Powered by Deep Web Technologies
Note: This page contains sample records for the topic "haleakala sw rift" 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

Haleakala SW Rift Zone Exploration | Open Energy Information  

Open Energy Info (EERE)

Haleakala SW Rift Zone Exploration Haleakala SW Rift Zone Exploration Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Haleakala SW Rift Zone Exploration Project Location Information Coordinates 20.63144440367°, -156.37383611407° 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":20.63144440367,"lon":-156.37383611407,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

2

Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

3

Geothermometry At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Geothermometry At Haleakala Volcano Area (Thomas, 1986) Geothermometry At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Geothermometry Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

4

Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Gas Flux Sampling Activity Date Usefulness useful DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one

5

Time-Domain Electromagnetics At Haleakala Volcano Area (Thomas, 1986) |  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Haleakala Volcano Time-Domain Electromagnetics At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes Controlled-source electromagnetic soundings were found to be substantially more successful in the southwest rift than either the Schlumberger or the self-potential studies. This was largely due to the ability of time-domain methods to penetrate high-resistivity surface layers and thus to define lower-resistivity sections at depth. The results of this sounding study, which was conducted at elevations ranging from 75 to 497 m a.s.l., generally indicated moderate- to lowresistivity (6 - 7 ohm.m) sections to depths of 1 km on the lower rift zone and higher resistivities (12-16

6

Direct-Current Resistivity Survey At Haleakala Volcano Area (Thomas, 1986)  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Haleakala Direct-Current Resistivity Survey At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles. Geophysical and geochemical surveys along this rift (southwest) were limited by difficult field conditions and access limitations. The geophysical program consisted of one Schlumberger sounding, one self-potential profile and one controlled-source electromagnetic sounding. The geochemical data collected included a reconnaissance soil mercury and

7

Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) | Open  

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 » Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Haleakala Volcano Area (Thomas, 1986) Exploration Activity Details Location Haleakala Volcano Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes The field survey program on the northwest rift zone consisted of soil mercury and radon emanometry surveys, groundwater temperature and chemistry studies, Schlumberger resistivity soundings and self-potential profiles.

8

Haleakala Volcano Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Haleakala Volcano Geothermal Area Haleakala Volcano Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Haleakala Volcano 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 (7) 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

9

Rift valley  

Science Journals Connector (OSTI)

Valleys of subsidence with long steep parallel walls, as originally defined...J. W. Gregory (1894). rift valleys are evidently the geomorphic equivalents of or...Rift Valley Structure..., Vol. V). Quennell be...

Rhodes W. Fairbridge

1968-01-01T23:59:59.000Z

10

Rift Zone | Open Energy Information  

Open Energy Info (EERE)

Rift Zone Rift Zone Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Print PDF Rift Zone Dictionary.png Rift Zone: A divergent plate boundary within a continent Other definitions:Wikipedia Reegle Tectonic Settings List of tectonic settings known to host modern geothermal systems: Extensional Tectonics Subduction Zone Rift Zone Hot Spot Non-Tectonic Strike-Slip The Rio Grande Rift exemplifies rift zone tectonics - increased volcanic activity and the formation of graben structures (reference: science-art.com) Rift valleys occur at divergent plate boundaries, resulting in large graben structures and increased volcanism. The East African Rift is an example of a continental rift zone with increased volcanism, while the Atlantic's spreading Mid-Ocean Ridge is host to an enormous amount of geothermal

11

The midcontinent rift system  

E-Print Network [OSTI]

.annualreviews.org/aronline Annual Reviews www.annualreviews.org/aronline Annual Reviews MIDCONTINENT RIFT SYSTEM 347 www.annualreviews.org/aronline Annual Reviews 348 VAN SCHMUS & HINZE mid-Michigan geophysical anomaly, east-continent geophysical anoma...). Subsequently, deep seismic reflection profiling by the Consortium for Continental Reflection Profiling (COCORP) identified a structural trough containing layered formations beneath the Phanerozoic sedimentary rocks and coinciding with the mid-Michigan anomaly...

Van Schmus, W. R.; Hinze, W. J.

1985-01-01T23:59:59.000Z

12

Gulf of California Rift Zone Geothermal Region | Open Energy...  

Open Energy Info (EERE)

Gulf of California Rift Zone Geothermal Region (Redirected from Gulf of California Rift Zone) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Gulf of California Rift...

13

Hawaii/Geothermal | Open Energy Information  

Open Energy Info (EERE)

Hawaii/Geothermal Hawaii/Geothermal < Hawaii Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Print PDF Hawaii Geothermal General Regulatory Roadmap Geothermal Power Projects Under Development in Hawaii Developer Location Estimated Capacity (MW) Development Phase Geothermal Area Geothermal Region Haleakala SW Rift Zone Exploration Ormat Technologies Inc , US Department of Energy Haleakala Southwest Rift Zone Haleakala Volcano Geothermal Area Hawaii Geothermal Region Puna Geothermal Venture Ormat Technologies Inc Pahoa, Hawaii 38 MW38,000 kW 38,000,000 W 38,000,000,000 mW 0.038 GW 3.8e-5 TW Kilauea East Rift Geothermal Area Hawaii Geothermal Region Add a geothermal project. Operational Geothermal Power Plants in Hawaii Owner Facility Type Capacity (MW) Commercial Online

14

Gulf of California Rift Zone Geothermal Region | Open Energy...  

Open Energy Info (EERE)

Gulf of California Rift Zone Geothermal Region Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Gulf of California Rift Zone Geothermal Region Details Areas (0) Power...

15

Soil Gas Sampling At Kilauea East Rift Geothermal Area (Cox,...  

Open Energy Info (EERE)

Soil Gas Sampling At Kilauea East Rift Geothermal Area (Cox, 1980) Exploration Activity Details Location Kilauea East Rift Geothermal Area Exploration Technique Soil Gas Sampling...

16

Rio Grande rift: problems and perspectives  

SciTech Connect (OSTI)

Topics and ideas addressed include: (1) the regional extent of the Rio Grande rift; (2) the structure of the crust and upper mantle; (3) whether the evidence for an axile dike in the lower crust is compelling; (4) the nature of faulting and extension in the crust; and (5) the structural and magmatic development of the rift. 88 references, 5 figures.

Baldridge, W.S.; Olsen, K.H.; Callender, J.F.

1984-01-01T23:59:59.000Z

17

Mid-continent rift system: a frontier hydrocarbon province  

SciTech Connect (OSTI)

The Mid-continent rift system can be traced by the Mid-continent geophysical anomaly (MGA) from the surface exposure of the Keweenawan Supergroup in the Lake Superior basin southwest in the subsurface through Wisconsin, Minnesota, Iowa, Nebraska, and Kansas. Outcrop and well penetrations of the late rift Keweenawan sedimentary rocks reveal sediments reflecting a characteristic early continental rift clastic sequence, including alluvial fans, deep organic-rich basins, and prograding fluvial plains. Sedimentary basins where these early rift sediments are preserved can be located by upward continuation of the aeromagnetic profiles across the rift trend and by gravity models. Studies of analog continental rifts and aulacogens show that these gravity models should incorporate (1) a deep mafic rift pillow body to create the narrow gravity high of the MGA, and (2) anomalously thick crust to account for the more regional gravity low. Preserved accumulations of rift clastics in central rift positions can then be modeled to explain the small scale notches which are found within the narrow gravity high. Indigenous oil in Keweenawan sediments in the outcrop area and coaly partings in the subsurface penetrations of the Keweenawan clastics support the analogy between these rift sediments and the exceptionally organic-rich sediments of the East African rift. COCORP data across the rift trend in Kansas show layered deep reflectors and large structures. There is demonstrable source, reservoir, and trap potential within the Keweenawan trend, making the Mid-Continent rift system a frontier hydrocarbon province.

Lee, C.K.; Kerr, S.D. Jr.

1984-04-01T23:59:59.000Z

18

Mid-Continent rift system: a frontier hydrocarbon province  

SciTech Connect (OSTI)

The Mid-Continent rift system can be traced by the Mid-Continent geophysical anomaly (MGA) from the surface exposure of the Keweenawan Supergroup in the Lake Superior basin southwest in the subsurface through Wisconsin, Minnesota, Iowa, Nebraska, and Kansas. Outcrop and well penetrations of the late rift Keweenawan sedimentary rocks reveal sediments reflecting a characteristic early continental rift clastic sequence, including alluvial fans, deep organic-rich basins, and prograding fluvial plains. Sedimentary basins where these early rift sediments are preserved can be located by upward continuation of the aeromagnetic profiles across the rift trend and by gravity models. Studies of analog continental rifts and aulacogens show that these gravity models should incorporate (1) a deep mafic rift pillow body to create the narrow gravity high of the MGA, and (2) anomalously thick crust to account for the more regional gravity low. Preserved accumulations of rift clastics in central rift positions can then be modeled to explain the small scale notches which are found within the narrow gravity high. Indigenous oil in Keweenawan sediments in the outcrop area and coaly partings in the subsurface penetrations of the Keweenawan clastics support the analogy between these rift sediments and the exceptionally organic-rich sediments of the East African rift. COCORP data across the rift trend in Kansas show layered deep reflectors and large structures. There is demonstrable source, reservoir, and trap potential within the Keweenawan trend, making the Mid-Continent rift system a frontier hydrocarbon province.

Lee, C.K.; Kerr, S.D. Jr.

1984-04-01T23:59:59.000Z

19

Volcanism of the Kenya Rift Valley [and Discussion  

Science Journals Connector (OSTI)

...research-article Volcanism of the Kenya Rift Valley [and Discussion] B. C. King G. R...Robson R. B. McConnell The Kenya rift valley is a sector of the rift system of eastern...distances of 200 km or more both to the west and east and is broadly centred on the...

1972-01-01T23:59:59.000Z

20

REVIEW Open Access Towards a better understanding of Rift Valley  

E-Print Network [OSTI]

REVIEW Open Access Towards a better understanding of Rift Valley fever epidemiology in the south-west , Matthieu Roger1 and Betty Zumbo7 Abstract Rift Valley fever virus (Phlebovirus, Bunyaviridae be contaminated by close contact with infectious tissues or through mosquito infectious bites. Rift Valley fever

Paris-Sud XI, Université de

Note: This page contains sample records for the topic "haleakala sw rift" 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

Lower-crustal rifting in the Rukwa Graben, East Africa  

Science Journals Connector (OSTI)

......785-803. Foster A.N...African rift system, Tectonics...integrated study of crustal...503-518. Wheeler W.H. , 1994. Structural studies of transform...African rift system, PhD thesis...503-518. Wheeler, W.H...Structural studies of transform...African rift system, PhD thesis......

Ming Zhao; Charles A. Langston; Andrew A. Nyblade; Thomas J. Owens

1997-05-01T23:59:59.000Z

22

Stratigraphy and rifting history of the Mesozoic-Cenozoic Anza rift, Kenya  

SciTech Connect (OSTI)

Lithological and compositional relationships, thicknesses, and palynological data from drilling cuttings from five wells in the Anza rift, Kenya, indicate active rifting during the Late Cretaceous and Eocene-Oligocene. The earlier rifting possibly started in the Santonian-Coniacian, primarily occurred in the Campanian, and probably extended into the Maastrichtian. Anza rift sedimentation was in lacustrine, lacustrine-deltaic, fluvial, and flood-basin environments. Inferred synrift intervals in wells are shalier, thicker, more compositionally immature, and more poorly sorted than Lower Cretaceous ( )-lower Upper Cretaceous and upper Oligocene( )-Miocene interrift deposits. Synrift sandstone is mostly feldspathic or arkosic wacke. Sandstone deposited in the Anza basin during nonrift periods is mostly quartz arenite, and is coarser and has a high proportion of probable fluvial deposits relative to other facies. Volcanic debris is absent in sedimentary strata older than Pliocene-Holocene, although small Cretaceous intrusions are present in the basin. Cretaceous sandstone is cemented in places by laumontite, possibly recording Campanian extension. Early Cretaceous history of the Anza basin is poorly known because of the limited strata sampled; Jurassic units were not reached. Cretaceous rifting in the Anza basin was synchronous with rifting in Sudan and with the breakup and separation of South America and Africa; these events likely were related. Eocene-Oligocene extension in the Anza basin reflects different stresses. The transition from active rifting to passive subsidence in the Anza basin at the end of the Neogene, in turn, records a reconfigured response of east African plates to stresses and is correlated with formation of the East Africa rift.

Winn, R.D. Jr.; Steinmetz, J.C. (Marathon Oil Co., Littleton, CO (United States)); Kerekgyarto, W.L. (Marathon Oil Co., Houston, TX (United States))

1993-11-01T23:59:59.000Z

23

Hualalai Northwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Hualalai Northwest Rift Geothermal Area Hualalai Northwest Rift Geothermal Area (Redirected from Hualalai Northwest Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Hualalai Northwest Rift 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 (9) 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

24

Direct-Current Resistivity Survey At Mauna Loa Northeast Rift...  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Mauna Loa...

25

Gas Flux Sampling At Kilauea East Rift Geothermal Area (Thomas...  

Open Energy Info (EERE)

1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Kilauea East Rift Geothermal Area (Thomas, 1986) Exploration Activity...

26

A Geochemical Model of the Kilauea East Rift Zone | Open Energy...  

Open Energy Info (EERE)

exceeding the Curie point of basalt. The shallow ground-water hydrology and chemistry on the lower rift are strongly affected by natural thermal discharge from the rift...

27

Aedes Mosquito Saliva Modulates Rift Valley Fever Virus Pathogenicity  

E-Print Network [OSTI]

's capacity to effectively transfer arboviruses such as the Cache Valley and West Nile viruses. The roleAedes Mosquito Saliva Modulates Rift Valley Fever Virus Pathogenicity Alain Le Coupanec1 , Divya contro^le, Centre IRD de Montpellier, Montpellier, France Abstract Background: Rift Valley fever (RVF

Boyer, Edmond

28

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical  

Open Energy Info (EERE)

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Characteristics And The Effects Of Gas On Well Performance Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical Characteristics And The Effects Of Gas On Well Performance Details Activities (0) Areas (0) Regions (0) Abstract: This study, which focuses on the Aluto-Langano geothermal field, is part of the ongoing investigations of the geothermal systems in the Ethiopian Rift Valley. Aluto-Langano is a water-dominated gas-rich geothermal field, with a maximum temperature close to 360°C, in the Lakes District region of the Ethiopian Rift Valley. The upflow zone for the system lies along a deep, young NNE trending fault and is characterized by

29

Development Overview of Geothermal Resources In Kilauea East Rift Zone |  

Open Energy Info (EERE)

Development Overview of Geothermal Resources In Kilauea East Rift Zone Development Overview of Geothermal Resources In Kilauea East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Report: Development Overview of Geothermal Resources In Kilauea East Rift Zone Abstract This study reviews the geothermal resources associatedwith the Kilauea East Rift Zone (KERZ) of Hawaii islandby focusing on a holistic development strategy for additionalgeothermal production. A review of existing literature inthe fields of geology, drilling, power production and policychallenges, highlights critical issues for geothermalenterprises. A geological assessment of the hydrology,geochemistry, and structural features that characterize theregion is discussed. Available data are interpreted includinggeology, geochemistry, well depth and temperature.

30

Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Geothermometry Activity Date Usefulness useful DOE-funding Unknown Notes A reexamination of all groundwater sources in the Keaau area was undertaken in an effort to confirm the chemical and temperature anomalies that formed the primary basis on which the Keaau area was identified during the preliminary assessment survey. The data generated by this survey (Table 9) determined that all of the anomalous data present in the earlier data base were spurious and that the groundwater chemistry and temperatures in this

31

Mauna Loa Northeast Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Geothermal Area Mauna Loa Northeast Rift Geothermal Area (Redirected from Mauna Loa Northeast Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Northeast Rift 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 (6) 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

32

Aeromagnetic Survey At Hualalai Northwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Aeromagnetic Survey At Hualalai Northwest Rift Area Aeromagnetic Survey At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic survey data for Hualalai (Godson et al., 1981) clearly indicate an elongate northwest to southeast trending zone of extremely low total magnetic field over the summit region of Hualalai that extends into the upper northwest rift zone. It is extremely unlikely that the summit region is underlain by intrusive material old enough (greater than 700,000 years of age) to have been emplaced during a period of reversed magnetic field; therefore, the only alternative explanation possible (presuming the data are accurate) is that this region is underlain by material with very

33

Remote Sensing for Biodiversity Conservation of the Albertine Rift  

E-Print Network [OSTI]

183 10 Remote Sensing for Biodiversity Conservation of the Albertine Rift in Eastern Africa Samuel of biodiversity conservation is understanding how environmental factors influence species abundance 2003). The rapidly developing field of remote sensing has been invaluable to biodiversity conservation

Wang, Y.Q. "Yeqiao"

34

Thermal and mechanical development of the East African Rift System  

E-Print Network [OSTI]

The deep basins, uplifted flanks, and volcanoes of the Western and Kenya rift systems have developed along the western and eastern margins of the 1300 km-wide East African plateau. Structural patterns deduced from field, ...

Ebinger, Cynthia Joan

1988-01-01T23:59:59.000Z

35

Aluto-Langano Geothermal Field, Ethiopian Rift Valley- Physical...  

Open Energy Info (EERE)

the geothermal systems in the Ethiopian Rift Valley. Aluto-Langano is a water-dominated gas-rich geothermal field, with a maximum temperature close to 360C, in the Lakes...

36

Hydrocarbons in rift basins: the role of stratigraphy  

Science Journals Connector (OSTI)

...versus shallow-water environments...A (1999) Hydrocarbons in rift basins...Facies and hydrocarbon potential The...availability of water. This can either...form seals for hydrocarbons. The shallow-water environ- ments...

1999-01-01T23:59:59.000Z

37

An Integrated Geophysical Study Of The Northern Kenya Rift | Open Energy  

Open Energy Info (EERE)

Kenya Rift Kenya Rift Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: An Integrated Geophysical Study Of The Northern Kenya Rift Details Activities (0) Areas (0) Regions (0) Abstract: The Kenyan part of the East African rift is among the most studied rift zones in the world. It is characterized by: (1) a classic rift valley, (2) sheer escarpments along the faulted borders of the rift valley, (3) voluminous volcanics that flowed from faults and fissures along the rift, and (4) axial and flank volcanoes where magma flow was most intense. In northern Kenya, the rift faults formed in an area where the lithosphere was weakened and stretched by Cretaceous-Paleogene extension, and in central and southern Kenya, it formed along old zones of weakness at the

38

The onshore northeast Brazilian rift basins: An early Neocomian aborted rift system  

SciTech Connect (OSTI)

Early Cretaceous rift basins of northeastern Brazil illustrate key three-dimensional geometries of intracontinental rift systems, controlled mainly by the basement structures. These basins were formed and then abandoned during the early extension associated with the north-south-propagating separation of South America and Africa. During the early Neocomian, extensional deformation jumped from the easternmost basins (group 1: Sergipe Alagoas and Gabon basins; group 2: Reconcavo, Tucano, and Jatoba basins) to the west, forming a series of northeast-trending intracratonic basins (group 3: Araripe, Rio do Peixe, Iguatu, Malhada Vermelha, Lima Campos, and Potiguar basins). The intracratonic basins of groups 2 and 3 consist of asymmetric half-grabens separated by basement highs, transfer faults, and/or accommodation zones. These basins are typically a few tens of kilometers wide and trend northeast-southwest, roughly perpendicular to the main extension direction during the early Neocomian. Preexisting upper crustal weakness zones, like the dominantly northeast-southwest-trending shear zones of the Brazilian orogeny, controlled the development of intracrustal listric normal faults. Internal transverse structures such as transfer faults (Reconcavo basin and onshore Potiguar basin) and accommodation zones (onshore Potiguar basin and Araripe basin) were also controlled by the local basement structural framework. Transverse megafaults and lithostructural associations controlled the three main rift trends. The megashear zones of Pernanbuco (Brazil)-Ngaundere (Africa) apparently behaved like a huge accommodation zone, balancing extensional deformation along the Reconcavo-Jatoba/Sergipe Alagoas-Gabon trends with simultaneous extension along the Araripe-Potiguar trend. The Sergipe Alagoas-Gabon trend and the Potiguar basin represent the site of continued evolution into a marginal open basin following early Neocomian deformation.

Matos, R. (Cornell Univ., Ithaca, NY (USA))

1990-05-01T23:59:59.000Z

39

SEM Supports CMM-SW Level 3 | Department of Energy  

Office of Environmental Management (EM)

CMM-SW Key Process Areas (KPAs) and a crosswalk to the SEM chapters, work products, and web site location where these KPAs are addressed SEM Supports CMM-SW Level 3 More Documents...

40

Aeromagnetic Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Rift Area (Thomas, 1986) Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic data (Godson et al., 1981) for the lower northeast rift of Mauna Loa tend to substantiate this conclusion as well. The lower extension of the rift zone does not exhibit any significant magnetic features that would correspond to a thermal source within the inferred trace of the rift zone. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Aeromagnetic_Survey_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=40242

Note: This page contains sample records for the topic "haleakala sw rift" 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

Standard Insurance Company 1100 SW Sixth Avenue  

E-Print Network [OSTI]

Standard Insurance Company 1100 SW Sixth Avenue Portland OR 97204 www.standard.com Electronic Evidence Of Insurability Save Time: Provide Medical History Statements Online Standard Insurance Company is complete, allowing The Standard to begin the underwriting process immediately. The Web form is secure

Block, Louis

42

Magnetotellurics At Kilauea East Rift Area (Laney, 2005) | Open Energy  

Open Energy Info (EERE)

Magnetotellurics At Kilauea East Rift Area (Laney, Magnetotellurics At Kilauea East Rift Area (Laney, 2005) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes Magnetotelluric Imaging, G. Michael Hoversten. The project title derived from its inception. The project however moved from the application of MT on Kilauea in 2003 to the use of combined SP and conductivity mapping (MT) in 2004. The beginning of 2004 saw the completions of the Kilauea MT experiment by the acquisition of an additional 45 MT stations on Kilauea. We therefore decided to use the funds available to work at the Fort Bidwell Indian reservation where characterization work could be done at relatively low cost. We decided to perform a time lapse SP survey during a flow test

43

Kilauea Southwest Rift And South Flank Geothermal Area | Open Energy  

Open Energy Info (EERE)

Kilauea Southwest Rift And South Flank Geothermal Area Kilauea Southwest Rift And South Flank Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea Southwest Rift And South Flank 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 (8) 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.

44

Thermal Gradient Holes At Hualalai Northwest Rift Area (Thomas, 1986) |  

Open Energy Info (EERE)

Hualalai Northwest Rift Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Thermal Gradient Holes Activity Date Usefulness not useful DOE-funding Unknown Notes Although not part of the current effort, two deep (approximately 2000 m) exploratory wells were drilled on the north flank of Hualalai near Puu Waawaa cinder cone. The geophysical data used for siting these wells were proprietary and hence unavailable for publication; however, the temperatures measured at the bottoms of the wells were reported to be below 20degrees C. Chemical analysis of water samples taken from these wells did not provide useful geothermal data due to contamination of the well water with drilling muds References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

45

Mauna Loa Northeast Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Geothermal Area Mauna Loa Northeast Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Northeast Rift 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 (6) 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

46

Mauna Loa Southwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Mauna Loa Southwest Rift Geothermal Area Mauna Loa Southwest Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Mauna Loa Southwest Rift 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 (2) 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

47

Hualalai Northwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Hualalai Northwest Rift Geothermal Area Hualalai Northwest Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Hualalai Northwest Rift 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 (9) 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

48

Kilauea Southwest Rift And South Flank Geothermal Area | Open Energy  

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 » Kilauea Southwest Rift And South Flank Geothermal Area (Redirected from Kilauea Southwest Rift And South Flank Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea Southwest Rift And South Flank 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 (8) 10 References Area Overview Geothermal Area Profile Location: Hawaii

49

Direct-Current Resistivity Survey At Hualalai Northwest Rift Area (Thomas,  

Open Energy Info (EERE)

Hualalai Northwest Rift Area (Thomas, Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes A total of seven Schlumberger soundings were performed on Hualalai. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Direct-Current_Resistivity_Survey_At_Hualalai_Northwest_Rift_Area_(Thomas,_1986)&oldid=510528" Category: Exploration Activities What links here Related changes

50

Kilauea East Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Kilauea East Rift Geothermal Area Kilauea East Rift Geothermal Area (Redirected from Kilauea East Rift Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea East Rift 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 Heat Source 8 Geofluid Geochemistry 9 NEPA-Related Analyses (0) 10 Exploration Activities (28) 11 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":19.47836,"lon":-154.8883,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

51

Hydrocarbons in rift basins: the role of stratigraphy  

Science Journals Connector (OSTI)

...succession that causes the shales to reach thermal maturity and generate hydrocarbons. Simple...T. J. 1988 Rift basins of interior Sudan--petroleum exploration and discovery...basins? Is that what we could call the thermal subsidence phase? J. J. Lambiase...

1999-01-01T23:59:59.000Z

52

On the nature of SW Sex  

E-Print Network [OSTI]

We present spectrophotometry of the eclipsing nova-like variable SW Sex. The continuum is deeply eclipsed and shows asymmetries due to the presence of a bright spot. We derive a new ephemeris and, by measuring the eclipse width, we are able to constrain the inclination to i > 75^o and the disc radius to R_D > 0.6 L_1. In common with other members of its class (of which it is the proto-type), SW Sex shows single-peaked emission lines which show transient absorption features and large phase shifts in their radial velocity curves. In addition, the light curves of the emission lines show a reduction in flux around phase 0.5 and asymmetric eclipse profiles which are not as deep as the continuum eclipse. Using Doppler tomography, we find that most of the line emission in SW Sex appears to originate from three sources: the secondary star, the accretion disc and an extended bright spot. The detection of the red star allows us to constrain the radial-velocity semi-amplitude of the secondary to K_R > 180 km/s and hence the component masses to M_1 = 0.3-0.7 Msun and M_2 < 0.3 Msun.

V. S. Dhillon; T. R. Marsh; D. H. P. Jones

1997-09-17T23:59:59.000Z

53

Watermark: Proposed Penalty (2011-SW-2908) | Department of Energy  

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

Proposed Penalty (2011-SW-2908) Proposed Penalty (2011-SW-2908) Watermark: Proposed Penalty (2011-SW-2908) May 10, 2012 DOE alleged in a Notice of Proposed Civil Penalty that Watermark Designs, Ltd. manufactured and distributed noncompliant showerhead basic model SH-FAL90 in the U.S. Federal law subjects manufacturers and private labelers to civil penalties if those parties distribute in the U.S. products that do not meet applicable water conservation standards. This civil penalty notice advises the company of the potential penalties and DOE's administrative process, including the company's right to a hearing. Watermark: Proposed Penalty (2011-SW-2908) More Documents & Publications Watermark: Order (2011-SW-2908) Watermark: Noncompliance Determination (2011-SW-2908) ET Industries: Proposed Penalty (2012-SE-2902

54

Magnetotellurics At Kilauea Southwest Rift And South Flank Area (Laney,  

Open Energy Info (EERE)

Laney, Laney, 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Kilauea Southwest Rift And South Flank Area (Laney, 2005) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes Magnetotelluric Imaging, G. Michael Hoversten. The project title derived from its inception. The project however moved from the application of MT on Kilauea in 2003 to the use of combined SP and conductivity mapping (MT) in 2004. The beginning of 2004 saw the completions of the Kilauea MT experiment by the acquisition of an additional 45 MT stations on Kilauea. We therefore decided to use the funds available to work at the Fort Bidwell

55

Upstream -- SW92-03&  

Office of Legacy Management (LM)

09 09 This page intentionally left blank Upstream -- SW00-01 a _______________________________________________________________________________________________________________________________________________ Analyte Unit 04/18/00 07/17/00 10/20/00 04/17/01 07/11/01 10/09/01 04/07/05 10/05/05 04/28/06 10/02/06 04/11/07 10/08/07 04/09/08 g _______________________________________________________________________________________________________________________________________________ Field Measurements Alkalinity b mg/L 196 130 263 218 196 98 145 202 228 183 227 186 213 Conductivity c μmhos/cm 1544 847 8190 792 652 632 562 1389 1011 1332 959 1157 613

56

Haleakala Volcano Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Date: Well Name: Location: Depth: Initial Flow Rate: "cf" is not declared as a valid unit of measurement for this property. The given value was not understood. Flow Test...

57

Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) | Open  

Open Energy Info (EERE)

Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Magnetics At Kilauea East Rift Area (Leslie, Et Al., 2004) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Ground Magnetics Activity Date Usefulness useful DOE-funding Unknown Notes Paper states "magnetic data" - no further clarification regarding type of magnetic survey. References Stephen C. Leslie, Gregory F. Moore, Julia K. Morgan (2004) Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Ground_Magnetics_At_Kilauea_East_Rift_Area_(Leslie,_Et_Al.,_2004)&oldid=390100"

58

Self Potential At Mauna Loa Southwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Southwest Rift Area (Thomas, 1986) Southwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Self Potential At Mauna Loa Southwest Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Southwest Rift Area Exploration Technique Self Potential Activity Date Usefulness not indicated DOE-funding Unknown Notes Field surveys in the South Point area were limited to a series of Schlumberger soundings and a self-potential traverse across the rift zone. The absence of groundwater wells and time and funding constraints precluded any geochemical field surveys. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Self_Potential_At_Mauna_Loa_Southwest_Rift_Area_(Thomas,_1986)&oldid=389751

59

A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano,  

Open Energy Info (EERE)

A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii Jump to: navigation, search OpenEI Reference LibraryAdd to library == A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, HawaiiThesis/Dissertation == Author Catherine King Skokan Organization Colorado School of Mines Published Publisher Not Provided, 1974 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii Citation [[Citation::Catherine King Skokan. 1974. A Time-Domain Electromagnetic Survey of the East Rift Zone Kilauea Volcano, Hawaii []. [ (!) ]: Colorado School of Mines.]] Retrieved from "http://en.openei.org/w/index.php?title=A_Time-Domain_Electromagnetic_Survey_of_the_East_Rift_Zone_Kilauea_Volcano,_Hawaii&oldid=682585"

60

Field Mapping At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Field Mapping At Kilauea East Rift Area (Thomas, Field Mapping At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Field Mapping Activity Date Usefulness useful DOE-funding Unknown Notes Geologic mapping on the East Rift Zone (ERZ) conducted by Peterson (1967), J. Moore (1971), and Wright and Fiske (1971) detailed historic lava flows originating in the ERZ and developed structural models of the rift based on the locations and progressions of recorded eruptive cycles. These studies have more recently been expanded by Holcomb (1980, 1981) and R. Moore (1982, 1983) who have presented more detailed mapping of all surface flows (historic and prehistoric), fissures and faulting on the eastern flank of the Kilauea shield. The model developed from these studies is of a rift

Note: This page contains sample records for the topic "haleakala sw rift" 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

Refraction Survey At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Refraction Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Refraction Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Seismic refraction surveys conducted by Broyles and Furumoto (1978) and Suyenaga et al. (1978) developed a cross-sectional model of the rift zone near the present site of HGP-A that proposed a 12- 17 km wide dike complex lying at a depth of 2 to 3 km (Fig. 51). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Refraction_Survey_At_Kilauea_East_Rift_Area_(Thomas,_1986)&oldid=386690"

62

Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60 m a.s.l, and located north of a prehistoric fissure, and a low-resistivity deep basement (20 m a.s.1.) to

63

Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area  

Open Energy Info (EERE)

Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60 m a.s.l, and located north of a prehistoric fissure, and a low-resistivity deep basement (20 m a.s.1.) to the south and east of this fissure (Figs 48, 49). These data suggest that a

64

A geochemical model of the Kilauea east rift zone | Open Energy Information  

Open Energy Info (EERE)

A geochemical model of the Kilauea east rift zone A geochemical model of the Kilauea east rift zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: A geochemical model of the Kilauea east rift zone Abstract N/A Author Donald Thomas Published Journal US Geological Survey Professional Paper 1350, 1987 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for A geochemical model of the Kilauea east rift zone Citation Donald Thomas. 1987. A geochemical model of the Kilauea east rift zone. US Geological Survey Professional Paper 1350. (!) . Retrieved from "http://en.openei.org/w/index.php?title=A_geochemical_model_of_the_Kilauea_east_rift_zone&oldid=682589" Categories: Missing Required Information References Uncited References Geothermal References

65

SwRI's HEDGE Technology for High Efficiency, Low Emissions Gasoline...  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

SwRI's HEDGE Technology for High Efficiency, Low Emissions Gasoline Engines SwRI's HEDGE Technology for High Efficiency, Low Emissions Gasoline Engines Presentation given at the...

66

Core Holes At Kilauea East Rift Geothermal Area (Bargar, Et Al...  

