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1

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...

2

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

3

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

4

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

5

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

6

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

7

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

8

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"

9

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

10

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"

11

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"

12

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

13

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

14

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

15

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

16

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

17

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

18

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

19

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

20

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

Note: This page contains sample records for the topic "rift area thomas" 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

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

22

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

23

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

24

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

25

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

26

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

27

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

28

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

29

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

30

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

31

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

32

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

33

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

34

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...

35

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

36

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

37

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

38

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

39

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...

40

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.

Note: This page contains sample records for the topic "rift area thomas" 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

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

42

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

43

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

44

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

45

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

46

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":""}]}

47

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

48

Geothermometry At Honokowai Area (Thomas, 1986) | Open Energy Information  

Open Energy Info (EERE)

Geothermometry At Honokowai Area (Thomas, 1986) Geothermometry At Honokowai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Honokowai Area (Thomas, 1986) Exploration Activity Details Location Honokowai Area Exploration Technique Geothermometry Activity Date Usefulness not indicated DOE-funding Unknown Notes Temperature and groundwater chemistry analyses were performed on three wells along the alluvial fan above Honokowai. Water temperatures were approximately 20degrees C and normal basal aquifer water chemistry was observed (Table 4). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Geothermometry_At_Honokowai_Area_(Thomas,_1986)&oldid=387033"

49

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":""}]}

50

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

51

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.

52

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"

53

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...

54

Geothermometry At Lahaina-Kaanapali Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Lahaina-Kaanapali Area (Thomas, 1986) Lahaina-Kaanapali Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Lahaina-Kaanapali Area (Thomas, 1986) Exploration Activity Details Location Lahaina-Kaanapali Area Exploration Technique Geothermometry Activity Date Usefulness not indicated DOE-funding Unknown Notes Groundwater temperature and chemistry surveys were similarly unable to identify any detectable thermal influence on the basal groundwaters. Silica concentrations and water temperatures (Table 4) were within the normal range expected for basal groundwaters receiving a limited amount of irrigation return water; chloride/magnesium ratios ranged downward from normal seawater values. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

55

Aeromagnetic Survey At Kawaihae Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Kawaihae Area (Thomas, 1986) Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness useful DOE-funding Unknown Notes The aeromagnetic data noted above refer to a low-level aeromagnetic survey that was flown over the entire island of Hawaii at an altitude of approximately 300 m. The results of the survey over Kawaihae clearly indicate an anomalously magnetized body between the town of Waimea and Kawaihae Bay to the west. 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_Kawaihae_Area_(Thomas,_1986)&oldid=402415

56

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"

57

Mercury Vapor At Lualualei Valley Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Lualualei Valley Area (Thomas, 1986) Mercury Vapor At Lualualei Valley Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Lualualei Valley Area (Thomas, 1986) Exploration Activity Details Location Lualualei Valley Area Exploration Technique Mercury Vapor Activity Date Usefulness useful DOE-funding Unknown Notes Soil mercury and radon emanation surveys were performed over much of the accessible surface of Lualualei Valley (Cox and Thomas, 1979). The results of these surveys (Figs 7 and 8) delineated several areas in which soil mercury concentrations or radon emanation rates were substantially above normal background values. Some of these areas were apparently coincident with the mapped fracture systems associated with the caldera boundaries.

58

Field Mapping At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Field Mapping At Mokapu Penninsula Area (Thomas, Field Mapping At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Field Mapping Activity Date Usefulness useful DOE-funding Unknown Notes Geological mapping on Mokapu (Cox and Sinton, 1982) identified at least three separate volcanic vents within the study area and several other vents forming small islets around Mokapu. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from "http://en.openei.org/w/index.php?title=Field_Mapping_At_Mokapu_Penninsula_Area_(Thomas,_1986)&oldid=510748" Category: Exploration Activities What links here Related changes Special pages Printable version Permanent link Browse properties 429 Throttled (bot load)

59

Geothermometry At Lualualei Valley Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Geothermometry At Lualualei Valley Area (Thomas, 1986) Geothermometry At Lualualei Valley Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Lualualei Valley Area (Thomas, 1986) Exploration Activity Details Location Lualualei Valley Area Exploration Technique Geothermometry Activity Date Usefulness useful DOE-funding Unknown Notes Yhe extensive set of groundwater chemical data compiled for the wells in the valley (Table 1) showed that two of the primary indicators that have been commonly used in Hawaii for identifying geothermal potential (i.e. silica concentration and chloride to magnesium ion ratios) were anomalous in the groundwater of this survey area (Cox and Thomas, 1979). Several wells located on the caldera boundaries were found to have both

60

Water Sampling At Kauai Area (Thomas, 1986) | Open Energy Information  

Open Energy Info (EERE)

Kauai Area (Thomas, 1986) Kauai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Water Sampling At Kauai Area (Thomas, 1986) Exploration Activity Details Location Kauai Area Exploration Technique Water Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes Groundwater geochemical data compiled for Kauai during the preliminary assessment identified a few very weak water chemistry anomalies, and although these anomalies could be interpreted to be the result of residual heat associated with Kauai's late-stage volcanism, the great age of this activity as well as the absence of any other detectable thermal effects suggests that this is very unlikely. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

Note: This page contains sample records for the topic "rift area thomas" 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

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

62

Mercury Vapor At Kawaihae Area (Thomas, 1986) | Open Energy Information  

Open Energy Info (EERE)

Mercury Vapor At Kawaihae Area (Thomas, 1986) Mercury Vapor At Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Mercury Vapor Activity Date Usefulness not useful DOE-funding Unknown Notes The soil geochemistry yielded quite complex patterns of mercury concentrations and radonemanation rates within the survey area (Cox and Cuff, 1981c). Mercury concentrations (Fig. 38) showed a general minimum along the Kawaihae-Waimea roads and a broad trend of increasing mercury concentrations toward both the north and south. There is no correlation apparent between the mercury patterns and either the resistivity sounding data or the surface geology in the area. The radon emanometry data (Fig.

63

Geothermometry At Kawaihae Area (Thomas, 1986) | Open Energy Information  

Open Energy Info (EERE)

Geothermometry At Kawaihae Area (Thomas, 1986) Geothermometry At Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Geothermometry At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Geothermometry Activity Date Usefulness useful DOE-funding Unknown Notes Groundwater chemical data are limited due to the small number of wells near Kawaihae; however, the data that are available strongly substantiate the presence of a thermal resource. A measured water temperature of 31 degrees C in one well is clearly above normal ambient temperatures, and the chloride/magnesium ion ratio in the same well is elevated substantially above the normal range (Table 8). Both of these data provide strong evidence that at least a low-level thermal anomaly is present in the area.

64

Mercury Vapor At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mokapu Penninsula Area (Thomas, 1986) Mokapu Penninsula Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Mercury Vapor Activity Date Usefulness not useful DOE-funding Unknown Notes The high degree of cultural activity (e.g. residential areas, streets, jet runways, etc.) on Mokapu both limited the extent of the soil geochemical surveys performed and rendered their interpretation much more difficult. Soil mercury concentrations and radon emanometry data on the peninsula showed a few localized high values (Figs 13, 14), but no consistent correlation between the anomalous zones and geologic features could be

65

Aeromagnetic Survey At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Aeromagnetic Survey At Mokapu Penninsula Area (Thomas, 1986) Aeromagnetic Survey At Mokapu Penninsula Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Aeromagnetic Survey At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Aeromagnetic Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes A separate geophysical analysis performed on the Koolau caldera area (Kauahikaua, 1981 a) synthesized existing self-potential, gravity, seismic and aeromagnetic data with recently acquired resistivity soundings. An analysis of the observed remnant magnetization within the caldera complex suggested that subsurface temperatures ranged from less than 300degrees C to no more than 540degrees C. The resistivity data indicated that the

66

Soil Sampling At Molokai Area (Thomas, 1986) | Open Energy Information  

Open Energy Info (EERE)

Soil Sampling At Molokai Area (Thomas, 1986) Soil Sampling At Molokai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Soil Sampling At Molokai Area (Thomas, 1986) Exploration Activity Details Location Molokai Area Exploration Technique Soil Sampling Activity Date Usefulness useful DOE-funding Unknown Notes Due to the very small potential market on the island of Molokai for geothermal energy, only a limited effort was made to confirm a resource in the identified PGRA. An attempt was made to locate the (now abandoned) water well that was reported to have encountered warm saline fluids. The well was located but had caved in above the water table and thus no water sampling was possible. Temperature measurements in the open portion of the well were performed, but no temperatures significantly above ambient were

67

Static Temperature Survey At Molokai Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Molokai Area (Thomas, 1986) Molokai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Static Temperature Survey At Molokai Area (Thomas, 1986) Exploration Activity Details Location Molokai Area Exploration Technique Static Temperature Survey Activity Date Usefulness useful DOE-funding Unknown Notes Due to the very small potential market on the island of Molokai for geothermal energy, only a limited effort was made to confirm a resource in the identified PGRA. An attempt was made to locate the (now abandoned) water well that was reported to have encountered warm saline fluids. The well was located but had caved in above the water table and thus no water sampling was possible. Temperature measurements in the open portion of the well were performed, but no temperatures significantly above ambient were

68

Self Potential At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Self Potential At Mokapu Penninsula Area (Thomas, Self Potential At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Self Potential Activity Date Usefulness not indicated DOE-funding Unknown Notes A separate geophysical analysis performed on the Koolau caldera area (Kauahikaua, 1981 a) synthesized existing self-potential, gravity, seismic and aeromagnetic data with recently acquired resistivity soundings. An analysis of the observed remnant magnetization within the caldera complex suggested that subsurface temperatures ranged from less than 300degrees C to no more than 540degrees C. The resistivity data indicated that the electrical basement, to a depth of 900 m, had resistivities ranging from 42 ohm.m to more than 1000 ohm.m, which is considered to be within the

69

Water Sampling At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Water Sampling At Mokapu Penninsula Area (Thomas, Water Sampling At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Water Sampling Activity Date Usefulness could be useful with more improvements DOE-funding Unknown Notes Chemical analysis of groundwater from Mokapu was severely restricted by the absence of drilled wells; the only groundwater sources present were five shallow, brackish ponds, Chemical data indicated that all of the ponds consisted of seawater diluted by varying amounts of fresh surface water; no thermal alteration was revealed by the water chemistry (Table 2). Available temperature and water chemistry data on the Koolau caldera area were also assessed as part of the Mokapu study. The results of this analysis (Table

70

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

71

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...

72

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

73

Ground Gravity Survey At Mokapu Penninsula Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Ground Gravity Survey At Mokapu Penninsula Area Ground Gravity Survey At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Ground Gravity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes A separate geophysical analysis performed on the Koolau caldera area (Kauahikaua, 1981 a) synthesized existing self-potential, gravity, seismic and aeromagnetic data with recently acquired resistivity soundings. An analysis of the observed remnant magnetization within the caldera complex suggested that subsurface temperatures ranged from less than 300degrees C to no more than 540degrees C. The resistivity data indicated that the electrical basement, to a depth of 900 m, had resistivities ranging from 42 ohm.m to more than 1000 ohm.m, which is considered to be within the

74

Direct-Current Resistivity At Lualualei Valley Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Lualualei Valley Area (Thomas, 1986) Lualualei Valley Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Lualualei Valley Area (Thomas, 1986) Exploration Activity Details Location Lualualei Valley Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Three Schlumberger resistivity soundings were performed in Lualualei Valley (Mattice and Kauahikaua, 1979). K840 Interpretation of the resistivity soundings suggests that the source of the warm water layer within the valley was the dense dike complex associated with the ancient magma chamber of Waianae volcano. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii Retrieved from

75

Direct-Current Resistivity Survey At Lualualei Valley Area (Thomas, 1986) |  

Open Energy Info (EERE)

Lualualei Valley Area (Thomas, 1986) Lualualei Valley Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Lualualei Valley Area (Thomas, 1986) Exploration Activity Details Location Lualualei Valley Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness useful DOE-funding Unknown Notes Three Schlumberger resistivity soundings were performed in Lualualei Valley (Mattice and Kauahikaua, 1979). K840 Interpretation of the resistivity soundings suggests that the source of the warm water layer within the valley was the dense dike complex associated with the ancient magma chamber of Waianae volcano. References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii

76

Field Mapping At Lualualei Valley Area (Thomas, 1986) | Open...  

Open Energy Info (EERE)

primarily toward identifying the lithology and structure of the Waianae caldera (Sinton, 1979). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment...

77

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"

78

Gas Flux Sampling At Lualualei Valley Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Gas Flux Sampling At Lualualei Valley Area (Thomas, 1986) Gas Flux Sampling At Lualualei Valley Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Lualualei Valley Area (Thomas, 1986) Exploration Activity Details Location Lualualei Valley Area Exploration Technique Gas Flux Sampling Activity Date Usefulness useful DOE-funding Unknown Notes Soil mercury and radon emanation surveys were performed over much of the accessible surface of Lualualei Valley (Cox and Thomas, 1979). The results of these surveys (Figs 7 and 8) delineated several areas in which soil mercury concentrations or radon emanation rates were substantially above normal background values. Some of these areas were apparently coincident with the mapped fracture systems associated with the caldera boundaries.

79

Direct-Current Resistivity At Honokowai Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Honokowai Area (Thomas, 1986) Honokowai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Honokowai Area (Thomas, 1986) Exploration Activity Details Location Honokowai Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not useful DOE-funding Unknown Notes Three Schlumberger resistivity surveys were attempted on the alluvial plain around Honokowai (Fig. 22). Two of the soundings penetrated to a moderate-resistivity basement, interpreted to be seawater-saturated basalt, whereas the other sounding encountered a high-resistivity intermediate layer which could not be adequately penetrated to allow resolution of the basement resistivity (Mattice, 1981). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

80

Direct-Current Resistivity Survey At Honokowai Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

Honokowai Area (Thomas, 1986) Honokowai Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Honokowai Area (Thomas, 1986) Exploration Activity Details Location Honokowai Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not useful DOE-funding Unknown Notes Three Schlumberger resistivity surveys were attempted on the alluvial plain around Honokowai (Fig. 22). Two of the soundings penetrated to a moderate-resistivity basement, interpreted to be seawater-saturated basalt, whereas the other sounding encountered a high-resistivity intermediate layer which could not be adequately penetrated to allow resolution of the basement resistivity (Mattice, 1981). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

Note: This page contains sample records for the topic "rift area thomas" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
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81

Mercury Vapor At Lahaina-Kaanapali Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Mercury Vapor At Lahaina-Kaanapali Area (Thomas, 1986) Mercury Vapor At Lahaina-Kaanapali Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Mercury Vapor At Lahaina-Kaanapali Area (Thomas, 1986) Exploration Activity Details Location Lahaina-Kaanapali Area Exploration Technique Mercury Vapor Activity Date Usefulness not indicated DOE-funding Unknown Notes The soil mercury concentration and radon emanometry patterns observed for the Lahaina prospect were similar to those found in Olowalu. Several localized zones of high mercury concentration or enhanced radon emanation were observed, but showed little relationship to each other or to the recognized geologic structure in the area. The data were interpreted to suggest that there might be a small thermal anomaly to the northeast of the

82

Gas Flux Sampling At Lahaina-Kaanapali Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Gas Flux Sampling At Lahaina-Kaanapali Area (Thomas, 1986) Gas Flux Sampling At Lahaina-Kaanapali Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Lahaina-Kaanapali Area (Thomas, 1986) Exploration Activity Details Location Lahaina-Kaanapali Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not indicated DOE-funding Unknown Notes The soil mercury concentration and radon emanometry patterns observed for the Lahaina prospect were similar to those found in Olowalu. Several localized zones of high mercury concentration or enhanced radon emanation were observed, but showed little relationship to each other or to the recognized geologic structure in the area. The data were interpreted to suggest that there might be a small thermal anomaly to the northeast of the

