-04-01T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


301

CX-100147 Categorical Exclusion Determination  

Office of Energy Efficiency and Renewable Energy (EERE)

Wasatch Solar Project Award Number: DE-EE0006903 CX(s) Applied: A9, A11 Date: 12/12/2014 Location(s): UT Office(s): Golden Field Office

302

Slip rate variations on normal faults during glacialinterglacial changes in surface loads  

Science Journals Connector (OSTI)

... Here we use finite-element models to investigate why four parallel normal faultsthe Wasatch, West Valley, Oquirrh and Stansbury faults in the eastern Basin and Range Province, Utahhave experienced ... We now test whether the Late Pleistocene/Holocene increase in slip rates of the Wasatch, West Valley, Oquirrh and Stansbury normal faults may be due to isostatic rebound caused by the ...

Ralf Hetzel; Andrea Hampel

2005-05-05T23:59:59.000Z

303

NETL: Oil & Natural Gas Technologies Reference Shelf - Presentation on Gas  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Gas and Oil in Utah: Potential, New Discoveries, and Hot Plays Gas and Oil in Utah: Potential, New Discoveries, and Hot Plays Gas and Oil in Utah: Potential, New Discoveries, and Hot Plays Author: Thomas C. Chidsey, Petroleum Section Chief, Utah Geological Survey, Salt Lake City, UT. Venue: International Oil Scouts Association’s 84th annual meeting, Stein Eriksen Lodge, Park City, UT, June 17–20, 2007, (http://www.oilscouts.com/index-main.html [external site]). Abstract: Utah’s natural gas and oil exploration history extends back more than 100 years, fluctuating greatly due to discoveries, price trends, and changing exploration targets. During the boom period of the early 1980s, activity peaked at over 500 wells per year. After slowing in the 1990s, drilling activity has again increased, reaching an all-time peak of 1,058 wells spudded and over 2,000 APDs (application for permit to drill) filed in 2006. This increase in activity has been spurred by high prices for both natural gas and oil and by the perception that Utah is highly prospective and underexplored. In recent years, the proportion of new wells exploring for gas has increased greatly. Total cumulative natural gas production from Utah fields now exceeds 8 Tcf. Recent successful drilling has been expanding reserves by about 10 percent per year, one of the highest rates of gas reserves increase in the country. Although gas production from some fields declined during the late 1990s, two factors caused overall gas production to increase. The development of coalbed natural gas (CBNG) accumulations in the Cretaceous Ferron Sandstone play, in particular Drunkards Wash field in central Utah, has increased the State’s annual gas production by 20–30 percent. Also, deeper exploratory and development drilling in the eastern and southern Uinta Basin during the past 5 years has led to discoveries of substantial gas accumulations in tight-sand reservoirs of the Tertiary Wasatch Formation, Cretaceous Mesaverde Group, and Jurassic Entrada and Wingate Sandstones. Significant potential exists for other coalfields (Book Cliffs, Sego, and Wasatch Plateau) around the Uinta Basin to yield CBNG, and the extent of deeper conventional and tight-gas plays remains to be explored. In addition, shale gas reservoirs in the Mississippian Manning Canyon Shale, Pennsylvanian Hermosa Group, and Cretaceous Mancos Shale of central, southeastern, and northeastern Utah, respectively, have tremendous untapped potential. Utah oilfields have produced a cumulative total of 1.3 billion barrels (bbl) of oil. Although annual production decreased from a peak of 41 million bbl in 1985 to 13 million bbl in 2003, the trend has since reversed, and 2005 production reached nearly 17 million bbl. A component (about one-third of the increase) of this turnaround has been the 2004 discovery of Covenant field in the central Utah thrust belt, or "Hingeline." This new field has already produced 3 million bbl of Mississippian-sourced oil from the Jurassic Navajo Sandstone in a thrusted anticline formed during the Sevier orogeny. This new oil play is the focus of extensive leasing and exploration activity—comparable to the late 1970s and early 1980s in the Utah-Wyoming salient of the thrust belt to the north.

304

Record of Decision: Stabilization of Plutonium Solutions Stored in the F-Canyon Facility at the Savannah River Site  

Broader source: Energy.gov (indexed) [DOE]

24 24 Federal Register / Vol. 60, No. 35 / Wednesday, February 22, 1995 / Notices determination have been corrected, and the SEA or LEA is, in all other respects, in compliance with the requirements of the applicable program; (2) SEA has submitted to the Secretary a plan for the use of the funds to be awarded under the grantback arrangement that meets the requirements of the program, and to the extent possible, benefits the population that was affected by the failure to comply or by the misexpenditures that resulted in the audit exception; and (3) Use of funds to be awarded under the grantback arrangement in accordance with the SEA's plan would serve to achieve the purposes of the program under which the funds were originally granted. C. Plan for Use of Funds Awarded Under a Grantback Arrangement

305

Depositional environment and hydrodynamic flow in Guadalupian Cherry Canyon sandstone, West Ford and West Geraldine fields, Delaware Basin, Texas  

E-Print Network [OSTI]

and entrapment of hydrocarbons. Delaware Mountain Group sediments are currently generating oil. Decementation enhances the reservoir by the formation of secondary porosity. The reservoir sandstones have an aver age porosity of 26$ and an aver age permeability... of 24 md. Oil accumulates in stratigraphic traps located along the updip meander loops of tur bidite channels. A tilted oil/water contact in West Ford and West Ger aldine fields indicates that hydrodynamic flow is pr esent. Heads calculated...

Linn, Anne Marie

2012-06-07T23:59:59.000Z

306

Analyzing the connectivity potential of landscape geomorphic systems: a radar remote sensing and GIS approach, Estufa Canyon, Texas, USA  

E-Print Network [OSTI]

of rainfall over Panther Junction and and Chisos Basin, Big Bend National Park, Texas??????????. 28 5 The distribution of the average monthly temperature over a period extending from 1948 to 2001 at Chisos Basin and Panther Junction climatic... stations, Big Bend National Park, Texas??????????.. 29 6 The diurnal variation at both Chisos Basin and Panther Junction stations, Big Bend National Park, Texas?????????????????... 31 7 Rock disintegration in the high gravel terrace...

Ibrahim, ElSayed Ali Hermas

2005-11-01T23:59:59.000Z

307

Vegetation patterns of Pine Canyon, Big Bend National Park, Texas, in relation to elevation and slope aspect  

E-Print Network [OSTI]

and richness, and stem density are also analyzed. Communities encountered on the south-facing slope, from low to high elevation, are: Chihuahuan Desert shrubland, sotol grassland, open oak shrubland, mixed shrubland, and oak-pinyon-juniper woodland. Communities...

Harris, Bryan Joseph

1997-01-01T23:59:59.000Z

308

Lateral Continuity of the Eagle Ford Group Strata in Lozier Canyon and Antonio Creek, Terrell County, Texas  

E-Print Network [OSTI]

for Identification Used in This Study. After Harms and others (1975), Reineck and Singh (1975), Campbell (1967). Wave Current Symmetrical and asymmetrical Asymmetrical Convex up with bi directional downlap Rarely Convex up, usually onlap on one side Boundary Lozier..., fish bones; locally common rare gastropods, 3-20-in (8-50 cm) wood fragments; plesiosaur skeleton, framboidal pyrite; rare quartz silt Very dark gray...

Gardner, Rand D

2013-09-24T23:59:59.000Z

309

Origin of upper Bell Canyon Reservoir Sandstones (Guadalupian), El Mar and Paduca Fields, Southeast New Mexico and West Texas  

E-Print Network [OSTI]

AR Z a. 55J ct M Y O POROS I T PERM m4 I IO 0 D LD TENNESEE GAS 8 OIL STATE MONSANTO 3 LEA CO. , N M Rm = 0. 034 at 95 F BHT PERF 4609 34 IPF 52 BOPD 7 FIG. 7 ? Gamma ray ? Sonic logs of Lamer Shale, Ramsey Sandstone, Ford Shale... depth of 4500 ft in El Nar field, Loving County, Texas, and at 4600 ft in Paduca field, Lea County, New Mexico. Entrapment of oil is by capillary-pressure differences and is possibly enhanced by hydrodynamic flow. Total oil columns are approximately...

Weinmeister, Marcus Paul

2012-06-07T23:59:59.000Z

310

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program-based on advanced reservoir management methods- can significantly improve oil recovery. The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry.

Murphy, M.B.

1997-10-30T23:59:59.000Z

311

Williams Holding Lease Steamflood Demonstration Project: Cat Canyon Oil Field. Third progress report, July 1978-November 1979  

SciTech Connect (OSTI)

This report discusses pilot operations and results during this period. The performance of the displacement steam generator, the status of the sulfur dioxide scrubbing system, well workovers and the results of drilling four thermal observation wells are examined. Additional computer thermal simulation studies are discussed in detail and a new production performance projection is made. Finally, project economics and future operations are summarized.

Ditmore, T.L.

1980-06-01T23:59:59.000Z

312

ADVANCED OIL RECOVERY TECHNOLOGIES FOR IMPROVED RECOVERY FROM SLOPE BASIN CLASTIC RESERVOIRS, NASH DRAW BRUSHY CANYON POOL, EDDY COUNTY, NM  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program based on advanced reservoir management methods can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry.

Mark B. Murphy

2003-10-31T23:59:59.000Z

313

ADVANCED OIL RECOVERY TECHNOLOGIES FOR IMPROVED RECOVERY FROM SLOPE BASIN CLASTIC RESERVOIRS, NASH DRAW BRUSHY CANYON POOL, EDDY COUNTY, NM  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program based on advanced reservoir management methods can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry.

Mark B. Murphy

2004-01-31T23:59:59.000Z

314

Trace element abundances in the Rock Canyon Anticline, Pueblo, Colorado, marine sedimentary section and their relationship to  

E-Print Network [OSTI]

also correspond with a positive excursion in carbon isotopic composition of seawater. Hydrothermal that intermittent hydrothermal activity on a massive scale triggered abrupt changes in carbon burial and deep ocean d13 C isotope excursion. The metal abundance anomalies indicate that intermittent hydrothermal

Bralower, Timothy J.

315

Roles of Host Species, Geographic Separation, and Isolation in the Seroprevalence of Jamestown Canyon and Snowshoe Hare Viruses in Newfoundland  

Science Journals Connector (OSTI)

...JCV among cattle on farms situated on a wind-exposed seacoast compared with that for cattle on farms located in a wind-protected boreal freshwater landscape...collected from a variety of domestic and wildlife host species. These species were sampled...

Gregory Goff; Hugh Whitney; Michael A. Drebot

2012-07-13T23:59:59.000Z

316

Late Pleistocene to Recent sediment transport pathways of the Green Canyon OCS area, northern Gulf of Mexico  

E-Print Network [OSTI]

remobilizes sediments which are then carried further downslope. These remobilized sediments may be transported as debris flows or other undifferentiated high-density flows, or may develop into turbidity currents which deposit graded sediments in response...

Swanson, John Patrick

2012-06-07T23:59:59.000Z

317

Depositional patterns and reservoir morphology of Guadalupian Cherry Canyon sandstones, Indian Draw Field, Eddy County, New Mexico  

E-Print Network [OSTI]

in the field is a combination structural-stratigraphic trap. The properties of the sandstones in conjunction with complex local stra- tigraphy control reservoir production ' n the field. An 15 A 6l R28E ~O 12 33 34 23 24 35 ~ ' ~ 14 36 13 15... diagram of the mechanical and electrical instrumentation of a high? resolution dipmeter tool showing the electrode system, caliper, and deviation system. Lower part of diagram shows the resistivity correlation curves and re- lationship of the borehole...

Phillips, Sandra

1981-01-01T23:59:59.000Z

318

ADVANCED OIL RECOVERY TECHNOLOGIES FOR IMPROVED RECOVERY FROM SLOPE BASIN CLASTIC RESERVOIRS, NASH DRAW BRUSHY CANYON POOL, EDDY COUNTY, NM  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program-based on advanced reservoir management methods-can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry. This is the twenty-eighth quarterly progress report on the project. Results obtained to date are summarized.

Mark B. Murphy

2002-09-30T23:59:59.000Z

319

Structural restoration of Louann Salt and overlying sediments, De Soto Canyon Salt Basin, northeastern Gulf of Mexico  

E-Print Network [OSTI]

The continental margin of the northeastern Gulf of Mexico is suited for seismic stratigraphic analysis and salt tectonism analysis. Jurassic strata include the Louann Salt on the continental shelf and upper slope of the Destin Dome OCS area...

Guo, Mengdong

2012-06-07T23:59:59.000Z

320

Changes in the water surface profile of the Colorado River in Grand Canyon, Arizona, between 1923 and 2000  

E-Print Network [OSTI]

mouths and deposit large boulders into the river [Cooley et al., 1977; Webb et al., 1989; Melis et al fans or boulder bars even further downstream. When viewed in profile, the water surface is stepped, of that material by main stem Colorado River floods [Kieffer, 1985; Webb et al., 1999a]. Reworking consists of both

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


321

Frequency and initiation of debris flows in Grand Canyon, Arizona Peter G. Griffiths and Robert H. Webb  

E-Print Network [OSTI]

: Floods; 1860 Hydrology: Runoff and streamflow; KEYWORDS: debris flows, mass wasting, geomorphology, Grand and remove or reposition boulders [Webb et al., 1989]. Boulders in the river are also subject to slow, long., 1994; Webb et al., 1999b] owing to debris flow deposition. The large boulders deposited in the river

322

Age of Barrier Canyon-style rock art constrained by cross-cutting relations and luminescence dating techniques  

Science Journals Connector (OSTI)

...3 ka, the basal flood deposits of the T1 were...distinct packages of flood deposits are preserved (31), dating...of loose sediment the boulder landed upon. The two OSL...5000-year record of extreme floods and climate change in the...Scientific Study of Rock Art (Boulder, CO). The authors declare...