Open Energy Info (EERE)

Activity Details Location Kilauea East Rift Geothermal Area Exploration Technique Core Holes Activity Date 1989 - 1991 Usefulness useful DOE-funding Unknown Exploration...

67

Connection of the Panama fracture zone with the Galapagos rift zone, eastern tropical Pacific  

Science Journals Connector (OSTI)

Magnetic data recently collected in the eastern tropical Pacific confirm that the Galapagos rift zone is connected to the Panama fracture zone by a short north-south...

Paul J. Grim

1970-08-01T23:59:59.000Z

68

Architecture of turbidite sandstone bodies in a rift-lake setting, Gabon Basin, offshore Gabon  

Science Journals Connector (OSTI)

The Lower Cretaceous Lucina Formation, part of the lacustrine syn-rift fill of the Gabon Basin, contains both channelized and non-channelized...c. 200 m.

R. D. A. Smith

1995-01-01T23:59:59.000Z

69

Integrating metrics in an ontological framework supporting SW-FMEA  

Science Journals Connector (OSTI)

The development process of safety-critical systems benefits from the early identification of failures affecting them. Several techniques have been designed in order to face this issue, among them Failure Mode Effect Analysis (FMEA). Although FMEA has ... Keywords: SW engineering, SW metrics, automated reasoning, dependability and safety, failure mode effects analysis (FMEA), ontologies

Irene Bicchierai, Giacomo Bucci, Carlo Nocentini, Enrico Vicario

2012-06-01T23:59:59.000Z

70

An ontological approach to systematization of SW-FMEA  

Science Journals Connector (OSTI)

Failure Mode and Effects Analysis (FMEA) is a widely used dependability and safety technique aiming at systematically identifying failure modes, their generating causes and their effects on the system. While FMEA has been mainly thought for hardware ... Keywords: SW engineering, SW-FMEA, V-model, automated reasoning, ontologies, reliability availability maintainability and safety

Irene Bicchierai; Giacomo Bucci; Carlo Nocentini; Enrico Vicario

2012-09-01T23:59:59.000Z

71

SW MICHIGAN APPLE MATURITY REPORT ISSUE 1 August 25, 2010  

E-Print Network [OSTI]

SW MICHIGAN APPLE MATURITY REPORT ISSUE 1 ­ August 25, 2010 Bill Shane, Diane Brown-Rytlewski, and Mark Longstroth Michigan State University This is the first of weekly apple maturity report for SW. See the Michigan State University apple web site (apples.msu.edu) for more information, including

72

S.W. Williston Diptera Research Fund November 4, 2013  

E-Print Network [OSTI]

1 S.W. Williston Diptera Research Fund November 4, 2013 The S.W. Williston Diptera Research Fund about Diptera. Samuel Wendell Williston (Fig. 1) was a great biologist, who made significant achievements epitomize what this fund was established to support. The Williston Fund is administered

Mathis, Wayne N.

73

Geophysical and Structural Aspects of the Central Red Sea Rift Valley  

Science Journals Connector (OSTI)

...Structural Aspects of the Central Red Sea Rift Valley F. K. Kabbani Eight aeromagnetic traverses...trend northwesterly beginning immediately west of the 1000 m bathymetric contour. Depth...structural aspects of the central Red Sea rift valley Kabbani F. K. Author 89 97 A discussion...

1970-01-01T23:59:59.000Z

74

A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica  

Science Journals Connector (OSTI)

......ARB, Adelie Rift Block; BB, Bight Basin; BC, Budd Coast; CWL, central...and post-rift sediments of the Bight Basin is interpreted at the base of the...and GA-199/09) across the Bight Basin (Fig. 1). The parameters utilized......

D. I. Close; A. B. Watts; H. M. J. Stagg

2009-05-01T23:59:59.000Z

75

Time-Domain Electromagnetics At Kilauea Southwest Rift And South Flank Area  

Open Energy Info (EERE)

And South Flank Area And South Flank Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Time-Domain Electromagnetics At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes The assessment effort consisted of a reexamination of existing Schlumberger sounding (Hussong and Cox, 1967; Adams et al., 1970) and time-domain electromagnetic (Klein and Kauahikaua, 1975) data for the rift area (Kauahikaua and Mattice, 1981) The electrical resistivity data acquired on the southwest rift delineated two distinct basement resistivity structures northwest of the rift zone: a high-resistivity basement at approximately 60

76

Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano,  

Open Energy Info (EERE)

Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii Jump to: navigation, search OpenEI Reference LibraryAdd to library : Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, HawaiiInfo Graphic/Map/Chart Authors Frank A. Trusdell and Richard B. Moore Published U.S. GEOLOGICAL SURVEY, 2006 DOI Not Provided Check for DOI availability: http://crossref.org Online Internet link for Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii Citation Frank A. Trusdell,Richard B. Moore. Geologic Map of the Middle East Rift Geothermal Subzone, Kilauea Volcano, Hawaii. []. Place of publication not provided. U.S. GEOLOGICAL SURVEY. 2006. Available from: http://pubs.usgs.gov/imap/2614/downloads/pdf/2614map_508.pdf.

77

Direct-Current Resistivity At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Electrical resistivity studies performed on the Kilauea East Rift Zone have employed a variety of techniques. Bipole mapping was conducted by Keller et al. (1977a) as part of the Hawaii Geothermal Project (HGP) geoscience program and was able to provide data on the regional resistivity structure of the summit and eastern flank of Kilauea. The model developed indicated several different types of resistivity sections depending on the location

78

Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone  

Open Energy Info (EERE)

Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Internal Structure Of Puna Ridge- Evolution Of The Submarine East Rift Zone Of Kilauea Volcano, Hawaii Details Activities (3) Areas (1) Regions (0) Abstract: Multichannel seismic reflection, sonobuoy, gravity and magnetics data collected over the submarine length of the 75 km long Puna Ridge, Hawaii, resolve the internal structure of the active rift zone. Laterally continuous reflections are imaged deep beneath the axis of the East Rift Zone (ERZ) of Kilauea Volcano. We interpret these reflections as a layer of abyssal sediments lying beneath the volcanic edifice of Kilauea. Early

79

Gas Flux Sampling At Kilauea East Rift 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 » Gas Flux Sampling At Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes Radon emanometry data for the same locality (Fig. 61) (Cox, 1980) similarly presented a complicated pattern of radon outgassing along the lower rift zone. Even though complexities are present within the rift zone, there

80

Direct-Current Resistivity Survey At Kilauea East Rift Area (Thomas, 1986)  

Open Energy Info (EERE)

Kilauea East Rift Area (Thomas, 1986) Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Electrical resistivity studies performed on the Kilauea East Rift Zone have employed a variety of techniques. Bipole mapping was conducted by Keller et al. (1977a) as part of the Hawaii Geothermal Project (HGP) geoscience program and was able to provide data on the regional resistivity structure of the summit and eastern flank of Kilauea. The model developed indicated several different types of resistivity sections depending on the location

Note: This page contains sample records for the topic "haleakala sw rift" 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

Aeromagnetic Survey At Kilauea Southwest Rift And South Flank Area (Thomas,  

Open Energy Info (EERE)

Thomas, Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Kilauea Southwest Rift And South Flank Area (Thomas, 1986) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes Aeromagnetic data (Godson et al., 1981) for the southwest rift appears to substantiate the presence of a thermal resource; there is a marked bipolar magnetic anomaly paralleling the rift zone from the summit to the lower rift near the coast suggesting either that intense hydrothermal alteration has occurred or that subsurface temperatures exceed the Curie temperature. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

82

Mercury Vapor At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Kilauea East Rift Area (Thomas, Mercury Vapor At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The sampling network for soil mercury concentrations undertaken by Cox (1981) identified a complicated pattern of mercury concentrations throughout the lower Puna area (Fig. 60). The highest soil mercury concentrations found were generally located within the rift zone, but an analysis of the data showed that soil type and soil pH also had a marked impact on mercury concentration. Making corrections for these effects improved the correspondence between the surface geological expression of the rift zone and the mercury concentrations observed; interpretation of

83

Ground Gravity Survey At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Ground Gravity Survey At Kilauea East Rift Area Ground Gravity Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Ground Gravity Survey Activity Date Usefulness useful DOE-funding Unknown Notes This model was later expanded through the examination of detailed and regional gravity data (Krivoy and Eaton, 1961) and regional aeromagnetic data (Malahoff and Woollard, 1966) to a three-dimensional map of the rift zone (Furumoto, 1978b). This model projected a dike complex (presumably at high temperatures) which has a width of approximately 20 km near the summit of Kilauea that narrows to approximately 12 km at the lower quarter of the subaerial portion of the rift (Fig. 52). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

84

Mercury Vapor At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mauna Loa Northeast Rift Area (Thomas, 1986) Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes Soil mercury and radon emanometry sampling conducted in the Keaau prospect were similarly unable to define any anomalies that could reasonably be interpreted to be due to subsurface thermal effects. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Mercury_Vapor_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=390060

85

Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The Hualalai lower northwest rift and southern flank were sampled for soil mercury concentration and radon emanation rates (Cox and Cuff, 1981d). The data generated by these surveys yielded complex patterns of mercury concentrations and radon emanation rates that generally did not show coincident anomalies (Figs 42, 43). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

86

Isotopic Analysis At Kilauea East Rift Area (Quane, Et Al., 2000) | Open  

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 » Isotopic Analysis At Kilauea East Rift Area (Quane, Et Al., 2000) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Isotopic Analysis- Rock At Kilauea East Rift Area (Quane, Et Al., 2000) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Isotopic Analysis- Rock Activity Date Usefulness not indicated DOE-funding Unknown References S. L. Quane, M. O. Garcia, H. Guillou, T. P. Hulsebosch (2000) Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Retrieved from "http://en.openei.org/w/index.php?title=Isotopic_Analysis_At_Kilauea_East_Rift_Area_(Quane,_Et_Al.,_2000)&oldid=687735"

87

Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Thermal Gradient Holes At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Thermal Gradient Holes Activity Date Usefulness useful DOE-funding Unknown Notes Two separate phases of geothermal exploratory drilling have occurred on the lower East Rift. The first was essentially a wildcat venture with relatively little surface exploratory data having been gathered, whereas the second was initiated after somewhat more geoscience information had been acquired under the Hawaii Geothermal Project. The results of the successful exploratory drilling program on the Kilauea

88

Ground Gravity Survey At Rio Grande Rift Region (Aiken & Ander, 1981) |  

Open Energy Info (EERE)

Rio Grande Rift Region (Aiken & Ander, 1981) Rio Grande Rift Region (Aiken & Ander, 1981) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Rio Grande Rift Region (Aiken & Ander, 1981) Exploration Activity Details Location Rio Grande Rift Geothermal Region Exploration Technique Ground Gravity Survey Activity Date Usefulness useful DOE-funding Unknown References Carlos L.V. Aiken, Mark E. Ander (1981) A Regional Strategy For Geothermal Exploration With Emphasis On Gravity And Magnetotellurics Retrieved from "http://en.openei.org/w/index.php?title=Ground_Gravity_Survey_At_Rio_Grande_Rift_Region_(Aiken_%26_Ander,_1981)&oldid=401473" Category: Exploration Activities What links here Related changes Special pages Printable version

89

Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes Soil mercury and radon emanometry sampling conducted in the Keaau prospect were similarly unable to define any anomalies that could reasonably be interpreted to be due to subsurface thermal effects. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Gas_Flux_Sampling_At_Mauna_Loa_Northeast_Rift_Area_(Thomas,_1986)&oldid=389039"

90

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From  

Open Energy Info (EERE)

Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Seismic And Gravity Data Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Structure Of The Lower East Rift Zone Of Kilauea Volcano, Hawaii, From Seismic And Gravity Data Details Activities (2) Areas (1) Regions (0) Abstract: Two seismic refraction surveys were carried out in 1976 and 1977 on the east rift zone of Kilauea volcano as part of an exploratory program for geothermal resources. The short traverse seismic refraction survey of January 1976 delineated the upper surface structure of the east rift, revealing velocities of 2.5 km/s under the Kalapana line and 3.1 km/s under the Leilani line beneath a surface layer of low, but variable velocity. This survey was not successful in determining the depth of the

91

Gas Flux Sampling At Hualalai Northwest Rift Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Hualalai Northwest Rift Area (Thomas, 1986) Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes The Hualalai lower northwest rift and southern flank were sampled for soil mercury concentration and radon emanation rates (Cox and Cuff, 1981d). The data generated by these surveys yielded complex patterns of mercury concentrations and radon emanation rates that generally did not show coincident anomalies (Figs 42, 43). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

92

Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Self Potential At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Self Potential Activity Date Usefulness not indicated DOE-funding Unknown Notes Self-potential surveys conducted over the summit and flank of Hualalai (Jackson and Sako, 1982; D. B. Jackson, pers. commun., 1983) indicate an elongate self-potential anomaly extending across the summit and down the northwest rift to Kaupulehu Crater. The positively polarized anomaly extends over an area of approximately 6 km 2 and has been interpreted to be the result of one or more buried high-temperature intrusive bodies (Jackson

93

Zoe Industries: Noncompliance Determination (2011-SW-2912) | Department of  

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

Zoe Industries: Noncompliance Determination (2011-SW-2912) Zoe Industries: Noncompliance Determination (2011-SW-2912) Zoe Industries: Noncompliance Determination (2011-SW-2912) September 28, 2011 DOE issued a Notice of Noncompliance Determination to Zoe Industries, Inc. finding that Giessdorf 150043 model, a showerhead, does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Zoe must immediately notify each person (or company) to whom Zoe distributed the noncompliant products that the product does not meet Federal standards. In addition, Zoe must provide to DOE documents and records showing the number of units Zoe distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil penalties. Zoe Industries: Noncompliance Determination (2011-SW-2912)

94

Hudson-Reed: Noncompliance Determination (2011-SW-2909) | Department of  

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

Noncompliance Determination (2011-SW-2909) Noncompliance Determination (2011-SW-2909) Hudson-Reed: Noncompliance Determination (2011-SW-2909) September 28, 2011 DOE issued a Notice of Noncompliance Determination, finding that Hudson-Reed Limited's "HEAD16" showerhead does not meet the applicable water conservation standard. DOE determined the showerhead was noncompliant based on DOE testing. Hudson-Reed must immediately notify each person (or company) to whom Hudson-Reed distributed the noncompliant products that the product does not meet Federal standards. In addition, Hudson-Reed must provide to DOE documents and records showing the number of units Hudson-Reed distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil penalties. Hudson-Reed: Noncompliance Determination (2011-SW-2909)

95

Kilauea East Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Kilauea East Rift Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Kilauea East Rift 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 Heat Source 8 Geofluid Geochemistry 9 NEPA-Related Analyses (0) 10 Exploration Activities (28) 11 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":19.47836,"lon":-154.8883,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

96

Compound and Elemental Analysis At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Flank Flank Area (Coombs, Et Al., 2006) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Compound and Elemental Analysis At Kilauea Southwest Rift And South Flank Area (Coombs, Et Al., 2006) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Compound and Elemental Analysis Activity Date Usefulness not indicated DOE-funding Unknown References Michelle L. Coombs, Thomas W. Sisson, Peter W. Lipman (2006) Growth History Of Kilauea Inferred From Volatile Concentrations In Submarine-Collected Basalts Retrieved from "http://en.openei.org/w/index.php?title=Compound_and_Elemental_Analysis_At_Kilauea_Southwest_Rift_And_South_Flank_Area_(Coombs,_Et_Al.,_2006)&oldid=510423"

97

Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan, Et Al.,  

Open Energy Info (EERE)

Morgan, Et Al., Morgan, Et Al., 2010) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan, Et Al., 2010) Exploration Activity Details Location Rio Grande Rift Geothermal Region Exploration Technique Data Acquisition-Manipulation Activity Date Usefulness useful regional reconnaissance DOE-funding Unknown Notes San Luis Basin (south-central CO) regional study. References Paul Morgan, Peter Barkmann, Charles Kluth, Matthew Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Retrieved from "http://en.openei.org/w/index.php?title=Data_Acquisition-Manipulation_At_Rio_Grande_Rift_Region_(Morgan,_Et_Al.,_2010)&oldid=401472" Category: Exploration

98

Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island | Open  

Open Energy Info (EERE)

Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Geoelectric Studies on the East Rift, Kilauea Volcano, Hawaii Island Abstract Three geophysical research organizations, working together under the auspices of the Hawaii Geothermal Project, have used several electrical and electromagnetic exploration techniques on Kilauea volcano, Hawaii to assess its geothermal resources. This volume contains four papers detailing their methods and conclusions. Keller et al. of the Colorado School of Mines used the dipole mapping and time-domain EM sounding techniques to define low resistivity areas around the summit and flanks of Kilauea. Kauahikaua and Klein of the Hawaii Institute of Geophysics then detailed the East Rift

99

Time-Domain Electromagnetics At Kilauea East Rift Area (Thomas, 1986) |  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Kilauea East Rift Time-Domain Electromagnetics At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes A series of time-domain electromagnetic (TDEM) soundings were also performed in the lower East Rift Zone as part of the HGP exploration program (Klein and Kauahikaua, 1975; Kauahikaua and Klein, 1977); this work was recently expanded to include additional TDEM and vertical electrical soundings, and the entire data set was reinterpreted (Kauahikaua, 1981b; Kauahikaua and Mattice, 1981). The resistivity model presented by Kauahikaua (1981b) suggests that moderate to high basement resistivities, corresponding to cold freshwater saturated basalts, are present north of

100

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On  

Open Energy Info (EERE)

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From Soh 1 Details Activities (4) Areas (1) Regions (0) Abstract: Deep drilling has allowed for the first time an examination of most of the shield stage of a Hawaiian volcano when it is centered over the hotspot and most of its volume is produced. We determined the lithologies, ages, geochemical characteristics and accumulation rates of rocks from the continuously cored, ~1.7 km deep Scientific Observation Hole (SOH) 1, which was drilled into Kilauea's East Rift Zone. The uppermost ~750 m of this hole contain relatively unaltered subaerially quenched lavas; the lower

Note: This page contains sample records for the topic "haleakala sw rift" 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

Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) |  

Open Energy Info (EERE)

Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Static Temperature Survey At Kilauea East Rift Area (Rudman & Epp, 1983) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Static Temperature Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Drilling of HGP-A was completed on April 28, 1976. An equilibrium temperature was not measured in HGP-A; the well was flashed before the drilling disturbance was dissipated. However, before the mud was pumped out, temperatures in the well were measured at 15, 75, 97,145, and 193 hours, and at 13, 21, and 22 days after circulation of the drilling mud stopped. These temperature data are shown in Fig. 2. Between 305 m and 914

102

History and Results of Surface Exploration in the Kilauea East Rift Zone |  

Open Energy Info (EERE)

History and Results of Surface Exploration in the Kilauea East Rift Zone History and Results of Surface Exploration in the Kilauea East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: History and Results of Surface Exploration in the Kilauea East Rift Zone Abstract Government-funded surveys of the Kilauea East Rift Zone have resulted in a wealth of geophysical and geochemical data from an active volcanic area. All data are clearly of academic interest; Hawaii was used as a testing ground for various geophysical methods in the early days of geothermal exploration. Some surveys, such as gravity and magnetic, are useful a regional perspective for determining broad structural trends and grossly identifying magmatic intrusions. Seismic data are currently being used for a more sitespecific purpose: to determine fault locations and geometries.

103

Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank  

Open Energy Info (EERE)

Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Area (Wyss, Et Al., 2001) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Teleseismic-Seismic Monitoring At Kilauea Southwest Rift And South Flank Area (Wyss, Et Al., 2001) Exploration Activity Details Location Kilauea Southwest Rift And South Flank Area Exploration Technique Teleseismic-Seismic Monitoring Activity Date Usefulness could be useful with more improvements DOE-funding Unknown Notes In spite of the complications discovered in this b-value analysis of Kilauea's South Flank, there are many similarities with the case histories of the other volcanoes we have studied, and the correlation of high b-value anomalies withmagma reservoirs is confirmed.

104

Self Potential At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Self Potential At Kilauea East Rift Area (Thomas, Self Potential At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Self Potential Activity Date Usefulness useful DOE-funding Unknown Notes An extensive network of self-potential surveys have been performed over the summit and flanks of Kilauea as part of the HGP exploration surveys and in separate studies of the source mechanism for the potential anomalies observed (Zablocki, 1976, 1977). The geothermal exploration surveys were performed primarily on the lower East Rift Zone and identified four separate self-potential anomalies (Fig. 59) (Zablocki, 1977). The source mechanism for the anomalies observed was inferred to be the result of electrokinetic phenomena; thermal groundwater escaping from a geothermal

105

Micro-Earthquake At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Micro-Earthquake At Kilauea East Rift Area (Thomas, Micro-Earthquake At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Micro-Earthquake Activity Date Usefulness not indicated DOE-funding Unknown Notes Microseismic and ground noise studies were performed along the East Rift Zone in an effort to identify areas in which earthquake activity might suggest rock fracturing as a result of cold water coming into contact with heated reservoir rocks (Furumoto, 1978a). One of the microseismic surveys utilized an array of seven seismometers to monitor earthquake activity in the vicinity of the then proposed site of the HGP-A well (Fig. 53) (Suyenaga and Furumoto, 1978). The second microearthquake study utilized only two seismometers located near the junction of the Pahoa-Kalapana and

106

Water Sampling At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Water Sampling At Kilauea East Rift Area (Thomas, Water Sampling At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Water Sampling Activity Date Usefulness useful DOE-funding Unknown Notes Studies of groundwater and coastal spring- sources that have identified thermal fluids on the lower East Rift Zone date back to the early part of this century (Guppy, 1906). More recent investigations of temperature and groundwater chemistry were performed for the HGP geoscience program (Macdonald, 1977; McMurtry et al., 1977; Epp and Halunen, 1979). Epp and Halunen (1979) identified several warm water wells, one having a temperature in excess of 90degrees C, and coastal springs in lower Puna; temperature profiles obtained by this study indicated that in some

107

Magmatic History Of The East Rift Zone Of Kilauea Volcano, Hawaii...  

Open Energy Info (EERE)

History Of The East Rift Zone Of Kilauea Volcano, Hawaii Based On Drill Core From SOH 1 Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Magmatic...

108

Climate-driven variations in geothermal activity in the northern Kenya rift valley  

Science Journals Connector (OSTI)

... In the northern Kenya rift valley, geothermal activity is associated with a series of Quaternary volcanoes (Fig. 1). Hot, ... tables, a consequence of the semi-arid to arid climate of the region.

N. C. Sturchio; P. N. Dunkley; M. Smith

1993-03-18T23:59:59.000Z

109

AUSTRALIAN-ANTARCTIC RIFTING PESA Eastern Australasian Basins Symposium III Sydney, 1417 September, 2008 271  

E-Print Network [OSTI]

AUSTRALIAN-ANTARCTIC RIFTING PESA Eastern Australasian Basins Symposium III Sydney, 14­17 September Bight region to chron 20 farther to the west (Sayers et al. 2001; Colwell et al. 2006). Alternatively

Müller, Dietmar

110

Long-term changes in chemical features of waters of seven Ethiopian rift-valley lakes  

Science Journals Connector (OSTI)

Chemical and chlorophyll a concentrations of seven Ethiopian rift-valley lakes were studied during 19902000. Results ... 1960 and 1990 in an attempt to detect long-term changes. Three different trends are appare...

G. M. Zinabu; Elizabeth Kebede-Westhead; Zerihun Desta

2002-06-01T23:59:59.000Z

111

Direct-Current Resistivity Survey At Mauna Loa Southwest Rift Area (Thomas,  

Open Energy Info (EERE)

Area (Thomas, Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Mauna Loa Southwest Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Southwest Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Field surveys in the South Point area were limited to a series of Schlumberger soundings and a self-potential traverse across the rift zone. The absence of groundwater wells and time and funding constraints precluded any geochemical field surveys. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Direct-Current_Resistivity_Survey_At_Mauna_Loa_Southwest_Rift_Area_(Thomas,_1986)&oldid=510541"

112

E-Print Network 3.0 - african rift system Sample Search Results  

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

.H. Baker, P.A. Mohr and L.A.J. Williams, Geology of the eastern rift system of Africa, Geol. Soc. Am., Spec... .V., Amsterdam - Printed in The Netherlands 5 Small-scale...

113

Watermark: Noncompliance Determination (2011-SW-2908) | Department of  

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

Noncompliance Determination (2011-SW-2908) Noncompliance Determination (2011-SW-2908) Watermark: Noncompliance Determination (2011-SW-2908) September 26, 2011 DOE issued a Notice of Noncompliance Determination to Watermark Designs, Ltd. finding that model SH-FAL-90, a showerhead, does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Watermark Designs must immediately notify each person (or company) to whom Watermark Designs distributed the noncompliant products that the product does not meet Federal standards. In addition, Watermark Designs must provide to DOE documents and records showing the number of units Watermark Designs distributed and to whom. The manufacturer and/or private labeler of the product may be subject to civil

114

Patterson: Noncompliance Determination (2011-SW-2911) | Department of  

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

Patterson: Noncompliance Determination (2011-SW-2911) Patterson: Noncompliance Determination (2011-SW-2911) Patterson: Noncompliance Determination (2011-SW-2911) July 12, 2013 DOE issued a Notice of Noncompliance Determination to Dan Patterson finding that the "ThunderHead" showerhead basic model manufactured by ET Industries, Inc. and imported by Dan Patterson does not comport with the water conservation standards. DOE determined the product was noncompliant based on DOE testing. Patterson must immediately notify each person (or company) to whom Patterson distributed the noncompliant products that the product does not meet Federal standards. In addition, Patterson must provide to DOE documents and records showing the number of units Patterson distributed and to whom. The manufacturer and/or private labeler of the

115

Sioux Valley SW Elec Coop | Open Energy Information  

Open Energy Info (EERE)

SW Elec Coop SW Elec Coop Jump to: navigation, search Name Sioux Valley SW Elec Coop Place Colman, South Dakota Utility Id 17267 Utility Location Yes Ownership C NERC Location MRO NERC MRO Yes Activity Distribution Yes References EIA Form EIA-861 Final Data File for 2010 - File1_a[1] SGIC[2] LinkedIn Connections CrunchBase Profile No CrunchBase profile. Create one now! This article is a stub. You can help OpenEI by expanding it. Sioux Valley Southwestern Electric Cooperative, Inc. Smart Grid Project was awarded $4,016,368 Recovery Act Funding with a total project value of $8,032,736. Utility Rate Schedules Grid-background.png commercial electric heat rate Commercial commercial general service - single phase Commercial commercial general service - three phase Commercial

116

E-Print Network 3.0 - atlantic littoral sw Sample Search Results  

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

atlantic littoral sw Page: << < 1 2 3 4 5 > >> 1 Technical Report A-93-4 February 1993 Summary: . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2...

117

Biotechnology Industry Organization 1201 Maryland Avenue SW, Suite 900  

E-Print Network [OSTI]

Biotechnology Industry Organization 1201 Maryland Avenue SW, Suite 900 Washington DC 20024 Contact, but are manufactured from renewable resources. Recent advances in biotechnology are now making it possible are home to much of the world's leading industrial biotechnology, which enables the creation of a wide

118

Culex pipiens, an Experimental Efficient Vector of West Nile and Rift Valley Fever Viruses in the Maghreb Region  

E-Print Network [OSTI]

Culex pipiens, an Experimental Efficient Vector of West Nile and Rift Valley Fever Viruses, Daaboub J, et al. (2012) Culex pipiens, an Experimental Efficient Vector of West Nile and Rift Valley Institut Pasteur, Department of Virology, Arboviruses and Insect Vectors, Paris, France Abstract West Nile

Paris-Sud XI, Université de

119

Aeromagnetic Survey At Kilauea East Rift Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Thomas, 1986) Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Kilauea East Rift Area (Thomas, 1986) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes More recent aeromagnetic data (Godson et al., 1981) generally substantiate the presence of a nearly continuous rift zone from the Kilauea summit down to sea level; the apparent width of the magnetic anomaly does not appear to match that projected by Furumoto (1978a) or Broyles et al. (1979); however, to date, no detailed analysis of the more recent data has been completed (R. B. Moore, pers. commun., 1984). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

120

Control of Well Ks-8 in the Kilauea Lower East Rift Zone | Open Energy  

Open Energy Info (EERE)

of Well Ks-8 in the Kilauea Lower East Rift Zone of Well Ks-8 in the Kilauea Lower East Rift Zone Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Control of Well Ks-8 in the Kilauea Lower East Rift Zone Abstract In June 1991, a well located in Hawaii kicked and unloaded at 3,476 ft (1,059 m). This well was estimatedto have a possible bottomhole temperature of 650°F (343°C)and a reservoir pressure approaching 2,300 psi 5,858 Immediate attempts to kill the well were unsuccessful, and the long processof well control was started. Besides the harsh geological and reservoir conditions encountered,the scarce availability of materials in a remote location and long distance transportation of necessary equipment figured heavily in to the time delay of the final kill procedure of the

Note: This page contains sample records for the topic "haleakala sw rift" 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

Conduction Models Of The Temperature Distribution In The East Rift Zone Of  

Open Energy Info (EERE)

Conduction Models Of The Temperature Distribution In The East Rift Zone Of Conduction Models Of The Temperature Distribution In The East Rift Zone Of Kilauea Volcano Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Conduction Models Of The Temperature Distribution In The East Rift Zone Of Kilauea Volcano Details Activities (2) Areas (1) Regions (0) Abstract: Temperature variations in the 1966-meter Hawaii Geothermal Project well HGP-A are simulated by model studies using a finite element code for conductive heat flow. Three models were generated: a constant temperature source from a vertical dike; a constant heat-generating magma chamber; and a transient heat source from a tapered vertical dike. Fair correlation is obtained between the HGP-A well temperature and the tapered dike 125 years after it is injected with an initial (transient) 1200°C

122

Time-Domain Electromagnetics At Hualalai Northwest Rift Area (Thomas, 1986)  

Open Energy Info (EERE)

Time-Domain Electromagnetics At Hualalai Northwest Time-Domain Electromagnetics At Hualalai Northwest Rift Area (Thomas, 1986) Exploration Activity Details Location Hualalai Northwest Rift Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes Three time-domain electromagnetic soundings were conducted on the middle northwest rift at elevations of 280-320 m (Fig. 40) (Kauahikaua and Mattice, 1981). These soundings penetrated to a greater depth than the Schlumberger soundings and two of them were able to resolve basement resistivities ranging from 9 to 12 ohm-m at depths of 1500 to 1800 m. One sounding detected a 9 ohm.m layer at 600 m depth that was underlain by a more resistive basement. These results suggest that thermal fluids may be responsible for the low-resistivity basement, whereas the high-resistivity

123

SW(A)93-006 STATEMENT OF CONSIDERATIONS  

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

SW(A)93-006 SW(A)93-006 STATEMENT OF CONSIDERATIONS Request by Cummins Power Generation, Inc. for an Advance Waiver of Domestic and Foreign Patent Rights to Inventions made under the Dish/Stirling Joint Venture Program between Sandia National Laboratories and Cummins Power Generation, Inc. in response to Contract No. 69-7763, DOE Docket No. W(A)93-006. The Petitioner, Cummins Power Generation (CPG), Inc., has requested a waiver of all domestic and foreign patent rights to inventions which it may conceive or first actually reduce to practice in the course of work under the Dish/Stirling Joint Venture Program between Petitioner and Sandia National Laboratories Contract No. 69-7763. Sandia National Laboratories is operated by Sandia Corporation for the U.S. Department of

124

U.S. DEPARTMENT OF ENERGY 1000 Independence Ave, SW  

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

1000 Independence Ave, SW 1000 Independence Ave, SW Washington, DC 20585 In the Matter of: ) Case Number: 2010-SE-2301 Leader Electronics Inc. ) NOTICE OF ALLOWANCE TO RESUME DISTRIBUTION Date issued : September 13, 2010 Manufacturers of certain covered products which have been determined by the Department of Energy (DOE) to be non-compliant with the applicable energy conservation standard may be allowed to resume distribution, per 10 CFR § 430.70 (a)(6)(v), if additional testing results supplied by the manufacturer results in a determination of compliance. On August 24, 2010, DOE issued a Notice of Non-Compliance Determination based on test results submitted by Leader Electronics showing that certain models were noncompliant. After an internal review, Leader Electronics determined that the original test results reported to DOE were incorrect.