83

Gas Flux Sampling At Mokapu Penninsula Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Gas Flux Sampling At Mokapu Penninsula Area (Thomas, 1986) Gas Flux Sampling At Mokapu Penninsula Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not useful DOE-funding Unknown Notes The high degree of cultural activity (e.g. residential areas, streets, jet runways, etc.) on Mokapu both limited the extent of the soil geochemical surveys performed and rendered their interpretation much more difficult. Soil mercury concentrations and radon emanometry data on the peninsula showed a few localized high values (Figs 13, 14), but no consistent correlation between the anomalous zones and geologic features could be

84

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

Open Energy Info (EERE)

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

85

Direct-Current Resistivity At Kawaihae Area (Thomas, 1986) | Open Energy  

Open Energy Info (EERE)

Kawaihae Area (Thomas, 1986) Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes In addition to the aeromagnetic data, the field survey program in Kawaihae included six Schlumberger resistivity soundings between Kawaihae and Waimea (Kauahikaua and Mattice, 1981). The results of these sounding (Fig. 35) detected apparent resistivity differences in the surface rock depending on whether the soundings were done on Kohala or Mauna Kea lavas (Figs 36, 37), whereas uniform resistivities of 650- 850 ohm.m were found at depths of

86

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

Open Energy Info (EERE)

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

87

Direct-Current Resistivity At Lahaina-Kaanapali Area (Thomas, 1986) | Open  

Open Energy Info (EERE)

At Lahaina-Kaanapali Area At Lahaina-Kaanapali Area (Thomas, 1986) Exploration Activity Details Location Lahaina-Kaanapali Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Four Schlumberger soundings were performed along the coastal strip adjacent to Lahaina town (Fig. 22). Three of the four soundings were able to detect a moderate to low-resistivity basement that was interpreted to be basalt saturated with seawater at 20degrees C (Mattice, 1981). None of the resistivity sounding data in this area indicated subsurface resistivities lower than could be accounted for by local ambient temperatures (Mattice and Lienert, 1980). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In Hawaii

88

Gas Flux Sampling At Kawaihae Area (Thomas, 1986) | Open Energy Information  

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 Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Gas Flux Sampling At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Gas Flux Sampling Activity Date Usefulness not useful DOE-funding Unknown Notes The soil geochemistry yielded quite complex patterns of mercury concentrations and radonemanation rates within the survey area (Cox and Cuff, 1981c). Mercury concentrations (Fig. 38) showed a general minimum along the Kawaihae-Waimea roads and a broad trend of increasing mercury

89

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

Open Energy Info (EERE)

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

90

Direct-Current Resistivity Survey At Lahaina-Kaanapali Area (Thomas, 1986)  

Open Energy Info (EERE)

Survey At Survey At Lahaina-Kaanapali Area (Thomas, 1986) Exploration Activity Details Location Lahaina-Kaanapali Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Four Schlumberger soundings were performed along the coastal strip adjacent to Lahaina town (Fig. 22). Three of the four soundings were able to detect a moderate to low-resistivity basement that was interpreted to be basalt saturated with seawater at 20degrees C (Mattice, 1981). None of the resistivity sounding data in this area indicated subsurface resistivities lower than could be accounted for by local ambient temperatures (Mattice and Lienert, 1980). References Donald M. Thomas (1 January 1986) Geothermal Resources Assessment In

91

Direct-Current Resistivity Survey At Kawaihae 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 Survey At Kawaihae Area (Thomas, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Kawaihae Area (Thomas, 1986) Exploration Activity Details Location Kawaihae Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes In addition to the aeromagnetic data, the field survey program in Kawaihae included six Schlumberger resistivity soundings between Kawaihae and Waimea (Kauahikaua and Mattice, 1981). The results of these sounding (Fig. 35)

92

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

93

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...

94

Direct-Current Resistivity Survey At Mokapu Penninsula Area (Thomas, 1986)  

Open Energy Info (EERE)

Direct-Current Resistivity Survey At Mokapu Direct-Current Resistivity Survey At Mokapu Penninsula Area (Thomas, 1986) Exploration Activity Details Location Mokapu Penninsula Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Geophysical surveys on Mokapu were restricted to three Schlumberger soundings (Fig. 17). The results of these soundings appeared to indicate a highly resistive surface section underlain by one or more layers of intermediate to low resistivity (Fig. 18). Basement resistivities in all cases were less than 3 ohm.m and were interpreted to correspond to alluvial layers saturated with cold seawater (Lienert, 1982). --- A separate geophysical analysis performed on the Koolau caldera area (Kauahikaua, 1981 a) synthesized existing self-potential, gravity, seismic and aeromagnetic

95

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

96

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

97

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

98

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

99

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

100

NREL: Biomass Research - Thomas Foust  

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

Thomas Foust Thomas Foust Photo of Thomas Foust Dr. Thomas Foust is an internationally recognized expert in the biomass field. His areas of expertise include feedstock production, biomass-to-fuels conversion technologies, and environmental and societal sustainability issues associated with biofuels. He has more than 20 years of research and research management experience, specializing in biomass feedstocks and conversion technologies. As National Bioenergy Center Director, Dr. Foust guides and directs NREL's research efforts to develop biomass conversion technologies via biochemical and thermochemical routes, as well as critical research areas addressing the sustainability of biofuels. This research focuses on developing the necessary science and technology for converting biomass to biofuels,

Note: This page contains sample records for the topic "rift area thomas" 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

Optical Diagnostics Thomas Tsang  

E-Print Network [OSTI]

Optical Diagnostics Thomas Tsang · tight environment · high radiation area · non-serviceable area · passive components · optics only, no active electronics · transmit image through flexible fiber bundle #12;New imaging fiber bundle Core size: 12 µm, diameter: 1/8" Optical Diagnostics Total fiber counts ~50

McDonald, Kirk

102

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

103

NREL: Energy Analysis - Thomas Jenkin  

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

Thomas Jenkin Thomas Jenkin Photo of Thomas Jenkin. Thomas Jenkin is a member of the Washington D.C. Office in the Strategic Energy Analysis Center. Senior Energy Analyst On staff since August 2004 Phone number: 202-488-2219 E-mail: thomas.jenkin@nrel.gov Areas of expertise Valuation and risk management Market structure and operation of natural gas and power markets Economic analysis of storage technologies Research and development (R&D) Primary research interests R&D and commercialization of energy technologies Risk and uncertainty The value of storage Economic and market analysis of renewable energy technologies Education and background training MPPM, Yale School of Management D.Phil. in physics, University of Oxford B.Sc. in physics, University of Bristol Teaching experience

104

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

105

Thomas Kirchstetter  

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

Thomas Kirchstetter Thomas Kirchstetter Sustainable Energy Systems Group Lawrence Berkeley National Laboratory 1 Cyclotron Road MS 70R0108B Berkeley CA 94720 Office Location: 90-2024J (Office), 70-215 (Lab) (510) 486-7071 TWKirchstetter@lbl.gov Dr. Kirchstetter is a Staff Scientist at Lawrence Berkeley National Laboratory, where he is a Deputy Leader in the Sustainable Energy Systems Group and a member of the Heat Island Group. He studies the role of particulate matter in the environment as it relates to energy use, climate, and air quality. He has more than 50 refereed archival journal papers and holds a concurrent appointment at the University of California, Berkeley as an Associate Adjunct Professor in the Civil and Environmental Engineering Department. Tom's current research interests include:

106

Monroe Thomas, Mechanical Technician  

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

Monroe Thomas, Mechanical Technician Print The weekend before the ALS was scheduled to start up again after the most recent shutdown, mechanical technician Monroe Thomas kept...

107

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...

108

Thomas Richardson  

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

Richardson Richardson Electrochemical Technologies Group Lawrence Berkeley National Laboratory 1 Cyclotron Road MS 62-0203 Berkeley CA 94720 Office Location: 62-0321 (510) 486-8619 TJRichardson@lbl.gov This publications database is an ongoing project, and not all Division publications are represented here yet. Publications 2012 Liu, Xiaosong, Jun Liu, Ruimin Qiao, Yan Yu, Hong Li, Liumin Suo, Yong-sheng Hu, Yi-De Chuang, Guojiun Shu, Fangcheng Chou et al. "Phase Transformation and Lithiation Effect on Electronic Structure of LixFePO4: An In-Depth Study by Soft X-ray and Simulations." Journal of the American Chemical Society 134, no. 33 (2012): 13708-13715. 2011 Chen, Guoying, Alpesh K. Shukla, Xiangyun Song, and Thomas J. Richardson. "Improved Kinetics and Stabilities in Mg-Sybstained Li-MnPO4." J. of

109

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

110

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

111

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

112

NREL: Energy Analysis - Thomas R. Schneider  

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

Thomas R. Schneider Thomas R. Schneider Photo of Thomas R. Schneider Thomas R. Schneider is a member of the Washington D.C. Office in the Strategic Energy Analysis Center. Principal Analyst - Strategic Energy Analysis On staff since March 2009 Phone number: 202-488-2206 E-mail: thomas.schneider@nrel.gov Areas of expertise Distributed generation and storage Advanced power generation and transmission technologies Technology assessment Strategic and scenario planning R&D policy and management Primary research interests Variable renewable resources and the grid Role of electrification in society Energy efficiency and demand response Energy storage Education and background training Ph.D. in physics, University of Pennsylvania B.S., Stevens Institute of Technology (High Honors) Prior work experience

113

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.

114

Iran Thomas Auditorium, 8600  

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

Thursday, December 6, 2012 11:00 am Iran Thomas Auditorium, 8600 1000 Shapes and 1000 Uses of Designer Carbon Nanostructures David Tomnek Physics and Astronomy Department,...

115

Iran Thomas Auditorium, 8600  

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

February 17, 2011 2:00 pm Iran Thomas Auditorium, 8600 Field-Based Simulations for the Design of Polymer Nanostructures Glenn H. Fredrickson Mitsubishi Professor of Chemical...

116

Iran Thomas Auditorium, 8600  

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

April 19, 2013 11:00 am Iran Thomas Auditorium, 8600 New Methods for Controlling the Structures and Functions of Synthetic Polymers Christopher Bielawski University of Texas at...

117

Iran Thomas Auditorium, 8600  

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

August 27, 2010 11:00 am Iran Thomas Auditorium, 8600 Theory of dielectric and ferroelectric properties of ultrathin films and superlattices David Vanderbilt Department of Physics...

118

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

119

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

120

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.

Note: This page contains sample records for the topic "rift area thomas" 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

Western Area Power Administration (WFP) | Department of Energy  

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

future. Western Area Power Administration Responsible Contacts Thomas Wheeler Director, Workforce Analysis & Planning Division E-mail thomas.wheeler@hq.doe.gov Phone (202)...

122

Thomas Johnson | Department of Energy  

Office of Environmental Management (EM)

Thomas Johnson About Us Thomas Johnson - Technical Writer for the Office of Fossil Energy Most Recent An Important Step Forward for CCUS November 20...

123

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

124

Iran Thomas Auditorium, 8600  

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

September 27, 2012 2:00 pm Iran Thomas Auditorium, 8600 Exploring the Physics of Graphene with Local Probes Joseph A. Stroscio Center for Nanoscale Science and Technology, NIST...

125

Iran Thomas Auditorium, 8600  

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

May 3, 2012 4:00 pm Iran Thomas Auditorium, 8600 Understanding the Behavior of Nanoscale Magnetic Heterostructures: How Microscopy Can Help Amanda K. Petford-Long Center for...

126

Iran Thomas Auditorium, 8600  

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

October 5, 2012 11:00 am Iran Thomas Auditorium, 8600 Role of van der Waals Interactions in Physics, Chemistry, and Biology Matthias Scheffler Fritz-Haber-Institut der...

127

Pilar Thomas | Department of Energy  

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

Pilar Thomas Pilar Thomas About Us Pilar Thomas - Deputy Director, Office of Indian Energy Policy and Programs Pilar Thomas Pilar Thomas (Pascua Yaqui) is the Deputy Director in the Office of Indian Energy Policy and Programs. As Deputy Director, Ms. Thomas assists the Director in developing national energy policy and programs related to Indian energy development. Ms. Thomas is also responsible for developing and implementing policy efforts within the Department and federal government to achieve the Office's Indian Energy policy objectives. Prior to joining the Department, Ms. Thomas served as the Deputy Solicitor for Indian Affairs in the U.S. Department of the Interior. Appointed as Deputy Solicitor in September 2009, Ms. Thomas was responsible for providing day to day legal advice and counsel to the Secretary, the

128

St. Thomas More College St. Thomas More College (STM)  

E-Print Network [OSTI]

leaders that will, in turn, build a more just and sustainable society. For those who so desire, we offerSt. Thomas More College #12;St. Thomas More College (STM) You can take STM classes as part of your U of S degree program even if you are not an STM student. 2 | St. Thomas More College University

Saskatchewan, University of

129

Thomas Wheeler | Department of Energy  

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

Description Departmental staffing budget; PMA scorecard; hiring metrics Last Name Wheeler First Name THomas Title Director, Workforce Analysis & Planning Division...

130

The Terry Thomas  

High Performance Buildings Database

Seattle, WA The Terry Thomas was designed to provide a healthy and creative work environment that would illustrate the possibilities of sustainable design. The project was driven by a future tenant who needed a new office space to accommodate a rapidly expanding architectural practice. The firm wanted to remain in the same neighborhood where it had operated for seventeen years, yet in a building that would exemplify commitment to sustainable design. The Terry Thomas is located in Seattle's up-and-coming South Lake Union neighborhood, adjacent to downtown.

131

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

132

Thomas Weaver art director  

E-Print Network [OSTI]

, G'04, Jeff Wakefield photography Steven Alvarez, Raj Chawla, Alain Denis, Michael Lewis, Shayne Lynn Theresa Miller Vermont Quarterly 86 South Williams Street Burlington, VT 05401 (802) 656-1100 theresa South Williams Street Burlington, VT 05401 (802) 656-2005 thomas.weaver@uvm.edu vermont Quarterly

Hayden, Nancy J.