Joel L. Pederson; Melissa S. Chapot; Steven R. Simms; Reza Sohbati; Tammy M. Rittenour; Andrew S. Murray; Gary Cox

2014-01-01T23:59:59.000Z

323

High-Resolution Carbon Isotope Stratigraphy, Pennsylvanian Snaky Canyon Formation, East-Central Idaho: Implications for Regional and Global Correlations  

E-Print Network [OSTI]

................................................... 25 Table 2 Average ?18O and ?13C by rock classification and age ............................. 34 Table 3 Electron microprobe analyses of carbonate matrix and skeletal grains .... 38 Table 4 North American and International stage boundary ages... of the Bloom Member (Fig. 2) consists primarily of medium-dark-gray skeletal wackestone (?44%), skeletal packstone (?26%), mudstone (?13%), and siltstone (?11%), with the remaining 6% composed of grainstone, calcisiltstone, algal boundstone, and bedded...

Jolley, Casey

2012-07-16T23:59:59.000Z

324

2011 Los Alamos National Laboratory Riparian Inventory Results  

SciTech Connect (OSTI)

A total length of 36.7 kilometers of riparian habitat were inventoried within LANL boundaries between 2007 and 2011. The following canyons and lengths of riparian habitat were surveyed and inventoried between 2007 and 2011. Water Canyon (9,669 m), Los Alamos Canyon (7,131 m), Pajarito Canyon (6,009 m), Mortandad Canyon (3,110 m), Two-Mile Canyon (2,680 m), Sandia Canyon (2,181 m), Three-Mile Canyon (1,883 m), Canyon de Valle (1,835 m), Ancho Canyon (1,143 m), Canada del Buey (700 m), Sandia Canyon (221 m), DP Canyon (159 m) and Chaquehui Canyon (50 m). Effluent Canyon, Fence Canyon and Potrillo Canyon were surveyed but no areas of riparian habitat were found. Stretches of inventoried riparian habitat were classified for prioritization of treatment, if any was recommended. High priority sites included stretches of Mortandad Canyon, LA Canyon, Pajarito Canyon, Two-Mile Canyon, Sandia Canyon and Water Canyon. Recommended treatment for high priority sites includes placement of objects into the stream channel to encourage sediment deposition, elimination of channel incision, and to expand and slow water flow across the floodplain. Additional stretches were classified as lower priority, and, for other sites it was recommended that feral cattle and exotic plants be removed to aid in riparian habitat recovery. In June 2011 the Las Conchas Wildfire burned over 150,000 acres of land in the Jemez Mountains and surrounding areas. The watersheds above LA Canyon, Water Canyon and Pajarito Canyon were burned in the Las Conchas Wildfire and flooding and habitat alteration were observed in these canyon bottoms (Wright 2011). Post fire status of lower priority areas may change to higher priority for some of the sites surveyed prior to the Las Conchas Wildfire, due to changes in vegetation cover in the adjacent upland watershed.

Norris, Elizabeth J. [Los Alamos National Laboratory; Hansen, Leslie A. [Los Alamos National Laboratory; Hathcock, Charles D. [Los Alamos National Laboratory; Keller, David C. [Los Alamos National Laboratory; Zemlick, Catherine M. [Los Alamos National Laboratory

2012-03-29T23:59:59.000Z

325

CALIBRATION OF LOW ENERGY PRODUCTION OF 36 AND THE CREATION OF AN EXPOSURE AGE CALCULATOR  

E-Print Network [OSTI]

Copper Canyon to calibrate Pf(0)36 Cl. We show that for the Copper Canyon calibration site Pf(0)36 Cl . . . . . . . . . . . . . . . . . . . . . 18 2.5 Copper Canyon site schematic . . . . . . . . . . . . . .

Borchers, Brian

326

The Black Mountains turtlebacks: Rosetta stones of Death Valley tectonics  

E-Print Network [OSTI]

turtleback in the north, the Copper Canyon turtleback, and the Mormon Point turtleback in the south. Although at Badwater; 6 Ma at Copper Canyon; 8 Ma at Mormon Point. At Mormon Point and Copper Canyon turtlebacks

Miller, Marli Bryant

327

Photo Gallery - Hanford Site  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Before Cocooning N Reactor Before Cocooning U Canyon Aerial U Canyon Aerial Aerial Photo of 200 West Groundwater Treatment Facility Aerial Photo of 200 West Groundwater...

328

uth93a1.tmp  

National Nuclear Security Administration (NNSA)

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . ...49 4.2.6 Fortymile Canyon Tanks . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . ...49 4.2.6.1 Site...

329

California State University, Desert Studies Consortium and LSA Associates, Inc. Old Ores: mines and mineral marketing  

E-Print Network [OSTI]

......................................................................................................................................................................77 Age constraints of the Copper Canyon Formation, Death Valley National Park, California Torrey

de Lijser, Peter

330

As part of the Long Term Agricultural Research Network, we are studying attributes of Criollo cattle and comparing  

E-Print Network [OSTI]

­ "New World" Cattle n Obtained from isolated areas of Sierra Tarahumara (Copper Canyon) in southwestern

331

The Guadalupe Blanco River Trust and the Guadalupe-Blanco River Authority: Creating and  

E-Print Network [OSTI]

· Gorge Preservation Society (GPS), 2006 ­ Ecotourism and education at the Canyon Reservoir Gorge, which

332

Ke iko H. Hattori Jerey D. Keith Contribution of mac melt to porphyry copper mineralization  

E-Print Network [OSTI]

mineralization: evidence from Mount Pinatubo, Philippines, and Bingham Canyon, Utah, USA Received: 15 April 2001 Canyon, Utah, site of the largest copper and gold deposit in North America at 38 Ma. The Bingham Canyon and selenium (Hattori 1993, 1996). We suggest that a sim- ilar process took place at 38 Ma at Bingham Canyon

333

Federal Compensation to Idaho for Public Domain Federal Lands, 1988-99 FederalCompensationtoIdaho  

E-Print Network [OSTI]

........................................................................................................ 9 Figure 7. Bingham County Federal Payments........................................................................................................ 12 Figure 15. Canyon County Federal Payments

O'Laughlin, Jay

334

uide for the University of Utah Air Quality  

E-Print Network [OSTI]

pollution. Regulating air pollution is a priority of the federal government because air pollution can cause adverse health effects in humans.1 The Wasatch Front is plagued with poor air quality during the winter to trapped pollution. Air pollution in the Salt Lake Valley is characterized by high levels of particulate

Tipple, Brett

335

COLORADO PLATEAU PINYON-JUNIPER WOODLAND extent exaggerated for display  

E-Print Network [OSTI]

and foothills of the Colorado Plateau region from the Western Slope of Colorado to the Wasatch Range, and southCOLORADO PLATEAU PINYON-JUNIPER WOODLAND S.Kettler extent exaggerated for display JUNIPERUS at all (Reid et al. 1999). COLORADO PLATEAU PINYON-JUNIPER WOODLAND 1 REVISED: SEPTEMBER 2005 #12;A

336

Bulletin of the American Museum of Natural History  

Science Journals Connector (OSTI)

...author's name whose work in codification is historic. The work is confessedly intri-cate...Four-horned Pely-cosaurian from the Permian of Texas " is described in article XI...especially the Wasatch of the Big Horn Basin, where they predominate over all other...

L. P. Gratacap

1909-05-28T23:59:59.000Z

337

A Reaction-Transport-Mechanical Approach to Modeling the Interrelationships Among Gas Generation, Overpressuring, and Fracturing: Implications for the Upper Cretaceous Natural Gas Reservoirs of the Piceance Basin, Colorado  

Science Journals Connector (OSTI)

...in 1995. His current research interests...He has done internships and contract...Department of Energy's Multiwell...Wasatch and the Green River formations...mineralogy of the Green River Formation...in 1995. His current research interests...He has done internships and contract...

Dorothy F. Payne; Kagan Tuncay; Anthony Park; John B. Comer; Peter Ortoleva

338

Depositional environment of lower Green River Formation sandstones (Eocene), Red Wash field (Uinta Basin), Uintah County, Utah  

E-Print Network [OSTI]

control on reservoir properties, and predict reservoir geometry and morphology. This thesis follows the f'ormat and style nf the American Associa- tion of Petroleum Geolo ists Bulletin. WYOMING UTAH MO?T U i N T~ ~WASATCH MTS. /y 8'G ROOSEVELT...

McClain, Anthony Scott

2012-06-07T23:59:59.000Z

339

Surface wave phase velocities of the Western United States from a two-station method  

Science Journals Connector (OSTI)

......Columbia Plateau flood basalts, HLP and...Rio Grande Rift), Colorado Plateau, WF (Wasatch...Rocky Mountains in Colorado, possibly reflecting...the Columbia River flood basalts to the east...the Columbia River flood basalts and the northeastern...colocated with the Colorado Plateau, possibly......

Anna Foster; Gran Ekstrm; Meredith Nettles

2014-01-01T23:59:59.000Z

340

Notice of Comment Period for the Klondike III/Biglow Canyon Wind Integration EIS (DOE/EIS-0374) (12/06/05)  

Broader source: Energy.gov (indexed) [DOE]

635 Federal Register 635 Federal Register / Vol. 70, No. 233 / Tuesday, December 6, 2005 / Notices Program activity Performance goals * Cost Goals * Efficiency Environmental Advanced Power Systems ............. 45-50% higher heating value (HHV) efficiency to electricity by 2010 Multi-product capability (e.g. power and hydrogen) with over 60% efficiency by 2015 Sulfur Dioxide (SO 2 ): >99% removal NO X : < 0.01 lb/million Btu Hg: >90% removal Carbon Diox- ide (CO 2 ) capture: >90% 2012 goal: <10% increase in cost of electricity services in zero emission advanced gasification plants integrated with carbon sequestration. Carbon Sequestration .................... Efficiency of current and new plants consistent with cost of electricity target 90% CO 2 capture and sequestra-

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


341

U.S. Environmental Protection Agency Notice of Availability (DOE/EIS-0374: Klondike III/Biglow Canyon Wind Integration Project - September 2006)  

Broader source: Energy.gov (indexed) [DOE]

463 Federal Register 463 Federal Register / Vol. 71, No. 184 / Friday, September 22, 2006 / Notices Grand Mesa, Uncompahgre and Gunnison National Forests, Gunnison County, CO. Summary: No formal comment letter was sent to the preparing agency. EIS No. 20060267, ERP No. F-BLM- K65290-CA, Ukiah Resource Management Plan, Implementation, Several Counties, CA. Summary: EPA does not object to the selected actions, and believes that the management actions presented in the Resource Management Plan will minimize human exposure to naturally occurring asbestos (NOA) within the jurisdiction of the Ukiah Field Office. EIS No. 20060320, ERP No. F-NRC- F06026-IL, Early Site Permit (ESP) at the Exelon ESP Site, Application for ESP on One Additional Nuclear Unit, within the Clinton Power Station

342

Notice of Comment Period for the Klondike III/Biglow Canyon Wind Integration EIS (DOE/EIS-0374) (12/06/05)  

Broader source: Energy.gov (indexed) [DOE]

635 Federal Register 635 Federal Register / Vol. 70, No. 233 / Tuesday, December 6, 2005 / Notices Program activity Performance goals * Cost Goals * Efficiency Environmental Advanced Power Systems ............. 45-50% higher heating value (HHV) efficiency to electricity by 2010 Multi-product capability (e.g. power and hydrogen) with over 60% efficiency by 2015 Sulfur Dioxide (SO 2 ): >99% removal NO X : < 0.01 lb/million Btu Hg: >90% removal Carbon Diox- ide (CO 2 ) capture: >90% 2012 goal: <10% increase in cost of electricity services in zero emission advanced gasification plants integrated with carbon sequestration. Carbon Sequestration .................... Efficiency of current and new plants consistent with cost of electricity target 90% CO 2 capture and sequestra-

343

Report of Energy Efficiency Study and Metering/Utilities Profile for Electricity Deregulation at West Texas A&M University (WTAMU) Canyon, Texas  

E-Print Network [OSTI]

water is supplied to the campus loop. Recommended Energy Measures 1. Optimize ChW pumping system operation. 2. Balance the ChW loop. 11 Electricity Deregulation Metering Options Whole Campus Metering The WTAMU campus is served by two primary substations... system receives pulse data from both of the main electrical substations. The KYZ pulse from the north sub-station is direct wired to the powerhouse DDC panel and the south sub-station pulse is wired to the DDC panel in the Activity Center. WTAMU...

Zhu, Y.; Bryant, J.; Turner, W. D.; Claridge, D. E.

1999-01-01T23:59:59.000Z

344

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico, Class III  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program based on advanced reservoir management methods can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry.

Murphy, Michael B.

2002-02-21T23:59:59.000Z

345

Advanced Oil Recovery Technologies for Improved Recovery From Slope Basin Clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico  

SciTech Connect (OSTI)

The overall goal of this project is to demonstrate that an advanced development drilling and pressure maintenance program based on advanced reservoir management methods can significantly improve oil recovery. The plan included developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced methods. A key goal is to transfer advanced methodologies to oil and gas producers in the Permian Basin and elsewhere, and throughout the US oil and gas industry.

Mark B. Murphy

1998-04-30T23:59:59.000Z

346

Advanced Oil Recovery Technologies for Improved Recovery From Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico  

SciTech Connect (OSTI)

The overall goal of this project is to demonstrate that an advanced development drilling and pressure maintenance program based on advanced reservoir management methods can significantly improve oil recovery. The plan included developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced methods. A key goal is to transfer advanced methodologies to oil and gas producers in the Permian Basin and elsewhere, and throughout the US oil and gas industry.

Mark B. Murphy

1997-04-30T23:59:59.000Z

347

Selected growth and interaction characteristics of seafloor faults in the central Mississippi Canyon Offshore Continental Shelf (OCS) area, northern Gulf of Mexico  

E-Print Network [OSTI]

for dealing with potentially active seafloor faults is avoidance?placing the seafloor facility, structure foundation, pilings, or pipeline in such a way that the potential for damage to the infrastructure is well within design limits for the design lifetime...