125

File:Sw swppp guide.pdf | Open Energy Information  

Open Energy Info (EERE)

Sw swppp guide.pdf Sw swppp guide.pdf Jump to: navigation, search File File history File usage File:Sw swppp guide.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 2.7 MB, MIME type: application/pdf, 50 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:54, 13 November 2012 Thumbnail for version as of 10:54, 13 November 2012 1,275 × 1,650, 50 pages (2.7 MB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup

126

Comparative Precambrian stratigraphy and structure along the Mid-Continent rift  

SciTech Connect (OSTI)

The Mid-Continent rift is a geophysically identified tectonic structure that has been traced from Kansas northeastward into the Lake Superior district. A related arm has been identified by gravity as extending from eastern Lake Superior southeastward into the lower peninsula of Michigan. This rift is of Precambrian (Keweenawan) age and began developing approximately 1.1 b.y.B.P. For most of its extent, this continental-class rift system is buried below Phanerozoic strata. Outcrops are found only in east-central Minnesota, northwestern Wisconsin, and the upper peninsula of Michigan. The most accepted tectonic model of the Mid-Continent rift is that of a central horst partly covered by clastic rocks, bounded by high-angle faulting, and flanked by basins filled with clastic rocks. This model was developed in conjunction with field studies in the southwestern Lake Superior area, and generally has been adopted for Minnesota, Iowa, Nebraska, and Kansas. A comparable model has yet to be presented for the related arm extending into southern Michigan. 6 figures.

Dickas, A.B.

1986-03-01T23:59:59.000Z

127

The transition between the Sheba Ridge and Owen Basin: rifting of old oceanic lithosphere  

Science Journals Connector (OSTI)

......between the Sheba Ridge and Owen Basin: rifting of old oceanic lithosphere...Northwest Arabian Sea, in The Ocean Basins and Margins: the Indian Ocean...E to near 58"E in the 'bight' between two ridges projecting...continental margins of the Owen Basin and Gulf of Aden (Fig. 5......

Carol A. Stein; James R. Cochran

1985-04-01T23:59:59.000Z

128

Assessment of U.S. Agriculture Sector and Human Vulnerability to a Rift Valley Fever Outbreak  

E-Print Network [OSTI]

on the assessment of the U.S. agricultural sector and human vulnerability to a Rift Valley Fever (RVF) outbreak and the value of a select set of alternative disease control strategies. RVF is a vector-borne, zoonotic disease that affects both livestock and humans...

Hughes, Randi Catherine

2011-08-08T23:59:59.000Z

129

6Seismic stratigraphy and subsidence history of the United Arab Emirates (UAE) rifted margin  

E-Print Network [OSTI]

6Seismic stratigraphy and subsidence history of the United Arab Emirates (UAE) rifted margin and into the oil window in response of formation of a foreland basin (Ali and Watts 2009). Foreland basins develop by lithospheric flexure in front of migrating thrust and fold loads (e.g., Price 1971; Beaumont 1981

Watts, A. B. "Tony"

130

3D Graph Visualization with the Oculus Rift Virtual Graph Reality  

E-Print Network [OSTI]

3D Graph Visualization with the Oculus Rift Virtual Graph Reality Farshad Barahimi, Stephen Wismath regarding three- dimensional (3D) representations of graphs. However, the actual usefulness of such 3D reality environment such as a CAVE, or · printed as a physical model with a 3D printer. Early studies

Wismath, Stephen

131

The electrical resistivity structure of the crust beneath the northern Main Ethiopian Rift  

E-Print Network [OSTI]

The electrical resistivity structure of the crust beneath the northern Main Ethiopian Rift K containing partial melt. The crust is much more resistive beneath the southern plateau, and has no resistivity contrast between the upper and lower crust. The inferred geoelectric strike direction

132

Geometry and scaling relations of a population of very small rift-related normal faults  

E-Print Network [OSTI]

normal faults within the Solite Quarry of the Dan River rift basin range in length from a few millimetres AND SCALING RELATIONS The small normal faults are present in quarries of the Virginia Solite Corporation outcrops and quarried boulders (Fig. 2). The fault traces are typically straight, although the fault tips

133

E-Print Network 3.0 - area sw spain Sample Search Results  

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

from temperature profiles... , SW Spain Large altitudinal changes A variable; R mma Gran Canaria island Guiniguada NE basins; 0... to the peninsular territory of Spain map...

134

Forrestal Building, 1000 Independence Avenue, S.W.,  

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

THURSDAY, THURSDAY, APRIL 3, 2003 + + + + + The Committee met in Room 8E089 in the Forrestal Building, 1000 Independence Avenue, S.W., Washington, D.C., at 8:30 a.m., Jay Breidt, Chair, presiding. PRESENT: F. JAY BREIDT Chair MARK BERNSTEIN Committee Member JOHNNY BLAIR Committee Member JAE EDMONDS Committee Member MOSHE FEDER Committee Member JAMES K. HAMMITT Committee Member NEHA KHANNA Committee Member WILLIAM G. MOSS Committee Member NAGARAJ K. NEERCHAL Committee Member POLLY A. PHIPPS Committee Member RANDY R. SITTER Committee Member ALSO PRESENT: GUY CARUSO Administrator, Energy Information Administration HOWARD GRUENSPECHT Deputy Administrator, EIA BILL WEINIG EIA CALVIN KENT Invited Guest CRYSTAL LINKLETTER Invited Guest

135

Microsoft Word - Appendix C SW Samples.doc  

Office of Legacy Management (LM)

Analytical Results for Surface Water Samples, Analytical Results for Surface Water Samples, January 2000 through April 2011 This page intentionally left blank Upstream -- SW00-01 a _______________________________________________________________________________________________________________________________________________ Analyte Unit 04/18/00 07/17/00 10/20/00 04/17/01 07/11/01 10/09/01 04/07/05 10/05/05 04/28/06 10/02/06 04/11/07 10/08/07 04/09/08 g _______________________________________________________________________________________________________________________________________________ Field Measurements Alkalinity c mg/L -- -- -- -- -- -- -- -- -- -- -- -- -- Alkalinity b mg/L 196 130 263 218 196 98 145 202 228 183 227 186 213

136

Towards a better understanding of Rift Valley fever epidemiology in the south-west of the Indian Ocean  

Science Journals Connector (OSTI)

Rift Valley fever virus (Phlebovirus, Bunyaviridae) is an arbovirus causing intermittent epizootics and sporadic epidemics primarily in East Africa. Infection causes severe and often fatal illness in young sheep,...

Thomas Balenghien; Eric Cardinale; Vronique Chevalier; Nohal Elissa

2013-09-01T23:59:59.000Z

137

Characterization and Mapping of the Gene Conferring Resistance to Rift Valley Fever Virus Hepatic Disease in WF.LEW Rats  

E-Print Network [OSTI]

Rift Valley Fever Virus is a plebovirus that causes epidemics and epizootics in sub-Saharan African countries but has expanded to Egypt and the Arabian Peninsula. The laboratory rat (Rattus norvegicus) is susceptible to RVFV and has been shown...

Callicott, Ralph J.

2010-01-14T23:59:59.000Z

138

Owens Valley A Major Rift between the Sierra Nevada Batholith and Basin and Range Province, U.S.A.  

Science Journals Connector (OSTI)

Quaternary volcanic features associated with the rift include: 1) Long Valley, a 17 by 32 km rhyolitic caldera...3...of Bishop Tuff, 2) Mono Craters rhyolitic ring structure north of Long Valley, 3) Big Pine basa...

Michael F. Sheridan

1978-01-01T23:59:59.000Z

139

Secure Systems Editor: S.W. Smith, sws@cs.dartmouth.edu  

E-Print Network [OSTI]

Secure Systems Editor: S.W. Smith, sws@cs.dartmouth.edu side of the picture--the computers which we train students, young and old, to be effective cyber-citizens; and the media coverage or produce more effective tailors. S.W. SMITH Dartmouth College T oalargeextent,computingsystemsareu

Smith, Sean W.

140

K.Grill: Proposed Penalty (2011-SW-2902) | Department of Energy  

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

K.Grill: Proposed Penalty (2011-SW-2902) K.Grill: Proposed Penalty (2011-SW-2902) K.Grill: Proposed Penalty (2011-SW-2902) June 10, 2011 DOE alleged in a Notice of Proposed Civil Penalty that Kenneth Grill manufactured and distributed noncompliant showerheads in the U.S. Federal law subjects manufacturers and private labelers to civil penalties if those parties distribute in the U.S. products that do not meet applicable water conservation standards. This civil penalty notice advises the company of the potential penalties and DOE's administrative process, including the company's right to a hearing. K.Grill: Proposed Penalty (2011-SW-2902) More Documents & Publications K.Grill: Order (2011-SW-2902) Mackle Company: Proposed Penalty (2010-SE-0106) Nationwide Industries: Proposed Penalty (2011-CW-2803

Note: This page contains sample records for the topic "haleakala sw rift" 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

Direct-Current Resistivity Survey At Mauna Loa Northeast Rift Area (Thomas,  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Mauna Loa Direct-Current Resistivity Survey At Mauna Loa Northeast Rift Area (Thomas, 1986) Exploration Activity Details Location Mauna Loa Northeast Rift Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The vertical electrical sounding surveys encountered few difficulties and were able to resolve basement resistivities in all locations. The resistivity sections derived indicated a 3000- 20,000 ohm.m surface layer underlain by a 500- 900 ohm-m cold freshwatersaturated layer and a basement layer of less than 100 ohm.m (Kauahikaua and Mattice, 1981). The depth of penetration of these soundings was estimated to be about 800 m to 900 m b.s.1. and thus the basement resistivities probably correspond to basalts

142

Modeling-Computer Simulations At Kilauea East Rift Area (Rudman & Epp,  

Open Energy Info (EERE)

Rudman & Epp, Rudman & Epp, 1983) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Modeling-Computer Simulations At Kilauea East Rift Area (Rudman & Epp, 1983) Exploration Activity Details Location Kilauea East Rift Area Exploration Technique Modeling-Computer Simulations Activity Date Usefulness useful DOE-funding Unknown Notes Three models were generated: a constant temperature source from a vertical dike; a constant heat-generating magma chamber; and a transient heat source from a tapered vertical dike. Fair correlation is obtained between the HGP-A well temperature and the tapered dike 125 years after it is injected with an initial (transient) 1200degrees C temperature. Results provide background information from which to evaluate the importance of water

143

Defmod - Parallel multiphysics finite element code for modeling crustal deformation during the earthquake/rifting cycle  

E-Print Network [OSTI]

In this article, we present Defmod, a fully unstructured, two or three dimensional, parallel finite element code for modeling crustal deformation over time scales ranging from milliseconds to thousands of years. Defmod can simulate deformation due to all major processes that make up the earthquake/rifting cycle, in non-homogeneous media. Specifically, it can be used to model deformation due to dynamic and quasistatic processes such as co-seismic slip or dike intrusion(s), poroelastic rebound due to fluid flow and post-seismic or post-rifting viscoelastic relaxation. It can also be used to model deformation due to processes such as post-glacial rebound, hydrological (un)loading, injection and/or withdrawal of compressible or incompressible fluids from subsurface reservoirs etc. Defmod is written in Fortran 95 and uses PETSc's parallel sparse data structures and implicit solvers. Problems can be solved using (stabilized) linear triangular, quadrilateral, tetrahedral or hexahedral elements on shared or distribut...

Ali, S Tabrez

2014-01-01T23:59:59.000Z

144

Hydrocarbon accumulation on rifted Continental Margin - examples of oil migration pathways, west African salt basins  

SciTech Connect (OSTI)

Examination of the oil fields in the Gabon, Lower Congo, and Cuanza basins allows modeling of oil migration and a more accurate ranking of prospects using geologic risk factors. Oil accumulations in these basins are in strata deposited during Cretaceous rift and drift phases, thus providing a diversity of geologic settings to examine. Oil accumulations in rift deposits are located on large faulted anticlines or in truncated units atop horst features. Many of these oil fields were sourced from adjacent organic shales along short direct migration paths. In Areas where source rock is more remote to fields or to prospective structures, faulting and continuity of reservoir rock are important to the migration of hydrocarbons. Because Aptian salts separate rift-related deposits from those of the drift stage, salt evacuation and faulting of the salt residuum are necessary for oil migration from the pre-salt sequences into the post-salt section. Oil migration within post-salt strata is complicated by the presence of salt walls and faulted carbonate platforms. Hydrocarbon shows in wells drilled throughout this area provide critical data for evaluating hydrocarbon migration pathways. Such evaluation in combination with modeling and mapping of the organic-rich units, maturation, reservoir facies, structural configurations, and seals in existing fields allows assessment of different plays. Based on this information, new play types and prospective structures can be ranked with respect to geologic risk.

Blackwelder, B.W.

1989-03-01T23:59:59.000Z

145

Mary's River SW Geothermal Project | Open Energy Information  

Open Energy Info (EERE)

Geothermal Project Geothermal Project Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Development Project: Mary's River SW Geothermal Project Project Location Information Coordinates 41.750555555556°, -115.30194444444° 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":41.750555555556,"lon":-115.30194444444,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

146

U.S. Department of Energy 1000 Independence Ave, SW  

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

U.S. Department of Energy 1000 Independence Ave, SW Washington, DC 20585 In the Matter of: Fuzhou Sunlight Lighting Electrical Appliance Co., Ltd. ) ) ) ) Case Number: 2010-SE-1402 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. On June 4, 2010, Westinghouse provided to DOE copies of NVLAP test reports for a variety of models of incandescent reflector lamps. Westinghouse also provided a spreadsheet summarizing the information from the test reports. In relevant part, the spreadsheet (and test reports) details the following information:

147

NETL: 2010 SW PA High School Science Bowl  

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

High School Science Bowl High School Science Bowl The U.S. Department of Energy's National Energy Technology Laboratory (DOE/NETL), and the Community College of Allegheny County (CCAC), South Campus, would like to invite you to participate in one of the premier scientific events for high school students, the Southwestern Pennsylvania High School Science Bowl 2010 on February 20, 2010. This will be NETL's 19th year sponsoring the high school competition. There is a change this year in the registration process from past years, all teams who are registering to complete, must do so through the National Science Bowl website by January 7, 2010. For those who are not familiar with the Science Bowl here are some highlights: The competition is open to high school students (school, scouts, home school) from Southwestern Pennsylvania (SW PA). Complete eligibility requirements are located at the National Science Bowl website.

148

U.S. Department of Energy 1000 Independence Ave., SW  

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

3, 2009 3, 2009 18809.03YK Submitted electronically to GC-62@hq.doe.gov Office of the Assistant General Counsel for Technology Transfer U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 Dear Mr. Gottlieb, Subject: Notice of Inquiry: Technology Transfer Practices at Department of Energy Laboratories (75 FR 72036) We are pleased to respond to the questions published in the Federal Register. The Lawrence Livermore National Laboratory (LLNL) is committed to DOE's mission to improve the Nation's global competitive posture and believes that the Lab's ability to partner and collaborate with industry, universities and others around the globe is key to achieving that goal. As Secretary Chu expressed in his statement to the Committee on

149

Microsoft Word - RFLMA CR 2010-06 Monitoring Results at SW027 Final.doc  

Office of Legacy Management (LM)

Report of Steps Taken Regarding Monitoring Results at Surface Water Report of Steps Taken Regarding Monitoring Results at Surface Water Point of Evaluation (POE) SW027 and Contact Record 2010-06 This page intentionally left blank 1 of 16 Report of Steps Taken Regarding Monitoring Results at Surface Water Point of Evaluation (POE) SW027 August 31, 2010 Introduction Surface water location SW027 is the Rocky Flats Legacy Management Agreement (RFLMA) POE at the eastern (downstream) end of the South Interceptor Ditch (SID), upstream of Pond C-2. The plutonium-239/240 (Pu) concentration measured at SW027 in samples collected through April 27, 2010, indicated that the 12-month rolling average of data from this monitoring point for the full month of April 2010 would likely exceed the RFLMA surface water standard when the

150

Palaeomagnetic and rock magnetic study of Lower Devonian sediments from Podolia, SW Ukraine: remagnetization problems  

Science Journals Connector (OSTI)

......study of Lower Devonian sediments from Podolia, SW Ukraine: remagnetization problems M. Jelenska 1 M. Kadzialko-Hofmokl...Institute of Geophysics, National Academy of Sciences of Ukraine, Kiev, Ukraine 3 Faculty of Geology, University of Warsaw, Warsaw......

M. Jele?ska; M. K?dzia?ko-Hofmokl; V. Bakhmutov; I. Poliachenko; P. Zi?kowski

2015-01-01T23:59:59.000Z

151

Rifting of the Izu-Bonin arc in the Quaternary and Mid-Oligocene  

SciTech Connect (OSTI)

Eruption of middle Eocene-lower Oligocene boninites and island arc tholeiites created the 200 km wide Izu-Bonin arc massif following the initiation of subduction {approximately}50 Ma. Mid-Oligocene rifting formed a 40-70 km wide forearc basin between the Eocene outer-arc high and the Eo-Oligocene arc (now the frontal arc high), with maximum extension at the latitudes of the Bonin Ridge and Trough. The Oligocene forearc basin was rapidly (100-300 m/m.y.) filled with turbidite and debris flow deposits produced by concurrent volcanism and erosion of the surrounding highs. Contemporaneous stretching in the backarc region produced dominantly east-dipping, NNE-trending, normal faults and culminated in backarc spreading in the Shikoku basin (25-15 Ma), isolating the Palau-Kyushu remnant arc. The forearc and remnant arc sediments record a dearth of volcanogenic input between 23 and 17 Ma; evidence that an arc volcanic minimum accompanied backarc spreading. The middle Miocene to Recent volcanic front formed 0(S)-50(N) km west of the Oligocene arc and has loaded and flexed the forearc. Further west, chains of submarine volcanoes erupted along the extension of Shikoku basin fracture zones. Basaltic sills were emplaced in the forearc. Explosive volcanism from rhyolitic calderas has increased dramatically since the late Pliocene, especially in the last 0.2 Ma. Since {approximately}2 Ma the arc has been stretched again, producing rapidly subsiding (300-2,250 m/m.y.) graben, immediately west of the volcanic front, which are segmented along strike by oblique transfer zones. The Sumisu Rift is partially filled with (<1.5 Ma) volcaniclastic turbidites and hemipelagic sediments and is intruded by backarc basin basalts. About 1 km of syn-rift uplift of the arc margin footwall has produced an unconformity, beneath surficial pumice, that extends back to pumiceous sediments >2.35 Ma.

Taylor, B. (Univ. of Hawaii, Honolulu (USA))

1990-06-01T23:59:59.000Z

152

Gravity-driven structures and rift basin evolution: Rio Muni Basin, offshore equatorial West Africa  

SciTech Connect (OSTI)

Offshore Equatorial Guinea, west Africa, gravity-driven nappes, more than 1 km thick and 15 km from head to toe, provide key evidence in reconstructing the late synrift: evolution of this part of the South Atlantic margin basin system. Furthermore, Aptian-Cenomanian carbonate and clastic rocks in the nappes` allochthonous hanging walls are attracting interest as a new exploration play in west Africa. The nappes exhibit a range of geometries that suggest they share many of the same deformation processes as thin-skin thrust and linked extensional fault systems. Not only are these structures significant in their own right, representing a rare example of gravity tectonics in the virtual absence of major halokinesis, but their presence may record an other-wise undetectable process active during the transition from a rift basin to a passive continental margin. A review of Equatorial Guinea in its pre-Atlantic configuration, alongside neighboring basins in Brazil (the Sergipe-Alagoas basin) and Gabon, suggests that gravity gliding was sustained by a relatively steep, westward paleoslope promoted by east-ward offset of the locus of thermal uplift from the rift basin (i.e., a simple shear model of basin formation). In contrast to gravity-driven structures in most postrift settings, the Equatorial Guinea nappes developed at the close of the Aptian-Albian synrift episode in response to a growing bathymetric deep caused by rapid subsidence outpacing restricted sedimentation.

Turner, J.P. [Univ. of Birmingham (United Kingdom)

1995-08-01T23:59:59.000Z

153

SW HARRISON SW MONTGOMERY  

E-Print Network [OSTI]

on weekends 1 $168 Non-Peak Not valid between 11am and 3pm; all days on weekends 1 $168 Motorcycle* Valid in PSU motorcycle zones; complimentary with regular permit purchase 1 $86 Evening Valid only after 3:30pm terms; sold during fall term only) Motorcycle permit is available at no charge if you've purchased

Bertini, Robert L.

154

From continental extension to seafloor spreading: crustal structure of the Goban Spur rifted margin, southwest of the UK  

Science Journals Connector (OSTI)

......central Great Australian Bight (Sayers 2001), oceanic...north by the Porcupine Basin and to the south by the...beneath the Porcupine Basin, southwest of Ireland...central Great Australian Bight, in Non-volcanic Rifting...the Porcupine Seabight Basin and adjacent continental......

Andrew D. Bullock; Timothy A. Minshull

2005-11-01T23:59:59.000Z

155

Crustal structure of the rifted volcanic margins and uplifted plateau of Western Yemen from receiver function analysis  

Science Journals Connector (OSTI)

......Besse J. On causal links between flood basalts and continental breakup. Earth...Ebinger C.J., Baker J., eds. (2002) Boulder, CO. 1-14. Vol 362. Milkereit B...chrono-stratigraphy of pre- and syn-rift bimodal flood volcanism in Ethiopia and Yemen. Earth......

Abdulhakim Ahmed; Christel Tiberi; Sylvie Leroy; Graham W. Stuart; Derek Keir; Jamal Sholan; Khaled Khanbari; Ismael Al-Ganad; Clmence Basuyau

2013-01-01T23:59:59.000Z

156

Sedimentary dynamics and extensional structuring related to early Cretaceous rifting of Neocomian and Barremian deposits of the interior basin of Gabon  

Science Journals Connector (OSTI)

Recent field and subsurface data about the early Neocomian Ndombo series and the Neocomian to mid-Barremian Schistes series of the interior basin of Gabon further our understanding of the initial stages of early Cretaceous N4060E extensional rifting. The syn-rift series comprise fluviallacustrine claystonessandstones, rare conglomerates, and carbonates. The syn-rift fill begins with braided-stream feldspathic sandstones. These are overlain first by fluviallacustrine deposits and then by predominantly lacustrinepalustrine claystones, which are potential petroleum source rocks. The claystones are eroded in part and are capped by the pre-Aptian angular unconformity marking the end of Cretaceous rifting in the interior basin. This change in syn-rift facies and depositional environments reflects a rise in base level in response to accelerated subsidence after the initial stage of rifting. The syn-rift deposits form two fining-upward sequences several 1001000m thick.

M. Mbina Mounguengui; J. Lang; M. Guiraud

2008-01-01T23:59:59.000Z

157

An Improved Daylight Correction for IR Loss in ARM Diffuse SW Measurements  

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

An Improved Daylight Correction for IR Loss An Improved Daylight Correction for IR Loss in ARM Diffuse SW Measurements C. N. Long, K. Younkin, and K. L. Gaustad Pacific Northwest National Laboratory Richland, Washington J. A. Augustine National Oceanic and Atmospheric Administration Air Resources Laboratory Surface Radiation Research Branch Boulder, Colorado Introduction A paper by Cess et al. (2000) notes that some clear-sky diffuse shortwave (SW) measurements they were using from the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site exhibited less than Rayleigh magnitude. Remarking that this is a physical impossibility, the obvious conclusion forwarded by the authors was that there was some problem with the ARM SGP diffuse SW data. Shortly thereafter, the problem of infrared (IR) loss from thermopile-based single black detector

158

Development and Evaluation of RRTMG_SW, a Shortwave Radiative Transfer Model for GCM Applications  

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

Development and Evaluation of RRTMG_SW, Development and Evaluation of RRTMG_SW, a Shortwave Radiative Transfer Model for General Circulation Model Applications M. J. Iacono, J. S. Delamere, E. J. Mlawer, and S. A. Clough Atmospheric and Environmental Research, Inc. Lexington, Massachusetts J.-J. Morcrette European Center for Medium-Range Weather Forecasts Reading, United Kingdom Y.-T. Hou National Centers for Environmental Prediction Camp Springs, Maryland Introduction The k-distribution shortwave radiation model developed for the Atmospheric Radiation Measurement (ARM) Program, RRTM_SW_V2.4 (Clough et al. 2004), utilizes the discrete ordinates radiative transfer model, DISORT, for scattering calculations and 16 g-points in each of its 16 spectral bands. DISORT provides agreement with line-by-line flux calculations to within 1 Wm

159

Geologic Characterization of the South Georgia Rift Basin for Source Proximal CO2 Storage  

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

Georgia Rift Basin for Source Proximal CO 2 Storage Michael G. Waddell and John M. Shafer Earth Sciences and Resources Institute University of South Carolina - Columbia Carbon Storage Program Infrastructure Annual Review Meeting Pittsburgh, PA November 15-17, 2011 Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011 Research Team Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011 John Shafer and Michael Waddell James Knapp and Camelia Knapp Lee Kurtzweil and Phil VanHollebeke C.W. "Bill" Clendenin Richard Berg James Rine Integrated Services Contract for Drilling/Coring/Logging - TBD Study Area Carbon Storage Program Infrastructure Annual Review Meeting - November 15-17, 2011

160

Single-particle cryo-electron microscopy of Rift Valley fever virus  

SciTech Connect (OSTI)

Rift Valley fever virus (RVFV; Bunyaviridae; Phlebovirus) is an emerging human and veterinary pathogen causing acute hepatitis in ruminants and has the potential to cause hemorrhagic fever in humans. We report a three-dimensional reconstruction of RVFV vaccine strain MP-12 (RVFV MP-12) by cryo-electron microcopy using icosahedral symmetry of individual virions. Although the genomic core of RVFV MP-12 is apparently poorly ordered, the glycoproteins on the virus surface are highly symmetric and arranged on a T = 12 icosahedral lattice. Our RVFV MP-12 structure allowed clear identification of inter-capsomer contacts and definition of possible glycoprotein arrangements within capsomers. This structure provides a detailed model for phleboviruses, opens new avenues for high-resolution structural studies of the bunyavirus family, and aids the design of antiviral diagnostics and effective subunit vaccines.

Sherman, Michael B. [Department of Biochemistry and Molecular Biology, University of Texas Medical Branch, Galveston, TX 77555 (United States); Sealy Center for Structural Biology and Molecular Biophysics, University of Texas Medical Branch, Galveston, TX 77555 (United States); Freiberg, Alexander N. [Department of Pathology, University of Texas Medical Branch, Galveston, TX 77555 (United States); Center for Biodefense and Emerging Infectious Diseases, University of Texas Medical Branch, Galveston, TX 77555 (United States); Holbrook, Michael R. [Department of Pathology, University of Texas Medical Branch, Galveston, TX 77555 (United States); Center for Biodefense and Emerging Infectious Diseases, University of Texas Medical Branch, Galveston, TX 77555 (United States); Institute for Human Infections and Immunity, University of Texas Medical Branch, Galveston, TX 77555 (United States); Watowich, Stanley J., E-mail: watowich@xray.utmb.ed [Department of Biochemistry and Molecular Biology, University of Texas Medical Branch, Galveston, TX 77555 (United States); Sealy Center for Structural Biology and Molecular Biophysics, University of Texas Medical Branch, Galveston, TX 77555 (United States); Center for Biodefense and Emerging Infectious Diseases, University of Texas Medical Branch, Galveston, TX 77555 (United States); Institute for Human Infections and Immunity, University of Texas Medical Branch, Galveston, TX 77555 (United States)

2009-04-25T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" 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

Ultrastructural study of Rift Valley fever virus in the mouse model  

SciTech Connect (OSTI)

Detailed ultrastructural studies of Rift Valley fever virus (RVFV) in the mouse model are needed to develop and characterize a small animal model of RVF for the evaluation of potential vaccines and therapeutics. In this study, the ultrastructural features of RVFV infection in the mouse model were analyzed. The main changes in the liver included the presence of viral particles in hepatocytes and hepatic stem cells accompanied by hepatocyte apoptosis. However, viral particles were observed rarely in the liver; in contrast, particles were extremely abundant in the CNS. Despite extensive lymphocytolysis, direct evidence of viral replication was not observed in the lymphoid tissue. These results correlate with the acute-onset hepatitis and delayed-onset encephalitis that are dominant features of severe human RVF, but suggest that host immune-mediated mechanisms contribute significantly to pathology. The results of this study expand our knowledge of RVFV-host interactions and further characterize the mouse model of RVF.

Reed, Christopher; Steele, Keith E.; Honko, Anna; Shamblin, Joshua; Hensley, Lisa E. [United States Army Medical Research Institute of Infectious Diseases (USAMRIID), Fort Detrick, MD (United States)] [United States Army Medical Research Institute of Infectious Diseases (USAMRIID), Fort Detrick, MD (United States); Smith, Darci R., E-mail: darci.smith1@us.army.mil [United States Army Medical Research Institute of Infectious Diseases (USAMRIID), Fort Detrick, MD (United States)

2012-09-15T23:59:59.000Z

162

Red tide detection and tracing using MODIS fluorescence data: A regional example in SW Florida coastal waters  

E-Print Network [OSTI]

Red tide detection and tracing using MODIS fluorescence data: A regional example in SW Florida-time data from the MODIS satellite sensor was used to detect and trace a harmful algal bloom (HAB), or red to interferences of other water constituents. The red tide that formed from November to December 2004 off SW

163

OligoceneMiocene tectonic evolution of the South Fiji Basin and Northland Plateau, SW Pacific Ocean: Evidence from  

E-Print Network [OSTI]

investigated parts of the southwest Pacific Ocean. It is a region of remnant volcanic arcs, plateaus and basins of the study area in the SW Pacific Ocean, showing geographic names and dredge locations from ChurkinOligocene­Miocene tectonic evolution of the South Fiji Basin and Northland Plateau, SW Pacific

Demouchy, Sylvie

164

Modeling the distribution of the West Nile and Rift Valley Fever vector Culex pipiens in arid and semi-arid regions of the Middle East and North Africa  

Science Journals Connector (OSTI)

The Middle East North Africa (MENA) region is under continuous threat of the re-emergence of West Nile virus (WNV) and Rift Valley Fever virus (RVF), two pathogens transmitted...Culex pipiens. Predicting areas at...

Amy K Conley; Douglas O Fuller; Nabil Haddad; Ali N Hassan

2014-06-01T23:59:59.000Z

165

Campus Rec | 210 ASRC -1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation  

E-Print Network [OSTI]

Campus Rec | 210 ASRC - 1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation Outdoor recreation. This is accomplished by offering adventure trips, non-credit instruction, team-building programs resource to the PSU community regarding outdoor recreation. DESCRIPTION The Climbing Center Student

Veerman, J. J. P.

166

Campus Rec | 210 ASRC -1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation  

E-Print Network [OSTI]

Campus Rec | 210 ASRC - 1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation Outdoor and environmentally conscious outdoor recreation. This is accomplished by offering adventure trips, non as the informational resource to the PSU community regarding outdoor recreation. This position is open to all currently

Daescu, Dacian N.

167

Campus Rec | 210 ASRC -1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation  

E-Print Network [OSTI]

Campus Rec | 210 ASRC - 1800 SW Sixth Avenue | Portland, OR 97201 www.pdx.edu/recreation Lifeguard Avenue | Portland, OR 97201 www.pdx.edu/recreation Type of work ­ position requires mostly sitting experience. Application can be found here: http://www.pdx.edu/recreation/employment-opportunities-0 o See

Bertini, Robert L.

168

A COMPARISON OF FRUIT REMOVAL BY BATS AND BIRDS FROM PIPER HISfIDUM SW.  

E-Print Network [OSTI]

... ; A COMPARISON OF FRUIT REMOVAL BY BATS AND BIRDS FROM PIPER HISfIDUM SW. (PIPERACEAE. Central AlOOrica (Received: January 5, 1989) ABSTRAC,r I measured fruit removal by bats and birds from in recently distubed second growth habitat during a period of heavy P. hispidum fruiting; plants are e

O'Donnell, Sean

169

For more than 50 years, Southwest Research Institute (SwRI) has sup-  

E-Print Network [OSTI]

For more than 50 years, Southwest Research Institute® (SwRI®) has sup- ported the oil and gas testing Oil & Gas Industry Support Design, Fabrication and Testing D017944 KEYWORDS Topsides Downhole laboratory n Tension and compression load frames n Torsion tower n Water tank n Deep ocean simulation

Chapman, Clark R.