133

Thomas Reddinger Director, Steam  

E-Print Network [OSTI]

Thomas Reddinger Director, Steam Operations Steven Richards Assistant Manager of Maintenance Supervisor (Distribution) Deborah Moorhead Office Coordinator III Martin Bower Steam Plant Operator Richard Redfield Steam Plant Operator SU Steam Station/Chilled Water Plant Bohdan Sawa Steam Plant Operator Robert

McConnell, Terry

134

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

135

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

136

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

137

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

138

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

139

Mr. Thomas Dwyer  

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

Thomas Dwyer Thomas Dwyer 5007 Clarevalley Drive Cincinnati, OH 45238 Dear Mr. Dwyer: Department of Energy Washington, DC 20585 OCT -4 2000 Re: OHA Case No. VBB-0005 This letter concerns the complaint of reprisal that you submitted to the Department of Energy under 10 C.F.R. Part 708. You have filed a petition for Secretarial review of the appeal decision issued to you on July 24, 2000. The Part 708 regulations applicable to the petition provide that the Secretary will reverse or revise an appeal decision by the Director of the Office of Hearings and Appeals only under extraordinary circumstances. 10 C.F.R. § 708.35(d). After fully evaluating all the issues that you raised in your filing dated September 8, 2000, I have determined that you have not shown that

140

Thomas B. Watson | BNL  

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

Thomas B. Watson Thomas B. Watson Chemist Watson is a Chemist and has been the leader of the Tracer Technology Group for 7 years. He has more than 21 years experience in atmospheric transport and dispersion research using intentionally released tracer compounds. His research has been focused on the processes of short- and long-range atmospheric diffusion, dispersion, and transport, and on the chemical transformation of natural and anthropogenic compounds in the atmosphere. Most of his work has been in the design, execution, and interpretation of field measurement programs and has been used in the development of predictive tools for the national security and emergency response communities. He has supervised tracer, release, sampling, and analysis for two field campaigns for Urban Dispersion Program and four programs for the

Note: This page contains sample records for the topic "rift area thomas" 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

BNL | Thomas Roser  

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

Roser Roser Thomas Roser Chair of the Collider-Accelerator Department photo of Thomas Roser With about 400 employees and an annual budget of $140 million, C-AD develops, improves and operates a suite of accelerators used for experiments by an international community of about 1,500 scientists. The department also designs and constructs new accelerators in support of the Laboratory's and national missions. Roser earned a Ph.D. in physics from the Swiss Federal Institute of Technology in Zurich in 1984. He became a research fellow at the University of Michigan in the same year and was appointed assistant professor of physics at the university in 1990. He joined Brookhaven Lab as an associate physicist in 1991, and, in 1994, he became the head of the Accelerator Division for Brookhaven's Alternating Gradient Synchrotron Department,

142

Automatic Fracture Reduction Thomas Albrecht and Thomas Vetter  

E-Print Network [OSTI]

Automatic Fracture Reduction Thomas Albrecht and Thomas Vetter University of Basel Abstract. We segmented from CT scans. The result of this virtual fracture reduction is intended to be used an operation plan. We propose to achieve automatic fracture reduction by fitting the bone fragments

Vetter, Thomas

143

Thomas Jefferson National Accelerator Facility Technology Marketing...  

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

Thomas Jefferson National Accelerator Facility Technology Marketing Summaries Here you'll find marketing summaries for technologies available for licensing from the Thomas...

144

Thomas Johnson, Jr | Department of Energy  

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

Thomas Johnson, Jr About Us Thomas Johnson, Jr, Director - Office of Environmental Management's Recovery Act Program Most Recent Celebrating Successes of Environmental Management...

145

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

146

NREL: Energy Sciences - Thomas Gennett  

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

Thomas Gennett Thomas Gennett Senior Scientist Photo of Thomas Gennett Phone: (303) 384-6628 Email: thomas.gennett@nrel.gov Thomas Gennett is currently a senior scientist at NREL and holds Professor Emeritus of Chemistry and Materials Science status with the Rochester Institute of Technology (RIT). At NREL, Dr. Gennett leads three distinct projects. One focuses on the mechanism of room temperature hydrogen adsorption for carbon based sorbents, the second on the development of advanced materials for direct methanol fuel cell anode catalysts, and the third on development of next generation transparent conductive oxides (TCOs) for photovoltaic applications. Previously, while a Professor at RIT, he was co-founder and director (2001-2003) of the highly successful NanoPower Research Laboratory. Dr. Gennett has had a strong collaboration

147

Thomas Edison | Department of Energy  

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

Thomas Edison Thomas Edison Tesla vs. Edison 62 likes Thomas Edison Inventor Known as "The Wizard of Menlo Park," Edison was an American inventor who developed the first commercially practical incandescent light bulb. A savvy businessman, he invented a number of other technologies that are still in use today -- including the an early stock ticker, a sound-recording phonograph and a two-way telegraph -- and holds the record for the most patents, ever. Learn more interesting facts about Edison in our Top 8 Things You Didn't Know About Thomas Alva Edison. Innovators Sort by: Random | Alphabetical | Rating (High to Low) | Rating (Low to High) Nikola Tesla Inventor 435 likes Nikola Tesla was born in the Austrian Empire (now Croatia) but moved to the United States to work for Thomas Edison

148

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...

149

Thomas D. Williams Assistant Administrator  

Gasoline and Diesel Fuel Update (EIA)

Thomas D. Williams Thomas D. Williams Assistant Administrator for Resource and Tecnology Management Duties Thomas D. Williams is the Assistant Administrator for Resource & Technology Management. He provides leadership and direction to oversee the management and operation of EIA's employee services, information technology policy and operations, and integrated planning, budget, procurement, evaluation and project management activity. Biography Thom is a career member of the Senior Executive Service with more than 27 years of professional experience in developing, linking, and implementing successful strategic, financial, human capital, operational, technology, and administrative policies and plans for federal research, science, engineering, and regulatory programs.

150

Iran Thomas Auditorium, 8600  

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

1, 2012 1, 2012 4:00 pm Iran Thomas Auditorium, 8600 Simulating the Formation of Carbonate Minerals: The Role of Nanoscale Phenomena in Non-Classical Nucleation Julian Gale Nanochemistry Research Institute Department of Chemistry, Curtin University, Australia CNMS D D I I S S C C O O V V E E R R Y Y SEMINAR SERIES Abstract: Calcium carbonate is an abundant mineral that exhibits three crystalline polymorphs, as well as an amorphous form, and represents a natural form of sequestered carbon. While the most stable calcite polymorph can grow as macroscopic single crystals, the process of biomineralisation can alternatively lead to complex polycrystalline assembles that serve as functional materials in nature. As such, the

151

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

152

AREA  

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

AREA AREA FAQ # Question Response 316 vs DCAA FAQ 1 An inquiry from CH about an SBIR recipient asking if a DCAA audit is sufficient to comply with the regulation or if they need to add this to their audit they have performed yearly by a public accounting firm. 316 audits are essentially A-133 audits for for-profit entities. They DO NOT replace DCAA or other audits requested by DOE to look at indirect rates or incurred costs or closeouts. DCAA would never agree to perform A-133 or our 316 audits. They don't do A-133 audits for DOD awardees. The purpose of the audits are different, look at different things and in the few instances of overlap, from different perspectives. 316

153

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...

154

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...

155

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

156

Thomas M. Stricker Currivitae Page 1 of 4 Name: Thomas Martin Stricker  

E-Print Network [OSTI]

Thomas M. Stricker Currivitae Page 1 of 4 Name: Thomas Martin Stricker Born: June 6, 1963 supercomputer, developed as a joint project of CMU, ARPA, SPAWAR and Intel Corporation. Thomas M. Stricker­2580 tomstr@cs.cmu.edu Curriculum vitae March 5, 1996 #12; Thomas M. Stricker Currivitae Page 2 of 4 1991

Shewchuk, Jonathan

157

Iran Thomas Auditorium, 8600  

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

Dieter Richter Jlich Centre for Neutron Science, Institute for Complex Systems, Germany Filling soft polymer matrices with nanoparticles with high specific surface area...

158

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.

159

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"

160

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

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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

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...

162

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

163

Curriculum Vitae THOMAS K. GREEN  

E-Print Network [OSTI]

Curriculum Vitae THOMAS K. GREEN Professor of Chemistry ADDRESS PERSONAL Department of Chemistry SUPPORT Principal Investigator 1985 "Coal Swelling in Amine Solvents" Exxon Education Foundation, $15,000, 1985. 1986 "Thermodynamics of Coal-Solvent Interactions" Research Corporation, $17,600, 1986. 1987

164

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

165

Mr. Thomas Mahl Granite City Steel Company  

Office of Legacy Management (LM)

8&v/ 8&v/ Mr. Thomas Mahl Granite City Steel Company 20th and State Streets Granite City, IL 62040 Dear Mr. Mahl: This is to notify you that the U.S. Department of Energy (DOE) has designated your company's facility for remedial action as a part of the Formerly Utilized Sites Remedial Action Program. Remedial activities are managed by the DOE Oak Ridge Field Office, and Ms. Teresa Perry (615-576-8956) will be the site manager. As a result of the designation decision, Ms. Perry will be the appropriate point of contact in the future. If you have any questions, please call me at 301-903-8149. W. Alexander Williams, PhD Designation and Certification Manager Division of Off-Site Programs Office of Eastern Area Programs Office of Environmental Restoration

166

John Thomas - Research Staff - FEERC  

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

John Thomas John Thomas R&D Staff Member Specialty: Automotive Fuel Economy, Emissions, and Aftertreatment John began his career at Oak Ridge National Laboratory in 1978 and has broad experience in fossil energy technology, fuels, combustion, energy conversion, combined heat and power and power generation systems. His most recent R&D efforts include the effects of intermediate ethanol fuel blends on the legacy vehicle fleet and non-road engines, ethanol/gasoline blend engine and vehicle performance and exploring emerging fuel and/or petroleum saving technologies on vehicles. Other recent work includes R&D involving a range of diesel exhaust emissions aftertreatment technologies including soot filters, NOx adsorber catalysts, hydrocarbon SCR, and urea

167

Independent Oversight Inspection, Thomas Jefferson National Accelerator  

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

Thomas Jefferson National Thomas Jefferson National Accelerator Facility - August 2008 Independent Oversight Inspection, Thomas Jefferson National Accelerator Facility - August 2008 August 2008 Inspection of Environment, Safety and Health Programs at the Thomas Jefferson National Accelerator Facility The U.S. Department of Energy (DOE) Office of Independent Oversight, within the Office of Health, Safety and Security (HSS), inspected environment, safety, and health (ES&H) programs at the DOE Thomas Jefferson Site Office (TJSO) and the Thomas Jefferson National Accelerator Facility (TJNAF) during May through July 2008. The ES&H inspection was performed by Independent Oversight's Office of Environment, Safety and Health Evaluations. In coordination with TJSO, TJNAF has taken a number of actions to develop a

168

Thomas selected as American Chemical Society Fellow  

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

Chemistry Division. Thomas received degrees from Middlebury College and-as a student of Glenn Seaborg, Nobel Prize winner and discoverer or codiscoverer of many of the actinide...

169

Info-Exch 2012- Thomas Johnson Presentation  

Broader source: Energy.gov [DOE]

EM Recovery Act Program Director Thomas Johnson gave a presentation on Recovery Act lessons learned at the 2012 Recovery Act Information Exchange.

170

Iran Thomas Auditorium, 8600 Environmental Transmission Electron...  

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

April 26, 2012 11:00 am Iran Thomas Auditorium, 8600 Environmental Transmission Electron Microscopy for Catalysis Research: The Example of Carbon Nanotubes Eric A. Stach Center for...

171

Independent Oversight Inspection, Thomas Jefferson National Accelerato...  

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

Jefferson National Accelerator Facility - August 2008 August 2008 Inspection of Environment, Safety and Health Programs at the Thomas Jefferson National Accelerator Facility...

172

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":""}]}

173

VEE-0032- In the Matter of Thomas Oil Company  

Broader source: Energy.gov [DOE]

On September 13, 1996, Thomas Oil Company (Thomas Oil) filed an Application for Exception with the Office of Hearings and Appeals (OHA) of the Department of Energy (DOE). In its application, Thomas...

174

Thomas Jefferson High School for Science & Technology National...  

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

Thomas Jefferson High School for Science & Technology National Science Bowl Champion Thomas Jefferson High School for Science & Technology National Science Bowl Champion May 2,...

175

Thomas Edison vs. Nikola Tesla | Department of Energy  

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

Thomas Edison vs. Nikola Tesla Thomas Edison vs. Nikola Tesla Addthis Duration 46:00 Topic Alternative Fuel Vehicles Renewables Smart Grid Transmission...

176

Optical Diagnostics Hg_jet_meeting, 01-18-05 Thomas Tsang  

E-Print Network [OSTI]

Optical Diagnostics Hg_jet_meeting, 01-18-05 Thomas Tsang · tight environment · high radiation area · non-serviceable area · passive components · optics only, no active electronics · back illuminated with a single fiber laser - pulsed laser X · transmit image through flexible fiber bundle #12;Optical

McDonald, Kirk

177

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

178

Independent Oversight Inspection, Thomas Jefferson National Accelerator Facility- August 2008  

Broader source: Energy.gov [DOE]

Inspection of Environment, Safety and Health Programs at the Thomas Jefferson National Accelerator Facility

179

Property:AreaGeology | Open Energy Information  

Open Energy Info (EERE)

AreaGeology AreaGeology Jump to: navigation, search Property Name AreaGeology Property Type String Description A description of the area geology This is a property of type String. Subproperties This property has the following 22 subproperties: A Amedee Geothermal Area B Beowawe Hot Springs Geothermal Area Blue Mountain Geothermal Area Brady Hot Springs Geothermal Area C Chena Geothermal Area Coso Geothermal Area D Desert Peak Geothermal Area D cont. Dixie Valley Geothermal Area E East Mesa Geothermal Area G Geysers Geothermal Area K Kilauea East Rift Geothermal Area L Lightning Dock Geothermal Area Long Valley Caldera Geothermal Area R Raft River Geothermal Area Roosevelt Hot Springs Geothermal Area S Salt Wells Geothermal Area Salton Sea Geothermal Area San Emidio Desert Geothermal Area

180

ORISE: Faculty Research Experiences - Dr. Thomas Liu  

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

Thomas Liu Thomas Liu Professor and student team develops flexible, free alternative to proprietary data analytics software Dr. Thomas Liu and Monty Bains Dr. Thomas Liu and Monty Bains research free web-based data analysis and visualization application as an alternative to common fee-based software. They are participating in the U.S. Department of Homeland Security's Summer Research Team Program for Minority Serving Institutions. The program is administered by the Oak Ridge Institute for Science and Education. Photo courtesy of Tamra Carpenter, Rutgers University. Click image to enlarge. Fifteen years ago people could not imagine the capabilities they would soon have through the Internet and supporting programs. The evolution of web technology moves at such a fast pace that most people focus on keeping pace

Note: This page contains sample records for the topic "rift area thomas" 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

Thomas G. Hinton | Savannah River Ecology Laboratory  

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

Hinton Curriculum Vitae Faculty & Scientists SREL Home Thomas G. Hinton Savannah River Ecology Laboratory P O Drawer E, Aiken, SC 29802 (803) 725-7454 office (803) 725-3309 fax...

182

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"

183

Wister Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

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

184

Truckhaven Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Truckhaven Geothermal Area Truckhaven Geothermal Area (Redirected from Truckhaven Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Truckhaven 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 (1) 9 Exploration Activities (8) 10 References Area Overview Geothermal Area Profile Location: California Exploration Region: Gulf of California Rift Zone 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.

185

Flint Geothermal Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Flint Geothermal Geothermal Area Flint Geothermal Geothermal Area (Redirected from Flint Geothermal Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Flint Geothermal 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: Colorado Exploration Region: Rio Grande Rift 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.