Wegner, Scott Ashley

2006-08-16T23:59:59.000Z

348

Evaluate Potential Means of Rebuilding Sturgeon Populations in the Snake River between Lower Granite and Hells Canyon Dams, 2000 Annual Report.  

SciTech Connect (OSTI)

The specific research goal of this project is to identify means to restore and rebuild the Snake River white sturgeon (Acipenser transmontanus) population to support a sustainable annual subsistence harvest equivalent to 5 kg/ha/yr (CBFWA 1997). Based on data collected, a white sturgeon adaptive management plan will be developed. This 2000 annual report covers the fourth year of sampling of this multi-year study. In 2000 white sturgeon were captured, marked, and population data were collected in the Snake and Salmon rivers. The Snake River was sampled between Lower Granite Dam (rkm 174) and the mouth of the Salmon River (rkm 303), and the Salmon River was sampled from its mouth upstream to Hammer Creek (rkm 84). A total of 53,277 hours of setline effort and 630 hours of hook-and-line effort was employed in 2000. A total of 538 white sturgeon were captured and tagged in the Snake River and 25 in the Salmon River. Since 1997, 32.8 percent of the tagged white sturgeon have been recaptured. In the Snake River, white sturgeon ranged in total length from 48 cm to 271 cm and averaged 107 cm. In the Salmon River, white sturgeon ranged in total length from 103 cm to 227 cm and averaged 163 cm. Using the Jolly-Seber open population estimator, the abundance of white sturgeon <60 cm, between Lower Granite Dam and the mouth of the Salmon River, was estimated at 2,725 fish, with a 95% confidence interval of 1,668-5,783. A total of 10 white sturgeon were fitted with radio-tags. The movement of these fish ranged from 54.7 km (34 miles) downstream to 78.8 km (49 miles) upstream; however, 43.6 percent of the detected movement was less than 0.8 km (0.5 mile). Both radio-tagged fish and recaptured white sturgeon in Lower Granite Reservoir appear to move more than fish in the free-flowing segment of the Snake River. No seasonal movement pattern was detected, and no movement pattern was detected for different size fish. Differences were detected in the length frequency distributions of white sturgeon in Lower Granite Reservoir and the free-flowing Snake River (Chi-Square test, P<0.05). The proportion of white sturgeon greater than 92 cm (total length) in the free-flowing Snake River has shown an increase of 31 percent since the 1970's. Analysis of the length-weight relationship indicated that white sturgeon in Lower Granite Reservoir had a higher relative weight factor than white sturgeon in the free-flowing Snake River. A von Bertalanffy growth curve was fitted to 138 aged white sturgeon. The results suggests fish are currently growing faster than fish historically inhabiting the study area, as well as other Columbia River basin white sturgeon populations. Artificial substrate mats were used to document white sturgeon spawning. A total of 34 white sturgeon eggs were recovered: 27 in the Snake River, and seven in the Salmon River.

Everett, Scott R.; Tuell, Michael A. (Nez Perce Tribe, Department of Fishereis Resource Management, Lapwai, ID)

2003-03-01T23:59:59.000Z

349

Advanced Oil Recovery Technologies for Improved Recovery from Slope Basin Clastic Reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, New Mexico, Class III  

SciTech Connect (OSTI)

The overall objective of this project was to demonstrate that a development program-based on advanced reservoir management methods-can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan included developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals were (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the U.S. oil and gas industry.

Murphy, Mark B.

2002-01-16T23:59:59.000Z

350

Simulation of the Impact of the SO2 Emissions from the Proposed Sithe Power Plant on the Grand Canyon and other Class I Areas  

E-Print Network [OSTI]

to simulate the proposed and existing power plant plumes during January 2001. Four-km MM5 wind fields wereSimulation of the Impact of the SO2 Emissions from the Proposed Sithe Power Plant on the Grand. Rodriguez Abstract A 1500 MW coal-fired power plant is proposed to be built by Sithe Energies Inc

Fischer, Emily V.

351

Characterization of the 3-D Properties of the Fine-Grained Turbidite 8 Sand Reservoir, Green Canyon 18, Gulf of Mexico  

E-Print Network [OSTI]

-grained turbidity currents is composed of alternating sand and shale layers, whose extension is assumed to be large. They correspond to levee and overbank deposits that are usually associated to channel systems. The high porosity values, coming from unconsolidated...

Plantevin, Matthieu Francois

2004-09-30T23:59:59.000Z

352

Regional characteristics, timing, and significance of dissolution and collapse features in Lower Cretaceous carbonate platform strata, Desoto Canyon area, offshore Alabama-Florida  

E-Print Network [OSTI]

Crust ts rasota Arch Continental Crust Thick r s ional I'ust miles 100 200 0 100 200 km Boundaries between crustal types Figure 4. Structure map of the Pre-Louann basement in the study area. The map also shows the study area in relation... Cretaceous Unconformity James Limestone~ WILCOX MIOINAY Cl yl SELT IA McSh L r Euraw Tuacalooaa W P WILCOX Cia lon R play Bl fao n EUIaw I Ecalooaa L C *I 68 TARE TNANET141 rr / NF/ 1NN our clA/ CENO/ I N AN 3/ 6 r Paleocene...

Iannello, Christine

2012-06-07T23:59:59.000Z

353

Processes Influencing the Diversity of Middle Permian Brachiopods in the Bell Canyon Formation of the Delaware Basin (West Texas, Guadalupe Mountains National Park)  

E-Print Network [OSTI]

be recessive; thin-bedded to medium bedded, no sedimentary structure observed, usually iron- stained, chert nodules or layers, can weather to platy or wavy usually between 2 and 10 cm, but can also be up to 15 cm or a thin as 1 cm, usually... to wavy laminations, normally graded, or structureless, chert in nodules and layers, commonly petroliferous, weathers platy, rubbly, slabby, or massive, grainy areas of fossils not necessarily lens shape or in stringers, occasionally...

Fall, Leigh Margaret

2011-10-21T23:59:59.000Z

354

Evaluate Potenial Means of Rebuilding Sturgeon Populations in the Snake River between Lower Granite and Hells Canyon Dams, 2002 Annual Report.  

SciTech Connect (OSTI)

The specific research goal of this project is to identify means to restore and rebuild the Snake River white sturgeon (Acipenser transmontanus) population to support a sustainable annual subsistence harvest equivalent to 5 kg/ha/yr (CBFWA 1997). Based on data collected, a white sturgeon adaptive management plan will be developed. This report presents a summary of results from the 1997-2002 Phase II data collection and represents the end of phase II. From 1997 to 2001 white sturgeon were captured, marked, and population data were collected in the Snake and Salmon. A total of 1,785 white sturgeon were captured and tagged in the Snake River and 77 in the Salmon River. Since 1997, 25.8 percent of the tagged white sturgeon have been recaptured. Relative density of white sturgeon was highest in the free-flowing segment of the Snake River, with reduced densities of fish in Lower Granite Reservoir, and low densities the Salmon River. Differences were detected in the length frequency distributions of white sturgeon in Lower Granite Reservoir, the free-flowing Snake River and the Salmon River (Chi-Square test, P<0.05). The proportion of white sturgeon greater than 92 cm (total length) in the free-flowing Snake River has shown an increase of 30 percent since the 1970's. Using the Jolly-Seber model, the abundance of white sturgeon <60 cm, between Lower Granite Dam and the mouth of the Salmon River, was estimated at 2,483 fish, with a 95% confidence interval of 1,208-7,477. Total annual mortality rate was estimated to be 0.14 (95% confidence interval of 0.12 to 0.17). A total of 35 white sturgeon were fitted with radio-tags during 1999-2002. The movement of these fish ranged from 53 km (33 miles) downstream to 77 km (48 miles) upstream; however, 38.8 percent of the detected movement was less than 0.8 km (0.5 mile). Both radio-tagged fish and recaptured white sturgeon in Lower Granite Reservoir appear to move more than fish in the free-flowing segment of the Snake River. No seasonal movement pattern was detected, and no movement pattern was detected for different size fish. Analysis of the length-weight relationship indicated that white sturgeon in Lower Granite Reservoir had a higher relative weight factor than white sturgeon in the free-flowing Snake River. The results suggest fish are currently growing faster than fish historically inhabiting the study area, as well as other Columbia River basin white sturgeon populations. Artificial substrate egg mats documented white sturgeon spawning in four consecutive years. A total of 49 white sturgeon eggs were recovered in the Snake River from 1999-2002, and seven from the Salmon River during 2000.

Everett, Scott R.; Tuell, Michael A.; Hesse, Jay A. (Nez Perce Tribe, Department of Fisheries Management, Lapwai, ID)

2004-02-01T23:59:59.000Z

355

Structural and stratigraphic evolution of the central Mississippi Canyon Area: interaction of salt tectonics and slope processes in the formation of engineering and geologic hazards  

E-Print Network [OSTI]

. The analysis focused on salt tectonics and sequence stratigraphy to develop a geologic model for the study area and its potential impact on engineering and geologic hazards. Salt in the study area was found to be established structural end-members derived from...

Brand, John Richard

2006-04-12T23:59:59.000Z

356

Evaluate Potential Means of Rebuilding Sturgeon Populations in the Snake River between Lower Granite and Hells Canyon Dams, 2001 Annual Report.  

SciTech Connect (OSTI)

The specific research goal of this project is to identify means to restore and rebuild the Snake River white sturgeon (Acipenser transmontanus) population to support a sustainable annual subsistence harvest equivalent to 5 kg/ha/yr (CBFWA 1997). Based on data collected, a white sturgeon adaptive management plan will be developed. This 2001 annual report covers the fifth year of sampling of this multi-year study. In 2001 white sturgeon were captured, marked, and population data were collected in the Snake and Salmon rivers. The Snake River was sampled between Lower Granite Dam (rkm 174) and the mouth of the Salmon River (rkm 303), and the Salmon River was sampled from its mouth upstream to Hammer Creek (rkm 84). A total of 45,907 hours of setline effort and 186 hours of hook-and-line effort was employed in 2001. A total of 390 white sturgeon were captured and tagged in the Snake River and 12 in the Salmon River. Since 1997, 36.1 percent of the tagged white sturgeon have been recaptured. In the Snake River, white sturgeon ranged in total length from 42 cm to 307 cm and averaged 107 cm. In the Salmon River, white sturgeon ranged in total length from 66 cm to 235 cm and averaged 160 cm. Using the Jolly-Seber model, the abundance of white sturgeon <60 cm, between Lower Granite Dam and the mouth of the Salmon River, was estimated at 2,483 fish, with a 95% confidence interval of 1,208-7,477. An additional 10 white sturgeon were fitted with radio-tags during 2001. The locations of 17 radio-tagged white sturgeon were monitored in 2001. The movement of these fish ranged from 38.6 km (24 miles) downstream to 54.7 km (34 miles) upstream; however, 62.6 percent of the detected movement was less than 0.8 km (0.5 mile). Both radio-tagged fish and recaptured white sturgeon in Lower Granite Reservoir appear to move more than fish in the free-flowing segment of the Snake River. No seasonal movement pattern was detected, and no movement pattern was detected for different size fish. Differences were detected in the length frequency distributions of white sturgeon in Lower Granite Reservoir and the free-flowing Snake River (Chi-Square test, P<0.05). The proportion of white sturgeon greater than 92 cm (total length) in the free-flowing Snake River has shown an increase of 30 percent since the 1970's. Analysis of the length-weight relationship indicated that white sturgeon in Lower Granite Reservoir had a higher relative weight factor than white sturgeon in the free-flowing Snake River. A von Bertalanffy growth curve was fitted to 309 aged white sturgeon. The results suggest fish are currently growing faster than fish historically inhabiting the study area, as well as other Columbia River basin white sturgeon populations. Artificial substrate mats were used to document white sturgeon spawning. A total of 14 white sturgeon eggs were recovered in the Snake River in 2001.

Everett, Scott R.; Tuell, Michael A. (Nez Perce Tribe, Department of Fisheries Resource Management, Lapwai, ID)

2003-03-01T23:59:59.000Z

357

Evaluate Potential Means of Rebuilding Sturgeon Populations in the Snake River between Lower Granite and Hells Canyon Dams, 1999 Annual Report.  

SciTech Connect (OSTI)

The specific research goal of this project is to identify means to restore and rebuild the Snake River white sturgeon (Acipenser transmontanus) population to support a sustainable annual subsistence harvest equivalent to 5 kg/ha/yr (CBFWA 1997). Based on data collected, a white sturgeon adaptive management plan will be developed. This 1999 annual report covers the third year of sampling of this multi-year study. In 1999 white sturgeon were captured, marked and population data were collected in the Snake and Salmon rivers. A total of 33,943 hours of setline effort and 2,112 hours of hook-and-line effort was employed in 1999. A total of 289 white sturgeon were captured and tagged in the Snake River and 29 in the Salmon River. Since 1997, 11.1 percent of the tagged white sturgeon have been recaptured. In the Snake River, white sturgeon ranged in total length from 27 cm to 261 cm and averaged 110 cm. In the Salmon River, white sturgeon ranged in total length from 98 cm to 244 cm and averaged 183.5 cm. Using the Jolly-Seber model, the abundance of white sturgeon < 60 cm, between Lower Granite Dam and the mouth of the Salmon River, was estimated at 1,823 fish, with a 95% confidence interval of 1,052-4,221. A total of 15 white sturgeon were fitted with radio-tags. The movement of these fish ranged from 6.4 km (4 miles) downstream to 13.7 km (8.5 miles) upstream; however, 83.6 percent of the detected movement was less than 0.8 kilometers (0.5 miles). Both radio-tagged fish and recaptured white sturgeon in Lower Granite Reservoir appear to move more than fish in the free-flowing segment of the Snake River. No seasonal movement pattern was detected, and no movement pattern was detected for different size fish. Differences were detected in the length frequency distributions of white sturgeon in Lower Granite Reservoir and the free-flowing Snake River (Chi-Square test, P < 0.05). The proportion of white sturgeon greater than 92 cm (total length) in the free-flowing Snake River has shown an increase of 29 percent since the 1970's. Analysis of the length-weight relationship indicated that white sturgeon in Lower Granite Reservoir were slightly larger than white sturgeon in the free-flowing Snake River. A von Bertalanffy growth curve was fitted to 49 aged white sturgeon. The results suggests the fish are currently growing faster than fish historicly inhabiting the study area, as well as other Columbia River basin white sturgeon populations. Artificial substrate mats were used to document white sturgeon spawning. Five white sturgeon eggs were recovered in the Snake River.