170

Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate accumulation  

E-Print Network [OSTI]

Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate simulating reflectors (BSRs) imply the potential existence of gas hydrates offshore southwestern Taiwan that the fluxes are very high in offshore southwestern Taiwan. The depths of the SMI are different at sites GH6

Lin, Andrew Tien-Shun

171

Wind Power Production in the Urban Environment S.J. Kooiman, S.W. Tullis*  

E-Print Network [OSTI]

Wind Power Production in the Urban Environment S.J. Kooiman, S.W. Tullis* Department of Mechanical are typical deterrents to operating wind turbines. However, with the aerodynamic performance advantages and the heightened wind speeds around buildings, the application for these turbines may be more advantageous than

Tullis, Stephen

172

Hydrothermal dolomites in SW Sardinia (Italy): evidence for a widespread late-Variscan fluid flow event  

E-Print Network [OSTI]

Hydrothermal dolomites in SW Sardinia (Italy): evidence for a widespread late-Variscan fluid flow, the Cambrian carbonates underwent ductile deformation and greenschist facies metamorphism. The same is true-temperature metamorphic rocks within the overlying nappes. It is assumed that a late-Variscan hydrothermal event, which

Boni, Maria

173

Hydrogen Storage Systems Analysis Meeting 955 L'Enfant Plaza North, SW, Suite 6000  

E-Print Network [OSTI]

Hydrogen Storage Systems Analysis Meeting 955 L'Enfant Plaza North, SW, Suite 6000 Washington, DC, 2005 #12;SUMMARY REPORT Hydrogen Storage Systems Analysis Meeting March 29, 2005 955 L'Enfant Plaza was to familiarize the DOE research community involved in hydrogen storage materials and process development

174

Organic matter in the Paleogene west European rift: Bresse and Valence salt basins (France)  

SciTech Connect (OSTI)

The Bresse and Valence basins are two adjacent segments of the West European rift. They contain thick Paleogene halite sequences including intercalated and interfingering siliciclastic material and carbonate and sulfate deposits. Source rock samples in this study were mainly taken from the depocenters because of maximum sampling coverage. Organic matter (OM) is generally immature and occurs primarily within intercalated nonhalitic beds. The Bresse basin seems to contain more OM in (1) the Intermediate Salt Formation (Priabonian), composed of alternating laminated carbonate and halite beds; (2) the upper part of the Upper Salt Formation (clayey carbonate beds; Rupelian), affected by synsedimentary halite solution; and (3) the solution breccia which immediate overlies the salt sequence. In the Valence basin, the organic-rich layers are concentrated in the Subsalt Formation (carbonate beds; Priabonian), and the upper part of the Lower Salt Formation (laminates; Rupelian). In both basins, type III organic matter is associated with terrigenous facies. Type I is abundant in the Valence basin (laminites), and type II seems to be more abundant in the Bresse basin. The amount of OM varies considerably, and we suppose it is higher toward the basin margins. From studies made in evaporite basins in other region, which are also known to have significant amounts of organic matter, we find a similar range of organic composition. Such studies are of interest because of their petroleum potential and for understanding precise depositional environments and waste disposal problems (gas generation with local heat source).

Curial, A.; Dumas, D.; Moretto, R.

1988-08-01T23:59:59.000Z

175

File:Const SW swppp template.pdf | Open Energy Information  

Open Energy Info (EERE)

Const SW swppp template.pdf Const SW swppp template.pdf Jump to: navigation, search File File history File usage File:Const SW swppp template.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 542 KB, MIME type: application/pdf, 40 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:53, 13 November 2012 Thumbnail for version as of 10:53, 13 November 2012 1,275 × 1,650, 40 pages (542 KB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup

176

File:Construction SW NOI modified 7-18-2011.pdf | Open Energy Information  

Open Energy Info (EERE)

SW NOI modified 7-18-2011.pdf SW NOI modified 7-18-2011.pdf Jump to: navigation, search File File history File usage File:Construction SW NOI modified 7-18-2011.pdf Size of this preview: 463 × 599 pixels. Other resolution: 464 × 600 pixels. Go to page 1 2 3 Go! next page → next page → Full resolution ‎(1,275 × 1,650 pixels, file size: 100 KB, MIME type: application/pdf, 3 pages) File history Click on a date/time to view the file as it appeared at that time. Date/Time Thumbnail Dimensions User Comment current 10:47, 13 November 2012 Thumbnail for version as of 10:47, 13 November 2012 1,275 × 1,650, 3 pages (100 KB) Dklein2012 (Talk | contribs) You cannot overwrite this file. Edit this file using an external application (See the setup instructions for more information) File usage There are no pages that link to this file.

177

Trace element and isotope geochemistry of geothermal fluids, East Rift Zone, Kilauea, Hawaii  

SciTech Connect (OSTI)

A research program has been undertaken in an effort to better characterize the composition and the precipitation characteristic of the geothermal fluids produced by the HGP-A geothermal well located on the Kilauea East Rift Zone on the Island of Hawaii. The results of these studies have shown that the chemical composition of the fluids changed over the production life of the well and that the fluids produced were the result of mixing of at least two, and possibly three, source fluids. These source fluids were recognized as: a sea water composition modified by high temperature water-rock reactions; meteoric recharge; and a hydrothermal fluid that had been equilibrated with high temperature reservoir rocks and magmatic volatiles. Although the major alkali and halide elements show clearly increasing trends with time, only a few of the trace transition metals show a similar trend. The rare earth elements, were typically found at low concentrations and appeared to be highly variable with time. Studies of the precipitation characteristics of silica showed that amorphous silica deposition rates were highly sensitive to fluid pH and that increases in fluid pH above about 8.5 could flocculate more than 80% of the suspended colloidal silica in excess of its solubility. Addition of transition metal salts were also found to enhance the recovery fractions of silica from solution. The amorphous silica precipitate was also found to strongly scavenge the alkaline earth and transition metal ions naturally present in the brines; mild acid treatments were shown to be capable of removing substantial fractions of the scavenged metals from the silica flocs yielding a moderately pure gelatinous by-product. Further work on the silica precipitation process is recommended to improve our ability to control silica scaling from high temperature geothermal fluids or to recover a marketable silica by-product from these fluids prior to reinjection.

West, H.B.; Delanoy, G.A.; Thomas, D.M. (Hawaii Univ., Honolulu, HI (United States). Hawaii Inst. of Geophysics); Gerlach, D.C. (Lawrence Livermore National Lab., CA (United States)); Chen, B.; Takahashi, P.; Thomas, D.M. (Hawaii Univ., Honolulu, HI (United States) Evans (Charles) and Associates, Redwood City, CA (United States))

1992-01-01T23:59:59.000Z

178

Chapter 8 - Rift Valley Fever Virus: A Virus with Potential for Global Emergence  

Science Journals Connector (OSTI)

Abstract Rift Valley fever virus (RVFV) is an important emerging zoonotic threat to veterinary and public health with potential to cause a severe socioeconomic impact on peoples livelihoods. The capacity of the virus to spread into new territories by crossing significant natural geographic barriers and re-emerge in endemic regions after long periods of silence, to cause large outbreaks in human and animal populations, constitutes a formidable challenge for public and veterinary health authorities as well as for scientific communities worldwide. In spite of recent advances in research on RVFV pathogenesis, molecular epidemiology, outbreak prediction, and development of new diagnostic tools and vaccines, some fundamental aspects of the epidemiology and ecology of the virus remain elusive. Large outbreaks of RVF are associated with anomalous high rainfalls leading to massive flooding and the resultant swarms of competent mosquito vectors transmitting the virus to a wide range of susceptible vertebrate species. However, the exact mechanism of RVFV natural transmission during interepizootic periods remains largely unknown, including the postulated long-term virus persistence in transovarially infected eggs of floodwater Aedes mosquito species, and the role of wild mammals as reservoirs. The presence of competent mosquito vectors in countries free of RVF, the wide range of mammals susceptible to the virus, the global changes in climate, and increased animal trade and travel are some of the factors that might contribute to international spread. This chapter provides the background to the major outbreaks, molecular biology and epidemiology of RVFV, and overviews aspects of ecology, host and vector range which make the virus a potential global emerging threat.

Janusz T. Paweska; Petrus Jansen van Vuren

2014-01-01T23:59:59.000Z

179

Terr. Atmos. Ocean. Sci., Vol. 17, No. 4, 933-950, December 2006 Methane Venting in Gas Hydrate Potential Area Offshore of SW  

E-Print Network [OSTI]

Potential Area Offshore of SW Taiwan: Evidence of Gas Analysis of Water Column Samples Tsanyao Frank Yang 1 areas offshore of SW Taiwan for analysis of dissolved gases. Some these samples show unusually high-shore and offshore of southwestern Taiwan (e.g., Chow et al. 2000; Yang et al. 2004; Chiu et al. 2006). The gases

Lin, Andrew Tien-Shun

180

Business Ymwet Centlsaem: Enclosed is AEC Special Nuclear Material License Yo. SW-551, as  

Office of Legacy Management (LM)

c-ii 3-y c-ii 3-y !WL?DF!i 70.424 SW-551, 9s renewed AUG 9 196s cmhustian En&merin~, Inc. %.lelcar Division tYindter, Connecticut ,~ttentionr ?tr. 5. ff. Shfp,penbmg: Business Ymwet Centlsaem: Enclosed is AEC Special Nuclear Material License Yo. SW-551, as renewed. Very tTuly yours, fkmald A. Nusshauaer, Chief Saurce 4 Specfel Wcleer Yaterials Brmch Ofvision of Meterbls Licensing EnClOSUWl W W m , as renwed DISTRIBUTION: Ccaplianee, HQs 2 w/encl. H. j. McAlduff, OR00 w/encl. D. George, ?MM w/mcl. N. Dtilos, ML w/emCl, C. Luke, ML w/end. Br. RF w/encl. Div. RF w/o encl. UNITED STATES ATOMIC ENERGY COMMISSION SPECIAL NUCLEAR MATERIAL LICENSE Pursuant to the Atomic Energy Act of 1954 and Title 10, Code of Federal Regulations, Chapter 1, Part 70, "Special Nuclear Material Regulations," a license is hereby issued authorizing the licensee

Note: This page contains sample records for the topic "haleakala sw rift" 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

Anomalous seafloor mounds in the northern Natal Valley, southwest Indian Ocean: Implications for the East African Rift System  

Science Journals Connector (OSTI)

Abstract The Natal Valley (southwest Indian Ocean) has a complicated and protracted opening history, as has the surrounding southwest Indian Ocean. Recently collected multibeam swath bathymetry and 3.5kHz seismic data from the Natal Valley reveal anomalous seafloor mounds in the northern Natal Valley. The significance, of these domes, as recorders of the geological history of the Natal Valley and SE African Margin has been overlooked with little attempt made to identify their origin, evolution or tectonic significance. This paper aims to describe these features from a morphological perspective and to use their occurrence as a means to better understand the geological and oceanographic evolution of this basin. The seafloor mounds are distinct in both shallow seismic and morphological character from the surrounding seafloor of the Natal Valley. Between 25km and 31km long, and 16km and 18km wide, these features rise some 400m above the sedimentary deposits that have filled in the Natal Valley. Such macro-scale features have not previously been described from the Natal Valley or from other passive margins globally. They are not the result of bottom water circulation, salt tectonics; rather, igneous activity is favoured as the origin for these anomalous seafloor features. We propose a hypothesis that the anomalous seafloor mounds observed in the Natal Valley are related to igneous activity associated with the EARS. The complicated opening history and antecedent geology, coupled with the southward propagation of the East African Rift System creates a unique setting where continental rift associated features have been developed in a marine setting.

Errol Wiles; Andrew Green; Mike Watkeys; Wilfried Jokat; Ralph Krocker

2014-01-01T23:59:59.000Z

182

Secretary Steven Chu U.S. Department of Energy 1000 Independence Avenue, S.W.  

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

3, 2009 3, 2009 Secretary Steven Chu U.S. Department of Energy 1000 Independence Avenue, S.W. Washington, D.C. 20585 Dear Secretary Chu: As a condition of receiving Florida's share of the $3.1 billion funding for the State Energy Program (SEP), pursuant to Section 41 0, Division A - Title IV of the American Recovery and Renewal Act of 2009 ( A R M ) , I am providing the following notification. I have received written assurance from the Florida Public Service Commission (FPSC) that it believes that the Florida Energy Efficiency and Conservation Act (Chapter 366, Florida Statutes) as implemented by the FPSC satisfies the requirements in Section 410(1) of the ARRA. Specifically, Florida's general policies ensure that utility financial incentives are aligned with helping their customers use energy more efficiently

183

U.S. Department of Energy Office of General Counsel GC-52 1000 Independence Avenue, SW  

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

7, 1998 7, 1998 U.S. Department of Energy Office of General Counsel GC-52 1000 Independence Avenue, SW Washington, D.C. 20585 REPORT TO CONGRESS ON THE PRICE-ANDERSON ACT I appreciate the opportunity on behalf of Battelle Memorial Institute to respond to the Department of Energy's December 31, 1997 Federal Register "Notice of inquiry concerning preparation of report to Congress on the Price-Anderson Act." Battelle is a nonprofit charitable trust, devoted principally to research and development, education, technology transfer and scientific innovation. Battelle has a vital interest in this report in view of its operational role at two national laboratories and other DOE facilities. Battelle also supports DOE and other Federal agency activities in international nuclear non-proliferation and related

184

Adesso Inc. U.S. DEPARTMENT OF ENERGY 1000 INDEPENDENCE A VE., SW  

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

Adesso Inc. Adesso Inc. U.S. DEPARTMENT OF ENERGY 1000 INDEPENDENCE A VE., SW WASHINGTON, DC 20585 ) ) ) SUBPOENA Case Number: 2010-SE-2002 FOR INFORMATION AND PRODUCTION OF DOCUMENTS To: Margaret Traub, CEO Adesso Inc. 21 Penn Plaza Suite 909 New York, NY 10001 Issued: March 23, 2010 Service by certified mail The U.S. Department of Energy (DOE) issues this Subpoena for Information and Production of Documents to Adesso Inc. (Adesso) pursuant to 42 U.S.C. § 6299 of the Energy Policy and Conservation Act (EPCA) and the regulations promulgated thereunder (10 C.F.R. § 430. 72). As you should be aware, pursuant to EPCA, DOE has established an energy conservation standard applicable to torchieres. See 42 U.S.C. § 6295(x); 10 CFR 430.32(t). Manufacturers and private

185

PUBLIC ACCESS: 955 LEnfant Plaza North, SW, Suite 1500, Washington, DC  

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

th th Meeting Unconventional Resources Technology Advisory Committee July 14, 2009 1:00 p.m. EASTERN WebEx/Conference Call Meeting PUBLIC ACCESS: 955 L'Enfant Plaza North, SW, Suite 1500, Washington, DC AGENDA 12:30 Registration; Begin call in to 800-number and login to WebEx Members, Chair, Designated Federal Officer, and Committee Manager 1:00 Call to Order - Welcome Chris Hall, Committee Chair Member Roll Call and the presence of a quorum Elena Melchert Committee Manager Meeting purpose and review of the agenda; Insights regarding future funding and other pending legislation; Draft 2010 Annual Plan delivery, and pending meetings in September and October 2009 Guido DeHoratiis Designated Federal Officer 1:25 Report from the Standing Subcommittee and

186

J.G. Tobin and S.-W. Yu Lawrence Livermore National Laboratory, Livermore, CA, USA  

National Nuclear Security Administration (NNSA)

Differentiation of 5f and 6d Components Differentiation of 5f and 6d Components in the Unoccupied Electronic Structure of UO 2 J.G. Tobin and S.-W. Yu Lawrence Livermore National Laboratory, Livermore, CA, USA Summary: One of the crucial questions of all actinide electronic structure determinations is the issue of 5f versus 6d character and the distribution of these components across the density of states. Here, two break-though experiments will be discussed, which have allowed the direct determination of the U5f and U6d contributions to the unoccupied density of states (UDOS) in Uranium Dioxide (UO 2 ). [1] First, a combined soft X-ray Absorption and Bremstrahlung Isochromat Spectroscopy (XAS and BIS, respectively) study of UO 2 will be discussed. [2] Second, a novel Resonant Inverse Photoelectron and X-ray Emission Spectroscopy (RIPES and

187

1000 Independence Avenue, SW, Washington, D.C., Carol G. Crawford, Chair,  

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

FRIDAY, FRIDAY, OCTOBER 25, 2002 The meeting was held at 8:30 in Room 8E-089 of the Department of Energy, 1000 Independence Avenue, SW, Washington, D.C., Carol G. Crawford, Chair, presiding. PRESENT: CAROL G. CRAWFORD, Ph.D. Chair F. JAY BREIDT, Ph.D. Vice Chair MARK BERNSTEIN, Ph.D. JOHNNY BLAIR JAE EDMONDS, Ph.D. JAMES K. HAMMITT, Ph.D. NICHOLAS W. HENGARTNER CALVIN A. KENT, Ph.D. WILLIAM G. MOSS, Ph.D. POLLY A. PHIPPS, Ph.D. RANDY R. SITTER, Ph.D. ROY WHITMORE, Ph.D. ALSO PRESENT: CALVIN A. KENT, Ph.D. Former Committee Member and EIA Administrator ENERGY INFORMATION ADMINISTRATION REPRESENTATIVES: GUY F. CARUSO Administrator MARY J. HUTZLER Acting Deputy Administrator NANCY J. KIRKENDALL Director, Statistics and Methods Group PAUL McARDLE, Ph.D.

188

5.@'Y`fNX^[',ZqV~...OE[V" ("OESwHSw"`ZZOES)  

E-Print Network [OSTI]

·[·ó`?,?,?,é,½,?`¶·Ý,?,«,?,¢,?,¢,¤Isolated Pentagon Rule (IPR),?Sî,?·C·¬'·?'ö,?·í,?5 ^õS?·",ð ·?`å,?,µ,?_"OS"O{"h,ðOE¸,ç,·,æ,¤,?·\\`¢,ð `I`ð,µ,?,¢,-,?Z©"®"I,?Ih-C60 ·\\`¢,ªOE`·¬,³,ê,é·D,±,? IPR ^ê"?,?}N·--?,?·¶·¬,³,ê,ét·[OE ",ª IPR ,ð­z,½,·,?,¢,¤¼'è,Í·,ZYt·[OE",?Sô½ Sw"I·\\`¢,ðOE^,?,é·ã,?,?

Maruyama, Shigeo

189

PUBLIC ACCESS: 955 LEnfant Plaza North, SW, Suite 1500, Washington, DC  

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

10 10 th Meeting Ultra-Deepwater Advisory Committee July 15, 2009, 8:00 a.m. EASTERN, WebEx/Conference Call Meeting PUBLIC ACCESS: 955 L'Enfant Plaza North, SW, Suite 1500, Washington, DC AGENDA 7:30 Registration; Begin Member call in 8:00 Call to Order - Welcome Arnis Judzis, Vice-Chair Member Roll Call and the presence of a quorum Elena Melchert, Committee Manager Meeting purpose and review of the agenda; Insights regarding future funding and other pending legislation; Draft 2010 Annual Plan delivery, and pending meetings in September and October 2009 Guido DeHoratiis Designated Federal Officer 8:25 Report from the Standing Subcommittee regarding Process; Member Q/A and Discussion Mary Jane Wilson

190

Archaeology in the Kilauea East Rift Zone: Part 1, Land-use model and research design, Kapoho, Kamaili and Kilauea Geothermal Subzones, Puna District, Hawaii Island  

SciTech Connect (OSTI)

The Puna Geothermal Resource Subzones (GRS) project area encompasses approximately 22,000 acres centered on the Kilauea East Rift Zone in Puna District, Hawaii Island. The area is divided into three subzones proposed for geothermal power development -- Kilauea Middle East Rift, Kamaili and Kapoho GRS. Throughout the time of human occupation, eruptive episodes along the rift have maintained a dynamic landscape. Periodic volcanic events, for example, have changed the coastline configuration, altered patterns of agriculturally suitable sediments, and created an assortment of periodically active, periodically quiescent, volcanic hazards. Because of the active character of the rift zone, then, the area`s occupants have always been obliged to organize their use of the landscape to accommodate a dynamic mosaic of lava flow types and ages. While the specific configuration of settlements and agricultural areas necessarily changed in response to volcanic events, it is possible to anticipate general patterns in the manner in which populations used the landscape through time. This research design offers a model that predicts the spatial results of long-term land-use patterns and relates them to the character of the archaeological record of that use. In essence, the environmental/land-use model developed here predicts that highest population levels, and hence the greatest abundance and complexity of identifiable prehistoric remains, tended to cluster near the coast at places that maximized access to productive fisheries and agricultural soils. With the possible exception of a few inland settlements, the density of archaeological remains expected to decrease with distance from the coastline. The pattern is generally supported in the regions existing ethnohistoric and archaeological record.

Burtchard, G.C.; Moblo, P. [International Archaeological Research Inst., Inc., Honolulu, HI (United States)

1994-07-01T23:59:59.000Z

191

Calculations of the electronic states of the HgI and HgTe molecules by the SCF-X?-SW method  

Science Journals Connector (OSTI)

The SCF-X?-SW method was used to study the electronic structure and calculate the spectroscopic constants of the HgI and HgTe molecules in the ground and excited electronic states.

V. M. Kovba; E. A. Pazyuk

2006-08-01T23:59:59.000Z

192

Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585  

Gasoline and Diesel Fuel Update (EIA)

U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 August 1, 2012 Presenter Bios (Arranged in presentation order) Anthony Radich Tony Radich is an economist with the Energy Information Administration. He is currently a member of the Biofuels and Emerging Technologies Team in the Petroleum, Natural Gas and Biofuels Analysis group of the Office of Energy Analysis. Dr. Radich has worked on biofuels issues since he joined EIA in 2001. He developed the cost models for the production of ethanol and biodiesel, the National Energy Modeling System, which is used to produce the EIA Annual Energy Outlook. He has served as a contributing author to numerous EIA publications, including the Annual Energy Outlook and the Short-Term

193

TGF-{beta}1 increases invasiveness of SW1990 cells through Rac1/ROS/NF-{kappa}B/IL-6/MMP-2  

SciTech Connect (OSTI)

Research highlights: {yields} Rac1 mediates TGF-{beta}1-induced SW1990 invasion through MMP-2 secretion and activation. {yields} NADPH-generated ROS act downstream of Rac1 in TGF-{beta}1-challenged SW1990 cells. {yields} TGF-{beta}1-stimulated ROS activate NF-{kappa}B in SW1990 cells. {yields} NF{kappa}B-induced IL-6 release is required for secretion and activation of MMP-2 in SW1990 cells. -- Abstract: Human pancreatic cancer invasion and metastasis have been found to correlate with increased levels of active matrix metalloproteinase 2 (MMP-2). The multifunctional cytokine transforming growth factor beta 1 (TGF-{beta}1) has been shown to increase both secretion of MMP-2 and invasion by several pancreatic cancer cell types. In the present study, we investigated the signaling pathway involved in TGF-{beta}1-promoted MMP-2 secretion and invasion by human pancreatic cancer cells SW1990. Using specific inhibitors, we found that stimulation of these tumor cells with TGF-{beta}1 induced secretion and activation of the collagenase MMP-2, which was required for TGF-{beta}1-stimulated invasion. Our results also indicate that signaling events involved in TGF-{beta}1-enhanced SW1990 invasiveness comprehend activation of Rac1 followed by generation of reactive oxygen species through nicotinamide adenine dinucleotide phosphate-oxidase, activation of nuclear factor-kappa beta, release of interleukin-6, and secretion and activation of MMP-2.

Binker, Marcelo G. [Departments of Medicine and Physiology, University of Toronto, Toronto, Ontario, Canada M5S 1A8 (Canada) [Departments of Medicine and Physiology, University of Toronto, Toronto, Ontario, Canada M5S 1A8 (Canada); CBRHC Research Center, Buenos Aires (Argentina); Binker-Cosen, Andres A. [CBRHC Research Center, Buenos Aires (Argentina)] [CBRHC Research Center, Buenos Aires (Argentina); Gaisano, Herbert Y. [Departments of Medicine and Physiology, University of Toronto, Toronto, Ontario, Canada M5S 1A8 (Canada)] [Departments of Medicine and Physiology, University of Toronto, Toronto, Ontario, Canada M5S 1A8 (Canada); Cosen, Rodica H. de [CBRHC Research Center, Buenos Aires (Argentina)] [CBRHC Research Center, Buenos Aires (Argentina); Cosen-Binker, Laura I., E-mail: laura.cosen.binker@utoronto.ca [Departments of Medicine and Physiology, University of Toronto, Toronto, Ontario, Canada M5S 1A8 (Canada); CBRHC Research Center, Buenos Aires (Argentina)

2011-02-04T23:59:59.000Z

194

Magnetic biomonitoring by moss bags for industry-derived air pollution in SW Finland  

Science Journals Connector (OSTI)

Abstract We provide the first detailed case study using Sphagnum papillosum moss bags for active magnetic monitoring of airborne industrial pollution in order to evaluate the actual role of various emission sources and the competence of current environmental protection actions relative to the air quality. The origin and spatial spreading of particulate matter (PM) based on magnetic, chemical, and SEM-EDX analyses was studied around the Industrial Park in Harjavalta, SW Finland. The data was collected during two 6-month sampling periods along 8km transects in 20102011. The results support our hypothesis that the main emission source of PM is not the CuNi smelter's pipe as presumed in previous chemical monitorings. We argue that the hot spot area within the severe impact pollution zone is related to slag processing and/or other unidentified industrial activity. At short distances various dust-providing sources outweigh the fly-ash load from the CuNi smelter's pipe. Active magnetic monitoring by moss bags will help in planning environmental actions as well as in improvement of health conditions for industrial staff and town residents living next to the Industrial Park.

Hanna Salo; Joni Mkinen

2014-01-01T23:59:59.000Z

195

Geology of the Western Part of Los Alamos National Laboratory (TA-3 to TA-16), Rio Grande Rift, New Mexico  

SciTech Connect (OSTI)

We present data that elucidate the stratigraphy, geomorphology, and structure in the western part of Los Alamos National Laboratory between Technical Areas 3 and 16 (TA-3 and TA-16). Data include those gathered by geologic mapping of surficial, post-Bandelier Tuff strata, conventional and high-precision geologic mapping and geochemical analysis of cooling units within the Bandelier Tuff, logging of boreholes and a gas pipeline trench, and structural analysis using profiles, cross sections, structure contour maps, and stereographic projections. This work contributes to an improved understanding of the paleoseismic and geomorphic history of the area, which will aid in future seismic hazard evaluations and other investigations. The study area lies at the base of the main, 120-m (400-ft) high escarpment formed by the Pajarito fault, an active fault of the Rio Grande rift that bounds Los Alamos National Laboratory on the west. Subsidiary fracturing, faulting, and folding associated with the Pajarito fault zone extends at least 1,500 m (5,000 ft) to the east of the main Pajarito fault escarpment. Stratigraphic units in the study area include upper units of the Tshirege Member of the early Pleistocene Bandelier Tuff, early Pleistocene alluvial fan deposits that predate incision of canyons on this part of the Pajarito Plateau, and younger Pleistocene and Holocene alluvium and colluvium that postdate drainage incision. We discriminate four sets of structures in the area between TA-3 and TA-16: (a) north-striking faults and folds that mark the main zone of deformation, including a graben in the central part of the study area; (b) north-northwest-striking fractures and rare faults that bound the eastern side of the principal zone of deformation and may be the surface expression of deep-seated faulting; (c) rare northeast-striking structures near the northern limit of the area associated with the southern end of the Rendija Canyon fault; and (d) several small east-west-striking faults. We consider all structures to be Quaternary in that they postdate the Tshirege Member (1.22 million years old) of the Bandelier Tuff. Older mesa-top alluvial deposits (Qoal), which may have a large age range but are probably in part about 1.13 million years old, are clearly faulted or deformed by many structures. At two localities, younger alluvial units (Qfo and Qfi) appear to be truncated by faults, but field relations are obscure, and we cannot confirm the presence of fault contacts. The youngest known faulting in the study area occurred in Holocene time on a down-to-the-west fault, recently trenched at the site of a new LANL Emergency Operations Center (Reneau et al. 2002).

C.J.Lewis; A.Lavine; S.L.Reneau; J.N.Gardner; R.Channell; C.W.Criswell

2002-12-01T23:59:59.000Z

196

RECONNAISSANCE ASSESSMENT OF CO2 SEQUESTRATION POTENTIAL IN THE TRIASSIC AGE RIFT BASIN TREND OF SOUTH CAROLINA, GEORGIA, AND NORTHERN FLORIDA  

SciTech Connect (OSTI)

A reconnaissance assessment of the carbon dioxide (CO{sub 2}) sequestration potential within the Triassic age rift trend sediments of South Carolina, Georgia and the northern Florida Rift trend was performed for the Office of Fossil Energy, National Energy Technology Laboratory (NETL). This rift trend also extends into eastern Alabama, and has been termed the South Georgia Rift by previous authors, but is termed the South Carolina, Georgia, northern Florida, and eastern Alabama Rift (SGFAR) trend in this report to better describe the extent of the trend. The objectives of the study were to: (1) integrate all pertinent geologic information (literature reviews, drilling logs, seismic data, etc.) to create an understanding of the structural aspects of the basin trend (basin trend location and configuration, and the thickness of the sedimentary rock fill), (2) estimate the rough CO{sub 2} storage capacity (using conservative inputs), and (3) assess the general viability of the basins as sites of large-scale CO{sub 2} sequestration (determine if additional studies are appropriate). The CO{sub 2} estimates for the trend include South Carolina, Georgia, and northern Florida only. The study determined that the basins within the SGFAR trend have sufficient sedimentary fill to have a large potential storage capacity for CO{sub 2}. The deeper basins appear to have sedimentary fill of over 15,000 feet. Much of this fill is likely to be alluvial and fluvial sedimentary rock with higher porosity and permeability. This report estimates an order of magnitude potential capacity of approximately 137 billion metric tons for supercritical CO{sub 2}. The pore space within the basins represent hundreds of years of potential storage for supercritical CO{sub 2} and CO{sub 2} stored in aqueous form. There are many sources of CO{sub 2} within the region that could use the trend for geologic storage. Thirty one coal fired power plants are located within 100 miles of the deepest portions of these basins. There are also several cement and ammonia plants near the basins. Sixteen coal fired power plants are present on or adjacent to the basins which could support a low pipeline transportation cost. The current geological information is not sufficient to quantify specific storage reservoirs, seals, or traps. There is insufficient hydrogeologic information to quantify the saline nature of the water present within all of the basins. Water data in the Dunbarton Basin of the Savannah River Site indicates dissolved solids concentrations of greater than 10,000 parts per million (not potential drinking water). Additional reservoir characterization is needed to take advantage of the SGFAR trend for anthropogenic CO{sub 2} storage. The authors of this report believe it would be appropriate to study the reservoir potential in the deeper basins that are in close proximity to the current larger coal fired power plants (Albany-Arabi, Camilla-Ocilla, Alamo-Ehrhardt, and Jedburg basin).

Blount, G.; Millings, M.

2011-08-01T23:59:59.000Z

197

Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585  

Gasoline and Diesel Fuel Update (EIA)

Advanced Biofuels Workshop Advanced Biofuels Workshop U.S. Energy Information Administration 1000 Independence Ave. SW, Room 2E-069 Washington, DC 20585 August 1, 2012 Contact Information Hosts: Mindi Farber-DeAnda Team Lead, Energy Information Administration, Biofuels and Emerging Technologies Mindi.Farber-DeAnda@eia.gov 202-586-6419 Vishakh Mantri, Ph.D, P.E. Chemical Engineer, Energy Information Administration, Biofuels and Emerging Technologies Team Vishakh.Mantri@eia.gov 202-586-4815 Presenters Biofuels Year in Review Anthony Radich Analyst, Energy Information Administration Anthony.Radich@eia.gov 202-586-0504 Biofuels Outlook Terrence Higgins Hart Downstream Energy Services thiggins@hartenergy.com 703-891-4815 703-891-4815 Sustainability of Biofuels

198

U.S. Department of Energy Office of General Counsel, GC-52 1000 Independence Avenue, S.W.  

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

U.S. Department of Energy Office of General Counsel, GC-52 1000 Independence Avenue, S.W. Washington, D.C. 20585 RE: University of California Comments on Price-Anderson Act Notice of Inquiry The University appreciates the opportunity to comment on the Notice of Inquiry (NOI) concerning preparation of a report to Congress on the Price-Anderson Act. The NOI poses a number of questions that attempt to identify potential issues that might arise in developing the report. The University includes its general comments in this letter and offers its responses to the specific questions in an attachment. The Price-Anderson Act provides an important guarantee to American citizens that they will be compensated for injuries sustained as a result of exposure to nuclear materials. This guarantee must remain in effect regardless of how the

199

Regional generalisations about the relationships between the environment and foraminifera along the SW Cape coast, South Africa  

Science Journals Connector (OSTI)

Abstract Factors influencing the composition of shallow water benthic foraminifera along the SW coast of South Africa at two locations (Table Bay, TB; St Helena Bay, SHB) ?200km from each other were examined. Small taxa dominated in both locations; living assemblages from SHB (28 species, Ammonia parkinsoniana dominant) differed from TB (34 species, Elphidium articulatum dominant). Environmental parameters were similar in both areas. Patchiness in assemblage structure was pronounced, differences between pipeline and non-pipeline sites within locations were evident in environmental parameters. Diversity was significantly correlated with grain size, the nitrogen and heavy metal content (especially Cd). These data represent the first for extant benthic Foraminifera from the southern Benguela upwelling area and is the first attempt at using foraminifera as indicators of pollution in this region. The data stressed the need for more than one sampling location to better understand the factors influencing foraminiferal assemblages in any regional context.