186

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

187

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

188

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

189

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

190

Building Shape Models from Lousy Data Marcel Luthi, Thomas Albrecht, and Thomas Vetter  

E-Print Network [OSTI]

Building Shape Models from Lousy Data Marcel L¨uthi, Thomas Albrecht, and Thomas Vetter Department information. We propose a method for building a statistical shape model from such "lousy" data sets all the intact parts are included in the model. The model building is then performed using the EM

Vetter, Thomas

191

Off-Policy Actor-Critic Thomas Degris thomas.degris@inria.fr  

E-Print Network [OSTI]

Off-Policy Actor-Critic Thomas Degris thomas.degris@inria.fr Flowers Team, INRIA, Talence, ENSTA the first actor-critic al- gorithm for off-policy reinforcement learning. Our algorithm is online work on actor-critic algorithms is lim- ited to the on-policy setting and does not take advantage

Paris-Sud XI, Université de

192

Truckhaven Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Truckhaven Geothermal Area Truckhaven Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Truckhaven 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 (1) 9 Exploration Activities (8) 10 References Area Overview Geothermal Area Profile Location: California Exploration Region: Gulf of California Rift Zone 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

193

Wister Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Wister Geothermal Area Wister Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Wister 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: California Exploration Region: Gulf of California Rift Zone 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

194

Ion beam figuring of small optical components Thomas W. Drueding  

E-Print Network [OSTI]

Ion beam figuring of small optical components Thomas W. Drueding Boston University College of Engineering Aerospace and Mechanical Engineering Department Boston, Massachusetts 02215 Steven C. Fawcett Albuquerque, New Mexico 87107 Thomas G. Bifano Boston University College of Engineering Aerospace

195

Direct Deposit When Message Passing meets Shared Thomas M. Stricker  

E-Print Network [OSTI]

Direct Deposit ­ When Message Passing meets Shared Memory Thomas M. Stricker May 19, 2000 CMU-CS-96 Copyright c by Thomas M. Stricker Supported in part by the Defense Advanced Research Projects Agency

196

Direct Deposit --When Message Passing meets Shared Thomas M. Stricker  

E-Print Network [OSTI]

Direct Deposit -- When Message Passing meets Shared Memory Thomas M. Stricker May 19, 2000 CMU Copyright c flby Thomas M. Stricker Supported in part by the Defense Advanced Research Projects Agency

197

Obsidian Cliff Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Page Page Edit with form History Facebook icon Twitter icon » Obsidian Cliff Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Obsidian Cliff 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: California Exploration Region: Gulf of California Rift Zone 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

198

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

199

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

200

Thomas R. Cech, RNA, and Ribozymes  

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

Thomas R. Cech, RNA, and Ribozymes Resources with Additional Information · Videos Thomas Cech Courtesy of Glenn Asakawa/ University of Colorado Thomas R. Cech conducted ground-breaking research that ‘established that RNA, like a protein, can act as a catalyst in living cells.'1 'Prior to Cech's research, most scientists believed that proteins were the only catalysts in living cells. In 1982, his research group showed that an RNA molecule from Tetrahymena, a single-celled pond organism, cut and rejoined chemical bonds in the complete absence of proteins. This discovery of self-splicing RNA provided the first exception to the long-held belief that biological reactions are always catalyzed by proteins. In 1989, Cech was awarded the Nobel Prize in Chemistry.'2

Note: This page contains sample records for the topic "rift area thomas" 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

2012 Annual Planning Summary for Thomas Jefferson Site Office  

Broader source: Energy.gov [DOE]

The ongoing and projected Environmental Assessments and Environmental Impact Statements for 2012 and 2013 within Thomas Jefferson Site Office.

202

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.

203

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

204

Conformal Mapping in Wing Aerodynamics Thomas Johnson  

E-Print Network [OSTI]

Conformal Mapping in Wing Aerodynamics Thomas Johnson June 4, 2013 Contents 1 Introduction 1 2 the first complete treatment of conformal mapping in aerodynamics. Near the beginning of the twentieth and aerodynamics. The purpose of this exposition is to give the reader an elementary intro- duction to the use

Morrow, James A.

205

On Infinitely Nested Radicals Brian Thomas  

E-Print Network [OSTI]

On Infinitely Nested Radicals Brian Thomas 1. Introduction #12;In "On Infinitely Nested Radicals nested radicals are explored. One example of a nested radical is the Golden Ratio, , which can be written as: (1.1) . . . Many questions arise from the study of nested radicals, such as: 1. What can we say

Morrow, James A.

206

LATTICES IN HYPERBOLIC BUILDINGS ANNE THOMAS  

E-Print Network [OSTI]

LATTICES IN HYPERBOLIC BUILDINGS ANNE THOMAS Introduction This survey is intended as a brief introduction to the theory of hyperbolic buildings and their lattices. Hyperbolic buildings are negatively of these buildings and the lattices in their automorphism groups involves a fascinating mixture of techniques from

Sydney, University of

207

Engineering Light Course instructor: Dr. Thomas Bifano  

E-Print Network [OSTI]

the semester, to untwinkle the stars with adaptive telescopes, to measure the speed of light using parts hacked Experiment: Measuring the speed of light 11/14/12 TBA 11/19/12 No Class 11/26/12 Project interim progressEngineering Light Course instructor: Dr. Thomas Bifano Office: PHO 936 E-mail: tgb@bu.edu Office

Guenther, Frank

208

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

209

MEMORANDUM FROM: THOMAS E. BROWN, DIRECTOR OFFICE OF CONTRACT MANAGEMENT  

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

,2008 ,2008 MEMORANDUM FROM: THOMAS E. BROWN, DIRECTOR OFFICE OF CONTRACT MANAGEMENT OFFICE OF PROCUREMENT AND ASSISTANCE MANAGEMENT SUBJECT: Contract Change Order Administration of Department of Energy Prime Contracts The purpose of this memorandum is to highlight the need for good contract administration of Department of Energy (DOE) contracts (non management and operating contracts) including those covered by DOE Order 413.3A, Program and Project Management for the Acquisition of Capital Assets. One of the focus areas of the DOE's efforts to improve contract and project management is the recopition that effectrve contract change order administration is critical to ensuring that contract and project requirements are met. Fundamentally, the award of an appropriate contract type that best

210

Thomas H. Cormen Charles E. Leiserson  

E-Print Network [OSTI]

-0-262-03384-8 (hardcover : alk. paper)--ISBN 978-0-262-53305-8 (pbk. : alk. paper) 1. Computer programming. 2. Computer algorithms. I. Cormen, Thomas H. QA76.6.I5858 2009 005.1--dc22 2009008593 10 9 8 7 6 5 4 3 2 1 #12 implementation in practice. Parallel computers--computers with multiple processing units--have become

Leiserson, Charles E.

211

aBubbleTree? Thomas H. Parker  

E-Print Network [OSTI]

on Rn \\ {0}. That limit loses energy. A bubble tree is a way of recovering the lost energy by keepingaBubbleTree? Thomas H. Parker 666 NOTICES OF THE AMS VOLUME 50, NUMBER 6 Some of the most important for functions u on a domain in R2, which arises as the variational equation of the energy (2) E(u) = |du|2 dvol

Parker, Thomas H.

212

Thomas-Fermi model: The leading correction  

Science Journals Connector (OSTI)

The correct treatment of strongly bound electrons is grafted smoothly onto the Thomas-Fermi computation of the total binding energy of neutral atoms. This provides a clearcut demonstration of the leading correction of relative order Z-13 which, with effects of relative order Z-23, gives an accurate account of the binding energy over a wide range of Z values. There is a brief discussion of relativistic corrections, with results that are somewhat at variance with previous numerical estimates.

Julian Schwinger

1980-11-01T23:59:59.000Z

213

Thomas-Fermi model: The second correction  

Science Journals Connector (OSTI)

A simple derivation is given for the first quantum correction to the Thomas-Fermi kinetic energy. Its application to the total binding energy of neutral atoms exploits the technique for handling strongly bound electrons that was developed in a preceding paper, and justifies the numerical value of the second correction adopted there. A proposal is made for extrapolating this improved description to the outer regions of the atom.

Julian Schwinger

1981-11-01T23:59:59.000Z

214

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...

215

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

216

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

217

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

218

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...

219

10 Questions for an Automotive Engineer: Thomas Wallner | Department of  

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

10 Questions for an Automotive Engineer: Thomas Wallner 10 Questions for an Automotive Engineer: Thomas Wallner 10 Questions for an Automotive Engineer: Thomas Wallner June 17, 2011 - 3:30pm Addthis Argonne mechanical engineer Thomas Wallner adjusts Argonne's "omnivorous engine," an automobile engine that Wallner and his colleagues have tailored to efficiently run on blends of gasoline, ethanol and butanol. | Courtesy of: Argonne National Laboratory. Argonne mechanical engineer Thomas Wallner adjusts Argonne's "omnivorous engine," an automobile engine that Wallner and his colleagues have tailored to efficiently run on blends of gasoline, ethanol and butanol. | Courtesy of: Argonne National Laboratory. Niketa Kumar Niketa Kumar Public Affairs Specialist, Office of Public Affairs Meet Thomas Wallner - automotive engineer extraordinaire, who hails from

220

Interacting viscous instabilities in microfluidic systems Thomas Cubaud*a  

E-Print Network [OSTI]

Interacting viscous instabilities in microfluidic systems Thomas Cubaud*a and Thomas G. Mason, evolution, and stability of microfluidic flows involving two or more miscible fluids that have different viscosities. When two liquids that have widely different viscosities are injected into a rigid microfluidic

Cubaud, Thomas

Note: This page contains sample records for the topic "rift area thomas" 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

Single element changes in electrical networks Thomas Berger,  

E-Print Network [OSTI]

University of Technology Page 2 / 13 #12;Example: electrical RLC network Z(s)i(s) = vs(s), Z(s) = s-1 1 C1Single element changes in electrical networks Thomas Berger, George Halikias and Nicos Karcanias, 2012 Single element changes in electrical networks Thomas Berger, George Halikias and Nicos Karcanias

Knobloch,Jürgen

222

Single element changes in electrical networks Thomas Berger,  

E-Print Network [OSTI]

, Ilmenau University of Technology Page 2 / 13 #12;Example: electrical RLC network Z(s)i(s) = vs(s), ZSingle element changes in electrical networks Thomas Berger, George Halikias and Nicos Karcanias, February 23, 2012 Single element changes in electrical networks Thomas Berger, George Halikias and Nicos

Knobloch,Jürgen

223

Outdoor Virtual Reality Bruce H. Thomas and Wayne Piekarski  

E-Print Network [OSTI]

Outdoor Virtual Reality Bruce H. Thomas and Wayne Piekarski Wearable Computer Laboratory University of South Australia Mawson Lakes, SA 5095 Australia Bruce.Thomas@unisa.edu.au Wayne@cs.unisa.edu.au ABSTRACT or augmented beyond the user's normal experience, and increase understanding 226Copyright held by the author

Thomas, Bruce

224

Hydrogen Storage -Overview George Thomas, Hydrogen Consultant to SNL*  

E-Print Network [OSTI]

Hydrogen Storage - Overview George Thomas, Hydrogen Consultant to SNL* and Jay Keller, Hydrogen volumetric density of gaseous fuels requires a storage method which compacts the fuel. Hence, hydrogen and cost-effective hydrogen storage? #12;4/14/03 3 Sandia National Laboratories From George Thomas, BES

225

Thomas P. D'Agostino | Department of Energy  

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

Thomas P. D'Agostino Thomas P. D'Agostino About Us Thomas P. D'Agostino - Under Secretary for Nuclear Security & Administrator, National Nuclear Security Administration Photo of Thomas D’Agostino Mr. Thomas Paul D'Agostino was sworn in on August 30, 2007, as the Under Secretary for Nuclear Security and Administrator of the National Nuclear Security Administration (NNSA). On September 3, 2009, President Obama announced that Mr. D'Agostino was his choice to continue serving as the Under Secretary for Nuclear Security and NNSA Administrator. The NNSA plays a critical role in ensuring the security of our Nation by maintaining the safety, security, and effectiveness of the U.S. nuclear weapons stockpile without nuclear testing; reducing the global danger from the proliferation of nuclear weapons and materials; providing the U.S. Navy

226

Fort Bliss Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Fort Bliss Geothermal Area Fort Bliss Geothermal Area (Redirected from Fort Bliss Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Fort Bliss 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 (22) 10 References Area Overview Geothermal Area Profile Location: Texas Exploration Region: Rio Grande Rift 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

227

New River Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

New River Geothermal Area New River Geothermal Area (Redirected from New River Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: New River 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 (13) 10 References Area Overview Geothermal Area Profile Location: California Exploration Region: Gulf of California Rift Zone 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.

228

Obsidian Cliff Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

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

229

Jemez Pueblo Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Jemez Pueblo Geothermal Area Jemez Pueblo Geothermal Area (Redirected from Jemez Pueblo Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Jemez Pueblo 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: New Mexico Exploration Region: Rio Grande Rift 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.

230

Socorro Mountain Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Socorro Mountain Geothermal Area Socorro Mountain Geothermal Area (Redirected from Socorro Mountain Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Socorro Mountain 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 (10) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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.

231

Jemez Mountain Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Jemez Mountain Geothermal Area Jemez Mountain Geothermal Area (Redirected from Jemez Mountain Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Jemez Mountain 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 (3) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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.

232

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

233

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

234

Florida Mountains Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Florida Mountains Geothermal Area Florida Mountains Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Florida Mountains 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: New Mexico Exploration Region: Rio Grande Rift 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

235

Socorro Mountain Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Socorro Mountain Geothermal Area Socorro Mountain Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Socorro Mountain 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 (10) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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

236

Jemez Mountain Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Jemez Mountain Geothermal Area Jemez Mountain Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Jemez Mountain 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 (3) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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

237

Flint Geothermal Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Flint Geothermal Geothermal Area Flint Geothermal Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Flint Geothermal 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: Colorado Exploration Region: Rio Grande Rift 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

238

New River Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

New River Geothermal Area New River Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: New River 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 (13) 10 References Area Overview Geothermal Area Profile Location: California Exploration Region: Gulf of California Rift Zone 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

239

Fort Bliss Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Fort Bliss Geothermal Area Fort Bliss Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Fort Bliss 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 (22) 10 References Area Overview Geothermal Area Profile Location: Texas Exploration Region: Rio Grande Rift 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 Developing Power Projects: 0

240

Jemez Pueblo Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Jemez Pueblo Geothermal Area Jemez Pueblo Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Jemez Pueblo 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: New Mexico Exploration Region: Rio Grande Rift 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

Note: This page contains sample records for the topic "rift area thomas" 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

Administrator Thomas D'Agostino, National Nuclear Security  

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

Thomas D'Agostino, National Nuclear Security Thomas D'Agostino, National Nuclear Security Administration, Addresses United Nations on Nuclear Disarmament | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Administrator Thomas D'Agostino, National Nuclear Security Administration, ... Speech Administrator Thomas D'Agostino, National Nuclear Security

242

Administrator Thomas D'Agostino, National Nuclear Security  

National Nuclear Security Administration (NNSA)

Thomas D'Agostino, National Nuclear Security Thomas D'Agostino, National Nuclear Security Administration, Addresses United Nations on Nuclear Disarmament | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Administrator Thomas D'Agostino, National Nuclear Security Administration, ... Speech Administrator Thomas D'Agostino, National Nuclear Security

243

Thomas Jefferson High School for Science & Technology National Science  

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

Thomas Jefferson High School for Science & Technology National Thomas Jefferson High School for Science & Technology National Science Bowl® Champion Thomas Jefferson High School for Science & Technology National Science Bowl® Champion May 2, 2005 - 12:40pm Addthis WASHINGTON, DC -- "The Incompleteness Theorem" was the answer to a question on mathematics that today clinched the 2005 National Science Bowl® championship for the Thomas Jefferson High School for Science & Technology team from Alexandria, Va. The team received its championship trophy after triumphing over 62 other regional team champions this weekend. The team members are: Logan Kearsley, Matthew Isakowitz, Sam Lederer, Lisa Marrone, Charlotte Seid and coach Sharon Baker. The team also won a research trip to Alaska, three Computer Based Laboratories and $1,000 for their school's science

244

DURBIN, EDWARD G., ANN G. DURBIN, THOMAS J. SMAYDA ...  

Science Journals Connector (OSTI)

Jun 24, 1982 ... Edward G. Durbin, Ann G. Durbin, Thomas J. Smayda, and Peter G. Verity .... Egg production in Acartia. 1201. 0. 0. 26 d: 23. E. 20 t? 17. 0. I lz. 2.