Tuell, Michael A.; Everett, Scott R. (Nez Perce Tribe, Department of Fisheries Resource Management, Lapwai, ID)

2003-03-01T23:59:59.000Z

358

Solar Resource Measurements in Canyon, Texas - Equipment Only Loan: Cooperative Research and Development Final Report, CRADA Number CRD-07-233  

SciTech Connect (OSTI)

Site-specific, long-term, continuous, and high-resolution measurements of solar irradiance are important for developing renewable resource data. These data are used for several research and development activities consistent with the NREL mission: establish a national 30-year climatological database of measured solar irradiances; provide high-quality ground-truth data for satellite remote sensing validation; support development of radiative transfer models for estimating solar irradiance from available meteorological observations; and provide solar resource information needed for technology deployment and operations. Data acquired under this agreement will be available to the public through NREL's Measurement & Instrumentation Data Center (MIDC) or the Renewable Resource Data Center (RReDC). The MIDC offers a variety of standard data display, access, and analysis tools designed to address the needs of a wide user audience (e.g., industry, academia, and government interests).

Andreas, A.

2014-07-01T23:59:59.000Z

359

Facies analysis of the Caballero Formation and the Andrecito Member of the Lake Valley Formation (Mississippian): implications for Waulsortian bioherm inception, Alamo Canyon area, Sacramento Mountains, New Mexico  

E-Print Network [OSTI]

sequence in which packstones and grainstones accumulated as localized in situ skeletal buildups. General facies trends indicate that deposition occured on a ramp with packstones and coarser clastics in the shallower, northern area, gradually changing... thinning of the lower Andrecito siliciclastic-rich facies; and 3) associated occurrences of upper Andrecito skeletal buildups. These trends lie parallel to basement block boundaries inferred from younger (Pennnsylvanian) structures, Sequence isopach...

Byrd, Thomas Martin

2012-06-07T23:59:59.000Z

360

Predicting spatial distribution of critical pore types and their influence on reservoir quality, Canyon (Pennsylvanian) Reef reservoir, Diamond M field, Texas  

E-Print Network [OSTI]

of the phylloid algal pioneer community. Approximately 50-60% of all rocks described in this study were classified as phylloid algal dominated automicritic reef facies. The remaining rocks consist of detrital (mainly skeletal) packstones and grainstones...; skeletal grains consist of algae fragments, bivalves, brachiopods, bryozoans, crinoids, forams (pellets, benthic, and encrusting), fusulinids, gastropods, sponge spicules and rare trilobite shells. Non-skeletal grains consisting of micritic clasts...

Fisher, Aaron Jay

2007-04-25T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


361

acid  

Office of Legacy Management (LM)

Acid/Pueblo Canyon, New Mexico, Site is Acid/Pueblo Canyon, New Mexico, Site is located near the town of Los Alamos, New Mexico, approximately 25 miles northwest of Santa Fe and 60 miles north-northeast of Albuquerque. The site is accessible from Canyon Road, which runs just south of the former waste treatment plant. The plant was situated on a mesa that forms the south rim of Acid Canyon. Acid Canyon is a small tributary near the head

362

CALIFORNIA STATE UNIVERSITY, FULLERTON INSTITUTIONAL RESEARCH AND ANALYTICAL STUDIES  

E-Print Network [OSTI]

% CYPRESS 143 5% SANTIAGO CANYON 128 4% SANTIAGO CANYON 120 5% IRVINE VALLEY 125 4% IRVINE VALLEY 107 4% GOLDEN WEST 124 4% GOLDEN WEST 137 5% COASTLINE 43 1% COASTLINE 26 1% TOTAL 1888 62% TOTAL 1541 58% LOS

de Lijser, Peter

363

CALIFORNIA STATE UNIVERSITY, FULLERTON INSTITUTIONAL RESEARCH AND ANALYTICAL STUDIES  

E-Print Network [OSTI]

% CYPRESS 114 6% SANTIAGO CANYON 167 4% SANTIAGO CANYON 90 4% IRVINE VALLEY 155 4% IRVINE VALLEY 87 4% GOLDEN WEST 139 3% GOLDEN WEST 80 4% COASTLINE 45 1% COASTLINE 25 1% TOTAL 2289 57% TOTAL 1190 59% LOS

de Lijser, Peter

364

Precision engineering: an evolutionary perspective  

Science Journals Connector (OSTI)

...sizes, Fresnels for solar concentrators, camera...Canyon, in northern New Mexico, has solar and lunar markings...Sinclair 1979 A unique solar marking construct. Science...Chaco Canyon, New Mexico. Archaeoastronomy in...

2012-01-01T23:59:59.000Z

365

Land and sea study of the northeastern golfe du Lion rifted margin: the Oligocene Miocene of southern Provence (Nerthe area, SE France)  

Science Journals Connector (OSTI)

...facies is characterized by semi-continuous, high amplitude...and Saint Tropez canyons - a submersible study. - Mar. Geol. , 27...Saint-Tropez canyons - A submersible study. - Mar. Geol. , 27...and southern Peri-Tethys platforms and the intermediate domains...

Julien Oudet; Philippe Mnch*; Jean Borgomano; Frdric Quillevere; Mihaela C. Melinte-Dobrinescu; Franois Demory; Sophie Viseur; Jean-Jacques Cornee

366

Inversion of Waveforms For Extreme Source Models With an Application to the Isotropic Moment Tensor Component  

Science Journals Connector (OSTI)

......component) in the source. Synthetic tests were used to examine the effect...structure of Silent Canyon caldera, Nevada Test Site, Bull. seism. Soc. Am., 77...structure of Silent Canyon caldera, Nevada Test Site, Bull. sebm. SOC. Am., 77......

D. W. Vasco; L. R. Johnson

1989-04-01T23:59:59.000Z

367

U.S. Department of Energy Categorical Exclusion ...  

Broader source: Energy.gov (indexed) [DOE]

H Canyon exhaust tunnel could result in a ground level release of Canyon (sand filtered) air following: 1) a PC2 seismic event and 2) the collapse of the 291-H stack liner. To...

368

CX-012175: Categorical Exclusion Determination | Department of...  

Broader source: Energy.gov (indexed) [DOE]

H Canyon exhaust tunnel could result in a ground level release of Canyon (sand filtered) air following: 1) a PC2 seismic event and 2) the collapse of the 291-H stack liner. To...

369

This Week In Petroleum Summary Printer-Friendly Version  

Annual Energy Outlook 2013 [U.S. Energy Information Administration (EIA)]

4 5,822 2010 2013 Dalmatian Murphy Desoto Canyon 48 5,876 2008 2013 Knotty Head Nexen Green Canyon 512 3,557 2005 2013 Big Foot Chevron Walker Ridge 29 5,235 2005 2014 Entrada...

370

Winter 2004 |1 celebrating natural resourcesU N I V E R S I T Y O F I D A H O | C o l l e g e o f N a t u r a l R e s o u r c e sWinter 2004 | Volume 21 Number 1  

E-Print Network [OSTI]

's Historical Legacy 7 Shattuck -- First Four-Year forestry Degree Program 7 McArdle, Bingham and Wellner 10, the groves of giant sequoias and the redwoods, the Canyon of the Colorado, the Canyon of the Yellowstone

Wellner, Jon A.

371

Demography, movement patterns, and mating system of leopard sharks (Triakis semifasciata) aggregating along the open coast of southern California, USA  

E-Print Network [OSTI]

Canyon, La Jolla, California, USA. Oral paper presented atMinneapolis, MN, USA. *Samuel H. Gruber Award for BestCanyon, La Jolla, California, USA. Oral paper presented at

Nosal, Andrew Phillip

2013-01-01T23:59:59.000Z

372

acid  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Acid/Pueblo Canyon, New Mexico, Site. Acid/Pueblo Canyon, New Mexico, Site. This site is managed by the U.S. Department of Energy Office of Legacy Management. Site Description and History The Acid/Pueblo Canyon, New Mexico, Site is located near the town of Los Alamos, New Mexico, approximately 25 miles northwest of Santa Fe and 60 miles north-northeast of Albuquerque. The site is accessible from Canyon Road, which runs just south

373

Mycena News The Mycological Society of San Francisco October, 2006, vol 57:10  

E-Print Network [OSTI]

in Tlaxcala and the Copper Canyon . MycoDigest: Mushrooms in the Waves Else Vellinga For showy mushrooms

California at Berkeley, University of

374

Introduction Latin American Map: You set the  

E-Print Network [OSTI]

: Copper Canyon © T. M. Whitmore #12;4: Coastal Plain looking E towards Sierra Madre Occidental © T. M

Lopez-Carr, David

375

U.S. Department of the Interior October 2013 U.S. Geological Survey  

E-Print Network [OSTI]

.'s (South Jordan, UT) Bingham Canyon Mine, near Salt Lake City, UT, also contributed to the lower domestic

376

University of Rhode Island inAdvance October 12, 2006  

E-Print Network [OSTI]

, a videographer, the students visited the Bingham Canyon copper mine in the Salt Lake area, saw Old Faithful spout

Rhode Island, University of

377

Updated Apr 2014 CURRICULUM VITAE  

E-Print Network [OSTI]

American Mine Services, for Kennecott Utah Copper Corp and Rio Tinto, at Bingham Canyon Mine, Utah, Dec

Yang, Zong-Liang

378

U.S. Department of the Interior August 2013 U.S. Geological Survey  

E-Print Network [OSTI]

Copper Corp.'s Bingham Canyon Mine after a rock slide on April 10 halted output. Mining of ore restarted

379

U.S. Department of the Interior July 2013 U.S. Geological Survey  

E-Print Network [OSTI]

that in March following the April 10 rock slide at Kennecott Utah Copper Corp.'s Bingham Canyon Mine. (See

380

Page 1 of 3 Rio Tinto Kennecott  

E-Print Network [OSTI]

the Bingham Canyon Mine, one of the largest copper mines in the world. Scholarship Details Rio Tinto Kennecott

van den Berg, Jur

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


381

U.S. Department of the Interior April 2013 U.S. Geological Survey  

E-Print Network [OSTI]

, where production at Kennecott Utah Copper's Bingham Canyon Mine decreased by 32,000 metric tons (t

382

U.S. Department of the Interior May 2013 U.S. Geological Survey  

E-Print Network [OSTI]

Corp.'s (subsidiary of Rio Tinto plc) Bingham Canyon Mine, 48 kilometers southwest of Salt Lake City

383

U.S. Department of the Interior February 2013 U.S. Geological Survey  

E-Print Network [OSTI]

production at the Bingham Canyon Mine in Utah. (See Copper in October 2012). Average daily refined copper

384

U.S. Department of the Interior May 2013 U.S. Geological Survey  

E-Print Network [OSTI]

Utah Copper Corp.'s (subsidiary of Rio Tinto plc) Bingham Canyon Mine, 48 kilometers southwest of Salt

385

U.S. Department of the Interior January 2013 U.S. Geological Survey  

E-Print Network [OSTI]

the fourth quarter 2012, mine production at the Bingham Canyon Mine in Utah was 38% higher and downstream

386

U.S. Department of the Interior June 2013 U.S. Geological Survey  

E-Print Network [OSTI]

for the first quarter of 2013 from its Bingham Canyon Mine in Utah, which can fluctuate significantly from month

387

Geomorphology and morphometric characteristics of alluvial fans, Guadalupe Mountains National Park and adjacent areas, west Texas and New Mexico  

E-Print Network [OSTI]

............................................................ 29 14 Alluvial fans along the Guadalupe Mountains in Big Dog Canyon........ 31 15 Alluvial fans along the Brokeoff Mountains in Big Dog Canyon........... 35 16 View of alluvial fans from their drainage basins.................................. 75 27 Salt Basin-Brokeoff Mountains alluvial fan group ................................. 76 28 Big Dog Canyon-Brokeoff Mountains alluvial fan group....................... 77 29 Big Dog Canyon-Guadalupe Mountains alluvial fan group...

Given, Jeffrey Lyle

2004-09-30T23:59:59.000Z

388

U.S. Department of the Interior January 2014 U.S. Geological Survey  

E-Print Network [OSTI]

Copper Corp.'s Bingham Canyon Mine in Utah, where production recovered faster than expected after a rock

389

National uranium resource evaluation: Sheridan Quadrangle, Wyoming and Montana  

SciTech Connect (OSTI)

The Sheridan Quadrangle of north-central Wyoming was evaluated for uranium favorability according to specific criteria of the National Uranium Resource Evaluation program. Procedures consisted of geologic and radiometric surveys; rock, water, and sediment sampling; studying well logs; and reviewing the literature. Five favorable environments were identified. These include portions of Eocene Wasatch and Upper Cretaceous Lance sandstones of the Powder River Basin and Lower Cretaceous Pryor sandstones of the Bighorn Basin. Unfavorable environments include all Precambrian, Cambrian, Ordovician, Permian, Triassic, and Middle Jurassic rocks; the Cretaceous Thermopolis, Mowry, Cody, Meeteetse, and Bearpaw Formations; the Upper Jurassic Sundance and Morrison, the Cretaceous Frontier, Meseverde, Lance, and the Paleocene Fort Union and Eocene Willwood Formations of the Bighorn Basin; the Wasatch Formation of the Powder River Basin, excluding two favorable areas and all Oligocene and Miocene rocks. Remaining rocks are unevaluated.