R. Toefy; M.J. Gibbons

2014-01-01T23:59:59.000Z

200

FAR-ULTRAVIOLET SPECTROSCOPY OF THE NOVA-LIKE VARIABLE KQ MONOCEROTIS: A NEW SW SEXTANTIS STAR?  

SciTech Connect (OSTI)

New optical spectra obtained with the SMARTS 1.5 m telescope and archival International Ultraviolet Explorer (IUE) far-ultraviolet (FUV) spectra of the nova-like variable KQ Mon are discussed. The optical spectra reveal Balmer lines in absorption as well as He I absorption superposed on a blue continuum. The 2011 optical spectrum is similar to the KPNO 2.1 m IIDS spectrum we obtained 33 years earlier except that the Balmer and He I absorption is stronger in 2011. Far-ultraviolet IUE spectra reveal deep absorption lines due to C II, Si III, Si IV, C IV, and He II, but no P Cygni profiles indicative of wind outflow. We present the results of the first synthetic spectral analysis of the IUE archival spectra of KQ Mon with realistic optically thick, steady-state, viscous accretion-disk models with vertical structure and high-gravity photosphere models. We find that the photosphere of the white dwarf (WD) contributes very little FUV flux to the spectrum and is overwhelmed by the accretion light of a steady disk. Disk models corresponding to a WD mass of {approx}0.6 M {sub Sun }, with an accretion rate of order 10{sup -9} M {sub Sun} yr{sup -1} and disk inclinations between 60 Degree-Sign and 75 Degree-Sign , yield distances from the normalization in the range of 144-165 pc. KQ Mon is discussed with respect to other nova-like variables. Its spectroscopic similarity to the FUV spectra of three definite SW Sex stars suggests that it is likely a member of the SW Sex class and lends support to the possibility that the WD is magnetic.

Wolfe, Aaron; Sion, Edward M. [Astronomy and Astrophysics, Villanova University, 800 Lancaster Avenue, Villanova, PA 19085 (United States); Bond, Howard E., E-mail: awolfe03@villanova.edu, E-mail: edward.sion@villanova.edu, E-mail: bond@stsci.edu [Department of Astronomy and Astrophysics, Pennsylvania State University, University Park, PA 16802 (United States)

2013-06-01T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" 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

* Clinical Concentration--SW722, SW855 and SW856 #Macro Concentration --SW883, SW886 and SW889  

E-Print Network [OSTI]

Practice with Adults* OR Social Innovation# 3 CR 2 undergraduate courses 6 CR 2 undergraduate courses 6 CR

Huang, Jianyu

202

Technology Survey to Support Revision to the Remedial Investigation/Feasibility Study Work Plan for the 200-SW-2 Operable Unit at the U.S. Department of Energys Hanford Site  

SciTech Connect (OSTI)

A survey of technologies was conducted to provide information for a Data Quality Objectives process being conducted to support revision of the Remedial Investigation/Feasibility Study Work Plan for the 200-SW-2 Operable Unit. The technology survey considered remediation and characterization technologies. This effort was conducted to address, in part, comments on the previous version of the Remedial Investigation/Feasibility Study Work Plan for the 200-SW-2 Operable Unit as documented in 200SW1 and 200SW2 Collaborative Workshops?Agreement, Completion Matrix, and Supporting Documentation. By providing a thorough survey of remediation and characterization options, this report is intended to enable the subsequent data quality objectives and work plan revision processes to consider the full range of potential alternatives for planning of the Remedial Investigation/Feasibility Study activities.

Truex, Michael J.; Johnson, Christian D.; Nimmons, Michael J.

2007-09-25T23:59:59.000Z

203

Detection of a large fraction of atomic gas not associated with star-forming material in M17 SW  

E-Print Network [OSTI]

We probe the column densities and masses traced by the ionized and neutral atomic carbon with spectrally resolved maps, and compare them to the diffuse and dense molecular gas traced by [C I] and low-$J$ CO lines toward the star-forming region M17SW. We mapped a 4.1pc x 4.7pc region in the [C I] 609 m$\\mu$ line using the APEX telescope, as well as the CO isotopologues with the IRAM 30m telescope. We analyze the data based on velocity channel maps that are 1 km/s wide. We correlate their spatial distribution with that of the [C II] map obtained with SOFIA/GREAT. Optically thin approximations were used to estimate the column densities of [C I] and [C II] in each velocity channel. The spatial distribution of the [C I] and all CO isotopologues emission was found to be associated with that of [C II] in about 20%-80% of the mapped region, with the high correlation found in the central (15-23 km/s ) velocity channels. The excitation temperature of [C I] ranges between 40 K and 100 K in the inner molecular region of ...

Perez-Beaupuits, J P; Ossenkopf, V; Spaans, M; Gusten, R; Wiesemeyer, H

2015-01-01T23:59:59.000Z

204

Evaluation of geothermal potential of Rio Grande rift and Basin and Range province, New Mexico. Final technical report, January 1, 1977-May 31, 1978  

SciTech Connect (OSTI)

A study was made of the geological, geochemical and geophysical characteristics of potential geothermal areas in the Rio Grande rift and Basin and Range province of New Mexico. Both regional and site-specific information is presented. Data was collected by: (1) reconnaissance and detailed geologic mapping, emphasizing Neogene stratigraphy and structure; (2) petrologic studies of Neogene igneous rocks; (3) radiometric age-dating; (4) geochemical surveying, including regional and site-specific water chemistry, stable isotopic analyses of thermal waters, whole-rock and mineral isotopic studies, and whole-rock chemical analyses; and (5) detailed geophysical surveys, using electrical, gravity and magnetic techniques, with electrical resistivity playing a major role. Regional geochemical water studies were conducted for the whole state. Integrated site-specific studies included the Animas Valley, Las Cruces area (Radium Springs and Las Alturas Estates), Truth or Consequences region, the Albuquerque basin, the San Ysidro area, and the Abiquiu-Ojo Caliente region. The Animas Valley and Las Cruces areas have the most significant geothermal potential of the areas studied. The Truth or Consequences and Albuquerque areas need further study. The San Ysidro and Abiquiu-Ojo Caliente regions have less significant geothermal potential. 78 figs., 16 tabs.

Callender, J.F.

1985-04-01T23:59:59.000Z

205

Phosphatidylinositol 5-phosphate 4-kinase type II beta is required for vitamin D receptor-dependent E-cadherin expression in SW480 cells  

SciTech Connect (OSTI)

Highlights: {yields} We analyzed Phosphatidylinositol 5-phosphate kinase II{beta} (PIPKII{beta}) function in cancer. {yields} PIPKII{beta} is required for vitamin D receptor-mediated E-cadherin upregulation in SW480. {yields} PIPKII{beta} suppresses cellular motility through E-cadherin induction in SW480 cells. {yields} Nuclear PIP{sub 2} but not plasma membrane-localized PIP{sub 2} mediates E-cadherin upregulation. -- Abstract: Numerous epidemiological data indicate that vitamin D receptor (VDR) signaling induced by its ligand or active metabolite 1{alpha},25-dihydroxyvitamin D{sub 3} (1{alpha},25(OH){sub 2}D{sub 3}) has anti-cancer activity in several colon cancers. 1{alpha},25(OH){sub 2}D{sub 3} induces the epithelial differentiation of SW480 colon cancer cells expressing VDR (SW480-ADH) by upregulating E-cadherin expression; however, its precise mechanism remains unknown. We found that phosphatidylinositol-5-phosphate 4-kinase type II beta (PIPKII{beta}) but not PIPKII{alpha} is required for VDR-mediated E-cadherin induction in SW480-ADH cells. The syntenin-2 postsynaptic density protein/disc large/zona occludens (PDZ) domain and pleckstrin homology domain of phospholipase C-delta1 (PLC{delta}1 PHD) possess high affinity for phosphatidylinositol-4,5-bisphosphate (PI(4,5)P{sub 2}) mainly localized to the nucleus and plasma membrane, respectively. The expression of syntenin-2 PDZ but not PLC{delta}1 PHD inhibited 1{alpha},25(OH){sub 2}D{sub 3}-induced E-cadherin upregulation, suggesting that nuclear PI(4,5)P{sub 2} production mediates E-cadherin expression through PIPKII{beta} in a VDR-dependent manner. PIPKII{beta} is also involved in the suppression of the cell motility induced by 1{alpha},25(OH){sub 2}D{sub 3}. These results indicate that PIPKII{beta}-mediated PI(4,5)P{sub 2} signaling is important for E-cadherin upregulation and inhibition of cellular motility induced by VDR activation.

Kouchi, Zen, E-mail: zkouchi@toyaku.ac.jp [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan)] [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan); Fujiwara, Yuki [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan)] [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan); Yamaguchi, Hideki [Division of Metastasis and Invasion Signaling, National Cancer Center Research Institute, 5-1-1 Tsukiji, Chuo-ku, Tokyo 104-0045 (Japan) [Division of Metastasis and Invasion Signaling, National Cancer Center Research Institute, 5-1-1 Tsukiji, Chuo-ku, Tokyo 104-0045 (Japan); PRESTO, Japan Science and Technology Agency, 4-1-8 Honcho, Kawaguchi-city, Saitama 332-0012 (Japan); Nakamura, Yoshikazu; Fukami, Kiyoko [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan)] [Laboratory of Genome and Biosignals, Tokyo University of Pharmacy and Life Sciences, 1432-1 Horinouchi, Hachioji-city, Tokyo 192-0392 (Japan)

2011-05-20T23:59:59.000Z

206

1000 Independence Avenue, SW  

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

* Construction * R&D * ManagementScientific Consultation and Analysis * Administrative Services * IT and Data Processing * Security * Engineering * Waste Treatment and Disposal...

207

Interim Report on SNP analysis and forensic microarray probe design for South American hemorrhagic fever viruses, tick-borne encephalitis virus, henipaviruses, Old World Arenaviruses, filoviruses, Crimean-Congo hemorrhagic fever viruses, Rift Valley fever  

SciTech Connect (OSTI)

The goal of this project is to develop forensic genotyping assays for select agent viruses, enhancing the current capabilities for the viral bioforensics and law enforcement community. We used a multipronged approach combining bioinformatics analysis, PCR-enriched samples, microarrays and TaqMan assays to develop high resolution and cost effective genotyping methods for strain level forensic discrimination of viruses. We have leveraged substantial experience and efficiency gained through year 1 on software development, SNP discovery, TaqMan signature design and phylogenetic signature mapping to scale up the development of forensics signatures in year 2. In this report, we have summarized the whole genome wide SNP analysis and microarray probe design for forensics characterization of South American hemorrhagic fever viruses, tick-borne encephalitis viruses and henipaviruses, Old World Arenaviruses, filoviruses, Crimean-Congo hemorrhagic fever virus, Rift Valley fever virus and Japanese encephalitis virus.

Jaing, C; Gardner, S

2012-06-05T23:59:59.000Z

208

Exploratory energy research program of the University of Hawaii at Manoa. Progress report  

SciTech Connect (OSTI)

Progress is reported from the University of Hawaii on: UHM rooftop solar energy laboratory; solar pond cleansing techniques; combustion properties of biomass pyrolysis products; high-temperature solar concentrator absorber; biological abatement of hydrogen sulfide during geothermal energy production; geothermal systems on submarine rift zones of the Hawaiian chain; nitrogenous products of OTEC chlorination; interaction of hydrogen and deuterium with transition metals and their alloys at high pressures; shallow magma chambers and geothermal potential of Haleakala, Maui; effects of OTEC waste water on phytoplankton; sodium-lithium geothermometer; breaking wave forces on OTEC pipes; seismic and thermal properties on basalts. (PSB)

Not Available

1984-01-01T23:59:59.000Z

209

RADIOACTIVE DEMONSTRATION OF FINAL MINERALIZED WASTE FORMS FOR HANFORD WASTE TREATMENT PLANT SECONDARY WASTE (WTP-SW) BY FLUIDIZED BED STEAM REFORMING (FBSR) USING THE BENCH SCALE REFORMER PLATFORM  

SciTech Connect (OSTI)

The U.S. Department of Energys Office of River Protection (ORP) is responsible for the retrieval, treatment, immobilization, and disposal of Hanfords tank waste. Currently there are approximately 56 million gallons of highly radioactive mixed wastes awaiting treatment. A key aspect of the River Protection Project (RPP) cleanup mission is to construct and operate the Waste Treatment and Immobilization Plant (WTP). The WTP will separate the tank waste into high-level and low-activity waste (LAW) fractions, both of which will subsequently be vitrified. The projected throughput capacity of the WTP LAW Vitrification Facility is insufficient to complete the RPP mission in the time frame required by the Hanford Federal Facility Agreement and Consent Order, also known as the Tri-Party Agreement (TPA), i.e. December 31, 2047. Therefore, Supplemental Treatment is required both to meet the TPA treatment requirements as well as to more cost effectively complete the tank waste treatment mission. In addition, the WTP LAW vitrification facility off-gas condensate known as WTP Secondary Waste (WTP-SW) will be generated and enriched in volatile components such as {sup 137}Cs, {sup 129}I, {sup 99}Tc, Cl, F, and SO{sub 4} that volatilize at the vitrification temperature of 1150C in the absence of a continuous cold cap (that could minimize volatilization). The current waste disposal path for the WTP-SW is to process it through the Effluent Treatment Facility (ETF). Fluidized Bed Steam Reforming (FBSR) is being considered for immobilization of the ETF concentrate that would be generated by processing the WTP-SW. The focus of this current report is the WTP-SW. FBSR offers a moderate temperature (700-750C) continuous method by which WTP-SW wastes can be processed irrespective of whether they contain organics, nitrates, sulfates/sulfides, chlorides, fluorides, volatile radionuclides or other aqueous components. The FBSR technology can process these wastes into a crystalline ceramic (mineral) waste form. The mineral waste form that is produced by co-processing waste with kaolin clay in an FBSR process has been shown to be as durable as LAW glass. Monolithing of the granular FBSR product is being investigated to prevent dispersion during transport or burial/storage, but is not necessary for performance. A Benchscale Steam Reformer (BSR) was designed and constructed at the SRNL to treat actual radioactive wastes to confirm the findings of the non-radioactive FBSR pilot scale tests and to qualify the waste form for applications at Hanford. BSR testing with WTP SW waste surrogates and associated analytical analyses and tests of granular products (GP) and monoliths began in the Fall of 2009, and then was continued from the Fall of 2010 through the Spring of 2011. Radioactive testing commenced in 2010 with a demonstration of Hanfords WTP-SW where Savannah River Site (SRS) High Level Waste (HLW) secondary waste from the Defense Waste Processing Facility (DWPF) was shimmed with a mixture of {sup 125/129}I and {sup 99}Tc to chemically resemble WTP-SW. Prior to these radioactive feed tests, non-radioactive simulants were also processed. Ninety six grams of radioactive granular product were made for testing and comparison to the non-radioactive pilot scale tests. The same mineral phases were found in the radioactive and non-radioactive testing. The granular products (both simulant and radioactive) were tested and a subset of the granular material (both simulant and radioactive) were stabilized in a geopolymer matrix. Extensive testing and characterization of the granular and monolith material were made including the following: ? ASTM C1285 (Product Consistency Test) testing of granular and monolith; ? ASTM C1308 accelerated leach testing of the radioactive monolith; ? ASTM C192 compression testing of monoliths; and ? EPA Method 1311 Toxicity Characteristic Leaching Procedure (TCLP) testing. The significant findings of the testing completed on simulant and radioactive WTP-SW are given below: ? Data indicates {sup 99}Tc, Re, Cs, and I

Crawford, C.; Burket, P.; Cozzi, A.; Daniel, G.; Jantzen, C.; Missimer, D.

2014-08-21T23:59:59.000Z

210

Upstream -- SW92-03&  

Office of Legacy Management (LM)

777 678 650 pH c s.u. 7.58 8.25 7.88 7.83 Temperature c C 6.5 15.7 16.1 8.8 Common Ions Ca b mgL 132 107 89.7 81.2 Chloride b mgL 7.26 10.7 8.57 22.9 Fluoride b gL 196 148...

211

Submarine Thermal Sprirngs on the Galpagos Rift  

Science Journals Connector (OSTI)

...McLean, Los Angeles County Museum of Natural History; the pogonophorans by M. Jones, National Mu-seum of Natural History; and the fish photo-graphs...examined by D. Cohen, National Museum of Natural History. 56. The analyses of 210Pb...

John B. Corliss; Jack Dymond; Louis I. Gordon; John M. Edmond; Richard P. von Herzen; Robert D. Ballard; Kenneth Green; David Williams; Arnold Bainbridge; Kathy Crane; Tjeerd H. van Andel

1979-03-16T23:59:59.000Z

212

A Microearthquakes Survey in the Ethiopian Rift  

Science Journals Connector (OSTI)

...density, highly porous airborne vol- canic ejecta near...explosions for such stress-release experiments cannot be...a)+e2 /7 f is the fraction of stress drop and a...Steinbrugge Pacific Fire Rating Bureau San Francisco...fault belt without the release of seismic energy. Hence...

Peter Molnar; Thomas J. Fitch; Laika Mariam Asfaw

213

Origin of the ore-forming fluids of the Tongchang porphyry CuMo deposit in the JinshajiangRed River alkaline igneous belt, SW China: Constraints from He, Ar and S isotopes  

Science Journals Connector (OSTI)

The JinshajiangRed River alkaline igneous belt with abundant CuMoAu mineralization, in the eastern IndianAsian collision zone, is an important Cenozoic magmatic belt formed under an intra-continental strike-slip system in southwestern (SW) China. The Tongchang deposit is a representative porphyry CuMo deposit in southern segment of the JinshajiangRed River alkaline igneous belt, with 8621t Cu @ 1.24wt.% and 17,060t Mo @ 0.218wt.%. In this study, He, Ar and S isotopic compositions of the Tongchang deposit were determined. He and Ar isotopic compositions suggest that the ore-forming fluids, with 3He/4He ratios varying from 0.17 to 1.50Ra and 40Ar/36Ar ratios from 299.1 to 347.3 for the deposit, are a mixture between a crust-derived fluid (MASW) with near atmospheric Ar and crustal He, and a mantle-derived fluid. However, the ?34S values of the hydrothermal pyrite samples ranging from 1.0 to 1.5 with an average of 1.2, indicate that the sulfur in the ore-forming fluids of the Tongchang deposit was primarily derived from the magma or indirectly mantle-derived without assimilation of crustal sulfur. In combination with previously published He and Ar isotopic data of the Yulong and Machangqing deposits in northern and central segments of the JinshajiangRed River alkaline igneous belt, respectively, the ore-forming fluids of the Yulong and Machangqing deposits are obviously richer in 3He and 40Ar, and poorer in 36Ar in comparison with the Tongchang deposit, implying that more mantle-derived fluids were involved in the ore-forming fluids of the Yulong and Machangqing deposits than those for the Tongchang deposit. This might be one of the most important factors producing larger scales of mineralization in the Yulong and Machangqing deposits than the Tongchang deposit.

Leiluo Xu; Xianwu Bi; Ruizhong Hu; Yongyong Tang; Guohao Jiang; Youqiang Qi

2014-01-01T23:59:59.000Z

214

Delta Faucet: Data Request (2010-SW-1603)  

Broader source: Energy.gov [DOE]

DOE requested test data from Delta Faucet Corporation for Delta Faucet's showerhead model "In2ition 75582".

215

Your Guide to 1912 SW 6th  

E-Print Network [OSTI]

the laundry rooms. Heat The heating in Ondine is run by a hot water heated coil fan system. Each room has and the warm air that is produced is disseminated throughout the unit using a fan. Each room has a control a heating system that is tied to the rest of the building. The coils are heated using a hot water structure

Latiolais, M. Paul

216

Rheology of the lithosphere in the East African Rift System  

Science Journals Connector (OSTI)

......Terrestrial heat flow studies in Cyprus and Kenya, PhD thesis, University...absolute temperature, R the gas constant, and B, n, and E...This work was supported by the Natural Sciences and Engineering Research...Terrestrial heat flow studies in Cyprus and Kenya, PhD thesis, University......

K. Fadaie; G. Ranalli

1990-08-01T23:59:59.000Z

217

Earthquake hazard in the Kenya Rift: the Subukia earthquake 1928  

Science Journals Connector (OSTI)

......Sketches, p. 6, Det. Publ. Works, Nairobi. Sikes, H. L., 1934. The underground water resources of Kenya colony, Publ. Gout. Kenya Col. & Protect., p. 22, plt. 21, London. Simmons, W. C., 1982a. Notes taken in the Nakuru area in connection......

N. N. Ambraseys

1991-04-01T23:59:59.000Z

218

Compound and Elemental Analysis At Kilauea East Rift Geothermal...  

Open Energy Info (EERE)

(XRF). The samples were made into thin sections as well as ground in a tungsten carbide grinding mill. A table of trace elements and amounts found during the analysis is...

219

Are buoyancy forces important during the formation of rifted margins?  

Science Journals Connector (OSTI)

......asterisks. (f) Peclet number vs margin extension. Letter code for margins: C = Carolina, C2 = Carolina (alternative...West (alternative), LE = Labrador East, NS = Nova Scotia, NS2 = Nova Scotia (alternative), NEW = Newfoundland margin, GEO......

Mark Davis; Nick Kusznir

2002-05-01T23:59:59.000Z

220

Mauna Loa Southwest Rift Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Date: Well Name: Location: Depth: Initial Flow Rate: "fcf" is not declared as a valid unit of measurement for this property. The given value was not understood. Flow Test...

Note: This page contains sample records for the topic "haleakala sw rift" 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

Mantle helium in hydrothermal plumes in the Galapagos Rift  

Science Journals Connector (OSTI)

... the laboratory for analysis on a 3He/4He ratio mass spectrometer as described previously3'5. Radon activities were measured at sea on six of these samples, using our normal shipboard ... 3He observed in the deep oceans, by seawater penetration and circulation in the basalts.Radon concentrations (Table 1) are reported as 'excess ...

J. E. LUPTON; R. F. WEISS; H. CRAIG

1977-06-16T23:59:59.000Z

222

Evaluation of Geothermal Potential of Rio Grande Rift and Basin...  

Open Energy Info (EERE)

age-dating; 4) geochemical surveying, including regional and site-specific water chemistry , stable isotopic analyses of thermal waters , whole-rock and mineral isotopic...

223

Groundwater Sampling At Kilauea East Rift Geothermal Area (Cox...  

Open Energy Info (EERE)

can be a useful geochemical indicator for geothermal exploration when other water chemistry techniques are ambiguous. This research was useful for locating some areas which...

224

The transatlantic rift in genetically modified food policy  

Science Journals Connector (OSTI)

The regulatory structures underlying United States and European Union policies regarding genetically modified (GM) food and crops are fundamentally different. The US regulates GM foods and crops as end product...

Celina Ramjou

2007-10-01T23:59:59.000Z

225

New regionalism and World Order: a long term Transatlantic "Rift"?.  

E-Print Network [OSTI]

??This research aims to compare the competing regionalisms and interregional policies of the European Union and those of the United States, by addressing a crucial (more)

POLLIO, EMANUELE

2009-01-01T23:59:59.000Z

226

Geothermal Resources of Rifts- a Comparison of the Rio Grande...  

Open Energy Info (EERE)

(> 200C). Greenschist facies metamorphism has been observed in several of the geothermal wells. Localized upper crustal melting is a distinct possibility and there is...

227

Static Temperature Survey At Rio Grande Rift Region (Morgan,...  

Open Energy Info (EERE)

Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Additional References Retrieved from "http:en.openei.orgwindex.php?titleStaticTem...

228

Data Acquisition-Manipulation At Rio Grande Rift Region (Morgan...  

Open Energy Info (EERE)

Sares (2010) Prospects For Electricity Generation In The San Luis Basin, Colorado, Usa Additional References Retrieved from "http:en.openei.orgwindex.php?titleDataAcqui...

229

Micro-Earthquake At Kilauea East Rift Geothermal Area (Kenedi...  

Open Energy Info (EERE)

to this study: Shear wave splitting, double difference earthquake location, and 3-D tomography. This study was beneficial in helping to improve the local velocity model, identify...

230

28 November 2011 Rifts cloud start of UN climate talks  

E-Print Network [OSTI]

and sustainability services leader at Ernst & Young. Nick Robins, head of HSBC's climate change group, is equally

231

U.S. Department of Energy 1000 Independence Ave, SW  

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

of, of, ) Westinghouse Lighting Corporation ) Case Number: 2010-CE-09/1001 Issued : August 5, 2010 NOTICE OF ALLOWANCE TO RESUME DISTRIBUTION Manufacturers of certain covered products which have been determined by the Department of Energy (DOE) to be non-compliant with the applicable energy conservation standard may be allowed to resume distribution, per 10 CFR § 430.70 (a)(6)(v), if additional testing results supplied by the manufacturer results in a determination of compliance. On June 14, 2010, DOE issued a Notice of Non-Compliance Determination based on test results submitted by Westinghouse showing that certain models were noncompliant. Westinghouse later admitted that the original test results were based on testing that was not performed in accordance with

232

U.S. Department of Energy 1000 Independence Ave, SW  

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

of: of: Aspen Manufacturing Case Number 2010-SE-0305 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. The compliance statement is a legal statement by the manufacturer that the information provided in its certification reports is true, accurate and complete, that the basic models certified meet the applicable energy conservation standard, that the energy efficiency information report is the result of testing performed in conformance with the applicable test requirements in 10 CFR part 430, subpart B; and that the manufacturer is

233

U.S. Department of Energy 1000 Independence Ave, SW  

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

of. of. Westinghouse Lighting Corporation Case Number : 2010-CE -09/ 1001 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. As of April 19, 2010, Westinghouse Lighting Corporation (Westinghouse) had not filed these documents with DOE. Accordingly, DOE issued a Notice of Proposed Civil Penalty for apparent violations of the certification requirements. On June 4, 2010, Westinghouse provided to DOE a compliance statement for incandescent reflector lamps and copies of test reports for a variety of models of incandescent reflector lamps.

234

Microsoft PowerPoint - SW HydropowerCouncil-060910.pptx  

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

CW appropriations are projected to decrease relative to inflation * The cost of the work we do is expected to increase at a rate greater than inflation increase at a rate...

235

DEC SW 40th Street | Department of Energy  

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

HW, CHW, and DHW service (8-9%). Data Collection to Establish Model for Geothermal District System. gshpamancherlakronaizldecsw40thst.pdf More Documents & Publications...

236

EFFLER, SW [ED.]. 1996. Limnological and engineering analysis of ...  

Science Journals Connector (OSTI)

EFFLER, S. W. [ED.]. 1996. Limnological and engineering analysis ... This book is about the natural history of fresh water, starting from the ground up, literally.

1999-03-11T23:59:59.000Z

237

EChO Payload electronics architecture and SW design  

E-Print Network [OSTI]

EChO is a three-modules (VNIR, SWIR, MWIR), highly integrated spectrometer, covering the wavelength range from 0.55 $\\mu$m, to 11.0 $\\mu$m. The baseline design includes the goal wavelength extension to 0.4 $\\mu$m while an optional LWIR module extends the range to the goal wavelength of 16.0 $\\mu$m. An Instrument Control Unit (ICU) is foreseen as the main electronic subsystem interfacing the spacecraft and collecting data from all the payload spectrometers modules. ICU is in charge of two main tasks: the overall payload control (Instrument Control Function) and the housekeepings and scientific data digital processing (Data Processing Function), including the lossless compression prior to store the science data to the Solid State Mass Memory of the Spacecraft. These two main tasks are accomplished thanks to the Payload On Board Software (P-OBSW) running on the ICU CPUs.

Focardi, M; Farina, M; Pancrazzi, M; Ottensamer, R; Lim, T L; Pezzuto, S; Micela, G; Pace, E

2014-01-01T23:59:59.000Z

238

SW 540 Campbell Spring 2014 THE UNIVERSITY OF TENNESSEE  

E-Print Network [OSTI]

Social Work (3 credits) Instructor: Robert J. Campbell, LCSW, BCD Time: 7:00-8:30 PM EST Wednesdays Email, 513, 522, 537 Code of Conduct It is the student's responsibility to have read the College of Social Work Ethical Academic and Professional Conduct Code that is in the College of Social Work MSSW Handbook

Grissino-Mayer, Henri D.

239

Innovations in Nuclear Infrastructure and Education From the SW Consortium  

SciTech Connect (OSTI)

This report describes the final expenditures for the INIE project during FY 08/09. (There were no expenditures during FY09/10 or during FY10/11.) To see the list of accomplishments done using the INIE funds, please see the reports included here. The last of the FY 07/08 funds were brought forward and used to complete two distance education modules teaching reactor experiments. These modules and parts from the modules are still being used and are being disseminated off-campus as a part of our distance education effort. The second largest expenditure was sending students to the ANS to present student papers on work that they had done the previous year underwritten by INIE funds. The remaining expenditures were IDC charges and minor travel expenses to give students a tour of a medical facility. Once again we wish to express of sincere appreciation of the INIE program and hope that the return on investment is appreciated by the DOE. Although INIE has come to a close, looking back at all the Consortium has accomplished is astounding. And, as was hoped, these funds have proved to be a springboard for continuing work, particularly at Texas A&M. With the resurgence of nuclear power, the utilities have realized that the nuclear workforce in the near future will be too small for the task of bringing dozens of new plants on line and have turned their attention to the URRs to help feed the workforce pipeline. The distance education modules developed at the A&M are soon to be broadcast throughout the country to help train a new generation of nuclear workers. Our students at the Nuclear Science Center at being snapped up by the nuclear power plants after graduating. Our research projects at A&M have all ended with new data, new ways of looking at old problems, and produced a covey of good students. I want to say 'Thanks' with utmost sincerity because without the INIE funds our efforts would yield a small fraction of the accomplishments you see in this report.

Warren Reece

2011-03-22T23:59:59.000Z

240

Forrestal Building, 1000 Independence Avenue, S.W.,  

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

Miller, EIA. MR. FREEDMAN: Stan Freedman, EIA. MS. JENNINGS: Aletha Jennings, EIA. MR. SMITH: Antoine Smith, EIA. MS. CAVANAUGH: Kathleen Cavanaugh, EIA. MR. SEDRANSK: Joe...

Note: This page contains sample records for the topic "haleakala sw rift" 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

U.S. Department of Energy 1000 Independence Ave, SW  

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

Advanced Distributor Products ) Case Number 2010-SE-0304 NOTICE OF NONCOMPLIANCE DETERMINATION CERTIFICATION Manufacturers of certain covered products are required to certify compliance with the applicable energy conservation standards through submission of a compliance statement and a certification report. 10 CFR § 430.62. See 42 U.S.C. 6296. The compliance statement is a legal statement by the manufacturer that the information provided in its certification reports is true, accurate and complete, that the basic models certified meet the applicable energy conservation standard, that the energy efficiency information report is the result of testing performed in conformance with the applicable test requirements in 10 CFR part 430, subpart B; and that the manufacturer is

242

U.S. Department of Energy 1000 Independence Ave, SW  

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

Case Number: 2010-SE-0103 Case Number: 2010-SE-0103 Whirlpool Corporation ) NOTICE OF COMPLIANCE DETERMINATION Issued on: July 08, 2010 On April 5, 2010, the Department of Energy (DOE) issued a Request for Data to Whirlpool Corporation (Whirlpool) in response to information received by DOE indicating that Whirlpool's Maytag refrigerator-freezer model "MSD2578VE" exceeds the applicable Federal energy conservation standard. On April 29, 2010, Whirlpool submitted to DOE a summary chart of its test data for the Maytag refrigerator-freezer model "MSD2578VE." In response to DOE's request for the underlying test data that formed the basis for the summary chart, Whirlpool submitted the raw test data to DOE on May 18, 2010. Whirlpool's Maytag refrigerator-freezer model "MSD2578VE" was selected for testing as part

243

FT-ICR `'u,SJ"-,t[OE",Z-- "OESw`Sw@HSwOEnOE<<@SBHSwU  

E-Print Network [OSTI]

/s),?,æ,Á,?·C"w^³3·~10-10 Torr ,?·,·^DFig. 3 ,?·¶·"·ª,?,ÍOE·[U·[·ö"-NX^·[OE¹,ª, ,é,ª

Maruyama, Shigeo

244

Brent C. Christner and John C. Priscu SW-1845 Page 1 of 6 Subglacial Lake Vostok (SW-1845)  

E-Print Network [OSTI]

heating and the insulation caused by the overlying ~4 km of ice, despite surface air temperatures commonly's expansive continental ice sheet. The realization that there was life on the Antarctic continent, other than conducted on a deep ice core from Vostok Station. These studies suggested that the cryosphere of Antarctica

Priscu, John C.