2000-02-09T23:59:59.000Z

245

Thermal cracking in disc brakes Thomas J. Mackin *,1  

E-Print Network [OSTI]

Thermal cracking in disc brakes Thomas J. Mackin *,1 , Steven C. Noe, K.J. Ball, B.C. Bedell, D, or hub, which is connected to the wheel and axle, and an inboard and outboard braking surface

Salvaggio, Carl

246

Choice of Weapons for the Truel Thomas S. Ferguson, UCLA  

E-Print Network [OSTI]

Choice of Weapons for the Truel Thomas S. Ferguson, UCLA 1. Truels. The truel is the extension at each other's. 2. Choosing Weapons for the Shubik Truel 1 #12;In the Shubik truel, contestants A, B

Ferguson, Thomas S.

247

TBU-0082- In the Matter of Thomas L. Townsend  

Broader source: Energy.gov [DOE]

Thomas L. Townsend (Townsend) appeals the dismissal of his complaint of retaliation and request for investigation filed under 10 C.F.R. Part 7081 by the Oak Ridge Operations Office (OR) of the...

248

MEMORANDUM FOR ELIZABETH MONTOYA TRANSITION TEAM FROM THOMAS...  

Energy Savers [EERE]

g December 1, 200S MEMORANDUM FOR ELIZABETH MONTOYA TRANSITION TEAM FROM THOMAS N. PYKE, J CHIEF INFORMATION OFFICER SUBJECT: Follow-up to our meeting this morning Carl Staton...

249

Iran Thomas Auditorium, 8600 Materials For Energy: In Situ Synchrotron...  

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

December 15, 2011 4:00 pm Iran Thomas Auditorium, 8600 Materials For Energy: In Situ Synchrotron X-Ray Studies for Materials Design and Discovery Stephen K. Streiffer Deputy...

250

Iran Thomas Auditorium, 8600 Determination of CO, H  

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

February 9, 2012 4:00 pm Iran Thomas Auditorium, 8600 Determination of CO, H 2 and H 2 O Coverage by XANES on Pt and Au During Water Gas Shift Reaction: Experiment and DFT Modeling...

251

Iran Thomas Auditorium, 8600 Fighting Cancer with Nanoparticle...  

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

October 13, 2011 4:00 pm Iran Thomas Auditorium, 8600 Fighting Cancer with Nanoparticle Medicines Mark E. Davis Chemical Engineering California Institute of Technology CNMS D D I I...

252

A taxonomy of granular partitions Thomas Bittner and Barry Smith  

E-Print Network [OSTI]

A taxonomy of granular partitions Thomas Bittner and Barry Smith Qualitative Reasoning Group. In Smith and Brogaard (2000) the notion of granular partition was introduced as a generalization of David

Forbus, Kenneth D.

253

A Theory of Granular Partitions Thomas Bittner and Barry Smith  

E-Print Network [OSTI]

CHAPTER 7 A Theory of Granular Partitions Thomas Bittner and Barry Smith Institute for Formal of part and whole relations (Smith, 1998) as a framework for ontological theorizing. Mereology is better

Bittner, Thomas

254

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

255

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

256

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"

257

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

258

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

259

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

260

The use of narrative during the Clarence Thomas-Anita Hill hearings October 11, 12, 13, 1991  

E-Print Network [OSTI]

fulfillment of the requirements for the degree of MASTER OF ARTS Approved as to style and content by: John H. Powers (Chair of Committee) Tarla R. Peterson (Member) Valerie Balester (Member) Martin J. Medhurst (Interim Head of Department) August.... John H. Powers There are any number of approaches that could be taken with subject matter with the richness and complexity of the Thomas-Hill Hearings. Therefore, I have limited this study to three main areas, they are: 1) the apparent turning over...

Willson, Marilee

2012-06-07T23:59:59.000Z

Note: This page contains sample records for the topic "rift area thomas" 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

A Large-Scale Deforestation Experiment: Effects of Patch Area  

E-Print Network [OSTI]

A Large-Scale Deforestation Experiment: Effects of Patch Area and Isolation on Amazon Birds Gonçalo,4 Thomas E. Lovejoy1,5 As compared with extensive contiguous areas, small isolated habitat patches lack many species. Some species disappear after isolation; others are rarely found in any small patch

Stouffer, Phil

262

The Nuclear Thomas-Fermi Model  

DOE R&D Accomplishments [OSTI]

The statistical Thomas-Fermi model is applied to a comprehensive survey of macroscopic nuclear properties. The model uses a Seyler-Blanchard effective nucleon-nucleon interaction, generalized by the addition of one momentum-dependent and one density-dependent term. The adjustable parameters of the interaction were fitted to shell-corrected masses of 1654 nuclei, to the diffuseness of the nuclear surface and to the measured depths of the optical model potential. With these parameters nuclear sizes are well reproduced, and only relatively minor deviations between measured and calculated fission barriers of 36 nuclei are found. The model determines the principal bulk and surface properties of nuclear matter and provides estimates for the more subtle, Droplet Model, properties. The predicted energy vs density relation for neutron matter is in striking correspondence with the 1981 theoretical estimate of Friedman and Pandharipande. Other extreme situations to which the model is applied are a study of Sn isotopes from {sup 82}Sn to {sup 170}Sn, and the rupture into a bubble configuration of a nucleus (constrained to spherical symmetry) which takes place when Z{sup 2}/A exceeds about 100.

Myers, W. D.; Swiatecki, W. J.

1994-08-01T23:59:59.000Z

263

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

264

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

265

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

266

Wind Power Opportunities in St. Thomas, USVI: A Site-Specific...  

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

Power Opportunities in St. Thomas, USVI: A Site-Specific Evaluation and Analysis Wind Power Opportunities in St. Thomas, USVI: A Site-Specific Evaluation and Analysis Utilizes a...

267

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

268

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

269

Ground radon survey of a geothermal area in Hawaii | Open Energy  

Open Energy Info (EERE)

radon survey of a geothermal area in Hawaii radon survey of a geothermal area in Hawaii Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Ground radon survey of a geothermal area in Hawaii Abstract Rates of ground radon emanation, inthe Puna geothermal area on the lower east riftof Kilauea volcano, were measured by alpha particle sensitive cellulose nitrate films. The survey successfully defined an area of thermal significance associated with the rift structure,and suggests that a thermally driven ground gas convection system exists within, and peripheralto, the rift. This type of survey was found suitable for the basaltic island environment characteristic of Hawaii and is now used in Hawaii as a routine geothermal exploration technique. Author Malcolm E. Cox Published Journal

270

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

271

Remarks by Administrator Thomas D'Agostino, National Nuclear Security  

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

on NRC International Regulators Conference on Nuclear on NRC International Regulators Conference on Nuclear Security | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Remarks by Administrator Thomas D'Agostino, National Nuclear ... Speech Remarks by Administrator Thomas D'Agostino, National Nuclear Security

272

Remarks by Administrator Thomas D'Agostino, National Nuclear Security  

National Nuclear Security Administration (NNSA)

on NRC International Regulators Conference on Nuclear on NRC International Regulators Conference on Nuclear Security | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Remarks by Administrator Thomas D'Agostino, National Nuclear ... Speech Remarks by Administrator Thomas D'Agostino, National Nuclear Security

273

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

274

San Juan Volcanic Field Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

San Juan Volcanic Field Geothermal Area San Juan Volcanic Field Geothermal Area (Redirected from San Juan Volcanic Field Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: San Juan Volcanic Field 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 (3) 10 References Area Overview Geothermal Area Profile Location: Colorado Exploration Region: Rio Grande Rift 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

275

Fenton Hill Hdr Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Fenton Hill Hdr Geothermal Area Fenton Hill Hdr Geothermal Area (Redirected from Fenton Hill Hdr Area) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Fenton Hill Hdr 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 (26) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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.

276

Labs at-a-Glance: Thomas Jefferson National Accelerator Facility | U.S. DOE  

Office of Science (SC) Website

Thomas Jefferson Thomas Jefferson National Accelerator Facility Laboratories Ames Laboratory Argonne National Laboratory Brookhaven National Laboratory Fermi National Accelerator Laboratory Lawrence Berkeley National Laboratory Oak Ridge National Laboratory Pacific Northwest National Laboratory Princeton Plasma Physics Laboratory SLAC National Accelerator Laboratory Thomas Jefferson National Accelerator Facility Laboratory Policy and Evaluation Safety, Security and Infrastructure Laboratory Science Highlights Contact Information Office of Science U.S. Department of Energy 1000 Independence Ave., SW Washington, DC 20585 P: (202) 586-5430 Labs at-a-Glance: Thomas Jefferson National Accelerator Facility Print Text Size: A A A RSS Feeds FeedbackShare Page Thomas Jefferson National Accelerator Facility Logo

277

Updated 1-12 Thomas H. Killion, Ph.D.  

E-Print Network [OSTI]

of Transition in July 2012. Dr. Killion is responsible for policy, planning, resourcing and execution managementUpdated 1-12 Thomas H. Killion, Ph.D. Director of Transition Office of Naval Research Initially joining ONR, Dr. Killion was the Director, Biometrics Identity Management Agency (BIMA), staring

278

Thomas P. Dee Deputy Assistant Secretary of the Navy  

E-Print Network [OSTI]

in the Office of the Under Secretary of Defense Acquisition, Technology and Logistics. While there he oversaw2/28/2013 Thomas P. Dee Deputy Assistant Secretary of the Navy (Expeditionary Programs and Logistics Management) Office of the Assistant Secretary of the Navy (Research, Development & Acquisition) Mr

279

Geodesic Regression on Riemannian Manifolds P. Thomas Fletcher  

E-Print Network [OSTI]

Geodesic Regression on Riemannian Manifolds P. Thomas Fletcher School of Computing, University a manifold-valued random variable and a real-valued independent parameter. The principle is to fit a geodesic is evaluated as the sum-of-squared geodesic distances from the model to the data, and this provides

Boyer, Edmond

280

Statement of Thomas E. Mason Director, Oak Ridge National Laboratory  

E-Print Network [OSTI]

Statement of Thomas E. Mason Director, Oak Ridge National Laboratory Before the Subcommittee Director of the U.S. Department of Energy's Oak Ridge National Laboratory (ORNL) in Oak Ridge, Tennessee, the Oak Ridge fusion program has drawn on the diverse resources afforded by ORNL's standing

Note: This page contains sample records for the topic "rift area thomas" 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

Thomas Banks Santa Cruz Institue for Particle Physics (SCIPP)  

E-Print Network [OSTI]

PROFESSIONAL PREPARATION Reed College Physics/Math B.A. 1969 Massachusetts Institute of Technology Physics PhThomas Banks Santa Cruz Institue for Particle Physics (SCIPP) UC Santa Cruz Department of Physics of Physics, University of California, Santa Cruz 1989-present Professor of Physics, Rutgers University 1986

California at Santa Cruz, University of

282

The `summation hack' as an outlier model Thomas P. Minka  

E-Print Network [OSTI]

The `summation hack' as an outlier model Thomas P. Minka August 22, 2003 (revised) Abstract The `summation hack' is the ad-hoc replacement of a product by a sum in a probabilistic expression. This hack that the hack does make sense probabilistically, and can be best thought of as replacing an outlier

Minka,Tom

283

Tamara I. Ahrens & Thomas H. Lee Center for Integrated Systems  

E-Print Network [OSTI]

of Electrical Engineering Stanford University Ring Oscillator vs. LC Oscillator Ring Oscillator: Dissipates allTamara I. Ahrens & Thomas H. Lee Center for Integrated Systems Department of Electrical Engineering Stanford University Tamara I. Ahrens Center for Integrated Systems Department of Electrical Engineering

Lee, Thomas H.

284

Learning to Rank and Quadratic Assignment Thomas Mensink  

E-Print Network [OSTI]

Learning to Rank and Quadratic Assignment Thomas Mensink TVPA - XRCE & LEAR - INRIA Grenoble NICTA Sydney, Australia Abstract In this paper we show that the optimization of several ranking of quadratic assignment problems. Both the task of test-time predic- tion of the best ranking and the task

Paris-Sud XI, Université de

285

SIR THOMAS BROWNE: HIS SKULL, PORTRAITS, AND ANCESTRY: INTRODUOTORY NOTE  

Science Journals Connector (OSTI)

......was given in 17.23 by Mr Benjamin Mackerell, Author of the History...Doctor comes from the pen of Mr Benjamin Mackerell, who copied the...following*: "The Late Dr. Jeffery gave notice to Sr. Thomas...this Ins. M.S. Johannis Jeffery S.T.P. etc . Aprilis JErae......

M. L. TILDESLEY; ARTHUR KEITH

1923-08-01T23:59:59.000Z

286

Workshop-based Security Safeguard Selection with AURUM Thomas Neubauer  

E-Print Network [OSTI]

Workshop-based Security Safeguard Selection with AURUM Thomas Neubauer Vienna University functionality by introducing the AURUM Workshop, which allows the selection of efficient safeguards based approach is used for selecting safeguards. This paper extends the functionality of AURUM by introducing

287

Environmental Governance: An Economic Perspective Thomas P. Lyon  

E-Print Network [OSTI]

1 Environmental Governance: An Economic Perspective Thomas P. Lyon Forthcoming in Magali Delmas University Press. 1. Introduction From an economic perspective, it is natural to think of the "demand of as coming from government in the form of legislation and regulation, outcomes of the political process

Lyon, Thomas P.

288

Discriminative frequent subgraph mining with optimality guarantees Marisa Thoma  

E-Print Network [OSTI]

processes, such as active or inactive in an anti- cancer screen, toxic or non-toxic to human beings [21Discriminative frequent subgraph mining with optimality guarantees Marisa Thoma Hong Cheng Arthur July 7, 2010 Abstract The goal of frequent subgraph mining is to detect subgraphs that frequently occur

Kriegel, Hans-Peter

289

ELECTRONIC ATTACKS Thomas M. Chen, Southern Methodist University  

E-Print Network [OSTI]

1 Chapter 74 ELECTRONIC ATTACKS Thomas M. Chen, Southern Methodist University Matthew C. Elder An understanding of electronic attacks is an essential prerequisite to building strong cyber defenses. This chapter gives an overview of the major electronic attacks encountered today, proceeding through the basic steps

Chen, Thomas M.

290

Curriculum Vitae Donald Thomas Lysle, Ph.D.  