Damp, J N; Jennings, M D

1982-04-01T23:59:59.000Z

390

Research on Chrysomelidae, Volume 2, pp. 131151, Koninklijke Brill, Leiden, 2009 Flea beetle diversity of the Sierra Tarahumara, Copper  

E-Print Network [OSTI]

diversity of the Sierra Tarahumara, Copper Canyon, Mexico (Chrysomelidae: Alticinae)1 Plates 27­32 David G Tarahumara (Copper Canyon or Barranca del Cobre), a section of the Sierra Madre Occidental of Chihuahua. The biogeographical affinities and host plants of the Copper Canyon Alticinae are also discussed. Resumen. Este

Mathis, Wayne N.

391

52 WILDCAT CREEK --A SCIENTIFIC STUDY Bank and Terrace Condition by Reach  

E-Print Network [OSTI]

, revetted, and stable banks were measured and graphed for the Upper Alluvial Plain and Lower Canyon Segments for each segment. About 35% more revetments exist in the Upper Alluvial Plain than intheLowerCanyon,whereastheCanyonhas33%morelengthoferod- ing bank than the Upper Alluvial Plain. The Lower Canyon has 2% more stable

392

U.S. Department of the Interior U.S. Geological Survey  

E-Print Network [OSTI]

Tributaries of the Colorado River in Grand Canyon Introduction Sediment supply and transport in Grand Canyon is an important management issue because of the presence and operation of Glen Canyon Dam on the Colorado River (U have been limited to major tributaries, such as the Paria and Little Colorado Rivers and Kanab

393

Performance Measurement in Small Texas Metropolitan Planning Organizations  

E-Print Network [OSTI]

for Planning (CMAP) all of which house populations of over 1.5 million residents. Medium sized MPOs include: Wasatch Front Regional Council (WFRC) in Utah, Metroplan in Arkansas, and Metropolitan Area Planning Agency (MAPA) in Nebraska which all have... ? www.wfrc.org/cms/index.php?option=com_content&view=article&id=92&Itemi d=78 ? Metroplan ? www.metroplan.org/index.php?fuseaction=p0007.&mod=44 ? MAPA ? www.mapacog.org/long-range-transportation-planning ? Collier County MPO ? www...

Moore, Devin 1984-

2012-10-16T23:59:59.000Z

394

Gas Mileage of 2005 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

5 GMC Vehicles 5 GMC Vehicles EPA MPG MODEL City Comb Hwy 2005 GMC Canyon 2WD 4 cyl, 2.8 L, Automatic 4-spd, Regular Gasoline Compare 2005 GMC Canyon 2WD View MPG Estimates Shared By Vehicle Owners 16 City 18 Combined 23 Highway 2005 GMC Canyon 2WD 4 cyl, 2.8 L, Manual 5-spd, Regular Gasoline Compare 2005 GMC Canyon 2WD View MPG Estimates Shared By Vehicle Owners 18 City 21 Combined 24 Highway 2005 GMC Canyon 2WD 5 cyl, 3.5 L, Automatic 4-spd, Regular Gasoline Compare 2005 GMC Canyon 2WD 16 City 18 Combined 22 Highway 2005 GMC Canyon 2WD 5 cyl, 3.5 L, Manual 5-spd, Regular Gasoline Compare 2005 GMC Canyon 2WD 17 City 19 Combined 23 Highway 2005 GMC Canyon 4WD 4 cyl, 2.8 L, Automatic 4-spd, Regular Gasoline Compare 2005 GMC Canyon 4WD 15 City 17 Combined 21 Highway 2005 GMC Canyon 4WD 4 cyl, 2.8 L, Manual 5-spd, Regular Gasoline

395

Gas Mileage of 2006 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

6 GMC Vehicles 6 GMC Vehicles EPA MPG MODEL City Comb Hwy 2006 GMC Canyon 2WD 4 cyl, 2.8 L, Automatic 4-spd, Regular Gasoline Compare 2006 GMC Canyon 2WD 15 City 18 Combined 22 Highway 2006 GMC Canyon 2WD 4 cyl, 2.8 L, Manual 5-spd, Regular Gasoline Compare 2006 GMC Canyon 2WD View MPG Estimates Shared By Vehicle Owners 18 City 20 Combined 25 Highway 2006 GMC Canyon 2WD 5 cyl, 3.5 L, Automatic 4-spd, Regular Gasoline Compare 2006 GMC Canyon 2WD 17 City 19 Combined 22 Highway 2006 GMC Canyon 2WD 5 cyl, 3.5 L, Manual 5-spd, Regular Gasoline Compare 2006 GMC Canyon 2WD 17 City 19 Combined 23 Highway 2006 GMC Canyon 4WD 4 cyl, 2.8 L, Automatic 4-spd, Regular Gasoline Compare 2006 GMC Canyon 4WD 15 City 17 Combined 21 Highway 2006 GMC Canyon 4WD 4 cyl, 2.8 L, Manual 5-spd, Regular Gasoline

396

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM. Quarterly technical progress report, October 1--December 31, 1996 (fifth quarter)  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program--based on advanced reservoir management methods--can significantly improve oil recovery. The plan includes developing a control area using standard reservoir management techniques while comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program, can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the US oil and gas industry. Results so far are described on geology, engineering, 3-D seismic, reservoir characterization and simulation, and technology transfer.

NONE

1997-01-31T23:59:59.000Z

397

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM. Quarterly technical progress report, April 1, 1996--June 30, 1996  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program based on advanced reservoir management methods can significantly improve oil recovery. The demonstration plan includes developing a control area using standard reservoir management techniques and comparing the performance of the control area with an area developed using advanced reservoir management methods. Specific goals to attain the objective are: (1) to demonstrate that a development drilling program and pressure maintenance program, based on advanced reservoir management methods, can significantly improve oil recovery compared with existing technology applications, and (2) to transfer the advanced methodologies to oil and gas producers in the Permian Basin and elsewhere in the U.S. oil and gas industry.

Murphy, M.B.

1996-07-26T23:59:59.000Z

398

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM. Quarterly technical progress report, July 1--September 30, 1996 (fourth quarter)  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program based on advanced reservoir management methods can significantly improve oil recovery. The demonstration plan includes developing a control area using standard reservoir management techniques and comparing the performance of the control area with an area developed using advanced reservoir management methods. Specific goals to attain the objective are: (1) to demonstrate that a development drilling program and pressure maintenance program, based on advanced reservoir management methods, can significantly improve oil recovery compared with existing technology applications, and (2) to transfer the advanced methodologies to oil and gas producers in the Permian Basin and elsewhere in the US oil and gas industry. Results obtained to date are summarized on the following: geology, engineering, 3-D seismic, reservoir characterization and simulation, and technology transfer.

NONE

1996-10-31T23:59:59.000Z

399

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM. Quarterly technical progress report, January 1--March 31, 1998  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program--based on advanced reservoir management methods--can significantly improve oil recovery at the Nash Draw Pool (NDP). The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the US oil and gas industry. Results obtained to date are summarized for the following: geostatistics and reservoir mapping; reservoir engineering; reservoir characterization/reservoir simulation; miscible recovery simulations; and technology transfer.

NONE

1998-04-30T23:59:59.000Z

400

Advanced oil recovery technologies for improved recovery from slope basin clastic reservoirs, Nash Draw Brushy Canyon Pool, Eddy County, NM. Quarterly technical progress report (seventh quarter), April 1--June 30, 1997  

SciTech Connect (OSTI)

The overall objective of this project is to demonstrate that a development program -- based on advanced reservoir management methods -- can significantly improve oil recovery. The plan includes developing a control area using standard reservoir management techniques and comparing its performance to an area developed using advanced reservoir management methods. Specific goals are (1) to demonstrate that an advanced development drilling and pressure maintenance program can significantly improve oil recovery compared to existing technology applications and (2) to transfer these advanced methodologies to oil and gas producers in the Permian Basin and elsewhere throughout the US oil and gas industry. Results obtained to date are summarized.

NONE

1997-07-30T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


401

Type B Accident Investigation Board Report of the Plutonium Intake between August 4, 1996, and February 10, 1997, by a Crane Operator at the Savannah River Site F-Canyon  

Broader source: Energy.gov [DOE]

This report is an independent product of an accident investigation board appointed by Dr. Mario P. Fiori, Manager, Savannah River Operations Office, U.S. Department of Energy.

402

Notice of Intent To Prepare a Draft Environmental Impact Statement and Conduct Public Scoping on the Adoption of a Long-Term Experimental and Management Plan for the Operation of Glen Canyon Dam  

Broader source: Energy.gov (indexed) [DOE]

35 Federal Register 35 Federal Register / Vol. 76, No. 129 / Wednesday, July 6, 2011 / Notices should be 4-wheel drive and have heavy-duty tires due to the terrain. To sign on for the tour, contact Sherry Foot, Special Programs Coordinator, (801) 539-4195, no later than close of business July 25, 201l. On August 5, a business meeting will be held to discuss the ecological, social, and economic values that can be created by the proposed grazing strategy (follow-up to the field tour); RAC voting in support of the Rich County Project subgroup report; RAC subgroup report on the draft BLM Utah Instruction Memorandum on the Statewide Travel Management Planning Policy; Air Quality status update; a conference call with BLM's Director Abbey on the RAC's involvement with the America's

403

Characterization of oil and gas reservoirs and recovery technology deployment on Texas State Lands  

SciTech Connect (OSTI)

Texas State Lands oil and gas resources are estimated at 1.6 BSTB of remaining mobile oil, 2.1 BSTB, or residual oil, and nearly 10 Tcf of remaining gas. An integrated, detailed geologic and engineering characterization of Texas State Lands has created quantitative descriptions of the oil and gas reservoirs, resulting in delineation of untapped, bypassed compartments and zones of remaining oil and gas. On Texas State Lands, the knowledge gained from such interpretative, quantitative reservoir descriptions has been the basis for designing optimized recovery strategies, including well deepening, recompletions, workovers, targeted infill drilling, injection profile modification, and waterflood optimization. The State of Texas Advanced Resource Recovery program is currently evaluating oil and gas fields along the Gulf Coast (South Copano Bay and Umbrella Point fields) and in the Permian Basin (Keystone East, Ozona, Geraldine Ford and Ford West fields). The program is grounded in advanced reservoir characterization techniques that define the residence of unrecovered oil and gas remaining in select State Land reservoirs. Integral to the program is collaboration with operators in order to deploy advanced reservoir exploitation and management plans. These plans are made on the basis of a thorough understanding of internal reservoir architecture and its controls on remaining oil and gas distribution. Continued accurate, detailed Texas State Lands reservoir description and characterization will ensure deployment of the most current and economically viable recovery technologies and strategies available.

Tyler, R.; Major, R.P.; Holtz, M.H. [Univ. of Texas, Austin, TX (United States)] [and others

1997-08-01T23:59:59.000Z

404

Gas Mileage of 2008 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

8 GMC Vehicles 8 GMC Vehicles EPA MPG MODEL City Comb Hwy 2008 GMC Acadia AWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2008 GMC Acadia AWD View MPG Estimates Shared By Vehicle Owners 16 City 18 Combined 22 Highway 2008 GMC Acadia FWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2008 GMC Acadia FWD View MPG Estimates Shared By Vehicle Owners 16 City 19 Combined 24 Highway 2008 GMC Canyon 2WD 4 cyl, 2.9 L, Automatic 4-spd, Regular Gasoline Compare 2008 GMC Canyon 2WD View MPG Estimates Shared By Vehicle Owners 18 City 20 Combined 24 Highway 2008 GMC Canyon 2WD 4 cyl, 2.9 L, Manual 5-spd, Regular Gasoline Compare 2008 GMC Canyon 2WD 18 City 20 Combined 24 Highway 2008 GMC Canyon 2WD 5 cyl, 3.7 L, Automatic 4-spd, Regular Gasoline Compare 2008 GMC Canyon 2WD

405

Untitled-1  

Office of Legacy Management (LM)

fact sheet provides information about the Bayo Canyon, New Mexico, Site. fact sheet provides information about the Bayo Canyon, New Mexico, Site. This site is managed by the U.S. Department of Energy Office of Legacy Management. Site Description and History The Bayo Canyon, New Mexico, Site is located approx- imately 3 miles west of Los Alamos, New Mexico, 25 miles northwest of Santa Fe, and 60 miles north- northeast of Albuquerque. Partly in Los Alamos County

406

E-Print Network 3.0 - area endangered species Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of Land Management over Endangered Species Act violations connected to Grand Canyon uranium mining... flycatchers, have been added to the endangered species list, and...

407

CX-008642: Categorical Exclusion Determination | Department of...  

Broader source: Energy.gov (indexed) [DOE]

Determination CX-008642: Categorical Exclusion Determination H-Canyon Dissolver Corrosion Rate Assessment CX(s) Applied: B3.6 Date: 05252012 Location(s): South Carolina...

408

E-Print Network 3.0 - adrar mountains fishes Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Canyon Summary: Hills Grass Valley Black Mountain Cleghorn Lakes North Algodones Dunes Fish Creek Mountains Coyote... Crater Mountain Sheep Ridge White Mountains Great Falls Basin...

409

EIS-0374: Record of Decision | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

4: Record of Decision EIS-0374: Record of Decision Klondike III Biglow Canyon Wind Integration Project The Bonneville Power Administration (BPA) has decided to implement the...

410

EIS-0374: EPA Notice of Availability of the Final Environmental...  

Broader source: Energy.gov (indexed) [DOE]

of Availability of the Final Environmental Impact Statement Klondike III Biglow Canyon Wind Integration Project, Sherman County, Oregon Final EIS, BPA, OR, Klondike III Wind...

411

ENVIRONMENTAL REVIEW FOR CATEGORICAL EXCLUSION DETERMINATION  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Canyon 230-kV Transmission Line, Phase II San Juan National Forest, Montezuma County, Colorado A. Brief Description of Proposal: Western Area Power Administration (Western)...