245

Structure of the Gabon Margin from integrated seismic reflection and gravity data  

Science Journals Connector (OSTI)

In the South Gabon Basin, deep multi-channel seismic reflection and gravity modeling analysis have shed light on key features of the structure of the margin. The thinned continental crust beneath the Gabon Margin appears to be composed of two distinct layers, separated by a clear, strong and more or less continuous reflector running in the 710s TWT window. The lower crust is characterized by a higher density, intermediate between the lower values of the upper crust and the denser values of the mantle. The lower crust is irregularly shaped and presents lateral thickness variations along the direction of thinning and along the coast. In the offshore thinned continental domain, the lower and upper crust form a 2025km thick body. Crustal thicknesses point to a relatively sharp and narrow transition, along a few tens of kilometers, between the unthinned and the thinned continental crust. The high density layer identified offshore Gabon presents similar characteristics in density, geometry and spatial distribution, as the underplated magmatic bodies observed along volcanic margins, e.g. along the South Atlantic Namibia Margin or the North Atlantic Vring Margin. Although this lower crustal body could possibly represent ultra mafic serpentinized rocks or high grade metamorphic crustal rocks, we suggest that it could be composed of mafic rocks. Magmas resulting from partial melting during rifting may underplate the crust and/or be intruded in the lower crust through a system of dykes and sills. In this view, the present-day crustal thicknesses along rifted margins, characterized by magmatic underplating and/or intrusion, are not representative of the thinning that the crust experienced during rifting. Results of this study point to relatively shallow sedimentary basins along the South Gabon Margin. The deepest offshore depocenters located under the westernmost side of the continental platform appear to be associated with the deepest syn-rift basins These basins seem to extend along 20 to 40km in the ~NESW direction with a present-day average thickness of 7.3km. Offshore Gabon, whereas the crustal thinning appears significant, the syn-rift deposit are not thick. We suggest that the area was anomalously uplifted during the rifting phase, due to an elevated thermal lithospheric gradient. The conclusions derived from our seismic and gravity analysis are consistent with the implications such a thermal anomaly would have on the tectonic evolution of a rifted margin with 1) an underplated high density lower crustal layer, 2) shallow depth syn-rift basins associated with a relatively thin crust and subsequently 3) elevated recorded subsidence rates in the initial post-rift stages.

Stphanie Dupr; Sierd Cloetingh; Giovanni Bertotti

2011-01-01T23:59:59.000Z

246

Cenozoic deformation in the George V Land continental margin (East Antarctica)  

Science Journals Connector (OSTI)

This investigation is based on the analysis of multichannel seismic data collected in the continental shelf of the George V Land, between 140E and 155E on the East Antarctic margin. Most of the East Antarctic continental shelf is covered by permanent, thick sea and terrestrial ice and it is therefore still unexplored. This is the reason why the tectonic deformation affecting the Antarctic margin during the Mesozoic rift from the Australian plate and the Cenozoic post-rift phase is poorly known. The few coastal polynyas (such as the Mertz polynya, in the George V Land continental shelf) are the only places where the oldest sedimentary section can be studied with the existing technology. The data presented were not collected to address tectonic questions, however the relevance of this study is to document for the first time the occurrence of rift and post-rift tectonic structures in the sedimentary section near the coast, where the oldest sediment section is shallowest. These considerations are particularly relevant as Mertz-Ninnis trough, also known as George V Basin is located near the area of transition (around the Spencer Fracture Zone) between the extensionally-dominated Wilkes LandGreat Australian Bight Basin conjugate segment of the AustralianAntarctic Rift and the transtensional, strike-slip kinematics of the Otway BasinSouth Tasman RiseOates Land segment. The tectonic structure in the George V Land sector presented in this study is two-fold with two rift phases: one being connected to the breakup process and the later one associated to a change in plate rotation. A former extensional phase opened structural grabens, with axis oriented WNWESE and possibly NESW. A latter transpressional phase reactivated previous structures and tilted, faulted and folded sedimentary strata, located in the inner continental shelf. The first tectonic phase is likely related with the Cretaceous rifting between the Antarctic and Australian plates. The second tectonic phase might be related to the onset of the fast spreading phase of PacificIndian Ocean, that caused uplift, inversion and folding of post-rift strata in a narrow eastwest oriented region, near coastal basement outcrop, in PaleoceneEocene times.

Laura De Santis; Giuliano Brancolini; Federica Donda; Phil O'Brien

2010-01-01T23:59:59.000Z

247

Shallow velocity model of the Rio Grande rift near Socorro, New Mexico  

Science Journals Connector (OSTI)

...f Joyita Hills, Los Pinos Mountains , and northern Chupadera Mesa, Valencia, Torrance, and Socorro Counties: U...the region from Socorro and San A n t o n i o east to Chupadera Mesa, Socorro C o u n t y , N e w Mex ico : U.S. Geologi...

248

Terrestrial Heat Flow along the Rio Grande Rift, New Mexico and Southern Colorado  

Science Journals Connector (OSTI)

...3 33 C H L O R I D E * 2 ( N M ) CHUPADERA- MESA ( NM ) " 33 1 9 3 4 0 6 " 1C7 4 2...35 0 9 1 0 6 1 6 HORSE "RANG"E MESA" t V I 3 T " 5 9 1 " 0 T " 0 7 I...I P E / E A S T ( N M ) SAN MATEO MESA ( N M ) SAN" PEDRT3 * 1 - ( N H...

249

Episodic Rifting of Phanerozoic Rocks in the Victoria Land Basin, Western Ross Sea, Antarctica  

Science Journals Connector (OSTI)

...Geological Survey multichannel seismic-reflection tracklines, and location of seismic line 407 (Fig. 2). 1085 the axis tow art iions of naginatic rocks. The faultsap-pear to cut sedimentary rocks near the seafloor and to show an increasing dis-Olacement...

ALAN K. COOPER; F. J. DAVEY

1985-09-13T23:59:59.000Z

250

Hydrothermal manganese plumes in the Mid-Atlantic Ridge rift valley  

Science Journals Connector (OSTI)

... Fracture Zone at 1G? in August 1984. Manganese was measured on board ship by flameless atomic absorption after preconcentration with oxine9 to give a detection limit of 0.05 nmol ...

G. Klinkhammer; P. Rona; M. Greaves; H. Elderfield

1985-04-25T23:59:59.000Z

251

Capturing magma intrusion and faulting processes during continental rupture: Seismicity of the Dabbahu (Afar) rift  

Science Journals Connector (OSTI)

......SH-wave polarities using the grid search algorithm FOCMEC (Snoke...SH-waves were not tolerated in the grid search algorithm. We determined...Fig. 4). Impulsive and hybrid earthquakes cluster along the...Gundmundsson A. , 1995. Infrastructure and mechanics of volcanic systems......

C. J. Ebinger; D. Keir; A. Ayele; E. Calais; T. J. Wright; M. Belachew; J. O. S. Hammond; E. Campbell; W. R. Buck

2008-09-01T23:59:59.000Z

252

Earthquake-induced barium anomalies in the Lisan Formation, Dead Sea Rift valley, Israel  

E-Print Network [OSTI]

, of the BM crystallites therein. Mass balance calculations show that the mass of Ba2+ dissolved in the lake

Marco, Shmuel "Shmulik"

253

Late Jurassic rifting along the Australian North West Shelf: margin geometry and spreading ridge  

E-Print Network [OSTI]

of Geosciences, University of Sydney, NSW 2006, Australia. The Argo and Gascoyne Abyssal plains have revisited the marine magnetic anomaly record of the Argo and Gascoyne Abyssal Plains ­ M22A, in the Gascoyne Abyssal Plain, northwest of the Exmouth Plateau. The magnetic anomalies have

Müller, Dietmar

254

A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica  

Science Journals Connector (OSTI)

......GA-199 in the Great Australian Bight (GAB). Seamount...Block; BB, Bight Basin; BC, Budd Coast...anomalies in the Australian-Antarctic Basin: are they isochrons...framework for the Great Australian Bight: starting with......

D. I. Close; A. B. Watts; H. M. J. Stagg

2009-05-01T23:59:59.000Z

255

Why farm the city? Theorizing urban agriculture through a lens of metabolic rift  

E-Print Network [OSTI]

timbre, government agencies, non-governmental organizations and farmers' groups have touted the potential' is an effective framework for differentiating UA's multiple origins and functions across the Global North-graders from a nearby ele- mentary school plant a vegetable garden, the first of its kind at the White House

256

Master1RservoirsGologiquesDynamiquedesBassins-MichelSranne Post-rift tectonics on passive margins  

E-Print Network [OSTI]

postrift ? South Gabon 38 Master1RéservoirsGéologiquesDynamiquedesBassins-MichelSéranne Parameters : Niger delta evaporites décollement : Gabon margin 40 Master1Réservoirs view Evaporites = décollement shortening extension Salt tectonics = fonction (slope & load) Gabon

Demouchy, Sylvie

257

Outside influences and ruling Iran : the emergence of the rift with the West.  

E-Print Network [OSTI]

??Since the establishment of a united, Shia Persian empire in 1501 through to the overthrow of the last Shah in the Islamic Revolution, Iran and (more)

Campbell, Alana

2009-01-01T23:59:59.000Z

258

Dynamics of ice shelf rift propagation and iceberg calving inferred from geodetic and seismic observations  

E-Print Network [OSTI]

ice at the base of the ice shelf could produce a thicknessthat may produce larger amounts of marine ice near one riftice shelf com- bined with large Antarctic storm systems can produce

Bassis, Jeremy N.

2007-01-01T23:59:59.000Z

259

Remote sensing studies and morphotectonic investigations in an arid rift setting, Baja California, Mexico  

E-Print Network [OSTI]

with high resolution (15-m) for the entire eastern coast of Baja California. The main approach that we used to clearly represent all the lithological units in the investigated area was objectoriented classification based on fuzzy logic theory. The area...

El-Sobky, Hesham Farouk

2009-05-15T23:59:59.000Z

260

Hydrogeological aspects of fault zones on various scales in the Roer Valley Rift System  

E-Print Network [OSTI]

at the location of the fault zone. Finally, on a regional scale, hydraulic head patterns around the lignite mining to regional groundwater flow patterns. D 2003 Elsevier Science B.V. All rights reserved. Keywords: Faults B.V. All rights reserved. doi:10.1016/S0375-6742(03)00031-1 * Corresponding author. Fax: +31

Bense, Victor

Note: This page contains sample records for the topic "haleakala sw rift" 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

Dynamics of ice shelf rift propagation and iceberg calving inferred from geodetic and seismic observations  

E-Print Network [OSTI]

The theory of subcritical crack growth with applications tothe simple model of subcritical crack growth suggested by

Bassis, Jeremy N.

2007-01-01T23:59:59.000Z

262

Sedimentary record and tectonic implications of Mesozoic rifting in southeast Mongolia  

Science Journals Connector (OSTI)

...Mongolia, China, and tectonic...between north China and Siberia...Journal of Petroleum Geology...All-Union Export and Import Corporation...between north China and Siberia...Journal of Petroleum Geology...Ex-port and Import Corporation...

263

Petrologic study of a Miocene gabbro emplaced during initial rifting in the Red Sea  

E-Print Network [OSTI]

) on three samples for Ti, Al, Fe, Mg, Na, Mn, Cr, Sc, V, Co, Rb, Cs, 23 Ba, La, Ce, Nd, Sm, Eu, Tb, Yb, Lu, Hf, Th, and Ta. Miller (1973) did INAA on three samples for Ti, Al, Fe, Mg, Na, Ca, Mn, Cr, Sc, V, Co, Zr, Hf, Th, Ta, Ba, Cs, Ir, Ni, Au, La... at Oregon State University, Coles (1972), Miller (1973), and Palmer (1974 ) did M. S. theses in which they analyzed six of the Jabal at Tirf rocks studied in this thesis (Appendix I) . Coles (1972) did instrumental neutron activation analysis (INAA...

Johnston, Beatrice Bryant

1978-01-01T23:59:59.000Z

264

Microsoft PowerPoint - SW Fed Hydro Conference Jun 12 presentation Final [Compatibility Mode]  

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

Projects Projects Impacting Federal Projects Impacting Federal Power Tulsa District Tulsa District Beau Biffle Beau Biffle 13 June 2012 BUILDING STRONG ® Topics Topics  Interior Least Tern Operations and Habitat Creation  Tulsa Vision 2025  Dam Safety Issues ► Keystone ► Pine Creek ► Tenkiller  Lake Eufaula Advisory Committee  Lake Eufaula Advisory Committee  Tenkiller Downstream Fishery Issues  Broken Bow Seasonal Pool Update - Cultural Broken Bow Seasonal Pool Update Cultural Resources Impacts  Arkansas River Navigation Improvement BUILDING STRONG ®  Oklahoma Comprehensive Water Plan Update Interior Least Tern Operations and H bit t C ti Habitat Creation  2011 Breeding Season Survey Results: - Arkansas River System: 517 adults, 358 fledglings. Season totals exceeded

265

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

BOE Reserve Class BOE Reserve Class No 2001 reserves 0.1 - 10 MBOE 10.1 - 100 MBOE 100.1 - 1,000 MBOE 1,000.1 - 10,000 MBOE 10,000.1- 100,000 MBOE > 100,000 MBOE Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

266

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

Liquids Reserve Class Liquids Reserve Class No 2001 liquids reserves 0.1 - 10 Mbbl 10.1 - 100 Mbbl 100.1 - 1,000 Mbbl 1,000.1 - 10,000 Mbbl 10,000.1- 100,000 Mbbl Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

267

Reading Room 1E-190, Forrestal Building, 1000 Independence Ave., SW.,  

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

239 / Thursday, December 14, 1989 / Notices 239 / Thursday, December 14, 1989 / Notices Public Participation: The meeting is open to the public. The Chairperson of the Panel is empowered to conduct the meeting in a fashion that will, in the Chairperson's judgment, facilitate the orderly conduct of business. Any member of the public who wishes to make oral statements pertaining to agenda items should contact the Executive Director at the address or telephone number listed above. Requests must be received at least 5 days prior to the meeting and reasonable provision will be made to include the presentation on the agenda. It is requested that oral presenters provide 15 copies of their statements at the time of their presentations. Minutes: Available for public review and copying approximately 30 days following the meeting at the Public

268

Microsoft PowerPoint - SW Regional Hydropower Conference - June 2007.ppt  

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

of Engineers® of Engineers® Vision Statement Vision Statement Be the premier stewards of entrusted hydropower resources US Army Corps of Engineers® Mission Statement Mission Statement Provide reliable hydroelectric power services at the lowest possible cost, consistent with sound business principles, in partnership with other Federal hydropower generators, the Power Marketing Administrations, and Preference Customers, to benefit the Nation. US Army Corps of Engineers® Mission Statement Mission Statement Provide reliable hydroelectric power services at the lowest possible cost, consistent with sound business principles, in partnership with other Federal hydropower generators, the Power Marketing Administrations, and Preference Customers, to benefit the Nation. US Army Corps

269

Northwest Power and Conservation Council 851 S.W. Sixth Avenue, Suite 1100  

E-Print Network [OSTI]

in the region. Inland Power is a cooperative electric utility serving approximately 39,000 consumers in portions towards achieving the Power Plan goals but will also likely be used by various elected officials and other

270

Neogene salt in SW Iran and its interaction with Zagros folding  

Science Journals Connector (OSTI)

...formations) southwestward from rising thrust sheets into the adjacent subsiding Neogene foreland...interference of side effects and focus seismic energy. In processing, preliminary knowledge...169. SauraE., VergesJ., HomkeS., BlancE., Serra-KielJ., BernaolaG., CascielloE...

I. ABDOLLAHIE FARD; M. SEPEHR; S. SHERKATI

271

UCRL-JC-116524 PREPRINT The Beaverhead Impact Structure, SW Montana...  

Office of Scientific and Technical Information (OSTI)

of several hundred kilometers. Proximal ejecta deposits (e.g. Bunte breccia, Ries , Germany; (Pohl and others., 1977)) as well as distal ejecta (e.g. Acraman, Australia; (Gostin...

272

Independent Scientific Review Panel for the Northwest Power and Conservation Council; 851 SW 6th  

E-Print Network [OSTI]

and Conservation Council From: ISRP and ISAB Subject: Review of the Draft Columbia River Basin Research Plan as a planning and prioritizing tool. The ISAB/RP understood that to be a preliminary review and suggested a follow-up review of a revised plan. The November 2005 version of the plan is much improved from the draft

273

Seismic attribute analyses of lower Permian (Wolfcampian-Leonardian) carbonate buildups, SW Midland, Texas  

E-Print Network [OSTI]

set of attributes that directly indicate the buildup locations. After extensive trial of various attributes, the variance attribute was selected as the optimum seismic attribute. The resultant 3 D variance volume was used to detect the buildup locations...

Decalf, Carole Christiane

2012-06-07T23:59:59.000Z

274

Developments in High Efficiency Engine Technologies and an Introduction to SwRI's Dedicated EGR Concept  

Broader source: Energy.gov [DOE]

Provides overview of high efficiency engine technologies and introduces a dedicated exhaust gas recirculation concept where EGR production and gas stream is separate from the rest of the exhaust

275

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network [OSTI]

are still depressed. For 2012-2019, Council staff compared the PNUCC's NRF 2011 and Bonneville's Book recovery post 2015 In reviewing the NRF and draft White Book forecasts methodology and savings are not represented in these forecasts in By year 2020, NRF analysis includes about 1 book considers about 90 MWa

276

RTF 2012 Business Plan Page 1 851 S.W. Sixth Avenue, Suite 1100  

E-Print Network [OSTI]

measures and maintain standardized protocols for verification and evaluation of energy savings. The RTF has, or practices not specifically evaluated by the RTF can be estimated. Review measurement and verification-related measure evaluations. Upon request of program sponsors, review plans for measurement and verification

277

Citizens' Utility Board of Oregon 610 S.W. Broadway, Suite 308  

E-Print Network [OSTI]

for the Future Role of the Bonneville Power Administration in Power Supply Dear Mr. Walker, The Citizens' Utility-227-1984 Fax 503-274-2956 April 22, 2004 Mark Walker Director of Public Affairs Northwest Power & Conservation Board of Oregon thanks the members and staff of the Northwest Power and Conservation Council

278

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348  

E-Print Network [OSTI]

agencies, Bonneville Power Administration, state energy offices and/or state utility regulatory agencies or sex, as provided by Title VI of the Civil Rights Act of 1964, be excluded from participation in committee to the Northwest Power and Conservation Council (Council), is soliciting consultant Statements

279

Original2/06; revised 9/14 sw Preceptor Manual  

E-Print Network [OSTI]

to demonstrate the ability to design, provide, manage, and coordinate evidenced ­ based, culturally competent. Use technology and information systems effectively for the management of resources and patient the plan of care for clients and their families 6. Demonstrate best practices in the delegation of care. 7

Cui, Yan

280

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network [OSTI]

TO: Council Members FROM: Charlie Grist SUBJECT: Energy Efficiency Industry Briefing on Conservation minimum efficiency standards, offer programs and do research. In addition, a host of other entities do Phil Washington August 30, 2012 Energy Efficiency Industry Briefing on Conservation Implementation

Note: This page contains sample records for the topic "haleakala sw rift" 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

ltrfooterltrfooter851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161  

E-Print Network [OSTI]

is transportation and the other two key areas of potential improvement are building energy use and more diverse distributed and renewable energy supplies. The 2012 Washington State Energy Strategy is posted FROM: Terry Morlan SUBJECT: Presentation on the Washington State Energy Strategy In December

282

Northwest Power and Conservation Council 851 S.W. Sixth Avenue, Suite 1100  

E-Print Network [OSTI]

of natural gas and cost of CO2 emissions. Large supplies of hydro power in the region, low load growth level greenhouse gas regulatory policies will influence future electricity prices, CO2 emission levels and state policies, coupled with low natural gas prices, are affecting CO2 emissions and electricity prices

283

E-Print Network 3.0 - area sw china Sample Search Results  

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

(f). 35 of the South China Sea is changed to land... ) to the Turan plate and Caspian areas (the small ... Source: Chinese Academy of Sciences, Institute of Atmospheric...

284

The dumortierite supergroup. II. Three new minerals from the Szklary pegmatite, SW Poland: Nioboholtite,  

E-Print Network [OSTI]

2O3 5.92, 2.26, 16.02; Sb2O3 10.81, 11.48, 10.31; FeO 0.51, 0.13, 0.19; H2O (calc.) 0.05, ?, ?, Sum

Ma, Chi

285

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network [OSTI]

TO: Power Committee FROM: Massoud Jourabchi SUBJECT: Data Center Loads in the Northwest Staff will present an update to the analysis of electric load from the data centers in the region. This presentation is an update to the work that showed there is about 600 MWa of connected load in all forms of data centers

286

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network [OSTI]

the interplay between the natural gas and electricity demand as more gas-fired generation enters the picture The Sixth Power Plan called for improving natural gas forecasting to better include the interplay fired TO: Power Committee FROM: Massoud Jourabchi SUBJECT: Enhancing Natural Gas Demand Forecasting

287

Transit and Parking Services Oregon State University, 606 SW 15th  

E-Print Network [OSTI]

___________________________________ Color ___________________________________ Registered Owner Information Registered Owner Information. Permits are hangtag style, excluding motorcycle & utility carts, and must be displayed on the rearview Chapter 576 Division 30). http://parking.oregonstate.edu/ and http://arcweb.sos.state.or.us/ 4. I have

Escher, Christine

288

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348 Executive Director  

E-Print Network [OSTI]

database, Pacific Northwest Utilities Conference resource database. Database updates are an ongoing process. ________________________________________ q:\\kd\\presentations\\council meetings\\council mtg 6-12\\generation database update cm.docx 851 S Regional Forecast resource database. Database updates are an ongoing process, but this presentation

289

Bole epiphytic bryophytes on Lithocarpus xylocarpus (Kurz) Markgr. in the Ailao Mountains, SW China  

Science Journals Connector (OSTI)

This secondary Lithocarpus forest (SLF) experienced clear cutting by local people about...1992). It is dominated by L. hancei, L. xylocarpus and Vaccinium duclouxii (Levl.) Hand.-Mazz., and shares many dominate t...

Liang Song; Wen-yao Liu; Wen-zhang Ma; Zheng-hong Tan

2011-03-01T23:59:59.000Z

290

biodiversity surveys of the nyungwe forest reserveIn S.W. Rwanda  

E-Print Network [OSTI]

studies and census of Mountain Gorillas by George Schaller in Congo (1959), creation of Nouabale-Ndoki National Park in Congo Republic (1993), research and conservation throughout civil strife in Rwanda and Democratic Republic of Congo (1980-2000), reallocation of proposed forest concessions to protected areas

Fashing, Peter J.

291

851 S.W. Sixth Avenue, Suite 1100 Portland, Oregon 97204-1348  

E-Print Network [OSTI]

in the analysis) and about 250 megawatts of new small hydro and hydro upgrades should be realized. Steve Crow 503 in the analysis) of new small hydro and hydro upgrades should be realized. 503-222-5161 800-452-5161 503) of new small hydro and hydro upgrades should be realized. #12;2 · Wind generation serving Northwest loads

292

Northwest Power and Conservation Council 851 S.W. Sixth Avenue, Suite 1100  

E-Print Network [OSTI]

nwcouncil.org Revised Fuel Price Forecasts for the Seventh Power Plan July 2014 Fuel Price Forecast #12 significant changes that would affect its power plan. This revised forecast for fuel prices will be used. The projected price range for this fuel is broader, reflecting greater uncertainty about its future supply

293

Longevity of the Permian Emeishan mantle plume (SW China): 1 Ma, 8 Ma or 18 Ma?  

Science Journals Connector (OSTI)

...GREGORY SHELLNUTT MEI-FU ZHOU DAN-PING YAN YANBIN WANG Author for correspondence...Bowring, S. A., Erwin, D. H., Jin, Y. G., Martin, M. W., Davidek...Hongge Fe-V-Ti deposit in the Pan-Xi area, southwestern China. Mineralium Deposita...

J. GREGORY SHELLNUTT; MEI-FU ZHOU; DAN-PING YAN; YANBIN WANG

294

UNIT N~E C-S31 Sw1tchvard REGULA-TORY STATUS CERCLA  

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

STATUS Av I DATES OPERATED 1951 to oresent SITEPROCESS DESCRIPTION: Power transformer and switchyard. solvents were used to clean transformer external surfaces. WASTE...

295

SwRI's HEDGE Technology for High Efficiency, Low Emissions Gasoline Engines  

Broader source: Energy.gov [DOE]

Presentation given at the 16th Directions in Engine-Efficiency and Emissions Research (DEER) Conference in Detroit, MI, September 27-30, 2010.

296

Preliminary Analysis of ARM SGP Area Sky Cover and Downwelling SW Irradiance  

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

Clarifying and Implementing a Stricter DOD Definition Across Datastreams Clarifying and Implementing a Stricter DOD Definition Across Datastreams C. Sivaraman, B. Ermold, M. Macduff Pacific Northwest National Laboratory Definition of DOD: All dimension, attribute and variable types and names are considered part of a DOD. A change in any part of the DOD is considered a version change. Outcomes: ACRF enforces greater consistency in data Downstream users benefit (DQ, VAPs, scientists) Identify inconsistencies across datastreams Datastream development is more efficient BODS interface, updated libraries Improved data analysis tools for ACRF and ARM Visual Datastream history tool (below) Issues with current DOD history: The DOD History page: http://science.arm.gov/tool/dod/showdod.php * Tracks both content and structure. * Needs Custom Configuration

297

SILO LILLI SID NEY SW BIG SPRINGS SLOSS LITT LE H OOT SILO JUR  

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

Gas Reserve Class Gas Reserve Class No 2001 gas reserves 0.1 - 10 MMCF 10.1 - 100 MMCF 100.1 - 1,000 MMCF 1,000.1 - 10,000 MMCF 10,000.1- 100,000 MMCF > 100,000 MMCF Basin Outline The mapped oil and gas field boundary outlines were created by the Reserves and Production Division, Office of Oil and Gas, Energy Information Administration pursuant to studies required by Section 604 of the Energy Policy and Conservation Act Amendments of 2000 (P.L. 106-469). The boundaries are not informed by subsurface structural information. The data and methods used in their creation are detailed in a report, "Scientific Inventory of Onshore Federal Lands' Oil and Gas Resources and Reserves and the Extent and Nature of Restrictions to Their Development", prepared by the US Departments of Interior, Agriculture and Energy.

298

E-Print Network 3.0 - area sw finland Sample Search Results  

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

BelgiumCzech Rep. Denm ark Finland France Germ any GreatBritain* Hungary ItalyNetherlands Norway Source: Columbia University - Waste-to-Energy Research and Technology Council...

299

New data reflect on the thermal antiquity of the Socorro magma body locale, Rio Grande Rift, New Mexico  

Science Journals Connector (OSTI)

...uplift of the Socorro magma body, in Lueth V.W., Lucas S.G., Chamberlin R.M., eds., Geology of the Chupadera Mesa Region: Socorro, New Mexico Geological Society, 60th Annual Field Conference Guidebook, p. 415a 424. a Touloukain...

Marshall Reiter; Richard M. Chamberlin; David W. Love

300

Nuclear Relocalization of Polyadenylate Binding Protein during Rift Valley Fever Virus Infection Involves Expression of the NSs Gene  

Science Journals Connector (OSTI)

...Academy of Sciences National Research Council Associateship. The opinions, interpretations, conclusions, and recommendations are ours...protein in the zoonotic capacity of orthobunyaviruses. Zoonoses Public Health 56 :285-296. 49. Szemiel, AM , A-B Failloux...

Anna Maria Copeland; Louis A. Altamura; Nicole M. Van Deusen; Connie S. Schmaljohn

2013-08-21T23:59:59.000Z

Note: This page contains sample records for the topic "haleakala sw rift" 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

Structural Control of Hydrology, Hydrogeology and Hydrochemistry along the Eastern Escarpment of the Jordan Rift Valley, JORDAN.  

E-Print Network [OSTI]

??The relationship of structural geology and hydrogeological characteristics NW Jordan. Superior 3 phase tectonic model was derived from re-evaluation of structural elements which are strongly (more)

Sahawneh, Julia

2011-01-01T23:59:59.000Z

302

Evolution post-rift de la marge du Golfe du Lion en Languedoc : Une marge pas si passive que a !  

E-Print Network [OSTI]

collaboration de Hubert Camus (Cenote) et Jean-Yves Reynaud (MNHN) Une excursion organisée pour l'UPA, du 29Miocène. Commentcitercedocument?:Séranne,M.,Camus,H.,Reynaud,J.Y.2011,Evolution postriftdelamargedu

Demouchy, Sylvie

303

Magmatism at the west Iberia non-volcanic rifted continental margin: evidence from analyses of magnetic anomalies  

Science Journals Connector (OSTI)

......recorded on land in the Lusitanian Basin (Ribeiro et al. 1979; Martins...tectonics in the Jeanne d'Arc Basin, offshore Newfoundland: implications...Australia: Great Australian Bight and western sections, Geol...in the Australian-Antarctic Basin: are they isochrons?, J......

S. M. Russell; R. B. Whitmarsh

2003-09-01T23:59:59.000Z

304

From continental extension to seafloor spreading: crustal structure of the Goban Spur rifted margin, southwest of the UK  

Science Journals Connector (OSTI)

......and the central Great Australian Bight (Sayers 2001...to examine in greater detail some inconsistencies...the Porcupine Basin and to the south...the Porcupine Basin, southwest of...of the central Great Australian Bight, in Non-volcanic......

Andrew D. Bullock; Timothy A. Minshull

2005-11-01T23:59:59.000Z

305

Magmatism at the west Iberia non-volcanic rifted continental margin: evidence from analyses of magnetic anomalies  

Science Journals Connector (OSTI)

......the production of greater volumes of melt leads...the Jeanne d'Arc Basin, offshore Newfoundland...margin of Australia: Great Australian Bight and western sections...magnetic anomalies in the Australian-Antarctic Basin: are they isochrons......

S. M. Russell; R. B. Whitmarsh

2003-09-01T23:59:59.000Z

306

Structural style and evolution of a Late Triassic rift basin in the Central High Atlas, Morocco: controls on sediment deposition  

E-Print Network [OSTI]

: controls on sediment deposition CATHERINE BAUDON*, IVAN FABUEL-PEREZ and JONATHAN REDFERN* North Africa, Oxford Road, Williamson Building, Manchester M13 9PL, UK Late Triassic continental sediments deposited dimension, geometry of the half-graben and created the accommodation for sediment deposition. The presence

Demouchy, Sylvie

307

Radioactivity concentrations in soil and vegetables from the northern Jordan Rift Valley and the corresponding dose estimates  

Science Journals Connector (OSTI)

......concept as applied to natural uranium. Health Phys (1985) 48:494-500...soil-to-plant transfer factors for uranium and thorium isotopes and 226Ra...Zunic Z. S. Determination of depleted uranium in environmental samples by gamma-spectroscopic......

Anas M. Ababneh; Maisoun S. Masa'deh; Zaid Q. Ababneh; Mufeed A. Awawdeh; Abdalmajeid M. Alyassin

2009-02-01T23:59:59.000Z

308

On the evolution of rifted continental margins: comparison of models and observations for the Nova Scotian margin  

Science Journals Connector (OSTI)

......Cenozoic geology of the Yerington district, Nevada, and implications...Rhodehamel, E. C., 1976. Geothermal gradients help predict petroleum...at t + = 00 due to initial heating is given by 712 where the relationship...produced in about 60 Ma by heating of the region landward of the......

Christopher Beaumont; Charlotte E. Keen; Ross Boutilier

1982-09-01T23:59:59.000Z

309

Spatial and temporal population genetics at deep-sea hydrothermal vents along the East Pacific Rise and Galpagos Rift  

E-Print Network [OSTI]

Ecological processes at deep-sea hydrothermal vents on fast-spreading mid-ocean ridges are punctuated by frequent physical disturbance. Larval dispersal among disjunct vent sites facilitates the persistence of sessile ...