E-Print Network [OSTI]

Curriculum Vitae Donald Thomas Lysle, Ph.D. Kenan Distinguished Professor Behavioral Neuroscience-962-2537 University of North Carolina Email: dlysle@email.unc.edu Chapel Hill, NC 27599-3270 Education Ph.D Abuse Research Grant (Renewal of R01-DA-13371): Behavioral Factors in Heroin's Effect on Nitric Oxide

Crews, Stephen

291

Thomas Drugman PhD student -FNRS research Fellow  

E-Print Network [OSTI]

Thomas Drugman PhD student - FNRS research Fellow Affiliation TCTS Lab - FPMs Mons Belgium/emotive speech production from the initial trained system. The key idea of a HMM-based synthesizer is to generate situations. Indeed contextual factors such as stress-related, locational, syntaxical or phone identity

Dupont, Stéphane

292

Deep Web Integration with VisQI Thomas Kabisch  

E-Print Network [OSTI]

Deep Web Integration with VisQI Thomas Kabisch Humboldt-Universit¨at zu Berlin Berlin, Germany of Deep Web sources. Building sys- tems which would be able to automatically use all or a large fraction of all Deep Web sources of a given domain, such as airline reservation in the USA, would offer great

Meng, Weiyi

293

Human Factors Aspects of Power System Voltage Visualizations Douglas A. Wiegmann Aaron M. Rich Thomas J. Overbye Yan Sun  

E-Print Network [OSTI]

Thomas J. Overbye Yan Sun Institute of Aviation Institute of Aviation Elect. & Comp. Eng. Elect. & Comp

294

Fenton Hill Hdr Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Fenton Hill Hdr Geothermal Area Fenton Hill Hdr Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Fenton Hill Hdr 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 (26) 10 References Area Overview Geothermal Area Profile Location: New Mexico Exploration Region: Rio Grande Rift 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

295

San Juan Volcanic Field Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

San Juan Volcanic Field Geothermal Area San Juan Volcanic Field Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: San Juan Volcanic Field 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 (3) 10 References Area Overview Geothermal Area Profile Location: Colorado Exploration Region: Rio Grande Rift 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

296

Twenty-Nine Palms Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Twenty-Nine Palms Geothermal Area Twenty-Nine Palms Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Twenty-Nine Palms 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: California Exploration Region: Gulf of California Rift Zone 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

297

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

298

Chocolate Mountains Geothermal Area | Open Energy Information  

Open Energy Info (EERE)

Chocolate Mountains Geothermal Area Chocolate Mountains Geothermal Area Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Resource Area: Chocolate Mountains 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 Map: Chocolate Mountains Geothermal Area Chocolate Mountains Geothermal Area Location Map Area Overview Geothermal Area Profile Location: California Exploration Region: Gulf of California Rift Zone GEA Development Phase: Phase II - Resource Exploration and Confirmation Coordinates: 33.352°, -115.353° Loading map... {"minzoom":false,"mappingservice":"googlemaps3","type":"ROADMAP","zoom":14,"types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"geoservice":"google","maxzoom":false,"width":"600px","height":"350px","centre":false,"title":"","label":"","icon":"","visitedicon":"","lines":[],"polygons":[],"circles":[],"rectangles":[],"copycoords":false,"static":false,"wmsoverlay":"","layers":[],"controls":["pan","zoom","type","scale","streetview"],"zoomstyle":"DEFAULT","typestyle":"DEFAULT","autoinfowindows":false,"kml":[],"gkml":[],"fusiontables":[],"resizable":false,"tilt":0,"kmlrezoom":false,"poi":true,"imageoverlays":[],"markercluster":false,"searchmarkers":"","locations":[{"text":"","title":"","link":null,"lat":33.352,"lon":-115.353,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

299

Remarks by Administrator Thomas D'Agostino, National Nuclear Security  

National Nuclear Security Administration (NNSA)

to the Energy Facility Contractors Group | National Nuclear to the Energy Facility Contractors Group | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Remarks by Administrator Thomas D'Agostino, National Nuclear ... Speech Remarks by Administrator Thomas D'Agostino, National Nuclear Security Administration, to the Energy Facility Contractors Group

300

Mr. Richard T. Thomas General Counsel for Petroleum Operations  

Office of Legacy Management (LM)

j&,J"[Di-' JAQ--- j&,J"[Di-' JAQ--- hl 3. ) :j .I Y ' ! <' Department of Energy Washington, D.C. 20545 NOV 1 1984 Mr. Richard T. Thomas General Counsel for Petroleum Operations P.O. Box 391 Ashland, Kentucky 41114 Dear Mr. Thomas: I am enclosing a copy of the radiological survey report for the Ashland Oil Company (former Haist property), Tonawanda, New York (Enclosure l), which was conducted in July 1976 (copies were sent to your Buffalo, New York, office on August 17, 1978). The results of the survey indicate levels of radioactive contamination above current guidelines. As noted in the report, the radioactive residues on the site do not pose a health hazard provided they (the residues) were not disturbed in the past or will not be disturbed in the future; i.e.,

Note: This page contains sample records for the topic "rift area thomas" 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

Thomas County, Georgia: Energy Resources | Open Energy Information  

Open Energy Info (EERE)

Thomas County, Georgia: Energy Resources Thomas County, Georgia: Energy Resources Jump to: navigation, search Equivalent URI DBpedia Coordinates 30.8417409°, -83.8473015° 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":30.8417409,"lon":-83.8473015,"alt":0,"address":"","icon":"","group":"","inlineLabel":"","visitedicon":""}]}

302

Thomas Jefferson Site Office Homepage | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Home Home Thomas Jefferson Site Office (TJSO) TJSO Home About Current Projects Contract Management Environment, Safety and Health (ES&H) Resources Contact Information Thomas Jefferson Site Office U.S. Department of Energy 12000 Jefferson Avenue Newport News, VA 23606 P: (757) 269-7140 Thomas Jefferson Site Office Pictured Right: Thomas Jefferson Site Office Staff TJSO Staff Photo 1 of 2 Print Text Size: A A A RSS Feeds FeedbackShare Page The Thomas Jefferson Site Office (TJSO) is an organization within the U.S. Department of Energy's Office of Science with responsibility to oversee and manage the Management and Operating (M&O) contract for the Thomas Jefferson National Accelerator Facility (TJNAF) in Newport News, Virginia. TJNAF is one of ten Office of Science Laboratories and is a single program

303

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

304

Generalized charge-screening in relativistic ThomasFermi model  

SciTech Connect (OSTI)

In this paper, we study the charge shielding within the relativistic Thomas-Fermi model for a wide range of electron number-densities and the atomic-number of screened ions. A generalized energy-density relation is obtained using the force-balance equation and taking into account the Chandrasekhar's relativistic electron degeneracy pressure. By numerically solving a second-order nonlinear differential equation, the Thomas-Fermi screening length is investigated, and the results are compared for three distinct regimes of the solid-density, warm-dense-matter, and white-dwarfs (WDs). It is revealed that our nonlinear screening theory is compatible with the exponentially decaying Thomas-Fermi-type shielding predicted by the linear response theory. Moreover, the variation of relative Thomas-Fermi screening length shows that extremely dense quantum electron fluids are relatively poor charge shielders. Calculation of the total number of screening electrons around a nucleus shows that there is a position of maximum number of screening localized electrons around the screened nucleus, which moves closer to the point-like nucleus by increase in the plasma number density but is unaffected due to increase in the atomic-number value. It is discovered that the total number of screening electrons, (N{sub s}?r{sub TF}{sup 3}/r{sub d}{sup 3} where r{sub TF} and r{sub d} are the Thomas-Fermi and interparticle distance, respectively) has a distinct limit for extremely dense plasmas such as WD-cores and neutron star crusts, which is unique for all given values of the atomic-number. This is equal to saying that in an ultrarelativistic degeneracy limit of electron-ion plasma, the screening length couples with the system dimensionality and the plasma becomes spherically self-similar. Current analysis can provide useful information on the effects of relativistic correction to the charge screening for a wide range of plasma density, such as the inertial-confined plasmas and compact stellar objects.

Akbari-Moghanjoughi, M. [Department of Physics, Faculty of Sciences, Azarbaijan Shahid Madani University, 51745-406 Tabriz, Iran and International Centre for Advanced Studies in Physical Sciences and Institute for Theoretical Physics, Ruhr University Bochum, D-44780 Bochum (Germany)

2014-10-15T23:59:59.000Z

305

Thomas Jefferson Site Office CX Determinations | U.S. DOE Office...  

Office of Science (SC) Website

Thomas Jefferson Site Office CX Determinations Safety and Security Policy (SSP) SSP Home About Frequently Used Resources Categorical Exclusion Determinations Continuity of...

306

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

307

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

308

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

309

UBC Social Ecological Economic Development Studies (SEEDS) Student Report Derek Guo, Drew Willms, Kliment Kuzmanovski, Ralph Mercado, Stuart Armstrong, Thomas Denton  

E-Print Network [OSTI]

, Kliment Kuzmanovski, Ralph Mercado, Stuart Armstrong, Thomas Denton UBC Botanical Garden Traffic System Re Group 19 Stuart Armstrong Thomas Denton Derek Guo KlimentKuzmanovski Ralph

310

Implementation of DOE NPH Requirements at the Thomas Jefferson National Accelerator Facility (TJNAF), a Non-Nuclear DOE Lab  

Broader source: Energy.gov [DOE]

Implementation of DOE NPH Requirements at the Thomas Jefferson National Accelerator Facility (TJNAF), a Non-Nuclear DOE Lab David Luke, DOE, Thomas Jefferson Site Office Stephen McDuffie, DOE, Office of the Chief of Nuclear Safety

311

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

312

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

313

SBOT VIRGINIA THOMAS JEFFERSON LAB POC Danny Llyod Telephone  

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

VIRGINIA VIRGINIA THOMAS JEFFERSON LAB POC Danny Llyod Telephone (757) 269-7121 Email lloyd@jlab.org ADMINISTATIVE / WASTE / REMEDIATION Facilities Support Services 561210 Employment Placement Agencies 561311 Travel Agencies 561510 Locksmiths 561622 Exterminating and Pest Control Services 561710 Janitorial Services 561720 Landscaping Services 561730 Carpet and Upholstery Cleaning Services 561740 Hazardous Waste Collection 562112 CONSTRUCTION Industrial Building Construction 236210 Commercial and Institutional Building Construction 236220 Water and Sewer Line and Related Structures Construction 237110 Power and Communication Line and Related Structures Construction 237130 Highway, Street, and Bridge Construction 237310 Other Heavy and Civil Engineering Construction 237990 Other Foundation, Structure, and Building Exterior Contractors

314

GenomeView: a next-generation genome browser Thomas Abeel1,2,3,  

E-Print Network [OSTI]

GenomeView: a next-generation genome browser Thomas Abeel1,2,3, *, Thomas Van Parys1,2 , Yvan Saeys GenomeView, a stand-alone genome browser specifically designed to visualize and manipulate a multitude of genomics data. GenomeView enables users to dynamically browse high volumes of aligned short-read data

Gent, Universiteit

315

Usability and Playability Issues for ARQuake Bruce Thomas, Nicholas Krul, Benjamin Close and Wayne Piekarski  

E-Print Network [OSTI]

1 Usability and Playability Issues for ARQuake Bruce Thomas, Nicholas Krul, Benjamin Close: #12;2 Bruce Thomas, Nicholas Krul, Benjamin Close and Wayne Piekarski the see-through display allows to walk through the information space. 5) The user interface additionally requires only a simple hand-held

Thomas, Bruce

316

Studienleiter Chemie und Molekulare Wissenschaften Sekretariat Studienleitung Prof. Thomas Wandlowski Sandra Zbinden  

E-Print Network [OSTI]

Studienleiter Chemie und Molekulare Wissenschaften Sekretariat Studienleitung Prof. Thomas Wandlowski Sandra Zbinden Departement für Chemie und Biochemie Departement für Chemie und Biochemie 6318057 e-mail: thomas.wandlowski@dcb.unibe.ch e-mail: sandra.zbinden@dcb.unibe.ch Bachelor in Chemie und

Mühlemann, Oliver

317

Thomas Ridder Dresdner Forum 2006 June 23, 2006 1 Modeling Dependency in Credit Portfolios  

E-Print Network [OSTI]

;Thomas Ridder · Dresdner Forum 2006 · June 23, 2006 · 2 outline 1 why does dependency matter? 2 · Dresdner Forum 2006 · June 23, 2006 · 3 outline 1 why does dependency matter? 2 correlation drivers 3 two;why does dependency matter? Thomas Ridder · Dresdner Forum 2006 · June 23, 2006 · 5 focus 2: credit

Schmidt, Klaus D.

318

Mawl: Integrated Web and Telephone Service Creation David Atkins, Thomas Ball*  

E-Print Network [OSTI]

Mawl: Integrated Web and Telephone Service Creation David Atkins, Thomas Ball* Thomas Baran in a device- independent manner. PML is a markup language and middleware for controlling and pro- gramming language separates the speci cation of service logic from the speci cation of the user interface

Atkins, David

319

Partially Implicit Motion of a Sharp Interface in Navier-Stokes Flow J. Thomas Beale  

E-Print Network [OSTI]

Partially Implicit Motion of a Sharp Interface in Navier-Stokes Flow J. Thomas Beale Department, Lowengrub and Shelley. This modified step is combined with the method of [J. T. Beale, A. T. Layton, 36]. Email address: beale@math.duke.edu (J. Thomas Beale) URL: www.math.duke.edu/faculty/beale (J

320

VBH-0005 - In the Matter of Thomas Dwyer | Department of Energy  

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

VBH-0005 - In the Matter of Thomas Dwyer VBH-0005 - In the Matter of Thomas Dwyer VBH-0005 - In the Matter of Thomas Dwyer This Decision involves a whistleblower complaint filed by Thomas Dwyer under the Department of Energy's (DOE) Contractor Employee Protection Program. From January 1996 to October 1997, Mr. Dwyer was employed as a pipefitter by Fluor Daniel Fernald (FDF), a DOE contractor responsible for the cleanup of the Fernald Environmental Management Project, a former DOE uranium production facility located about 18 miles northwest of Cincinnati, Ohio. Mr. Dwyer alleges that FDF first suspended him and then terminated him in retaliation for taking certain actions and making health and safety disclosures. vbh0005.pdf More Documents & Publications VBA-0005 - In the Matter of Thomas Dwyer

Note: This page contains sample records for the topic "rift area thomas" 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
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321

VWA-0018 - Deputy Secretary Decision - In the Matter of Thomas T. Tiller |  

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

Deputy Secretary Decision - In the Matter of Thomas T. Deputy Secretary Decision - In the Matter of Thomas T. Tiller VWA-0018 - Deputy Secretary Decision - In the Matter of Thomas T. Tiller This is a request for review by complainant Thomas T. Tiller of an Initial Agency Decision, issued by the Office of Hearings and Appeals (OHA), denying the two reprisal complaints that he filed pursuant to 10 C.F.R. Part 708, the regulation establishing the DOE Contractor Employee Protection Program. Mr. Tiller was employed by Wackenhut Services, Inc. (Wackenhut), a DOE contractor that provides paramilitary security support services at DOE's Savannah River Site in Aiken, South Carolina. Deputy Secretary Decision Affirming VWA-0018 Decision and Order More Documents & Publications OHA Whistleblower Cases Archive File VWA-0018 - In the Matter of Thomas T. Tiller

322

Hydrocarbon accumulation conditions and exploration direction of Baiyun-Liwan deep water areas in the Pearl River Mouth Basin  

Science Journals Connector (OSTI)

Abstract An integrated geologic study was performed in the Baiyun-Liwan deep water areas, Pearl River Mouth Basin, based on the achievements obtained during the past five exploration stages. The following understandings were obtained. (1) The Baiyun Sag has superior source rock conditions and has experienced three tectonic evaluation stages like rifting, rifting-depression and depression. The Wenchang-Enping Fms deposited during the rifting stage have large hydrocarbon generation potentials. During the rifting-depression and depression stages, the deposition in the study area was controlled by the Oligocene and Miocene shelf slope break zones. The Oligocene Zhuhai Fm shallow marine delta-longshore depositional system and the Miocene Zhujiang-Hanjiang Fms deep fan depositional system were formed, and they are the most favorable reservoir-caprock assemblages in the study area. (2) The Hydrocarbon accumulation pattern in the deep waters is different from that in the northern shallow waters. Shelf slope break zone, composite conduction system consisting of structural ridge, fault, sandbody, unconformity and fluid diapir as well as late tectonic movement are the three major factors controlling hydrocarbon migration and accumulation in the study area. (3) The Liwan 3-1 gas field is a typical example. The superior trapping conditions, high-quality reservoirs of delta distributary channel controlled by shelf slope break zone, vertical conduction system consisting of fault and diapir, as well as the overlying massive marine mudstone caprock provide favorable geologic conditions for the formation of large gas fields. Four areas were identified as the targets of gas exploration in the near future: the deep water fan system in the central sag, the structural-stratigraphic traps in the uplifted areas on both sides of the main sag of Baiyun, a series of large structural traps on the fault terrace to the southwest of the main sag, and the ultradeep frontiers in sags such as Liwan to the south of the main sag.