412

ENVIRONMENTAL REVIEW FOR CATEGORICAL EXCLUSION DETERMINATION  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Curecanti-Lost Canyon 230-kV Reconductoring Project San Miguel County, Colorado A. Brief Description of Proposal: In 2013, Western Area Power Administration (Western) Maintenance...

413

ENVIRONMENTAL REVIEW FOR CATEGORICAL EXCLUSION DETERMINATION  

Broader source: Energy.gov (indexed) [DOE]

Administration Curecanti-Lost Canyon 230-kV Reconductoring Project San Miguel County, Colorado A. Brief Description of Proposal: In 2013, Western Area Power Administration...

414

Dispersion of Light and Heavy Pollutants in Urban Scale Models: CO2 Laser Photoacoustic Studies  

Science Journals Connector (OSTI)

The distribution of pollutants in two urban scale models (point emission source and street canyon with extensive transport) was investigated by means of CO2 laser...

Zelinger, Z; Strik, M; Kubt, P; Civi, S; Grigorov, E; Jane?kov, R; Zavila, O; Nevrl, V; Herecov, L; Bailleux, S; Hork, V; Ferus, M; Skrnsk, J; Kozubkov, M; Drbkov, S; Janour, Z

2009-01-01T23:59:59.000Z

415

EA-1980: Public Scoping Notice | Department of Energy  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

Canyon-Round Valley Access Road System Improvements, Custer County, Idaho Bonneville Power Administration announced that, jointly with the Bureau of Land Management (BLM), it is...

416

B O N N E V I L L E P O W E R A D M I N I S T R A T I O N Journal  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

megawatts from the proposed Juniper Canyon II Wind Project. To interconnect the project, BPA would build a new substation, the Wood Creek Substation, along an existing BPA...

417

EIS-0183: Record of Decision | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

interconnection to the FCRTS at BPA's Jones Canyon Substation in Gilliam County, Oregon. BPA will expand this existing substation and install new equipment at the substation to...

418

Reading Room | Department of Energy  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

November 2008). February 2009. Records of Decision on Bonneville Power Administration's (BPA0 Leaning Juniper II Wind Project and Jones Canyon Substation Expansion tiered to BPA's...

419

E-Print Network 3.0 - area surface debris Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

canyons Summary: in the study area. Soil-water repellency was measured using the critical surface tension method to determine... area (NCDC, 2003) were used to determine daily...

420

Wildfire Policy in Transition Yellowstone  

E-Print Network [OSTI]

Wildfire Policy in Transition 1910 #12;Yellowstone 1988 #12;Colorado South Canyon Fire 1994 #12;#12;Wildfire Policy in Transition 1910 #12;

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


421

Decision-making in Electricity Generation Based on Global Warming Potential and Life-cycle Assessment for Climate Change  

E-Print Network [OSTI]

A case study of a hydroelectric power plant (Glen Canyon)over time. In the case of hydroelectric plants, besidesthe decommissioning of hydroelectric power plants. Although

Horvath, Arpad

2005-01-01T23:59:59.000Z

422

E-Print Network 3.0 - area imperial valley Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Universitt Heidelberg Collection: Biology and Medicine ; Physics 24 Camp Pendleton Kings Canyon Summary: BLM Wilderness BLM Wilderness Study Areas NPS Wilderness USFS...

423

E-Print Network 3.0 - angeles county california Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Collection: Environmental Sciences and Ecology ; Biology and Medicine 55 Camp Pendleton Kings Canyon Summary: County San Bernardino County Kern County Ventura County Los Angeles...

424

Sandia National Laboratories: Sandia National Laboratories: Locations...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Regional Park District Joshua Tree National Park Lassen Volcanic National Park Sequoia & Kings Canyon National Parks Yosemite National Park Cave exploring Diablo Grotto Moaning...

425

E-Print Network 3.0 - arrays monterey beach Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of Agricultural Sciences and Technology Summary: Francisco, Los Angeles, Yosemite, Kings Canyon and Sequoia National Parks, the Monterey Peninsula, Lake... Tahoe, beaches,...

426

E-Print Network 3.0 - aketajawe-lolobata national park Sample...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Forest Inyo National Forest Los Padres National Forest Los Angeles Yosemite National Park Kings Canyon... National Park Los Angeles San Diego Winema National Forest Nevada Arizona...

427

E-Print Network 3.0 - ankarafantsika national park Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Forest Inyo National Forest Los Padres National Forest Los Angeles Yosemite National Park Kings Canyon... National Park Los Angeles San Diego Winema National Forest Nevada Arizona...

428

E-Print Network 3.0 - anomaly imperial valley Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Commission Collection: Energy Storage, Conversion and Utilization 66 Camp Pendleton Kings Canyon Summary: Valley National Park Fort Irwin Mojave National Preserve Mono County...

429

E-Print Network 3.0 - altai mountains southern Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of South Bohemia Collection: Environmental Sciences and Ecology 67 Camp Pendleton Kings Canyon Summary: Rockhouse A Casa Diablo Southern Inyo Scodie Symmes Creek...

430

E-Print Network 3.0 - area-subsurface central nevada Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

California. Unpublished final... report to Sierra Nevada Global Change Program. Sequoia, Kings Canyon, and Yosemite National Parks. Labo... , USA. Journal of Biogeography...

431

E-Print Network 3.0 - aeolian sands underlain Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

deposition of reworked flood sand. Thompson and Potochnik (2000) concluded that sediment... of aeolian sand since the clo- sure of Glen Canyon Dam in 1963. Multiple sets of...

432

BURNING GROUND RD CDV-SMA-2.3  

E-Print Network [OSTI]

GROUND BUNKER 430 ANCHORRANCH V-SITE 260 332 RESTHOUSE 410 360 PLASTICS Cañon de Valle S-Site Canyon Fish

433

Hydrogen fuel closer to reality because of storage advances  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Hydrogen fuel closer to reality because of storage advances Advances made in rechargeable solid hydrogen fuel storage tanks. March 21, 2012 Field experiments on the Alamosa Canyon...

434

Employee Handbook  

E-Print Network [OSTI]

22, 23, 31 LBNL Employee Handbook 41 Insurance,34 42 LBNL Employee Handbook Strawberry Canyon RecreationalHotline to pro- 40 LBNL Employee Handbook Index A Activities

Bello, Madelyn

2008-01-01T23:59:59.000Z

435

DRAFT Central Plateau Cleanup Strategy  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Canyon disposition to validate approach and set realistic schedule * Deep Vadose Zone remedial investigation feasibility study work plan pulled forward three years 5 Public...

436

Nevada: Geothermal Brine Brings Low-Cost Power with Big Potential...  

Office of Environmental Management (EM)

April at the Florida Canyon Mine, Nevada, marked the beginning of another promising clean energy commercial enterprise. The Geothermal Technologies Office researches, develops, and...

437

,"Plant","Primary Energy Source","Operating Company","Net Summer...  

U.S. Energy Information Administration (EIA) Indexed Site

Landing Power Plant","Natural Gas","Dynegy -Moss Landing LLC",2529 2,"Diablo Canyon","Nuclear","Pacific Gas & Electric Co",2240 3,"San Onofre Nuclear Generating...

438

RAP Meeting Transcribed Flipcharts  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

on RCRA permit * F Reactor RIFS and D & H RIFS - distribute end of December * Thorium vault at U Canyon? * PA integration WM Area C (TWC lead, joint) * Public...

439

CX-011515: Categorical Exclusion Determination | Department of...  

Broader source: Energy.gov (indexed) [DOE]

dissolve, process, and neutralize used nuclear fuel (UNF) by blending with High AluminumLow Uranium (HALU) UNF in H-Canyon. CX-011515.pdf More Documents & Publications...

440

CX-007153: Categorical Exclusion Determination | Department of...  

Broader source: Energy.gov (indexed) [DOE]

Determination CX-007153: Categorical Exclusion Determination Glen Canyon substation Transformer Addition CX(s) Applied: B4.6 Date: 05052011 Location(s): Coconino County, Arizona...

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


441

Power Marketing  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Calculation BC E&OC Presentation Boulder Canyon Project Remarketing Effort Mead Transformer Presentation Final Hoover Coordinating Committee Meeting June 3, 2014 (PDF) Final...

442

Natural Gas Weekly Update, Printer-Friendly Version  

Gasoline and Diesel Fuel Update (EIA)

received a total of 8 bids, while the second highest accepted bid was the 34 million Green Canyon Block 551, awarded to Anadarko Petroleum Corporation and Newfield Exploration...

443

Dennis Yates Of Savannah River Operations Named 2013 Facility...  

Office of Environmental Management (EM)

River Site. The HB-Line is part of the H-Canyon, which conducts hazardous nuclear chemistry, packaging, and processing operations on plutonium and transuranic materials. Mr....

444

E-Print Network 3.0 - assurance system eqas Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

on page 14). Assessments of the effects of the cooling systems of six plants, Diablo Canyon, Huntington... in waste control and discharge. There is no question that the...

445

E-Print Network 3.0 - area middle fork Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Summary: Middle Fork Coyote Creek (8286 Acres) Santa Clara County 2205300104 Kelly Cabin Canyon (4283 Acres... Berryessa EastForkCoyote Cow Calera Penitencia LasAnimas Arroyo...

446

E-Print Network 3.0 - andean porphyry copper Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

in Utah have recorded overKEY WORDS: alkaline magma; Bingham; porphyry copper... Bingham Canyon porphyry copper deposit range in may also have effectively removed magmatic...

447

ch_4  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Moon National Monument and Wilderness Area, Hell's Half Acre Wilderness Study Area, Black Canyon Wilderness Study Area, Camas National Wildlife Refuge, Market Lake Wildlife...

448

Mining methods and geology of the Boston Consolidated Mine at Bingham, Utah .  

E-Print Network [OSTI]

??"This thesis does not so much attempt a detailed report on the geology of the disseminates ores of Bingham Canyon as a more particular description (more)

Boucher, James Leonidas

1914-01-01T23:59:59.000Z

449

E-Print Network 3.0 - acidic sulphate baths Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinatubo, Bingham Canyon and El Teniente Summary: . Mt. Pinatubo contains other Cu showings and...

450

EIS-0283-S2: Interim Action Determination  

Broader source: Energy.gov [DOE]

Surplus Plutonium Disposition Supplemental Environmental Impact Statement (Use of H-Canyon/HB-Line to Prepare Feed for the Mixed Oxide Fuel Fabrication at the Savannah River Site)

451

E-Print Network 3.0 - acidic sulphate solutions Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinatubo, Bingham Canyon and El Teniente Summary: . Mt. Pinatubo contains other Cu showings and...

452

U.S. Department of the Interior December 2012 U.S. Geological Survey  

E-Print Network [OSTI]

by a decline in Utah, where production at the Bingham Canyon Mine was 30% lower than that in the first 9 months

453

E-Print Network 3.0 - artificial underwater structure Sample...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Invertebrate Biomass in Skate Nurseries Gerald R. Hoff Summary: skate in Pribilof Canyon by an autonomous underwater vehicle show higher abundance of invertebrates... on...

454

E-Print Network 3.0 - alameda field kingman Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Use Timeline Summary: Turpin of Alameda County Clean Water Program, as part of the Crow Canyon Watershed Science Project... the fertility of the land, remarking on mustard fields...

455

? WHY THE VEATHER I' Mailed August 18, 1930. By Charles Fitzhugh Talman,  

E-Print Network [OSTI]

; the other poured a tremendous f l o o d down Bingham Canyon, Utah, near the worldrs h g a t opan-pit c o n o

456

SILVER--2003 68.1 References that include a section mark () are found in the Internet  

E-Print Network [OSTI]

reduction in byproduct silver generated at copper mines. Downtime at Kennecott Utah Copper Corp.'s Bingham Canyon Mine reduced productio

457

E-Print Network 3.0 - acid oxidation products Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

of oxidized, S-rich mafic magmas for giant Cu mineralization: Evidence from Pinatubo, Bingham Canyon and El Teniente Summary: eruption products show that mafic magma was...

458

E-Print Network 3.0 - almond formation outcrops Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

reservoirs outside the GOM. Examples The world-class outcrops of the Permian Brushy Canyon Formation... Use of outcrop analogues to predict lithology influence on the seismic...

459

Microbial gene functions enriched in the Deepwater Horizon deep-sea oil plume  

E-Print Network [OSTI]

Mexicos Mississippi Canyon area at a depth of 1,544 m releasing approximately 4.9 million barrels of crude

Lu, Z.

2012-01-01T23:59:59.000Z

460

EIS-0374: Final Environmental Impact Statement | Department of...  

Broader source: Energy.gov (indexed) [DOE]

Final Environmental Impact Statement EIS-0374: Final Environmental Impact Statement Klondike IIIBiglow Canyon Wind Integration Project This summary covers the major points of the...

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


461

EIS-0219: Record of Decision | Department of Energy  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

Canyon Facility, Savannah River Site, Aiken, SC Based on the analysis in the Final Environmental Impact Statement for the Stabilization of Plutonium Solutions Stored in the...

462

Safeguarding wetland on Laboratory property  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

wetland on Laboratory property Protecting our environment August 1, 2013 The wetlands in Sandia Canyon on Lab property provide a home to a large amount of wildlife. Work...