Fusaro, Abigail Jean

2008-01-01T23:59:59.000Z

310

Ernest Orlando Lawrence Berkeley National Laboratory  

E-Print Network [OSTI]

Rainwater ................................................................................... RW-1 Creeks ......................................................................................... CR-1 Stormwater .................................................................................SW-1

311

Ernest Orlando Lawrence Berkeley National Laboratory  

E-Print Network [OSTI]

Rainwater ...................................................................................RW-1 Creeks .........................................................................................CR-1 Stormwater ................................................................................. SW

312

LBL-27170 (2010) Site Environmental Report for 2009  

E-Print Network [OSTI]

Rainwater ................................................................................... RW-1 Creeks ......................................................................................... CR-1 Stormwater .................................................................................SW-1

313

LBL-27170 (2011) Site Environmental Report for 2010  

E-Print Network [OSTI]

Rainwater ................................................................................... RW-1 Creeks ......................................................................................... CR-1 Stormwater .................................................................................SW-1

314

Ernest Orlando Lawrence Berkeley National Laboratory  

E-Print Network [OSTI]

Ambient Air ............................................................................ AA-1 Rainwater-1 Stormwater ..............................................................................SW-1 #12

315

Observed Southern Ocean Cloud Properties and Shortwave Reflection. Part I: Calculation of SW Flux from Observed Cloud Properties  

Science Journals Connector (OSTI)

The sensitivity of the reflection of shortwave radiation over the Southern Ocean to the cloud properties there is estimated using observations from a suite of passive and active satellite instruments in combination with radiative transfer ...

Daniel T. McCoy; Dennis L. Hartmann; Daniel P. Grosvenor

316

HW-SW design flow of a nano-satellite using UML and CodeSimulink co-design environment  

E-Print Network [OSTI]

parts of each can be modeled in this way, converted into a CodeSimulink model to simulate to be a RAD (Rapid Application Development) in a great variety of systems, especially low-cost ones. I. INTRODUCTION In recent years many automated design flows have been created to develop embedded systems

317

Effects of Greater flamingo Phoenicopterus ruber on macrophytes, chironimds and turbidity in natural marshes in Doana, SW Spain.  

E-Print Network [OSTI]

resuspension. #12;3 Introduction Submerged vegetation has a major functional role in shallow wetlands, because it provides refuge for invertebrates, changes the nutrient dynamics of the system, prevents resuspension sediment resuspension (SCHEFFER et al. 1993, SCHEFFER 1998). However, the potential effects of benthivorous

Green, Andy J.

318

Molecular Dynamics of Formation Process of Fullerene "`@@SZRvi"OE`Hj <@Sw@@ZROEN--i"OE`H@j  

E-Print Network [OSTI]

,µ·Ct·[OE"·\\`¢,ðOE`·¬,·,é?"\\·«,?,?,¢,? OEY"¢,µ,½·DFig. 1 ,?·"x,ð3000K ,?·§OEä,µ,½OEn,?,?OEvZZOE

Maruyama, Shigeo

319

Culture and Psychological Responses to Environmental Shocks: Cultural Ecology of Sidama Impulsivity and Niche Construction in SW Ethiopia  

E-Print Network [OSTI]

: Ecological validity; personality; phenotypic plasticity; social ecological systems; cultural cognition on insights from social ecological systems, niche construction, cognitive science, psychometrics, and cultural1 Culture and Psychological Responses to Environmental Shocks: Cultural Ecology of Sidama

Quinlan, Robert

320

Integrated stratigraphy of the Early Miocene lacustrine deposits of Pag Island (SW Croatia): Palaeovegetation and environmental changes in the  

E-Print Network [OSTI]

lignite deposition and shallow lake facies. This suggests that both records are dominantly controlled Optimum. © 2009 Elsevier B.V. All rights reserved. 1. Introduction The Dinarids, and other areas

Utrecht, Universiteit

Note: This page contains sample records for the topic "haleakala sw rift" 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

Integrating Seeing Measurements into the Operations of Solar Telescopes  

E-Print Network [OSTI]

conditions for solar observations: Big Bear Solar Observatory in California, Haleakala on Maui, HawaiiIntegrating Seeing Measurements into the Operations of Solar Telescopes C. Denker and A. P. Verdoni New Jersey Institute of Technology, Center for Solar-Terrestrial Research 323 Martin Luther King Blvd

322

Cultivation, Capital, and Contamination: Urban Agriculture in Oakland, California  

E-Print Network [OSTI]

rift. Two historically interrelated processes, collectivelyprocess. I begin the chapter by differentiating among three interrelated

McClintock, Nathan

2011-01-01T23:59:59.000Z

323

US Continental Interior Precambrian-Paleozoic  

E-Print Network [OSTI]

= Reelfoot Rift, LD = La Salle deformation belt, WB = Williston Basin, IB = Illinois Basin, MB = Michigan

324

Thermochronometric analysis of the North Lunggar Rift: Implications for the timing of extension initiation and structural style of deformation in southern Tibet  

E-Print Network [OSTI]

.09 Transect 2 LNG0409 5336 31.42470 83.51310 4.0 0.24 4.6 0.37 LNG0209 4942 31.43337 83.55980 2.9 0.17 3.5 0.28 LNG0109 4880 31.43743 83.56670 2.7 0.23 3.4 0.58 Detrital MT06170601 31.68391 83.59858 MT06170602 31.69093 83.58551 42 Table 1. Summary of apatite...-Th)/He Replicate Analysis Sample Age (Ma) error (Ma) U (ppm) Th (ppm) 147Sm (ppm) Th/U He (nmol/g) mass (?g) Ft ESR (?m) StdDev LNG0109-1 2.7 0.2 24.0 8.0 27.1 0.3 0.2 1.4 0.6 38.2 LNG0109-2 3.0 0.2 19.0 12.4 84.0 0.7 0.3 4.7 0.7 58.3 LNG0109-3 2.6 0.2 17.8 7.7 10...

Sundell, Kurt Eric

2011-01-01T23:59:59.000Z

325

Evidence for constriction and Pliocene acceleration of east-west extension in the North Lunggar rift region of west central Tibet  

E-Print Network [OSTI]

Pliocene rates as high as >400C?Ma?1 and 410?mm?a?1. Footwall isotherms were significantly compressed during rapid exhumation resulting in an elevated transient geothermal gradient between 50 and 90C?km?1. The minimum magnitude of horizontal extension...

Sundell, Kurt E.; Taylor, Michael H.; Styron, Richard H.; Stockli, Daniel F.; Kapp, Paul; Hager, Christian; Liu, Deliang; Ding, Lin

2013-10-10T23:59:59.000Z

326

Subsurface temperatures and crustal strength changes within the seismogenic layer at Arroyo del Coyote in the Socorro seismic area, central Rio Grande Rift, New Mexico  

Science Journals Connector (OSTI)

...are outlined and stippled (Condie and Budding, 1979). A reliable heat-flow measurement has been made at the Chupadera Mesa site (Reiter et al., 1975). The heavy lines indicate Quaternary faults, after Machette et al. (1998) Figure...

Marshall Reiter

327

Complete genome sequence of the halophilic bacterium Spirochaeta africana type strain (Z-7692T) from the alkaline Lake Magadi in the East African Rift  

SciTech Connect (OSTI)

Spirochaeta africana Zhilina et al. 1996 is an anaerobic, aerotolerant, spiral-shaped bacte- rium that is motile via periplasmic flagella. The type strain of the species, Z-7692T, was iso- lated in 1993 or earlier from a bacterial bloom in the brine under the trona layer in a shallow lagoon of the alkaline equatorial Lake Magadi in Kenya. Here we describe the features of this organism, together with the complete genome sequence, and annotation. Considering the pending reclassification of S. caldaria to the genus Treponema, S. africana is only the second 'true' member of the genus Spirochaeta with a genome-sequenced type strain to be pub- lished. The 3,285,855 bp long genome of strain Z-7692T with its 2,817 protein-coding and 57 RNA genes is a part of the Genomic Encyclopedia of Bacteria and Archaea project.

Liolios, Konstantinos [U.S. Department of Energy, Joint Genome Institute; Abt, Birte [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Scheuner, Carmen [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Teshima, Hazuki [Los Alamos National Laboratory (LANL); Held, Brittany [Los Alamos National Laboratory (LANL); Lapidus, Alla L. [U.S. Department of Energy, Joint Genome Institute; Nolan, Matt [U.S. Department of Energy, Joint Genome Institute; Lucas, Susan [U.S. Department of Energy, Joint Genome Institute; Deshpande, Shweta [U.S. Department of Energy, Joint Genome Institute; Cheng, Jan-Fang [U.S. Department of Energy, Joint Genome Institute; Tapia, Roxanne [Los Alamos National Laboratory (LANL); Goodwin, Lynne A. [Los Alamos National Laboratory (LANL); Pitluck, Sam [U.S. Department of Energy, Joint Genome Institute; Pagani, Ioanna [U.S. Department of Energy, Joint Genome Institute; Ivanova, N [U.S. Department of Energy, Joint Genome Institute; Mavromatis, K [U.S. Department of Energy, Joint Genome Institute; Mikhailova, Natalia [U.S. Department of Energy, Joint Genome Institute; Huntemann, Marcel [U.S. Department of Energy, Joint Genome Institute; Pati, Amrita [U.S. Department of Energy, Joint Genome Institute; Chen, Amy [U.S. Department of Energy, Joint Genome Institute; Palaniappan, Krishna [U.S. Department of Energy, Joint Genome Institute; Land, Miriam L [ORNL; Rohde, Manfred [HZI - Helmholtz Centre for Infection Research, Braunschweig, Germany; Tindall, Brian [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Detter, J. Chris [U.S. Department of Energy, Joint Genome Institute; Goker, Markus [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Bristow, James [U.S. Department of Energy, Joint Genome Institute; Eisen, Jonathan [U.S. Department of Energy, Joint Genome Institute; Markowitz, Victor [U.S. Department of Energy, Joint Genome Institute; Hugenholtz, Philip [U.S. Department of Energy, Joint Genome Institute; Woyke, Tanja [U.S. Department of Energy, Joint Genome Institute; Klenk, Hans-Peter [DSMZ - German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Kyrpides, Nikos C [U.S. Department of Energy, Joint Genome Institute

2013-01-01T23:59:59.000Z

328

The balance between deposition and subsidence (tectonics) in a rift basin playa and its effect on the climatic record of an area: Evidence from Bristol Dry Lake, California  

SciTech Connect (OSTI)

Two continuous core intervals drilled in Bristol Dry Lake, a large (150 km{sup 2}) playa in the central Mojave Desert of California, penetrated over 500 m of sediment and did not reach basement. The repetitious nature of the alternating shallow brine pond halite and siliciclastic and the consistency of the carbonate isotopic data from the surface and core indicate a relatively stable brine composition for most of the history of Bristol Dry Lake. All sedimentary structures and primary halite fabrics in the core indicate shallow-water, brine-pond halite alternated with halite-saturated siliciclastic muds in the basin center. A delicate balance of subsidence and mechanical and chemical deposition of evaporite and siliciclastic minerals was necessary to maintain the largely ephemeral lake environment of deposition through over 550 m of basin fill. The alternating brine pond/saline lake setting in Bristol Dry Lake is not directly related to climatic influences, and the sediments do not record major climatic events demonstrated in other closed-basin lakes. The reason for this insensitivity to climatic events is explained by the interior location of the basin, the low relief of the mountains surrounding the catchment, the large surface area of the catchment, and the low average sedimentation rates. All of the above criteria are at least partially controlled by the tectonics of the area, which, in turn, affect the sedimentation rate and supply water to the basin. Therefore, it is important to consider the influence of the above factors in determining global versus local, or regional, climate curves for a particular basin.

Rosen, M.R. (CSIRO, Floreat Park (Australia))

1991-03-01T23:59:59.000Z

329

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

330

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

331

Miocene initiation and acceleration of extension in the South Lunggar rift, western Tibet: Evolution of an active detachment system from structural mapping and (U-Th)/He thermochronology  

E-Print Network [OSTI]

assump- tions about the thermal state of the crust, particularly that the geothermal gradient is constant with depth and does not change during faulting, and radiogenic heating is not signifi- cant. These assumptions have been shown to be inaccurate... geotherms; these complications have to be well constrained [e.g., Stockli et al., 2002], or ignored. Furthermore, simple regression lines are rarely weighted by age uncertainty, thereby failing to take this important age information into account. [9...

Styron, Richard H.; Taylor, Michael H.; Sundell, Kurt E.; Stockli, Daniel F.; Oalmann, Jeffrey A. G.; Mö ller, Andreas; McCallister, Andrew T.; Liu, Deliang

2013-07-20T23:59:59.000Z

332

Development and Evaluation of a Real-Time Reverse Transcription-Loop-Mediated Isothermal Amplification Assay for Rapid Detection of Rift Valley Fever Virus in Clinical Specimens  

Science Journals Connector (OSTI)

...those from West Africa, Egypt, and central, eastern...sera collected on a daily basis postinfection...increased international demand for validated molecular...ZH501EGY77 b 1977 Human Egypt E 105.8 ZH548EGY77 1977 Human Egypt E 106.3 VRL1187ZIM78...

C. A. Le Roux; T. Kubo; A. A. Grobbelaar; P. Jansen van Vuren; J. Weyer; L. H. Nel; R. Swanepoel; K. Morita; J. T. Paweska

2008-12-24T23:59:59.000Z

333

Lake-level rise in the late Pleistocene and active subaquatic volcanism since the Holocene in Lake Kivu, East African Rift  

E-Print Network [OSTI]

in the stratified depths of the lake. Lake Kivu's large size and population density extend the risk of a limnic Department of Earth Sciences, Royal Museum for Central Africa, Belgium f Renard Centre of Marine Geology for being one of the three `exploding lakes' in Africa (Kling et al., 1987; Halbwachs et al., 2004). Lakes

Gilli, Adrian

334

26.457 The Circle Map : 2 The two approaches of the handouts on the circle map illustrate a deep cultural rift between the approaches of the  

E-Print Network [OSTI]

, but elaborating the description of the Devil's staircase Cantor function result. Consider any differentiable) The devil's staircase for the standard circle map. We now finally come "full circle and re

King, Chris

335

Orientation of tectonic stresses in central Kentucky during U. Devonian/L. Mississippian times: Evidence from quartz veins (after gypsum) in NE-trending, systematic joints in shales  

SciTech Connect (OSTI)

Quartz replacing fibrous gypsum and anhydrite pseudomorphically (QAS; quartz after sulfate''), and preserving characteristic crack-seal'' and chickenwire'' textures, occurs in extensional veins at four locations in central KY. The veins occupy a systematic set of NE-SW-trending, vertical joints within the essentially flat-lying shales of the Renfro Member of the Mississippian Borden Formation and the Late Devonian New Albany Shale. The four QAS occurrences discovered to date are located northeast of the Borden Front. At one site in the New Albany Shale, QAS veins show clear evidence of penecontemporaneous deformation. It is proposed that at all QAS locations, gypsum precipitated in incipient joints before complete lithification of the sediment, and grew perpendicular to the fractures to form extensional veins in the soft but firm muds. The orientations of the joints now marked by QAS veins are broadly consistent with regional patterns of NE-SW-trending systematic joints and lineaments in southern IN and in central and eastern KY. These systematic fracture patterns do not correspond directly to known basement faults or rift systems, although they are consistent with modern stress directions in eastern and western KY, measured in situ in wells and by earthquake fault-plane solutions. It is proposed that this systematic trend marks the regional tectonic stress pattern characteristic of southern IN and central and eastern KY at, and since the Late Devonian. The evidence of penecontemporaneous sedimentary deformation in joints of U. Devonian age, marked and preserved by quartz replacement of early gypsum, is sufficient to show that while the systematic NE-trending joint set in KY may also be modern it is not uniquely so.

Grover, J.; Dupuis-Nouille, E.M. (Univ. of Cincinnati, Cincinnati, OH (United States). Dept. of Geology)

1992-01-01T23:59:59.000Z

336

Involvement of Peroxiredoxin I in Protecting Cells from Radiation-Induced Death  

Science Journals Connector (OSTI)

......measured at 532 nm. The total antioxidant capability (T-AOC) of SW480Con and SW480SiPrxI cells was assayed with a...SW480SiPrxI cells by radiation was due to its decreased T-AOC. T-AOC of SW480Con and SW480SiPrxI cells was deter- mined. As......

Bo Zhang; Yongping Su; Guoping Ai; Yan Wang; Tao Wang; Fengchao Wang

2005-09-01T23:59:59.000Z

337

Branch xylem density variations across the Amazon Basin  

E-Print Network [OSTI]

C. Penuela and E. Alvarez SW-Venezuela SCR-01 Terra firme R.Herrera SW-Venezuela SW-Venezuela SCR-04 SCR-05 Tall caatinga Terra firme R. Herrera R. Herrera

2009-01-01T23:59:59.000Z

338

Role of magmatism in continental lithosphere extension: an introduction to tectnophysics special issue  

SciTech Connect (OSTI)

The dynamics and evolution of rifts and continental rifted margins have been the subject of intense study and debate for many years and still remain the focus of active investigation. The 2006 AGU Fall Meeting session 'Extensional Processes Leading to the Formation of Basins and Rifted Margins, From Volcanic to Magma-Limited' included several contributions that illustrated recent advances in our understanding of rifting processes, from the early stages of extension to breakup and incipient seafloor spreading. Following this session, we aimed to assemble a multi-disciplinary collection of papers focussing on the architecture, formation and evolution of continental rift zones and rifted margins. This Tectonophysics Special Issue 'Role of magmatism in continental lithosphere extension' comprises 14 papers that present some of the recent insights on rift and rifted margins dynamics, emphasising the role of magmatism in extensional processes. The purpose of this contribution is to introduce these papers.

Van Wijk, Jolante W [Los Alamos National Laboratory

2008-01-01T23:59:59.000Z

339

Three-dimensional Kirchhoff-approximate generalized Radon transform imaging using teleseismic P-to-S scattered waves  

Science Journals Connector (OSTI)

......dense profiles, for example the Colorado Plateau/Rio Grande Rift Seismic...Starting 12 Ma, extensive eruption of flood basalt near the Owhyee Plateau resulted...Great Plains, Rio Grande Rift, and Colorado Plateau using receiver functions......

Kaijian Liu; Alan Levander

2013-01-01T23:59:59.000Z

340

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

standards. The agreement recommends new federal minimum efficiency standards for residential refrigerator) that these standards take effect on the following schedule: Refrigerator/Freezers Jan. 1, 2014 Clothes Washers Jan. 1 Efficiency Levels 0 100 200 300 400 500 600 Clothes Dryer Clothes Washers Dishwashers Freezers Refrigerator

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

generation to end--useuse ("generator("generator refrigerator")refrigerator") ·· FeaturesFeatures ­­ Sensors

342

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

capacity needs Transmission Use of natural gas for electric generation Reliance on power imports from messages, technical details Policy: identify and discuss policies that drive the plan Topics for Analysis, peak loads Conservation cost-effectiveness from regional and utility perspectives Factors affecting

343

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

planning is, in part, based on historical end-use estimates of hourly customer loads. Most of the end and is still widely used today. However, the ELCAP data is now nearly three decades old. Current load profiles years that may have altered the end-use performance landscape. In addition, the load profiles of new

344

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

pressure on pricesp p p Continued high production rates, Further technological advancement in exploration information in late June and are in the process of incorporating the new information into the forecast. When

345

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, harvestable, and sustainable. These regional salmon boards #12;provide a forum for everyone who has an interest in healthy salmon and sustainable watersheds to voice their views about how to achieve success. These collaborative processes, bringing together technical experts, stakeholders, policy makers, and local politicians

346

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

to improvements in system efficiency, water management, and weather conditions, total estimated regional through improvements in the irrigation system hardware efficiency improvements. Since the 5th Plan, almost through improvements in pump efficiency, leak reduction, conversion to lower pressure applications

347

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

-stream water enhancement and the production and use of electricity. SIGNIFICANCE: Irrigation efficiency in Irrigation Efficiency for Fish and Power BACKGROUND Irrigation is by far the largest consumptive use of water and improve water quality for fish. While some believe that irrigation efficiency improvements reduce power

348

Chemopreventive activity of compounds extracted from Casearia sylvestris (Salicaceae) Sw against DNA damage induced by particulate matter emitted by sugarcane burning near Araraquara, Brazil  

SciTech Connect (OSTI)

Ethanolic extract of Casearia sylvestris is thought to be antimutagenic. In this study, we attempted to determine whether this extract and casearin X (a clerodane diterpene from C. sylvestris) are protective against the harmful effects of airborne pollutants from sugarcane burning. To that end, we used the Tradescantia micronucleus test in meiotic pollen cells of Tradescantia pallida, the micronucleus test in mouse bone marrow cells, and the comet assay in mouse blood cells. The mutagenic compound was total suspended particulate (TSP) from air. For the Tradescantia micronucleus test, T. pallida cuttings were treated with the extract at 0.13, 0.25, or 0.50 mg/ml. Subsequently, TSP was added at 0.3 mg/ml, and tetrads from the inflorescences were examined for micronuclei. For the micronucleus test in mouse bone marrow cells and the comet assay in mouse blood cells, Balb/c mice were treated for 15 days with the extract3.9, 7.5, or 15.0 mg/kg body weight (BW)or with casearin X0.3, 0.25, or 1.2 mg/kg BWafter which they received TSP (3.75 mg/kg BW). In T. pallida and mouse bone marrow cells, the extract was antimutagenic at all concentrations tested. In mouse blood cells, the extract was antigenotoxic at all concentrations, whereas casearin X was not antimutagenic but was antigenotoxic at all concentrations. We conclude that C. sylvestris ethanolic extract and casearin X protect DNA from damage induced by airborne pollutants from sugarcane burning. -- Highlights: ? We assessed DNA protection of C. sylvestris ethanolic extract. ? We assessed DNA protection of casearin X. ? We used Tradescantia pallida micronucleus test as screening. ? We used comet assay and micronucleus test in mice. ? The compounds protected DNA against sugar cane burning pollutants.

Prieto, A.M. [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Clinical Analysis, Rua Expedicionrios do Brasil, 1621, Araraquara (Brazil)] [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Clinical Analysis, Rua Expedicionrios do Brasil, 1621, Araraquara (Brazil); Santos, A.G. [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Natural Principles and Toxicology, Rodovia Araraquara-Jau, km 01, Araraquara (Brazil)] [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Natural Principles and Toxicology, Rodovia Araraquara-Jau, km 01, Araraquara (Brazil); Csipak, A.R.; Caliri, C.M.; Silva, I.C. [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Clinical Analysis, Rua Expedicionrios do Brasil, 1621, Araraquara (Brazil)] [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Clinical Analysis, Rua Expedicionrios do Brasil, 1621, Araraquara (Brazil); Arbex, M.A. [UNIFESP Federal University of So Paulo, Paulista College of Medicine, Department of Internal Medicine, Rua Pedro de Toledo, 720, So Paulo (Brazil)] [UNIFESP Federal University of So Paulo, Paulista College of Medicine, Department of Internal Medicine, Rua Pedro de Toledo, 720, So Paulo (Brazil); Silva, F.S.; Marchi, M.R.R. [UNESP Univ. Estadual Paulista, Chemistry Institute, Department of Analytical Chemistry, Rua Francisco Degni, S/N, Araraquara (Brazil)] [UNESP Univ. Estadual Paulista, Chemistry Institute, Department of Analytical Chemistry, Rua Francisco Degni, S/N, Araraquara (Brazil); Cavalheiro, A.J.; Silva, D.H.S.; Bolzani, V.S. [UNESP Univ. Estadual Paulista, Chemistry Institute, Department of Organic Chemistry, Rua Francisco Degni, S/N, Araraquara (Brazil)] [UNESP Univ. Estadual Paulista, Chemistry Institute, Department of Organic Chemistry, Rua Francisco Degni, S/N, Araraquara (Brazil); Soares, C.P., E-mail: soarescp@hotmail.com [UNESP Univ. Estadual Paulista, College of Pharmaceutical Sciences, Department of Clinical Analysis, Rua Expedicionrios do Brasil, 1621, Araraquara (Brazil)

2012-12-15T23:59:59.000Z

349

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, by utilities, Bonneville, the Energy Trust of Oregon, the Northwest Energy Efficiency Alliance, and others to efficiency verification and tracking. We have not included renewables, low-income issues, or program best practices for example. Is that the correct scope of responsibility? 5) Funding · How can the RTF PAC best

350

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

described the ACEEE as "the repository of best practices on energy efficiency," and "everyone knows of Energy Efficiency in Buildings" Award: Ralph Cavanagh, Natural Resources Defense Council. Bruce Measure the Council with an award for energy efficiency. Cavanagh said the Council had been selected for the "2010

351

Explorao do Espao de Projeto em Hw/Sw Co-design de Sistemas Tempo-Real Embarcados Orientados a Objetos: o  

E-Print Network [OSTI]

Informática - UFRGS, Brasil 2 Departamento de Engenharia Elétrica - UFRGS, Brasil 3 Departamento de Automação e Sistemas - UFSC, Brasil 4 Departamento de Telemática ­ CEFET/CE, Brasil {etsilvajr, mawehrmeister

Wagner, Flávio Rech

352

A gas ion source for continuous-flow AMS R.J. Schneider a,*, S.-W. Kim a,c  

E-Print Network [OSTI]

A and negative ion currents up to 80 lA. Recently, the compact, permanent-magnet microwave plasma ion source and magnesium vapor charge-exchange canal were coupled to the recombinator injector of the 2.5 MV Tandetron magnet. Small samples containing several micromoles of CO2 could be entrained in a stream of argon used

Sessions, Alex L.

353

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

mussels can attach themselves to trailered boats and hitchhike between water bodies, there is great water and fire suppression #12;2 systems. They can also build up on spillway gates and other hydraulic

354

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

), where: · The available average annual energy 4 is defined as the sum of: o Non-hydro resource generation generation, accounting for maintenance and forced-outage rates and limited by fuel-supply constraints and, the Council's power plan serves as a blueprint for the types and amounts of resources the Northwest should

355

Occurrence of Hyperpycnal Flows and Hybrid Event Beds Related To Glacial Outburst Events In A Late Ordovician Proglacial Delta (Murzuq Basin, SW Libya)  

Science Journals Connector (OSTI)

...a subaerial channel sandstone (DP4) (car for scale). C) A thick sand-prone...DF1) in a lower-foreset position (car for scale). Fig. 7 Sedimentary logs...implications for reservoir modeling: Cretaceous Panther Tongue delta, Book Cliffs, Utah. American...

Flavia Girard; Jean-Franois Ghienne; Jean-Loup Rubino

356

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

utilities implementing energy efficiency measures. Small and rural utilities face challenges unique (Bonneville) and the Northwest Energy Efficiency Alliance (NEEA) provided additional funding to the study, and potential recommendations identified by Ecotope in its research. A final report is expected in mid-June. 1

357

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of natural gas · Fuel conversions · Fuel switching · Fuel choice· Fuel choice · Total energy efficiency All economic efficiency, and which the objective?y, j · Potential savings estimates · Need for Council policy discuss the status of the analysis. #12;Status Report on Direct Use of N t l GNatural Gas Power Committee

358

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

\\p04_supply side of energy2020 cm.docx #12;1/4/2012 1 REPORT ON ACTION ITEM ANLYS-9. DEVELOPMENT the efficiency of Council staff resources committed to operating two different models. ¢ Potential to reduce Jourabchi SUBJECT: Report on Action Item ANLYS-9: Development of the supply side of the demand forecasting

359

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, the Council directed the Regional Technical Forum (RTF) to develop energy efficiency acquisition process Final report and recommendations available online #12;6/2/2014 2 Small/Rural Subcommittee Background's lighting calculator Simplify irrigation measures Identify potential conservation measures for idle wind

360

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

volatility due to reliance on the wholesale electricity market Conservation 160 MWa per year limit reliance on the wholesale electricity market means lower cost and rate volatility Conservation Same limit meet their Renewable Portfolio Standard (RPS) energy targets Meets reliability and adequacy standards

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. Then the analysis compared the cost of those energy savings to the value of wholesale spot market power purchases, including the value of conservation compared to wholesale market power purchases and a generic look efficiency rather than purchasing the equivalent amount of energy from the market via power purchases

362

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

to Section 4(h)(12)(A) of the Northwest Power Act. The Council's bylaws, which include its organizational............................................................................................................. 9 Proving new energy-efficiency technologies.......................................................................... 9 Television energy efficiency

363

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, working through the subregional planning groups, to have a high likelihood of completion. Jeff Miller Sienkiewicz Shelly Richardson and Jim Miller­ Ed Sienkiewicz, Shelly Richardson, and Jim Miller · Anyone can

364

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for the area. Jeffrey Miller will brief the Council on a study done on the impacts of plant shut-down on the transmission system. Mr. Miller is Vice President and Manager of Planning for Columbia Grid, which conducted

365

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, but that will be tested at mid-term. Natural gas generation is already the fall-back resource in the plan, renewables in expectations about future natural gas supplies. Cost-effective technologies to obtain natural gas trapped the potential of shale gas was identified in the plan, the expected cost of developing it has been reduced

366

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

prices, tax credits and renewable energy credits present major uncertainties in the development that will be used for these analyses. Properly addressing climate change issues, impacts and mitigation strategies

367

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

between uranium mining and spent fuel · The marginal cost of operations is the market price of the fuel

368

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

FORM: Stacy Horton, Washington Council staff SUBJECT: High Level Indicators A web-based version. The development of this web-based report was a team effort which included work from Melissa Shavlik, John Harrison, Eric Schrepel, Nancy Leonard, Peter Paquet, and Stacy Horton. Stacy Horton will present the web

369

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

received on the Council's High Level Indicators web-report The Council released for public comment its High Level Indicator (HLI) web-report on June 15, 2012. This HLI web-report was developed in response meeting. Overall, comments received were supportive of the Council's effort to develop an HLI web

370

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Manager Eric Schrepel, Technical and Web Data Specialist Philip Thoennes, Fish and Wildlife Intern SUBJECT: Subbasin Dashboards Council staff has been crafting a concept for an interactive, web-based tool, which we

371

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

these issues and how we propose to address them in the draft plan at the June 30 Power Committee web meeting June 30 web conference electronic packet. In addition, a Power Point presentation summarizing case" · Results were described at a Power Committee web conference meeting (On Council agenda

372

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and one planned for August ­ 12/2/2010 · At meeting, 23 non-Council + 3 Council staff · On the web, 9 non-Council + 2 Council staff ­ 2/2/2011 · At meeting, 17 non-Council + 2 Council staff · On the web, 11 non-Council + 1 Council staff ­ 5/19/2011 · At meeting, 14 non-Council + 4 Council staff · On the web, 8 non

373

Cytology of SW Asian Chenopodiaceae: new data from Iran and a review of previous records and correlations with life forms and C4 photosynthesis  

Science Journals Connector (OSTI)

Lower polyploidy percentage in C4 plants compared to C3 plants in chenopods is also unexpected. Possible interpretations may include: (1) Many C4 species in our area are annuals with more recent origin. As the pe...