Lin Heming; Shi Hesheng

2014-01-01T23:59:59.000Z

323

A LIMITED LIABILITY PARTNERSHIP 1050 Thomas Jefferson Street, NW  

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

A LIMITED LIABILITY PARTNERSHIP A LIMITED LIABILITY PARTNERSHIP 1050 Thomas Jefferson Street, NW Seventh Floor Washington, DC 20007 (202) 298-1800 Phone (202) 338-2416 Fax MEMORANDUM TO: DOE Office of General Counsel FROM: Doug Smith DATE: August 29, 2013 RE: Record of Communication Concerning Ceiling Fan and Ceiling Fan Light Kit Framework Document-Docket No. EERE-2012-BT-STD-0045 This memo provides an overview of communications made to DOE staff on the subject of possible changes to standards and test procedures for ceiling fans and ceiling fan light kits. The communications occurred at a meeting held at 10:30 a.m. on August 20, 2013, following the close of the comment period on the initial framework document for ceiling fans and light kits. The meeting attendees included:

324

Mr. Thomas A. Dickerson Supervisor of Environmental Affairs  

Office of Legacy Management (LM)

3 3 932. . . - ,_ ' ,;. Department of Energy Washinglon.DC 20545 tie c"rT SEP 05 1990 pff, (>-.I Mr. Thomas A. Dickerson Supervisor of Environmental Affairs Carpenter Technology Corporation Engineering and Construction P. 0. Box 14662 Reading, Pennsylvania 19612-4662 Dear Mr. Dickerson: The Department of Energy (DOE) has completed its review of the preliminary radiological data from the surveys of your facility in Reading, Pennsylvania, completed in July and August 1988. We are pleased to inform you that the survey has verified that the radiological condition of your facility is in compliance with applicable DOE Guidelines and that no remedial action or further investigations are necessary. I am enclosing a copy of the survey report prepared by our

325

Commander, Seneca Army Depot Attention: Thomas Stincic, Safety Officer  

Office of Legacy Management (LM)

9 1986 9 1986 Department of Energy Washington, D .C. 20545 . Commander, Seneca Army Depot Attention: Thomas Stincic, Safety Officer Romulus, New York 14541 Dear Mr. Stincic: As you are aware, the Department of Energy is evaluating the radiological condition of sites formerly used by Department predecessors during the early years of nuclear energy development , and a portion of the Seneca Army Depot was identified as one such site. While our preliminary inves-tiga- tions did identify residual radioactive material on the site, it is our understanding that the Department of Army assumed responsibility for this residual radioactivity and has completed remedial action. We have not received a final report of this work and would appreciate receiving a copy

326

A Tony Thomas-Inspired Guide to INSPIRE  

SciTech Connect (OSTI)

The SPIRES database was created in the late 1960s to catalogue the high energy physics preprints received by the SLAC Library. In the early 1990s it became the first database on the web and the first website outside of Europe. Although indispensible to the HEP community, its aging software infrastructure is becoming a serious liability. In a joint project involving CERN, DESY, Fermilab and SLAC, a new database, INSPIRE, is being created to replace SPIRES using CERN's modern, open-source Invenio database software. INSPIRE will maintain the content and functionality of SPIRES plus many new features. I describe this evolution from the birth of SPIRES to the current day, noting that the career of Tony Thomas spans this timeline.

O'Connell, Heath B.; /Fermilab

2010-04-01T23:59:59.000Z

327

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

328

VWA-0018 - In the Matter of Thomas T. Tiller | Department of Energy  

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

In the Matter of Thomas T. Tiller In the Matter of Thomas T. Tiller VWA-0018 - In the Matter of Thomas T. Tiller This Decision concerns two whistleblower complaints filed by Thomas T. Tiller (Tiller) under the Department of Energy's (DOE) Contractor Employee Protection Program, 10 C.F.R. Part 708. At all times relevant to this proceeding, Tiller was employed by Wackenhut Services, Incorporated (Wackenhut), a DOE contractor that provides paramilitary security support services at the DOE's Savannah River Site in Aiken, South Carolina. Tiller contends in his first complaint that Wackenhut demoted him after he alleged that a senior level manager at Wackenhut had engaged in unethical and possible criminal conduct. In his second complaint, Tiller charges that Wackenhut retaliated against him after learning he had filed a Part 708

329

Remarks by NNSA Administrator Thomas P. D'Agostino, 12th Annual Small  

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

NNSA Administrator Thomas P. D'Agostino, 12th Annual Small NNSA Administrator Thomas P. D'Agostino, 12th Annual Small Business Conference & Expo, Kansas City, Missouri | National Nuclear Security Administration Our Mission Managing the Stockpile Preventing Proliferation Powering the Nuclear Navy Emergency Response Recapitalizing Our Infrastructure Continuing Management Reform Countering Nuclear Terrorism About Us Our Programs Our History Who We Are Our Leadership Our Locations Budget Our Operations Media Room Congressional Testimony Fact Sheets Newsletters Press Releases Speeches Events Social Media Video Gallery Photo Gallery NNSA Archive Federal Employment Apply for Our Jobs Our Jobs Working at NNSA Blog Home > Media Room > Speeches > Remarks by NNSA Administrator Thomas P. D'Agostino, ... Speech Remarks by NNSA Administrator Thomas P. D'Agostino, 12th Annual Small

330

VBA-0005 - In the Matter of Thomas Dwyer | Department of Energy  

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

VBA-0005 - In the Matter of Thomas Dwyer VBA-0005 - In the Matter of Thomas Dwyer VBA-0005 - In the Matter of Thomas Dwyer This Decision considers an Appeal of an Initial Agency Decision (IAD) issued on May 2, 2000, involving a complaint filed by Thomas Dwyer (Dwyer or the complainant) under the Department of Energy (DOE) Contractor Employee Protection Program, 10 C.F.R. Part 708. In his complaint, Dwyer claims that Fluor Daniel Fernald (FDF), a DOE contractor, suspended and then terminated his employment in retaliation for his making disclosures that are protected under Part 708. In the IAD, however, the Hearing Officer determined that FDF had shown that it would have terminated the complainant for his misconduct, even in the absence of the protected disclosures. As set forth in this decision, I have determined that Dwyer's Appeal must be

331

FIA-12-0023 - In the Matter of Thomas R. Thielen | Department of Energy  

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

23 - In the Matter of Thomas R. Thielen 23 - In the Matter of Thomas R. Thielen FIA-12-0023 - In the Matter of Thomas R. Thielen The Department of Energy's (DOE) Office of Hearings and Appeals (OHA) Director granted in part and denied in all other respects a Privacy Act Appeal filed by Thomas R. Thielen. Mr. Thielen filed a request with the DOE's Richland Operations Office for documents regarding a safety concern he raised to CH2M Hill Plateau Remediation Company (CHPRC). Richland issued a determination letter which stated that, according to CHPRC's contract with DOE, CHPRC's employee concern records are the property of the contractor and not subject to the provisions of the Freedom of Information Act or Privacy Act. Richland released a copy of Mr. Thielen's DOE employee concern file, but withheld portions of the

332

Adaptive Temporal Tone Mapping Shaun David Ramsey, J. Thomas Johnson III, Charles Hansen  

E-Print Network [OSTI]

University of Utah, Salt Lake City, Utah, USA Abstract Monitor intensity ranges are much lower than the rangeAdaptive Temporal Tone Mapping Shaun David Ramsey, J. Thomas Johnson III, Charles Hansen

Utah, University of

333

Communicated by P. M. A. Tigerstedt B. R. Thomas ( ) ' S. E. Macdonald  

E-Print Network [OSTI]

Communicated by P. M. A. Tigerstedt B. R. Thomas ( ) ' S. E. Macdonald Department of Renewable. E. Macdonald ' M. Hicks D. L. Adams ' R. B. Hodgetts Effects of reforestation methods on genetic

Macdonald, Ellen

334

Gareth Thomas, 1977 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

1970's Gareth Thomas, 1977 Print Text Size: A A A FeedbackShare Page Chemistry & Metallurgy: For his contributions to the study of diffusion and defects in solids,...

335

E-Print Network 3.0 - africa 1887-1889 thomas Sample Search Results  

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

Search Powered by Explorit Topic List Advanced Search Sample search results for: africa 1887-1889 thomas Page: << < 1 2 3 4 5 > >> 1 The Burke Library Archives (Columbia...

336

Nearly Singular Integrals in 3D Stokes Flow Svetlana Tlupova1,, J. Thomas Beale2  

E-Print Network [OSTI]

Nearly Singular Integrals in 3D Stokes Flow Svetlana Tlupova1,, J. Thomas Beale2 1 Department. Email addresses: stlupova@umich.edu (S. Tlupova), beale@math.duke.edu (J. T. Beale) http

337

A METHOD FOR COMPUTING NEARLY SINGULAR INTEGRALS J. THOMAS BEALE AND MING-CHIH LAI  

E-Print Network [OSTI]

A METHOD FOR COMPUTING NEARLY SINGULAR INTEGRALS J. THOMAS BEALE AND MING-CHIH LAI SIAM J. NUMER Department, Duke University, Durham, NC 27708-0320 (beale@math.duke.edu). The research of this author

Lai, Ming-Chih

338

Research Areas  

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

Areas Areas Research Areas Print Scientists from a wide variety of fields come to the ALS to perform experiements. Listed below are some of the most common research areas covered by ALS beamlines. Below each heading are a few examples of the specific types of topics included in that category. Click on a heading to learn more about that research area at the ALS. Energy Science Photovoltaics, photosynthesis, biofuels, energy storage, combustion, catalysis, carbon capture/sequestration. Bioscience General biology, structural biology. Materials/Condensed Matter Correlated materials, nanomaterials, magnetism, polymers, semiconductors, water, advanced materials. Physics Atomic, molecular, and optical (AMO) physics; accelerator physics. Chemistry Surfaces/interfaces, catalysts, chemical dynamics (gas-phase chemistry), crystallography, physical chemistry.

339

Thomas Jefferson's administration as viewed by his contemporaries in New England  

E-Print Network [OSTI]

THOMAS JEPZERSON'S ADMINISTRATION AS VIEWED BY HIS CONTEMPORARIES IN NZW ENGLAND A . Thesis by MARILYN ELAINE JARCHOW Submitted to the Graduate College of Texas AkM University in partial fulfillment of the requirement for the degree...(M ea o epar men em er August 1970 ABSTRACT Thomas Jefferson's Administration as Viewed by His Contemporaries in New England. (August 1970) Marilyn Elaine Jarohow, B. A. , California State College at Fullerton; Direoted by& Dr. Joseph M. Nance...

Jarchow, Marilyn Elaine

2012-06-07T23:59:59.000Z

340

Implementation of an iterative technique for a solution of the Thomas-Fermi equation  

E-Print Network [OSTI]

IMPLEMENTATION OF AN ITERATIVE TECHNIQUE FOR A SOLUTION OF THE THOMAS-FERMI EQUATION A Thesis by RAYMOND CALVERT FLAGG Submitted to the Graduate College of Texas A&M University in partial fulfillment of the requirement for the degree... of MASTER OF SCIENCE August 1978 Major Subject: Mathematics IMPLEMENTATION OF AN ITERATIVE TECHNIQUE FOR A SOLUTION OF THE THOMAS-FERMI EQUATION A Thesis by RAYMOND CALVERT FLAGG Approved as to sryle and content by: (Chairman of Committeeee ( ead...

Flagg, Raymond Calvert

2012-06-07T23:59:59.000Z

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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

Research Areas  

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

Research Areas Print Research Areas Print Scientists from a wide variety of fields come to the ALS to perform experiements. Listed below are some of the most common research areas covered by ALS beamlines. Below each heading are a few examples of the specific types of topics included in that category. Click on a heading to learn more about that research area at the ALS. Energy Science Photovoltaics, photosynthesis, biofuels, energy storage, combustion, catalysis, carbon capture/sequestration. Bioscience General biology, structural biology. Materials/Condensed Matter Correlated materials, nanomaterials, magnetism, polymers, semiconductors, water, advanced materials. Physics Atomic, molecular, and optical (AMO) physics; accelerator physics. Chemistry Surfaces/interfaces, catalysts, chemical dynamics (gas-phase chemistry), crystallography, physical chemistry.

342

coherence area  

Science Journals Connector (OSTI)

1....In an electromagnetic wave, such as a lightwave or a radio wave, the area of a surface (a) every point on which the surface is perpendicular to the direction of propagation, (b) over which the e...

2001-01-01T23:59:59.000Z

343

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

344

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

345

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

346

Radiological Areas  

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

Revision to Clearance Policy Associated with Recycle of Scrap Metals Originating from Revision to Clearance Policy Associated with Recycle of Scrap Metals Originating from Radiological Areas On July 13, 2000, the Secretary of Energy imposed an agency-wide suspension on the unrestricted release of scrap metal originating from radiological areas at Department of Energy (DOE) facilities for the purpose of recycling. The suspension was imposed in response to concerns from the general public and industry groups about the potential effects of radioactivity in or on material released in accordance with requirements established in DOE Order 5400.5, Radiation Protection of the Public and Environment. The suspension was to remain in force until DOE developed and implemented improvements in, and better informed the public about, its release process. In addition, in 2001 the DOE announced its intention to prepare a

347

UBC Social Ecological Economic Development Studies (SEEDS) Student Report Derek Guo, Drew Willms, Kliment Kuzmanovski, Ralph Mercado, Stuart Armstrong, Thomas Denton  

E-Print Network [OSTI]

, Kliment Kuzmanovski, Ralph Mercado, Stuart Armstrong, Thomas Denton UBC Botanical Garden Development Plan Plan CIVL 445 Engineering Design and Analysis I Group 19 Stuart Armstrong Thomas Denton Derek Guo

348

Thomas B. Cook,1971 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Thomas B. Cook,1971 Thomas B. Cook,1971 The Ernest Orlando Lawrence Award Lawrence Award Home Nomination & Selection Guidelines Award Laureates 2000's 1990's 1980's 1970's 1960's Ceremony The Life of Ernest Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2/Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301) 903-9395 E: lawrence.award@science.doe.gov 1970's Thomas B. Cook,1971 Print Text Size: A A A RSS Feeds FeedbackShare Page Weapons: For his significant contributions to the study of nuclear weapons effects, for his original work in the translation of this knowledge into advanced technology for peaceful and military uses of atomic energy, and for his outstanding contributions to the nation through his service as an

349

Thomas P. Guilderson, 2011 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Thomas P. Guilderson, 2011 Thomas P. Guilderson, 2011 The Ernest Orlando Lawrence Award Lawrence Award Home Nomination & Selection Guidelines Award Laureates 2000's 1990's 1980's 1970's 1960's Ceremony The Life of Ernest Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2/Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301) 903-9395 E: lawrence.award@science.doe.gov 2000's Thomas P. Guilderson, 2011 Print Text Size: A A A RSS Feeds FeedbackShare Page Biological and Environmental Sciences: For ground-breaking radiocarbon measurements of corals, advancements in understanding the paleo-history of ocean currents and ocean processes revealing past climate variability, and the elucidation of how physical and biogeochemical oceanic processes affect