463

Compound and Elemental Analysis At Northern Basin & Range Region (Cole,  

Open Energy Info (EERE)

Cole, Cole, 1983) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Compound and Elemental Analysis At Northern Basin & Range Region (Cole, 1983) Exploration Activity Details Location Northern Basin and Range Geothermal Region Exploration Technique Compound and Elemental Analysis Activity Date Usefulness not indicated DOE-funding Unknown Notes Wstern Utah hot springs: Antelope, Fish (Deadman), Fish (Wilson), Twin Peak, Cudahy, Laverkin, Grantsville, Crystal Prison, Arrowhead, Red Hill, Monroe, Joseph, Castilla, Saratoga, Thermo, Crater, Wasatch, Beck, Deseret, Big Spring, Blue Warm, Crystal Madsen, Udy, Cutler, Garland, Utah, Ogden, Hooper, Newcastle Area References David R. Cole (1983) Chemical And Isotopic Investigation Of Warm

464

NETL: National Methane Hydrates R&D Program- 2009 GOM JIP Expedition  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Green Canyon Block 955 Green Canyon Block 955 The gas hydrates JIP site selection team identified numerous potential targets in Green Canyon block 955. Three of these sites were drilled in Leg II. The wells are located in over 6,500 ft of water near the foot of the Sigsbee Escarpment. The locations are near a major embayment into the Escarpment (“Green Canyon”) which has served as a persistent focal point for sediment delivery into the deep Gulf of Mexico. Topographic map of the seafloor in the Green Canyon area. Topographic map of the seafloor in the Green Canyon area. Block 955 lies just seaward of the Sigsbee Escarpment in ~6,500 feet of water Green Canyon block 995 includes a prominent channel/levee complex that has transported and deposited large volumes of sandy sediment from the canyon to the deep Gulf of Mexico abyssal plain. The southwest corner of the block includes a recently developed structural high caused by deeper mobilization of salt. The crest of the structural high is cut by complex network of faults that can provide pathways for migrating fluids and gases. Geophysical data reviewed during assessment of the site revealed a complex array of geophysical responses near the inferred base of gas hydrate stability. Some of these responses are suggestive of free gas and some indicative of gas hydrate, but all are limited to depths that are near or below the inferred base of gas hydrate stability.

465

Baseline Rd. Colorado Ave.  

E-Print Network [OSTI]

Baseline Rd. Broadway Broadway Colorado Ave. Arapahoe Ave. Canyon Blvd. 28thSt. 9thSt. 6thSt. 13th Pearl St. Euclid FolsomSt. N Baseline Rd. Broadway Broadway Colorado Ave. Arapahoe Ave. Canyon Blvd. 28://www.banjobilly.com JUNE 12-13, 2009 JILA/CHEMISTRY & BIOCHEMISTRY, UNIVERSITY OF COLORADO, BOULDER A CELEBRATION OF 40

Lineberger, W. Carl

466

CORRELATION OF THE TRIASSIC FORMATIONS OF NORTH AMERICA EXCLUSIVE OF CANADA  

Science Journals Connector (OSTI)

...contain a larger proportion of car- bonate rocks and are presumably...assigned to the China Mountain and Panther Canyon formations. Accompanying...77 Owl Rock 28, 29, 30, 38 Panther Canyon 21 Pekin 75 Perkasie...S., 1876,Description of Car- boniferous and Triassic fossils...

467

NARCONON TREAT YOU LIKE THE DOPE.  

E-Print Network [OSTI]

of Leona Valley, Green Valley and Bouquet Canyon? Doyou want tolive inwhat could cometo be known as, "that for Leona Valley, Green Valley and Bouquet Canyon. Come to the Public Hearing. Stand shoulder to shoulder, 500 West Temple Street, Downtown, Los Angeles, CA 90012 GET WISE TO NARCONON, GO TO www

Touretzky, David S.

468

Fault Segments and Step-overs : : Implications for Geohazards and Biohabitats  

E-Print Network [OSTI]

the San Mateo, San Onofre, and Carlsbad trends is old (LatePoint Loma Mt. Soledad Carlsbad 117?15'W -R CF Z FZ CB FZ CB32?30'N SO La Jolla Canyon Carlsbad Canyon SONGS 117?30'W NI

Maloney, Jillian Marie

2013-01-01T23:59:59.000Z

469

Land and sea study of the northeastern golfe du Lion rifted margin: the Oligocene Miocene of southern Provence (Nerthe area, SE France)  

Science Journals Connector (OSTI)

...is characterized by semi-continuous, high...Total, Exploration Production, DGEP/GSR/TG...Saint Tropez canyons - a submersible study. - Mar. Geol...Saint-Tropez canyons - A submersible study. - Mar. Geol...southern Peri-Tethys platforms and the intermediate...

Julien Oudet; Philippe Mnch*; Jean Borgomano; Frdric Quillevere; Mihaela C. Melinte-Dobrinescu; Franois Demory; Sophie Viseur; Jean-Jacques Cornee

470

DOI: 10.1126/science.1155822 , 1070 (2008);320Science  

E-Print Network [OSTI]

the same age as the boulder at location 2, 45 ± 5 ka. Another constraint on the age of the canyon comes of the scoured-bedrock notch. The observations of scoured bedrock and plunge pools point toward a flood or floods able to transport boulders and carve the canyon in weeks or months, illustrating the power of rare

Garnero, Ed

471

GEOPHYSICAL RESEARCH LETTERS, VOL. ???, XXXX, DOI:10.1029/, New insights on the runout of large landslides in the  

E-Print Network [OSTI]

landslides in the Valles-Marineris Canyons, Mars E. Lajeunesse,1 C. Quantin,2 P. Allemand,2 and C. Delacourt2 from Viking Orbiters, the numerous landslides identified along the canyons of Valles- Marineris (VM of the rock mass. However nu- merical simulations (Harrison and Grimm [2003]) indicate that neither Bingham

Delacourt, Christophe

472

FINANCIAL REPORT June 30, 2003  

E-Print Network [OSTI]

. Other unique features include the outdoor walkway known as "the canyon". The east wall is curved to replicate the silhouette of the ship and curving balconies overlooking the canyon are an abstract of access President for Business Affairs Saundra L. Taylor Senior Vice President for Campus Life Janet E. Bingham Vice

Ziurys, Lucy M.

473

EM Issues Amended Decision to Expand Use of Nuclear Facility | Department  

Broader source: Energy.gov (indexed) [DOE]

Issues Amended Decision to Expand Use of Nuclear Facility Issues Amended Decision to Expand Use of Nuclear Facility EM Issues Amended Decision to Expand Use of Nuclear Facility April 1, 2013 - 12:00pm Addthis H-Canyon at Savannah River Site. The building is called a canyon because of its long rectangular shape and two continuous trenches that contains process vessels. H-Canyon at Savannah River Site. The building is called a canyon because of its long rectangular shape and two continuous trenches that contains process vessels. AIKEN, S.C. - EM issued an amended Record of Decision (ROD) to the Savannah River Site (SRS) Spent Nuclear Fuel Environmental Impact Statement to expand the operations of the H-Canyon Facility at SRS to support a major nuclear non-proliferation goal and save taxpayer dollars. DOE recently signed a contract allowing Atomic Energy of Canada Limited

474

EM Issues Amended Decision to Expand Use of Nuclear Facility | Department  

Broader source: Energy.gov (indexed) [DOE]

EM Issues Amended Decision to Expand Use of Nuclear Facility EM Issues Amended Decision to Expand Use of Nuclear Facility EM Issues Amended Decision to Expand Use of Nuclear Facility April 1, 2013 - 12:00pm Addthis H-Canyon at Savannah River Site. The building is called a canyon because of its long rectangular shape and two continuous trenches that contains process vessels. H-Canyon at Savannah River Site. The building is called a canyon because of its long rectangular shape and two continuous trenches that contains process vessels. AIKEN, S.C. - EM issued an amended Record of Decision (ROD) to the Savannah River Site (SRS) Spent Nuclear Fuel Environmental Impact Statement to expand the operations of the H-Canyon Facility at SRS to support a major nuclear non-proliferation goal and save taxpayer dollars. DOE recently signed a contract allowing Atomic Energy of Canada Limited

475

EIS-0480: Long-Term Experimental and Management Plan for the Operation of  

Broader source: Energy.gov (indexed) [DOE]

0: Long-Term Experimental and Management Plan for the 0: Long-Term Experimental and Management Plan for the Operation of Glen Canyon Dam EIS-0480: Long-Term Experimental and Management Plan for the Operation of Glen Canyon Dam SUMMARY Two agencies of the Department of the Interior, Bureau of Reclamation and National Park Service, are jointly preparing a Long-Term Experimental and Management Plan for the Glen Canyon Dam and an EIS for adoption of the Plan. The Glen Canyon Dam, on the Colorado River in northern, Arizona, generates hydroelectric power that is marketed by DOE's Western Area Power Administration, a cooperating agency. PUBLIC COMMENT OPPORTUNITIES None available at this time. DOCUMENTS AVAILABLE FOR DOWNLOAD July 6, 2011 EIS-0480: Notice of Intent to Prepare a Draft Environmental Impact Statement Long-Term Experimental and Management Plan for the Operation of Glen Canyon

476

bayo.cdr  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Bayo Bayo Canyon, New Mexico, Site. This site is managed by the U.S. Department of Energy Office of Legacy Management. Site Description and History The Bayo Canyon, New Mexico, Site is located approximately 3 miles west of Los Alamos, New Mexico, 25 miles northwest of Santa Fe, and 60 miles north-northeast of Albuquerque. Partly in Los Alamos County and partly in Santa Fe County, Bayo Canyon is one of numerous canyons that cut into the Pajarito Plateau in north-central New Mexico. The U.S. government owned the site from 1943 to 1967 as part of the Los Alamos National Laboratory (LANL) operations. The Manhattan Engineer District (MED) constructed facilities in Bayo Canyon in 1943 and 1944. MED and later the U.S. Atomic Energy Commission (AEC) used the site between 1944 and 1961 as a firing range for high explosive experiments in conjunction with research on nuclear development. These explosions

477

A Preliminary Study Of Older Hot Spring Alteration In Sevenmile Hole, Grand  

Open Energy Info (EERE)

Study Of Older Hot Spring Alteration In Sevenmile Hole, Grand Study Of Older Hot Spring Alteration In Sevenmile Hole, Grand Canyon Of The Yellowstone River, Yellowstone Caldera, Wyoming Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Preliminary Study Of Older Hot Spring Alteration In Sevenmile Hole, Grand Canyon Of The Yellowstone River, Yellowstone Caldera, Wyoming Details Activities (4) Areas (1) Regions (0) Abstract: Erosion in the Grand Canyon of the Yellowstone River, Yellowstone Caldera (640 ka), Wyoming, has exposed a cross section of older hydrothermal alteration in the canyon walls. The altered outcrops of the post-collapse tuff of Sulphur Creek (480 ka) extend from the canyon rim to more than 300 m beneath it. The hydrothermal minerals are zoned, with an advanced argillic alteration consisting of an association of quartz (opal)

478

Los Alamos National Laboratory: Long-Term Environmental Stewardship and  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Protections: Sediment Control = Contaminant Retention Protections: Sediment Control = Contaminant Retention LANL maintains hundreds of wells, stream sampling stations and stormwater control structures to protect waters. Map of Los Alamos townsite bordered by Pueblo and Los Alamos Canyons Los Alamos townsite bordered by Pueblo and Los Alamos Canyons Los Alamos Canyon weir Pueblo Canyon grade control structure Trap and remove sediment Willows Wildfires Stormwater structures Los Alamos Canyon dam and reservoir Stormwater controls after wildfire Hydroseeding LANL constrains the flow of contaminated sediments into the Rio Grande. Fact Check » « Every watershed at LANL has been evaluated and stormwater controls have been installed to keep contaminated sediment on LANL property. Every waste management area on mesa tops has been evaluated and 80% of planned controls

479

Boosting America's Hydropower Output | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

Boosting America's Hydropower Output Boosting America's Hydropower Output Boosting America's Hydropower Output October 9, 2012 - 2:10pm Addthis The Boulder Canyon Hydroelectric Facility's new, highly-efficient turbine. | Photo courtesy of the city of Boulder, Colorado. The Boulder Canyon Hydroelectric Facility's new, highly-efficient turbine. | Photo courtesy of the city of Boulder, Colorado. City of Boulder employees celebrate the completion of the Boulder Canyon Hydroelectric Modernization project. | Photo courtesy of the city of Boulder, Colorado. City of Boulder employees celebrate the completion of the Boulder Canyon Hydroelectric Modernization project. | Photo courtesy of the city of Boulder, Colorado. The Boulder Canyon Hydroelectric Facility's new, highly-efficient turbine. | Photo courtesy of the city of Boulder, Colorado.

480

Geothermal heating system for the Children's Museum of Utah  

SciTech Connect (OSTI)

The results of a study to determine the engineering and economic feasibility of using the Wasatch Hot Spring resource for space heating of the Children's Library building are presented. The Wasatch Hot Spring with a reported flow of about 63 gpm (240 l/min) at an average temperature of 104/sup 0/F is not capable of furnishing the needed heat for the Children's Museum building. The underground paths along which the thermal waters flow to their outlets at the Warm Springs Fault are not presently known. It is possible if the thermal water ascends from the deep layers of the earth along the Warm Springs Fault that increased geothermal flow at a higher temperature can be produced by drilling into the fault. Assuming that sufficient geothermal fluid quantity is produced by drilling in the area, an analysis is made of a geothermal heating system for the building based on different fluid temperatures. It is assumed that the present and planned heating systems be left intact with the gas fired boilers taking over during cold periods when the geothermal system fails to provide sufficient heat. Economic analysis shows that the geothermal system is very attractive, even for the lowest geothermal fluid temperature considered (110/sup 0/F).

Karlsson, T.