Seyed Mahmood Ghaffari; Zhila Balaei; Targol Chatrenoor

2014-07-01T23:59:59.000Z

374

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network [OSTI]

Greenland. These rocks were erupted between 61 and 52 Ma (Sinton and Duncan, this volume) and span the whole

375

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network [OSTI]

(Sinton and Duncan, this volume). The lava may be grouped into three main lithostratigraphic forma- tions

376

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network [OSTI]

MARGIN, ODP LEG 152, AND THE ROCKALL PLATEAU, DSDP LEG 811 Christopher W. Sinton2,3 and Robert A. Duncan2

377

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

!Natural Gas Supplies: Abundance! Shale Gas An Emerging Source of Significant Supply US Shale Gas Supply Areas BC Shale/Tight Gas Supply Areas #12;US Shale PlaysUS Shale Plays (source: MIT, 2010) BC G P d i SUBJECT: Presentation by Northwest Gas Association on Natural Gas Outlook The Northwest Gas Association

378

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

frontier #12;Page 3 5 Cost EffectivenessCost Effectiveness -- 11 Costs avoided by DR: Capacity cost Energy Effectiveness -- 22 Avoided capacity costs up to 95% of total Energy savings generally small, can be positive SUBJECT: Cost effectiveness workgroup of the PNW Demand Response Project - meeting September 12, 2008

379

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

discusses a potential new avoided cost methodology that blends forecast wholesale #12;power prices and the full cost of RPS resource development to arrive at an overall avoided cost for utilities with RPS. The forecast also provides a cost-effectiveness "bookend" to guide the initial conservation and resource

380

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

interactions with the fish and wildlife program; and · Appropriate avoided cost measures for resource decisions

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

experience, here or elsewhere #12;5 9 Cost EffectivenessCost Effectiveness Does DR avoid more expense than/Long Run -- 22 LR ­ system outgrowing hydro, adding wind, eventually needs peakers Avoided cost based, such as uncertainty regarding the amount and cost of demand response that is available and questions about the proper

382

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

investments on regional revenue requirements ignoredon regional revenue requirements ignored cost savings from avoided market purchasescost savings from avoided market purchases NearNear--term potential for savings--20142014 ­­ Conservation Avoids Market Purchases @Conservation Avoids Market Purchases @ $60/MWH$60/MWH ­­ Utility Share

383

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Power and Conservation Council Plan Case Assumptions · Forecasts of demand and fuel prices · RPS: Discussion of Climate Policy Analysis Climate change policies and their potential effects on the power system the likelihood of future carbon pricing policies that are being discussed or advocated, but also that the levels

384

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

SUBJECT: Wind Integration Forum Oversupply Recommendations Status Report The Wind Integration Forum (WIF for these efforts will be decided in the Wind Integration Forum Steering Committee once the recommendations have the unique characteristics of wind generation on the Northwest power system. In June 2011, the WIF Steering

385

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Resource Analyst SUBJECT: Report on the status of the Wind Integration Action Plan Work has been underway for more than two years on most of the sixteen actions set forth in the March 2007 Wind Integration Action Plan (WIAP). A meeting of the Policy Steering Committee of the Wind Integration Forum was held

386

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

responsibility for assessing new resource potential with Bonneville and utilities; · Developing an improved of policies; · Demonstrate and develop improved demand response programs, advance and test smart grid concepts to test new resources that have potential to provide energy, capacity, and flexibility to the power system

387

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

SUBJECT: Navigant Report Assessing Demand Response Program Potential for the Seventh Plan for Stakeholder and potential, with specific focus on the Northwest region. As a kick-off to preparing a Demand Response Review Stakeholder Review of Demand Response Assessment Per the request of the Northwest Power

388

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

electricity loads for the years 2010-2030. Depending on the market penetration rate assumptions, availability) area using AURORAxmp© and one of three plausible penetration scenarios. This study showed CO2 emissions

389

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. PGE recently concluded a successful small-scale pilot project using algae to capture and consume CO2 expensive environmental upgrades and the risk of carbon regulations, PGE has proposed a plan to phase out

390

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of 2008 and was used to develop the Sixth Power Plan. After an extensive peer review of the methodology following the release of the plan, the Forum revised the standard and the Council subsequently adopted the revised standard in December of 2011. The Council utilizes the standard in its power plan to ensure

391

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, Senior Power System Analyst SUBJECT: Draft Power Plan Chapter 10: Regional Adequacy Standards A draft version of the Sixth Power Plan's Chapter 10 (Regional Adequacy Standards) is attached for the committee's review and comments. This chapter describes the Council's recently adopted Northwest adequacy standard

392

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

standard and after a peer review of the overall methodology. While the 2008 standard was very useful, some calls for the Council to periodically review the adequacy standard and the methodology used to define of this standard effectively completes action item ADQ-3 in the Council's 6th Power Plan. Adoption of the energy

393

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Review (IPR). The IPR occurs every two years, or just prior to each rate case. It provides participants for inclusion in rate cases. Program spending levels are not dealt with in the rate case itself. The 2010 IPR through fiscal year 2017. The 2010 IPR consists of a series of technical and managerial workshops covering

394

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for the upcoming Integrated Program Review (IPR) · March: Release of long-term capital asset strategies · April/July: IPR to discuss FY13-15 expense and capital · September: IPR close-out · November: FY14-15 Initial Rate

395

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and 2017. BPA conducts its IPR processes every two years as a lead-in to its rate cases. BPA held the IPR at http://www.bpa.gov/Finance/FinancialPublicProcesses/IPR/2014IPRDocuments/May28 _IPR L E P O W E R A D M I N I S T R A T I O N EE Post-2011 Review and Integrated Program Review (IPR

396

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

's Capital in Review (CIR) and Integrated Program Review (IPR) process. The CIR and IPR are two significant Program Review (IPR): affords participants opportunity to review and comment on BPA's program level Review (CIR) Public Process May ­ July ~ Integrated Program Review (IPR) Public Process June ­ July

397

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, and heating, ventilation, and air conditioning (HVAC) equipment. RBSA sample design included all public states. This uniformity is largely due to the preemptive federal standards and the region's energy efficiency programs, which also use common standards across all factories and thus all new manufactured homes

398

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of our database to others in the region (in particular, the PNUCC Northwest Regional Forecast or NRF in the NRF whereas, for adequacy purposes, it may be shown to have a 92% availability (counting maintenance and forced outage rates). The difference highlights the two differing uses for the data. For the NRF

399

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Products and Services Measurement and Verification Foundational Support ALL #12;2013 Activity Detail 28% 36 Products and Services Measurement and Verification #12;27% 11% 24% 38% NEEA Funding by Type of Activity Technical Assistance Products and Services Measurement and Verification Foundational Suppo

400

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

.05 Actual $76 Actual Evaluation of Natural gas and oil prices may be warranted. #12;Shale gas resources to very significant changes in the outlook for natural gas supplies from shale formations. In addition Power Plan. The trends of natural gas prices are lower especially in the near term as shale gas

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

chloride (CaCl2). For each treatment, 10 juvenile mussels were reared in individual containers. A control of juvenile quagga mussels was observed when tested in water from the Columbia River amended with CaCl2

402

Subscriber access provided by SwRI Library | Phone (210) 522-2125 The Journal of Physical Chemistry B is published by the American Chemical  

E-Print Network [OSTI]

Cl, CaCl2, and MgSO4, with supplementary measurements of HCl. Below the eutectic temperature, electrical relaxations near the ice signature were identified for CaCl2 ·6H2O and MgSO4 ·11H2O but not for NaCl ·2H2OCl, CaCl2, and MgSO4, with supplementary measurements of HCl. 2. Background The relevant electrical

Stillman, David E.

403

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

­­ Increase saturation of central air conditioningIncrease saturation of central air conditioning Baseline a brief review of its assessment of the conservation potential in residential space conditioning (heating

404

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of the Bonneville Power Administration. PROPOSED ACTION: Finalize the draft report and submit to the Governors been affected by hydroelectric development. The Power Act requires the Bonneville Power Administration to fund the Council's fish and wildlife program. Bonneville is a federal power marketing authority within

405

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for a decision at the May meeting. BACKGROUND The Bonneville Power Administration, the Council, and the Columbia adjustments associated with the Quarterly Review. Department of Energy Bonneville Power Administration P-day public comment period on these requests. Bonneville Power Administration (BPA) will consider any

406

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, the Bonneville Power Administration (Bonneville) began to shift responsibility for financing and acquiring, in 1996 Congress directed Bonneville and the Northwest Power Planning Council (Council) to convene and renewable resource programs. In February 1999, Bonneville's Administrator requested the Council also task

407

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Division Bonneville Power Administration P.O. Box 3621 Portland, Oregon 97208 Dear Mr. Maslen: The purpose Reporting, Project #2009-002-00 In 2008-2009, the Bonneville Power Administration, the U.S. Army Corps document outlining the review process for the Accords, the Council recognizes Bonneville's commitment

408

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

budget. BACKGROUND The Council and Bonneville Power Administration (Bonneville) jointly invited Program under the Northwest Power Act. The Council, in its project funding recommendations to Bonneville reserved for Innovative projects is $2,000,000 total for Fiscal Year 2008 and 2009, per Bonneville

409

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Division Bonneville Power Administration P.O. Box 3621 Portland, Oregon 97208 Dear Mr. Maslen: The purpose Reservation of Oregon, Project #2008-311-00 In 2008-2009, the Bonneville Power Administration, the U.S. Army document outlining the review process for the Accords, the Council recognizes Bonneville's commitment

410

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, the Bonneville Power Administration (Bonneville) began to shift responsibility for financing and acquiring Power Administration. The existing charter, however, lacked a quorum requirement and is silent, in 1996 Congress directed Bonneville and the Northwest Power Planning Council (Council) to convene

411

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for discussion with the PPC panel. #12;1 May 15, 2008 Mr. Stephen J. Wright Administrator Bonneville Power Executive Committee agreed to forward the attached positions regarding the Bonneville Power Administration SUBJECT: PPC Panel on Bonneville Role in Conservation The Public Power Council has put together a panel

412

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

." The Bonneville Power Administration (Bonneville) and Corps of Engineers (Corps) responded to this recommendation Bonneville Dam #12;Drivers · Northwest Power and Conservation Council Fish and Wildlife Program (Council 2009 and evaluation activities. Bonneville and the Corps propose that the CEERP will meet the needs of the Council

413

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. The participants include 11 utilities and the Bonneville Power Administration. Pursuing a project of this breadth, Bonneville Power Administration, Smart Grid and Demand Response Program Director Evan Jones, PNNL #12; Washington Phil Rockefeller Washington October 29, 2013 MEMORANDUM TO: Power Committee FROM: Ben Kujala

414

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

to the committee and Council for a decision at the February meeting. BACKGROUND The Bonneville Power Administration Review. Department of Energy Bonneville Power Administration P.O. Box 3621 Portland, Oregon 97208. Bonneville Power Administration (BPA) will consider any public comments received by January 16, 2008, before

415

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Change Request Tracking Process for the Bonneville Power Administration (BPA) / Northwest Power to adopt within-year adjustments. At the September meeting, Council and Bonneville staffs will provide feedback before going any further with the proposed changes. BACKGROUND In 2004, Bonneville and the Council

416

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

the Council's recommendations to the Bonneville Power Administration for funding and implementing. Section 4(h)(10)(A) of the Northwest Power Act then calls on the Bonneville Power Administration: Council recommendation to Bonneville SIGNIFICANCE: This is the final category review since they began

417

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of the Bonneville Power Administration. The draft report was sent to you by e-mail. PROPOSED ACTION: Approve Power Administration to fund the Council's Columbia River Basin Fish and Wildlife Program. Bonneville. Bonneville, Northwest Requirements Utilities, and the Public Power Council asked that the paragraph

418

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and Wildlife Division Bonneville Power Administration P.O. Box 3621 Portland, OR 97208 Dear Mr. Maslen: Re and Conservation Council Fish and Wildlife Project Funding Recommendations to the Bonneville Power Administration's recommendations to the Bonneville Power Administration for the fish and wildlife projects Bonneville should fund

419

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and timely repayment of the Bonneville Power Administration's (Bonneville) debt to the federal Treasury.3 of Bonneville's debt to the Treasury. To make this assessment, a comparison is made between a regional power the early 1980s, thus giving the power system and Bonneville time to integrate and adjust to them. Because

420

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Counsel, and John Harrison, Information Officer SUBJECT: Bonneville Power Administration/U.S. Army Corps, the Administrator of the Bonneville Power Administration and the Northwestern Division Engineer of the U.S. Army: Stephen R. Oliver - Bonneville Power Administration VP Generation Asset Management and U.S. Entity Co

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Administration new Annual Project Reporting Template Russell Scranton and Jason Sweet from the Bonneville Power, Fish, Wildlife, Ecosystem Monitoring and Evaluation Manager SUBJECT: Briefing on Bonneville Power Administration (Bonneville) will provide an update on the new, standardized, annual project reporting template

422

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Friday, July 2, 1993 *35922 AGENCY: Bonneville Power Administration (BPA), DOE. ACTION: Revised Agency (Northwest Power Act or Act), 16 U.S.C. 839d(c), requires the *35923 Administrator of the Bonneville Power, Bonneville has a policy on the implementation of Section 6c of the Northwest Power Act, the provision

423

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of the Bonneville Power Administration. The draft report was sent to you by e-mail. PROPOSED ACTION: Release is the 12th year the Council has reported to the Northwest governors on Bonneville's fish and wildlife costs in the reports is provided by Bonneville and is not independently verified by the Council. At this meeting, staff

424

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Division Bonneville Power Administration P.O. Box 3621 Portland, Oregon 97208 Dear Mr. Maslen: The purpose in the tributaries below Bonneville Dam, Project #2008-710-00 On March 11, 2009 the Bonneville Power Administration (Bonneville) submitted a 2008 Federal Columbia River Power System (FCRPS) Biological Opinion (BiOp) project

425

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and Wildlife Division Bonneville Power Administration P.O. Box 3621 Portland, OR 97208 Dear Mr. Maslen: Re for Bonneville Power Administration (Bonneville) funding of projects solicited by the Council and Bonneville to Bonneville the Council's final decision document concluding the fish and wildlife project review process

426

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

the Bonneville Power Administration as its Vice President of Energy Efficiency on January 7, 2013. Before position at Bonneville is one of four vice president positions in the Power Services area headed by Senior, Power Planning Division Director SUBJECT: Introduction of Richard Génecé Richard Génecé joined

427

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

input on the Sixth Power Plan Mid-Term Assessment. A panel of stakeholders provided comments technical analysis of new issues in preparation for the Mid-Term Assessment or, if not now, in preparation of the region's expectations for the Mid-Term Assessment. At the June meeting, staff will update the Power

428

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

potential assessment. Both the Regional Technical Forum (RTF) and the Conservation Resources Advisory Washington Phil Rockefeller Washington September 30, 2014 MEMORANDUM TO: Power Committee FROM: Charlie Grist SUBJECT: Primer on Energy Efficiency Assessment Methodology Presenter: Charlie Grist Summary: Staff

429

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

will summarize the lessons learned from this experience. The presentation should give the Council a real-world supply. The system is also operated to protect the river's fish, including salmon, steelhead, sturgeon hydropower, BPA is the primary high-voltage transmission provider in the Columbia River Basin. Consistent

430

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, the Council was briefed on the adequacy of the Northwest's power supply. That current assessment indicated that the supply would continue to be adequate through 2015. Nonetheless, staff continues to work with utilities and others to review key assumptions regarding loads and resources and plans to reassess supply adequacy

431

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Interconnection options for three Balancing Authorities � BPA (BPA Troutdale Substation, Administration (BPA) continue to experience congestion resulting in curtailment. BPA has identified 2013 IRP "There are 25 `Cut-Planes' or `Constraint Points' or `Flow Gates' on BPA's transmission system

432

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and BPA--will explain why the project was undertaken, why it took seven years to bring it to fruition/Vantage Substation north through Wenatchee to Wells Dam Parties involved in the Joint Project 2 #12;3 #12;Timeline 2004 BPA identifies North Mid-C constraints 2006 NW Power Pool South Mid-C Study 2008 Columbia

433

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Commercial Real Estate Residential New Construction Commercial New Construction Commercial Lighting Irrigated Secondary Glazing Commercial New Construction/ Integrated Design Support ***Commercial Real Estate Goals Vision: Energy efficiency is a cornerstone of a vibrant sustainable Northwest Mission: Mobilize

434

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

be an issue for operations dependent upon forest products. Air quality and fuel transportation impacts may Long association with the forest products industry Boom in '80's, retirements in '90s, some post-2000

435

Capillary pressure saturation relations supercritical CO2 and brine in sand: High-pressure Pc(Sw) controller/meter measurements and capillary scaling predictions  

E-Print Network [OSTI]

Technology Laboratory (NETL), U.S. Department of Energyto acknowledge Robert Romanosky (NETL Strate- gic Center fornational laboratories: NETL, Lawrence Berke- ley National

Tokunaga, T.K.

2014-01-01T23:59:59.000Z

436

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

as a cultural resource and subsistence fishery at a base program level. Following is the draft recommendation Plan. The submittal was received from the lake Roosevelt Co- managers (i.e., Spokane Tribe, Colville with the management plan acknowledged the past history of the comprehensive management plan and the relation

437

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Manager SUBJECT: Council decision on Kokanee Plan for Lake Roosevelt. PROPOSED ACTION: The policy issue Roosevelt to continue as a cultural resource and subsistence fishery at a base program level. Following - Comprehensive Management Plan. The submittal was received from the lake Roosevelt Co- managers (i.e., Spokane

438

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

minimum efficiency standards on several products, including battery chargers, televisions and automatic after reviewing all current policies. more or less in pursuing conservation and renewable energy. p planning or implementation of the Council's power plan. Brian Dekiep, Montana's Energy Analyst

439

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Committee meeting on November 6, Paul Norman will summarize the OTOC report and possible follow. Major focus of OTOC since May meeting: Load Shifting #12;Load Shifting Concept: Change rate design, or provide other incentives to shift load into off-peak hours Conclusion: Potential is in hundreds

440

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

SUBJECT: Follow Up on Weather and Energy Efficiency Impacts on Loads At the Power Committee meeting in Boise in November, Massoud Jourabchi presented the forecast of Pacific Northwest electricity loads on year-to-year upward and downward impacts of weather on regional loads, as well as the more lasting load

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. It will focus on two of them in particular, regulation and load following, which have become issues? · What are the ancillary services? · Focus on regulation and load following · What special issues (for severe contingencies) · Ongoing · Regulation · Load following · Reactive power provision

442

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

largely on two specific ancillary services: regulation and load following. Staff explained how increased and load following services; · The resources currently available in the region that provide regulation and load following services; · The resources in the region which do not currently provide regulation

443

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

estimates of the future cost of CO2 production. This paper discusses a potential new avoided cost methodology that blends forecast wholesale power prices and the full cost of RPS resource development

444

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and Conservation Council Power System Costs and CO2 Emissions: 2030 0 10 20 30 40 50 60 70 80 90 Carbon Risk $45 COTonsPerYear(GenBased) Cost w/ CO2 Tax Cost w/o CO2 Tax CO2 Emissions 2005 CO2 Emissions #12;4 Northwest Power;5 Northwest Power and Conservation Council Frequency Distribution of CO2 Emissions in Carbon Target Scenarios

445

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

figure into the equation. Measured in terms of generation, CO2 emissions in the region are relatively low; but measured by consumption, CO2 emissions are much higher, and the carbon costs will follow consumption, she will be inescapable in order to cut CO2 emissions; large reductions in emissions are possible if there is time to add

446

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and resource analysts should use marginal CO2 production rates to evaluate the CO2 emissions cost associated measures and other resources with lower CO2 emissions. It is the CO2 emissions of the marginal resource presented in the paper is that the Northwest power system's total annual CO2 emissions could potentially

447

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

· Transmission capacities · California Greenhouse Cap and Trade Though the updates for the inputs were broad forecasting is a two part process 1. Long term capacity expansion ­ in combination with existing generating Solar PV utility scale capital cost estimates For reference, the 2013 Power Price Forecast Report

448

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Director 800-452-5161 www.nwcouncil.org Fax: 503-820-2370 W. Bill Booth Chair Idaho Bruce A. Measure Vice, and which are of interest for the sake of completeness, but unlikely to materially affect the determination is a new simple cycle gas turbine (SCCT) generator, and that the cost avoided by demand response

449

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. Staff worked with the Council's Natural Gas Advisory Committee (NGAC) to develop the proposed updates in the fuel markets that they anticipate will impact future, natural gas prices and price volatility. Staff and the NGAC comparison of forecasts from many sources suggest a tightening in the natural gas markets

450

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network [OSTI]

was punctuated by at least four early Mio- cene glaciations (Mi1, Mi1a, Mi1b, and Mi2 of Miller et al., 1991 (~17-15 Ma). A transient cool- ing/glaciation at ~16.5 Ma (= Mi2 of Miller et al., 1991) was fol- lowed

451

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

in electric sector GHG emissions relative to 2005 By 2020: · On track to meet (or exceed) 33% RPS by 2020 · 50% if counting rooftop PV (5%) and large hydro (13%) · 20% reduction in electric sector GHG emissions relative to 2005 · 6-8% rate increase due to 33% RPS #12;California's GHG Goals Meeting CA's GHG

452

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

the sale of BEF carbon offsets, fund projects that support new renewable energy projects from solar, wind to further the development and use of new renewable energy resources and restore watershed ecosystems. BEF of the Northwest Energy Efficiency Alliance. Margie will be making the presentation to the Council. More

453

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

obligations and commits the CPUC to monitoring the developing TREC market and taking actions necessary "to. · Retains the same definition of "bundled" and REC-only (TREC) transactions as set forth in the March 2010 decision. "Bundled" transactions are those where RECS and RPS- 1 The CA RPS requires IOUs regulated

454

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of planning for the regional power and gas systems Inter-regional power system and market linkages, including

455

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for the Seventh Plan Ben Kujala && Steven Simmons Why Coordinate? Increasing linkages between the power, natural gas and transmission systems andnatural gas and transmission systems and their constraints

456

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

interstate aspects of the electric power, natural gas, oil pipeline , and hydroelectric industries. NERC

457

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and stream segments that the Council recommends be protected from hydroelectric development, concluding the Council first designated protected areas in 1988, FERC has not licensed a new hydroelectric project or provide transmission support for a new hydroelectric development in a manner inconsistent with the Council

458

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

practices to the forefront of conversations in the region by system operators, utilities, independent power Capacity (MW) 500 1,000 1,500 2,000 2,500 MW Wind Solar Petroleum Natural gas Hydro Geothermal Coal 500 0

459

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

% biomass; 10% geothermal; 5% solar; 65% wind Large utility sales: Scheduled increments to 25% by 2025. (Medium utilities 10%; small 5% by 2025) OR 15% biomass; 15% geothermal; 20% solar; 50% wind IOU sales of the paper. · Added guidance to utilities regarding the use of the price forecasts to evaluate the cost

460

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

projects by California utilities, long-term contracts to California utilities for the output of Northwest to Northwest utilities, to California utilities. Information regarding the latter transactions appearsCapacity(MW) Geothermal Petroleum Wind Solar Natural gas Hydro Coal Biomass * In-service, under construction or planned

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, and to reduce peak loads at times when it is advantageous to utilities. The presentation will illustrateGenerators are not perfectly reliable and e.g. wind, solar have variable output Adjustments every few minutesAdjustments every

462

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Northwest Asotin County PUD Clark Public Utilities Kittitas County PUD Pend Oreille County PUD Benton County PUD Grant County PUD Mason County PUD 3 Tacoma Public Utilities City of Centralia Grays Harbor County PUDMunicipal Corporation 19571957 White Bluffs Solar Station (38 KWe) Columbia Generating Station (1,170 MWe) Nine Canyon

463

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

develop large amounts of solar power; if so, its generation profile will affect the wholesale power market response We agree that changing paradigms for energy efficiency, such as utilities with little or no load the next plan, the Council should try to reconcile its efficiency targets as they apply to I-937 utilities

464

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

topics, role of the GRAC, focus on preliminary solar photovoltaic resource assessment (utility scale around the region, including members from public utilities, investor owned utilities, Bonneville Power and rooftop).assessment (utility scale and rooftop). Good attendance and participation - 29 in person, 19

465

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

. The Evergreen State Solar Partnership connects jurisdictions, utilities, and solar professionals with the tools a showcase for solar successes, we make it easy for more jurisdictions and utilities to share in the benefits SUBJECT: The Evergreen State Solar Partnership Linda Irvine of Northwest Seed will join Tim Stearns

466

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

two utilities with service territories in the eastern part of the region. Oregon will be the focus efficiency programs for over 80 percent of Oregon's total retail utility customer base. Umatilla Electric promoting renewable energy at one of four regional solar energy centers established by then-President Carter

467

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

federal laboratory looking at the interactions of plug-in hybrid electric vehicles (PHEVs) with the power from dependence on foreign oil, he noted. We found the idle capacity of today's grid could supply 73- Meyer said. If you have only night-time charging, 43 percent of the vehicles could be fueled, he noted

468

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

to changes in ocean conditions, and good conditions for salmon are ocean currents with cold water from convened a panel to provide the latest information on adult salmon runs, ocean conditions, and mainstem but lower numbers, with some increases in 2008. 2. Ocean conditions, juvenile abundance index

469

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

turbine generators, reciprocating engine generators, steam-electric coal-fired power plants and advanced Natural gas reciprocating engines On-shore wind turbine generators Pulverized coal steam-electric Coal concentrating solar Solid biomass steam-electric Biogas generation Conventional geothermal Waste heat recovery

470

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

from the region's hydroelectric system. However, as constraints on the operation of the hydroelectric

471

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

the Cushman Hydroelectric project, located on the Skokomish River near Hood Canal on the Olympic Peninsula, fish passage, hatcheries, wildlife and recreation. #12;TACOMA POWER'S CUSHMAN HYDROELECTRIC PROJECT Powerhouse · Fish Passage · Hatcheries, Wildlife & Recreation · Summary #12;3 CUSHMAN HYDROELECTRIC PROJECT

472

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

has been retired. In addition, the capability of the existing installed hydroelectric system to meet to integrate variable generating resources (i.e., wind power). Since 1980, the hydroelectric system has lost agreement, announcement of construction schedule. Changes in Hydroelectric Power Increases in capability

473

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

in developing a resource plan for the region is to understand how its largest resource, namely the hydroelectric effects to reservoir elevations, refill probabilities, river flows, hydroelectric generation and cost change and related carbon policies, loss of hydroelectric flexibility due to wind integration

474

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, Photovoltaics, Landfill Gas, Wind, Biomass, Hydroelectric, Geothermal Electric, Geothermal Heat Pumps, CHP, Small Hydroelectric, Tidal, Wave, Ocean Thermal, Biodiesel, Fuel Cells Using Renewable Fuels September% by 2020 Solar Thermal Electric, Photovoltaics, Landfill Gas, Wind, Biomass, Hydroelectric, Geothermal

475

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and operation of hydroelectric facilities, while assuring the Pacific Northwest an adequate, efficient hydroelectric project on the Columbia River; establishing objectives for the development and operation of anadromous fish at, and between, the region's hydroelectric dams." The Act also allows recommendations

476

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

: Appendix M: Integrating Fish & Wildlife and Power Planning By statute, mainstem hydroelectric operations attachments (the Hydroelectric Generation section from Chapter 6 and Appendix M) describe how the plan accommodates changes in hydroelectric generation and cost related to fish and wildlife program actions

477

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Utility District No. 1 of Chelan County is one of three PUDs that own and operate large hydroelectric from wholesale sales of its hydroelectric power while mitigating the impacts of volatile spot market marketing activities, including auctions to sell shares of the output from its hydroelectric generating

478

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Other, CO2 free Coal Natural Gas Other, CO2 emitting Remaining US generation 2009 � 2013 average. EIA Data 5 - Big Differences in Portfolio Emissions 9 Utility x Hydro Wind Other, CO2 free Coal Natural gas footprint � Transportation is the largest contributor of CO2 in the Northwest � Northwest produces low

479

Saunders, A.D., Larsen, H.C., and Wise, S.W., Jr. (Eds.), 1998 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 152  

E-Print Network [OSTI]

, 1989). This glaciation was preceded by an influx of cold North Atlantic Deep Water (NADW. These kinds of investigations have already been applied to a large number of Deep Sea Drilling Project and ODP again during the middle Miocene, which coincides with the development of modern North Atlantic Deep

480

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network [OSTI]

or differential erosion. Tectonic mechanisms include faulting of crustal blocks, mobile basins with evolving arches and depo- centers, local flexural subsidence, or differential subsidence caused by sediment). However, the oxygen-isotope method can be af- fected by temperature and local salinity changes, and more

Note: This page contains sample records for the topic "haleakala sw rift" 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

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, there is participation from people and firms that specialize in creating public messages and branding. It was clear Bill Gaines, Tacoma Public Utilities Margie Harris, Energy Trust of Oregon Erin Holland, Edelman Public Skeahan, Cowlitz County Public Utility District Cal Shirley, Puget Sound Energy Phil Welker, Portland

482

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

utilities on their views. Their message was that they are committed to meeting conservation goals SUBJECT: Panels on Bonneville Conservation Role after 2011 In various forums, regional parties are discussing what Bonneville's role should be in conservation acquisition under the long-term regional dialogue

483

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

development of Demand- Side Management, Distributed Generation and Energy Efficiency resources. There was also and Conservation Council February 11, 2014 - Portland, OR Keegan Moyer Manager, Transmission Expansion Planning Expansion Planning and Policy Committee Purpose Oversee and maintain public planning database and models

484

Nanoscience D O I N GI ST I T U T EI N SW E I Z M A N NT H ETW H A  

E-Print Network [OSTI]

outside the cell · The goal: self assembling transistors made of DNA · Organic molecules to fine Sensors · Doing what comes naturally · Tomorrow's reporters ­ cells on a chip · Light reading · Of sieves nanoscopic drug delivery systems or achieve a far greener environment born of solar energy triumphs

Maoz, Shahar

485

Miller, K.G., and Snyder, S.W. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 150X  

E-Print Network [OSTI]

ascending order. Sequence boundaries are recognized by gamma-ray log excur- sions, hiatuses on the timing and magnitudes of sea-level changes (see summary by Miller, Chapter 1, this volume). The Paleocene). They concluded that there was a good match between the cycle chart and the record of deposition in New Jersey

486

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and Sandra Hirotsu SUBJECT: Update on California Renewable Energy Policy In a continuing effort to keep members up to date on California's renewable energy policy, staff will discuss the most recent activities of tradable renewable energy credits (TRECs) to meet the RES and allows for banking and trading of renewable

487

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, Senior Energy Policy Analyst, WA staff Gillian Charles, Energy Policy Analyst SUBJECT: Renewable, and Washington looked at where the region is currently at in terms of renewable energy acquisition and forecasted the need for future renewable development or renewable energy credit (REC) procurement. Following

488

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Gas-fired Units Contracts Hydro Wind NUGs Mid-C Transmission Available Dec Peak Load + 15.7% PM + Op Reserves Low Dec Peak Load + 15.7% PM + Op Reserves High Dec Peak Load + 15.7% PM + Op Reserves 917 MW 1

489

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, production tax credits (PTC), investment tax credits (ITC), and renewable energy credits (REC) to be used and supporting analysis Assumptions for renewable resource financial incentives and renewable energy credits of CO2 prices for the Portfolio Model Assumptions for renewable energy credits (RECs) and financial

490

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

, on the cost/benefit of switching to solar residential water heating." Because this is a comment on the paper and not on the annual report, and because the paper did not address solar energy as an alternative fuel for residential....................................................... 9 Council sees no cost benefit in switching fuels for residential space and water heating.. 10 Data

491

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

choices available for the plan. It provides a more consistent source of power than wind, in which most Resources Contact Us Updates January 2008 - Construction is complete and the Unit One power plant is now - The construction activities on Raft River Unit One power plant are nearly completed. During a testing phase

492

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

· Alternative rates of implementation for conservation · The consequences of breeching the dams on the lower penalty likelihood distribution Conservation base case New programs and re-evaluation of energy 170 Geothermal 0 0 0 52 104 156 169 and the larger of Wind 0 0 1200 1200 3000 3000 3000 RPS* req 0 26

493

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Assumptions (Wind) Other Generating Technologies assumptions Energy Efficiency (impact of standards) Demand and to assess the implementation of the power plan and the action plan in particular. There are five components Forecast Fuel Prices Electricity Prices Resource Costs Load - Resource Balance Implementation Status

494

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and fish and wildlife capital expenditures over the next 10 years. The draft letter will be sent to you to define its capital expenditure needs for the coming decade. In September, BPA unveiled a proposal, Director, Power Planning Division SUBJECT: Draft letter to Steve Wright regarding BPA's capital spending

495

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

and furnaces or to generate electricity for electrical space and water heating systems that provide served those electric space and water heating systems. After netting out the 21 trillion BTU decrease away from electric resistance where natural gas is already in the home for space heating. However

496

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

Buildings 5. Buildings Converting to Electric Space Conditioning or Water Heating Systems, and 6. These are the standards for: 1. New Electrically Heated Residential Buildings 2. Utility Conservation Programs for New the standards for New Electrically Heated Residential Buildings and for New Commercial Buildings set forth

497

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of supplemental wood heat in homes with electric heating systems. The reduction in supplemental wood use has two-effectiveness estimates for a wide range of residential space heating energy efficiency measures, including residential weatherization, ductless and air-source heat pumps and duct sealing. The RTF analysis to date has revealed

498

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

of them, a pilot program testing the feasibility of using electric water heating, electric space heating to the Pacific Northwest electric system. Contact us at Technology Innovation q:\\tm\\council mtgs\\2012\\january\\c07 through transmission and distribution to electricity-consuming equipment in customers' homes (see http

499

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

for electrical space and water heating systems that provide these services? The Council has deliberated gas water heating away from electric resistance where natural gas is already in the home for space no longer appear cost-effective; electric resistance water heat, and electric forced air furnace space heat

500

851 S.W. Sixth Avenue, Suite 1100 Steve Crow 503-222-5161 Portland, Oregon 97204-1348 Executive Director 800-452-5161  

E-Print Network [OSTI]

heating systems that provide these services? The Council has deliberated on this question since its fuel conversions involve shifting to natural gas water heating away from electric resistance where 55 gallons. Two technologies no longer appear cost-effective; electric resistance water heat