1984-07-01T23:59:59.000Z

Note: This page contains sample records for the topic "ozona canyon wasatch" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


481

Gas Mileage of 2011 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

1 GMC Vehicles 1 GMC Vehicles EPA MPG MODEL City Comb Hwy 2011 GMC Acadia AWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2011 GMC Acadia AWD View MPG Estimates Shared By Vehicle Owners 16 City 19 Combined 23 Highway 2011 GMC Acadia FWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2011 GMC Acadia FWD View MPG Estimates Shared By Vehicle Owners 17 City 19 Combined 24 Highway 2011 GMC Canyon 2WD 4 cyl, 2.9 L, Automatic 4-spd, Regular Gasoline Compare 2011 GMC Canyon 2WD 18 City 21 Combined 25 Highway 2011 GMC Canyon 2WD 4 cyl, 2.9 L, Manual 5-spd, Regular Gasoline Compare 2011 GMC Canyon 2WD 18 City 21 Combined 25 Highway 2011 GMC Canyon 2WD 5 cyl, 3.7 L, Automatic 4-spd, Regular Gasoline Compare 2011 GMC Canyon 2WD 17 City 19 Combined 23 Highway 2011 GMC Canyon 2WD 8 cyl, 5.3 L, Automatic 4-spd, Regular Gasoline

482

Gas Mileage of 2009 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

09 GMC Vehicles 09 GMC Vehicles EPA MPG MODEL City Comb Hwy 2009 GMC Acadia AWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2009 GMC Acadia AWD View MPG Estimates Shared By Vehicle Owners 16 City 19 Combined 23 Highway 2009 GMC Acadia FWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2009 GMC Acadia FWD View MPG Estimates Shared By Vehicle Owners 17 City 19 Combined 24 Highway 2009 GMC Canyon 2WD 4 cyl, 2.9 L, Automatic 4-spd, Regular Gasoline Compare 2009 GMC Canyon 2WD 18 City 20 Combined 24 Highway 2009 GMC Canyon 2WD 5 cyl, 3.7 L, Automatic 4-spd, Regular Gasoline Compare 2009 GMC Canyon 2WD 17 City 19 Combined 23 Highway 2009 GMC Canyon 2WD 4 cyl, 2.9 L, Manual 5-spd, Regular Gasoline Compare 2009 GMC Canyon 2WD 18 City 20 Combined 24 Highway 2009 GMC Canyon 2WD 8 cyl, 5.3 L, Automatic 4-spd, Regular Gasoline

483

Gas Mileage of 2012 Vehicles by GMC  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

2 GMC Vehicles 2 GMC Vehicles EPA MPG MODEL City Comb Hwy 2012 GMC Acadia AWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2012 GMC Acadia AWD View MPG Estimates Shared By Vehicle Owners 16 City 19 Combined 23 Highway 2012 GMC Acadia FWD 6 cyl, 3.6 L, Automatic 6-spd, Regular Gasoline Compare 2012 GMC Acadia FWD View MPG Estimates Shared By Vehicle Owners 17 City 19 Combined 24 Highway 2012 GMC Canyon 2WD 4 cyl, 2.9 L, Automatic 4-spd, Regular Gasoline Compare 2012 GMC Canyon 2WD 18 City 21 Combined 25 Highway 2012 GMC Canyon 2WD 4 cyl, 2.9 L, Manual 5-spd, Regular Gasoline Compare 2012 GMC Canyon 2WD 18 City 21 Combined 25 Highway 2012 GMC Canyon 2WD 8 cyl, 5.3 L, Automatic 4-spd, Regular Gasoline Compare 2012 GMC Canyon 2WD 14 City 16 Combined 20 Highway 2012 GMC Canyon 2WD 5 cyl, 3.7 L, Automatic 4-spd, Regular Gasoline

484

Power Economic Analysis  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

CRSP Management Center CRSP Management Center Western Area Power Administration January 2011 Power Economic Analysis of Operational Restrictions at Glen Canyon Dam In February, 1997, the operating criteria for Glen Canyon Dam were changed. Operation was restricted to a Modified Low Fluctuating Flow as described in the Operation of Glen Canyon Dam, Colorado River Storage Project, Arizona, Final Environmental Impact Statement, March, 1995. These restrictions reduced the operating flexibility of the hydroelectric power plant and therefore the economic value of the electricity it produced. The Environmental Impact Statement provided impact information to support the Record of Decision governing dam operations. The impact

485

NVN-087811 | Open Energy Information  

Open Energy Info (EERE)

87811 87811 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087811 CU at New York Canyon Geothermal Area for Geothermal/Exploration, New York Canyon Geothermal Exploration and Development General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant TGP Dixie Development Co Geothermal Area New York Canyon Geothermal Area Project Location Lovelock, Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 21 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates

486

EA-1736: Final Environmental Assessment | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

36: Final Environmental Assessment 36: Final Environmental Assessment EA-1736: Final Environmental Assessment Expansion of the Sanitary Effluent Reclamation Facility and Environmental Restoration of Reach S-2 of Sandia Canyon at Los Alamos National Laboratory, Los Alamos, New Mexico This Environmental Assessment (EA) considers two separate actions, the expansion of the Sanitary Effluent Reclamation Facility (SERF) and environmental restoration activities located within a portion of upper Sandia Canyon, designated as reach S-2. Both of these actions would take place adjacent to or within upper Sandia Canyon at Los Alamos National Laboratory (LANL). DOE/EA-1736, National Nuclear Security Administration, Final Environmental Assessment for the Expansion of the Sanitary Effluent Reclamation Facility

487

NVN-087791 | Open Energy Information  

Open Energy Info (EERE)

NVN-087791 NVN-087791 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087791 CU at New York Canyon Geothermal Area for Geothermal/Exploration, New York Canyon Geothermal Exploration and Development General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant TGP Dixie Development Company Geothermal Area New York Canyon Geothermal Area Project Location Lovelock, Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 28 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM

488

CX-006628: Categorical Exclusion Determination | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

8: Categorical Exclusion Determination 8: Categorical Exclusion Determination CX-006628: Categorical Exclusion Determination 221-F Canyon Truckwell Heating, Ventilation, and Air Conditioning System CX(s) Applied: B1.5 Date: 08/01/2011 Location(s): Aiken, South Carolina Office(s): Savannah River Operations Office Upate 8/1/11 An asbestos inspection was performed on Friday 7/29/11. It was determined that no asbestos was present. This inspection is documented in SRNS-N2000-2011-00128-ASB, Asbestos Inspection, Installation Of F-Canyon Truck Well A/C Ductwork, 7/29/2011, Knoderer, Mark. The F-Area 221-F Canyon Truckwell has been modified to incorporate three separate air locks, one additional egress air lock and an area within the Warm Canyon known as the Waste Handling Area (WHA)? Personnel are expected to man the facility and

489

CX-006625: Categorical Exclusion Determination | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

5: Categorical Exclusion Determination 5: Categorical Exclusion Determination CX-006625: Categorical Exclusion Determination 221-F Canyon Truckwell Heating, Ventilation, and Air Conditioning System CX(s) Applied: B1.5 Date: 07/29/2011 Location(s): Aiken, South Carolina Office(s): Savannah River Operations Office The F-Area 221-F Canyon Truckwell has been modified to incorporate three separate air locks, one additional egress air lock and an area within the Warm Canyon known as the Waste Handling Area (WHA)... Personnel are expected to man the facility and may be dressed in multiple layers of Personal Protective Equipment (PPE). The air being supplied to the truckwell is drawn in through the louvers through the Canyon Exhaust Fans, which ensures that the facility is negatively pressured ensuring that no

490

U.S. Department of Energy Categorical Exclusion Determination Form  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Stiffen Canyon Exhaust Fan 3 Motor Pedestal Stiffen Canyon Exhaust Fan 3 Motor Pedestal Savannah River Site Aiken/Aiken/South Carolina Canyon Exhaust Fan 3 has a history of elevated axial vibration, particularly at the free-end motor bearing. The H-Canyon Facility consulted an outside vendor. The attached report is the latest report from that vendor. In summary, the majority of vibration is driven by turbulence after flow and pressure change with varying facility configuration; however, the "condition of the motor pedestal indicates the possibility of less than desired dynamic stiffness of the motor base plate." The proposed activity is a modification to the fan motor pedestal to install these stiffeners. The PA will be implemented per a future DCF. The Design Engineering group has been tasked with the generation of this document. This PA includes shop

491

ENVIRONMENTAL REVIEW for CATEGORICAL EXCLUSION DETERMINATION  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Glen Canyon-Shiprock 230-kV Transmission Line Glen Canyon-Shiprock 230-kV Transmission Line Coconino, Navajo, and Apache Counties, Arizona, and San Juan County, New Mexico A. Brief Description of Proposal: Western Area Power Administration (Western) proposes to survey and inspect all areas along the Glen Canyon-Shiprock (Glen Canyon-Navajo, Kayenta-Navajo, and Kayenta-Shiprock) transmission line to conduct routine vegetation management inspection and danger tree removal on the transmission line. Trained crews will measure electrical clearance distances between the conductor and tree branches and cut down any trees that meet or exceed the allowable clearance distance. Any "danger" trees and vegetation that constitute an electrical hazard to the lines will be removed. Individual trees will be cut, lopped, and scattered within the existing

492

 

Broader source: Energy.gov (indexed) [DOE]

Consolidated Hazards Analysis for the HB-Line Documented Safety Basis Upgrade (U), U-CHA-H-00003, includes two specific events HB-7-001, Earthquake with subsequent fire and post seismic hydrogen explosions in process vessels and HB-7-004, Earthquake with post seismic hydrogen explosions in process vessels requiring protection. In addition to these HB-Line events the H-Canyon CHAP SRNS-TR-2008-00277 events GE-7-003 and GE-7-004 credit the H-canyon exhaust ventilation system(including Canyon, truckwell, railroad tunnel, and hot and warm crane maintenance areas) (Exhausts and filters air from designated ventilated areas). To ensure that the HB-Line events are protected and that the H-Canyon Exhaust Ventilation system is not impacted negatively by HB-Line exhaust flow during and after a seismic event, the HB-Line Supply and Room Exhaust fans are to be de-

493

EIS-0219: Record of Decision | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

Canyon Facility at Canyon Facility at the Savannah River Site, Aiken, SC The U.S. Department of Energy (DOE) has prepared and issued a Final Environmental Impact Statement (EIS) (DOE/EIS-0219, December 30, 1994), to assess the potential environmental impacts of stabilizing approximately 80,000 gallons of plutonium solutions currently stored in tanks in the F-Canyon chemical separations facility at the Savannah River Site (SRS) near Aiken, South Carolina. As long as the plutonium remains in solution there is a risk of releases and subsequent radiation exposure to workers, the public, and the environment from accidental criticality incidents, leaks, and disruptions of engineered systems from earthquakes. DOE/EIS-0219, Savannah River Operations Office; Record of Decision: Stabilization of Plutonium Solutions Stored in the F- Canyon Facility at

494

EIS-0427: Record of Decision | Department of Energy  

Broader source: Energy.gov (indexed) [DOE]

7: Record of Decision 7: Record of Decision EIS-0427: Record of Decision Interconnection of the Grapevine Canyon Wind Project, Coconino County, Arizona Western Area Power Administration (Western) received a request from Foresight Flying M, LLC (Foresight) to interconnect its proposed Grapevine Canyon Wind Project (Project) to Western's Glen Canyon-Pinnacle Peak No. 1 and No. 2 transmission lines. The Project would be located about 28 miles south and east of Flagstaff, in Coconino County, Arizona. On June 8, 2012, the Notice of Availability of the Final Environmental Impact Statement (EIS) for Grapevine Canyon Wind Project was published in the Federal Register (77 FR 34041). After considering the environmental impacts, Western has decided to allow Foresight's request for interconnection to

495

U.S. Department of Energy Categorical Exclusion Determination Form  

Broader source: Energy.gov (indexed) [DOE]

Stiffen Canyon Exhaust Fan 3 Motor Pedestal Stiffen Canyon Exhaust Fan 3 Motor Pedestal Savannah River Site Aiken/Aiken/South Carolina Canyon Exhaust Fan 3 has a history of elevated axial vibration, particularly at the free-end motor bearing. The H-Canyon Facility consulted an outside vendor. The attached report is the latest report from that vendor. In summary, the majority of vibration is driven by turbulence after flow and pressure change with varying facility configuration; however, the "condition of the motor pedestal indicates the possibility of less than desired dynamic stiffness of the motor base plate." The proposed activity is a modification to the fan motor pedestal to install these stiffeners. The PA will be implemented per a future DCF. The Design Engineering group has been tasked with the generation of this document. This PA includes shop

496

U.S. Department of Energy Categorical Exclusion Determination Form  

Broader source: Energy.gov (indexed) [DOE]

Glen Canyon Substation Stage 09- Glen Canyon Substation Stage 09- 50MVA 230/69KV Transformer addition Program or Field Office: DOE/Western/Desert Southwest Region Location(s) (City/County/State): Glen Canyon Substation, Page/Coconino County/Arizona Proposed Action Description: Submit by E-mail Western proposes to conduct electrical maintenance activities within the existing Glen Canyon Substation located at Page, Coconino County, Arizona. The project is on federal (Western-owned) property in Section 19 Township 41 N, Range 8 East, in every quarter sections 24 and 25, Coconino County, AZ, (Gila and Salt River Baseline and Meridian; Figure 1 ). The proposed scope of work includes the following (Figure 2): ·Install one 50MVA 230/69KV transformer to a new storage pad in the upper yard. The new pad will measure 26 feet 6 inches long by 16 feet

497

INTRODUCTION The Upper Permian (Guadalupian) Brushy  

E-Print Network [OSTI]

for oils being produced from reservoirs in the Brushy Canyon Formation to the east of the outcrop (Hays crustal shortening in the Marathon fold- and-thrust belt (Hills, 1984). During Leonardian- Guadalupian

Sageman, Brad

498

U.S. Department of Energy Categorical Exclusion ...  

Broader source: Energy.gov (indexed) [DOE]

H-Canyon Dissolver Corrosion Rate Assessment Savannah River Site AikenAikenSouth Carolina This is an EEC to cover the corrosion testing of materials in aqueous solutions which...

499

E-Print Network 3.0 - asperecito flanco occidental Sample Search...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Precipitation (mm) 421 12;12;12;2 34 5 1 12;2: Sierra Madre Occidental... : Copper Canyon T. M. Whitmore 12;4: Coastal Plain looking E towards Sierra Madre Occidental...

500

Sandia technologist Richard Simpson featured for helping solve...  

National Nuclear Security Administration (NNSA)

Richard Simpson has filled a canyon with soap bubbles, shot photos of flaming liquefied natural gas from a helicopter, floated balloons hundreds of feet in the air to calibrate...