350

Thomas Jefferson Site Office CX Determinations | U.S. DOE Office of Science  

Office of Science (SC) Website

Thomas Jefferson Site Office CX Thomas Jefferson Site Office CX Determinations Integrated Support Center (ISC) ISC Home About Services Freedom of Information Act (FOIA) Privacy Act Categorical Exclusion Determinations Contact Information Integrated Support Center Roxanne Purucker U.S. Department of Energy 9800 S. Cass Avenue Argonne, IL 60439 P: (630) 252-2110 Larry Kelly U.S. Department of Energy 200 Administration Road Oak Ridge, TN 37830 P: (865) 576-0885 Categorical Exclusion (CX) Determinations Thomas Jefferson Site Office CX Determinations Print Text Size: A A A RSS Feeds FeedbackShare Page As of October 31, 2010, there have been no CX determinations made. Categorical Exclusion Determination Documents (CX Determinations): * Determination Date Name of Action: Description Categorical Exclusion Number External link

351

Microsoft PowerPoint - Ralph_Thomas Energy Teaming Agreement Presentation  

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

Ralph C. Thomas III, Esquire Ralph C. Thomas III, Esquire Partner Barton Baker Thomas & Tolle LLP McLean, VA 10 th Annual U.S. Department of Energy Small Business Conference Small Businesses Leading the Way to Recovery and Reinvestment Presenters Name Page # 2 INTRODUCTION: WHAT IS A TEAMING AGREEMENT? ► "An arrangement pursuant to which . . . ► A. Two or more companies form a partnership or joint venture to act as a potential prime contractor; or ► B. A potential prime contractor agrees with one or more other companies to have them act as its subcontractor under a specified government contract or acquisition program" FAR 9.601 3 5 Reasons Why a Prime Would Be Interested in You Two Questions to Ask to Determine Which Reason Applies to You 4 SMALL BUSINESS'S OBJECTIVE IN NEGOTIATING

352

Thomas A. Weaver, 1985 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Thomas A. Weaver, 1985 Thomas A. Weaver, 1985 The Ernest Orlando Lawrence Award Lawrence Award Home Nomination & Selection Guidelines Award Laureates 2000's 1990's 1980's 1970's 1960's Ceremony The Life of Ernest Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2/Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301) 903-9395 E: lawrence.award@science.doe.gov 1980's Thomas A. Weaver, 1985 Print Text Size: A A A RSS Feeds FeedbackShare Page National Security: For his exceptional contributions to national security in the physics, design and leadership of x-ray laser experiments, which include work in atomic physics, radiate transfer and hydrodynamics, material science, and the development of complex diagnostics. These major

353

Thomas E. Wainwright, 1973 | U.S. DOE Office of Science (SC)  

Office of Science (SC) Website

Thomas E. Wainwright, 1973 Thomas E. Wainwright, 1973 The Ernest Orlando Lawrence Award Lawrence Award Home Nomination & Selection Guidelines Award Laureates 2000's 1990's 1980's 1970's 1960's Ceremony The Life of Ernest Orlando Lawrence Contact Information The Ernest Orlando Lawrence Award U.S. Department of Energy SC-2/Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301) 903-9395 E: lawrence.award@science.doe.gov 1970's Thomas E. Wainwright, 1973 Print Text Size: A A A RSS Feeds FeedbackShare Page Weapons: For fundamental and original contributions to the theory of design and outputs of nuclear explosives for the original development of computational methods for the calculation of statistical physics phenomena, and for many innovative advances in the study of transport and

354

Thomas Jefferson Site Office CX Determinations | U.S. DOE Office of Science  

Office of Science (SC) Website

Thomas Jefferson Site Office CX Determinations Thomas Jefferson Site Office CX Determinations Safety, Security and Infrastructure (SSI) SSI Home Facilities and Infrastructure Safeguards & Security Environment, Safety and Health (ES&H) Organization Chart .pdf file (82KB) Phone Listing .pdf file (129KB) SC HQ Continuity of Operations (COOP) Implementation Plan .pdf file (307KB) Categorical Exclusion Determinations SLI & SS Budget Contact Information Safety, Security and Infrastructure U.S. Department of Energy SC-31/Germantown Building 1000 Independence Ave., SW Washington, DC 20585 P: (301) 903-4097 F: (301) 903-7047 Categorical Exclusion (CX) Determinations Thomas Jefferson Site Office CX Determinations Print Text Size: A A A RSS Feeds FeedbackShare Page As of October 31, 2010, there have been no CX determinations made.

355

VBB-0005 - In the Matter of Thomas Dwyer | Department of Energy  

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

05 - In the Matter of Thomas Dwyer 05 - In the Matter of Thomas Dwyer VBB-0005 - In the Matter of Thomas Dwyer This letter concerns the complaint of reprisal that you submitted to the Department of Energy under 10 C.F.R. Part 708. You have filed a petition for Secretarial review of the appeal decision issued to you on July 24, 2000. The Part 708 regulations applicable to the petition provide that the Secretary will reverse or revise an appeal decision by the Director of the Office of Hearings and Appeals only under extraordinary circumstances. 10 C.F.R. § 708.35(d). After fully evaluating all the issues that you raised in your filing dated September 8, 2000, I have determined that you have not shown that extraordinary circumstances warranting Secretarial review exist in this case. No modification to the appeal decision by the OHA Director is

356

Finding of No Significant Impact Improvements at the Thomas Jefferson National Accelerator Facility Newsport News, Virginia  

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

IMPROVEMENTS AT THE THOMAS JEFFERSON NATIONAL ACCELERATOR FACILITY IMPROVEMENTS AT THE THOMAS JEFFERSON NATIONAL ACCELERATOR FACILITY NEWPORT NEWS, VIRGINIA AGENCY: U.S. DEPARTMENT OF ENERGY ACTION: FINDING OF NO SIGNIFICANT IMPACT SUMMARY: The U.S. Department of Energy (DOE) has completed an Environmental Assessment (DOE/EA-1384) for proposed Improvements at the Thomas Jefferson National Accelerator Facility (Jefferson Lab). Newport News, Virginia. Based on the results of the impacts analysis reported in the EA, DOE has determined that the proposed action is not a major Federal action that would significantly affect the quality of the human environment within the context of the National Environmental Policy Act of 1969 (NEPA). Therefore, preparation of an environmental impact statement (EIS) is not necessary, and DOE is issuing this Finding of No

357

An Architecture for Optimal AlltoAll Personalized Communication Susan Hinrichs, Corey Kosak, David R. O'Hallaron, Thomas M. Stricker, and Riichiro Take # \\Lambda  

E-Print Network [OSTI]

, David R. O'Hallaron, Thomas M. Stricker, and Riichiro Take # \\Lambda School of Computer Science Carnegie

Shewchuk, Jonathan

358

Symmetry energy of hot nuclei in the relativistic Thomas-Fermi approximation  

E-Print Network [OSTI]

We develop a self-consistent description of hot nuclei within the relativistic Thomas--Fermi approximation using the relativistic mean-field model for nuclear interactions. The temperature dependence of the symmetry energy and other physical quantities of a nucleus are calculated by employing the subtraction procedure in order to isolate the nucleus from the surrounding nucleon gas. It is found that the symmetry energy coefficient of finite nuclei is significantly affected by the Coulomb polarization effect. We also examine the dependence of the results on nuclear interactions and make a comparison between the results obtained from relativistic and nonrelativistic Thomas-Fermi calculations.

Zhang, Z W; Hu, J N; Shen, H

2014-01-01T23:59:59.000Z

359

A review of "Borders and Travellers in Early Modern Europe" edited by Thomas Betteridge  

E-Print Network [OSTI]

worked from very similar assumptions about the need for hermeneutic stability. Thomas Betteridge, ed. Borders and Travellers in Early Modern Europe. Aldershot:: Ashgate, 2007. vi + 196 pp. $99.95. Review by Li n d a McJa n n e t , Be n t L e y un i v... e r s i t y . As described by editor Thomas Betteridge, Borders and Travellers in Early Modern Europe provides ?a trans-European interdisciplinary inter- rogation of borders and travel in early modern Europe? (12). Of the eleven essays...

McJannet, Linda

2008-01-01T23:59:59.000Z

360

SYLLABUS FOR MATH 2250 Text: Hass, Weir, and Thomas,  

E-Print Network [OSTI]

: Integration 5.1­5.2 Area and Estimating with Finite Sums, Sigma Notation and Limits of Finite Sums 2 §5.1: #1, 55, 61, 63, 73 5.6 Substitution and Area Between Curves 2 §5.6: #1, 3, 7, 13, 25, 27, 31, 39, 47, 51, 45, 51, 53, 55, 56, 59, 72, 76, 77 3.4 The Derivative as a Rate of Change 2 §3.4: #1, 5, 7, 10, 11

Smith, Roy

Note: This page contains sample records for the topic "rift area thomas" 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.
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to obtain the most current and comprehensive results.


361

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

362

Environmental Assessment Proposed Improvements at the Thomas Jefferson National Accelerator Facility Newport News, Virginia  

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

84 84 Environmental Assessment Proposed Improvements at the Thomas Jefferson National Accelerator Facility Newport News, Virginia June 2002 U. S. Department of Energy Oak Ridge Operations Oak Ridge, Tennessee DOE/EA-1384 i TABLE OF CONTENTS Executive Summary.....................................................................................................................1 1. INTRODUCTION..................................................................................................................... 6 1.1 PREVIOUS ACTIONS ............................................................................................................................................. 6 1.2 SCOPE OF THIS PROPOSED ACTION..............................................................................................................

363

FDR3 --A Modern Refinement Checker for CSP Thomas Gibson-Robinson, Philip Armstrong,  

E-Print Network [OSTI]

FDR3 -- A Modern Refinement Checker for CSP Thomas Gibson-Robinson, Philip Armstrong, Alexandre.roscoe}@cs.ox.ac.uk Abstract. FDR3 is a complete rewrite of the CSP refinement checker FDR2, incorporating a significant number describe the new algorithm that FDR3 uses to construct its in- ternal representation of CSP processes

Oxford, University of

364

FDR3 --A Modern Refinement Checker for CSP Thomas Gibson-Robinson, Philip Armstrong,  

E-Print Network [OSTI]

FDR3 -- A Modern Refinement Checker for CSP Thomas Gibson-Robinson, Philip Armstrong, Alexandre.roscoe}@cs.ox.ac.uk Abstract. FDR3 is a complete rewrite of the CSP refinement checker FDR2, incorporating a significant number describe the new algorithm that FDR3 uses to construct its internal representation of CSP processes

Oxford, University of

365

Ising quantum chain and sequence evolution Holger Wagner 1) , Ellen Baake 2) , and Thomas Gerisch 1)  

E-Print Network [OSTI]

Ising quantum chain and sequence evolution Holger Wagner 1) , Ellen Baake 2) , and Thomas Gerisch 1 in molecular evolution is shown to be equivalent to an Ising quantum chain. Observable quantities, tailored and selection; Ising quantum chain; mean-#12;eld model; phase transition 1 Introduction Sequence space models

Baake, Ellen

366

Laser Excitation of a Fracture Source for Elastic Waves Thomas E. Blum* and Kasper van Wijk  

E-Print Network [OSTI]

Laser Excitation of a Fracture Source for Elastic Waves Thomas E. Blum* and Kasper van Wijk a transparent sample by focusing laser light directly onto this fracture. The associated displacement field, measured by a laser interferometer, has pronounced waves that are diffracted at the fracture tips. We

Snieder, Roel

367

State University of New York at Binghamton Thomas J. Watson School of Engineering and Applied Science  

E-Print Network [OSTI]

Statics ISE 211 Engineering Economics General Education Elective (A) Spring Math 304 Linear Algebra ISE Engineering Industrial and systems engineering is integral to American industry and economic growth. Its major3/24/2009 State University of New York at Binghamton Thomas J. Watson School of Engineering

Suzuki, Masatsugu

368

State University of New York at Binghamton Thomas J. Watson School of Engineering and Applied Science  

E-Print Network [OSTI]

211 Engineering Economics General Education Elective (A) Spring Math 304 Linear Algebra ISE 231 Human and systems engineering is integral to American industry and economic growth. Its major focus is on the design3/24/2009 State University of New York at Binghamton Thomas J. Watson School of Engineering

Suzuki, Masatsugu

369

State University of New York at Binghamton Thomas J. Watson School of Engineering and Applied Science  

E-Print Network [OSTI]

Engineering Economics & Project Management General Education Elective (H) Year 4 Fall ISE 420 Optimization and systems engineering is integral to American industry and economic growth. Its major focus is on the design8/27/2012 State University of New York at Binghamton Thomas J. Watson School of Engineering

Suzuki, Masatsugu

370

A Privacy-Aware Architecture For Demand Response Systems Stephen Wicker, Robert Thomas  

E-Print Network [OSTI]

A Privacy-Aware Architecture For Demand Response Systems Stephen Wicker, Robert Thomas School architectures that realize the benefits of demand response without requiring that AMI data be centrally-based demand response efforts in the face of public outcry. We also show that Trusted Platform Modules can

Wicker, Stephen

371

Corrosion Damage Detection with Piezoelectric Wafer Active Sensors Dustin Thomas, John Welter  

E-Print Network [OSTI]

1 Corrosion Damage Detection with Piezoelectric Wafer Active Sensors Dustin Thomas, John Welter Air a priority issue for today's Air Force. One of the most critical structural problems is corrosion. In fact the KC-135 now costs $1.2 billion a year to repair corrosion. In this paper, we plan to show the use

Giurgiutiu, Victor

372

On the duration of the Paleocene-Eocene thermal maximum Ursula Rohl and Thomas Westerhold  

E-Print Network [OSTI]

On the duration of the Paleocene-Eocene thermal maximum (PETM) Ursula Ro¨hl and Thomas Westerhold of California, Santa Cruz, California 95064, USA [1] The Paleocene-Eocene thermal maximum (PETM) is one of global warming and a massive perturbation of the global carbon cycle from injection of isotopically light

Zachos, James

373

Multicomponent density-functional theory for electrons and nuclei Thomas Kreibich  

E-Print Network [OSTI]

Multicomponent density-functional theory for electrons and nuclei Thomas Kreibich Institut für a general multicomponent density-functional theory in which electrons and nuclei are treated completely , 71.10. w I. INTRODUCTION Density-functional theory DFT is among the most suc- cessful approaches

Gross, E.K.U.

374

Multi Criteria Analysis for bioenergy systems assessments Thomas Buchholz a,, Ewald Rametsteiner b  

E-Print Network [OSTI]

Multi Criteria Analysis for bioenergy systems assessments Thomas Buchholz a,?, Ewald Rametsteiner b Available online 11 November 2008 Keywords: Multi Criteria Analysis Bioenergy Sustainability a b s t r a c t Sustainable bioenergy systems are, by definition, embedded in social, economic, and environmental contexts

Vermont, University of

375

Augmented Foam Sculpting for Capturing 3D Models Michael R. Marner Bruce H. Thomas  

E-Print Network [OSTI]

Augmented Foam Sculpting for Capturing 3D Models Michael R. Marner Bruce H. Thomas University. A designer physically sculpts a 3D model from foam using a hand-held hot wire foam cut- ter. Both the foamD model from foam using a hand-held hot wire foam cutter. Both the foam and cutting tool are tracked

Thomas, Bruce

376

Red Cloud with MATLAB case study Thomas Cleland Neural Algorithms: Understanding the Complex  

E-Print Network [OSTI]

Red Cloud with MATLAB case study Thomas Cleland ­ Neural Algorithms: Understanding the Complex resources and commonly requested software, e.g., MATLAB, make it most efficient to outsource to a cloud be completed in an interactive timeframe (minutes to hours) on Red Cloud with MATLAB. The results from

Walter, M.Todd

377

UAV Formation Flight using 3D Potential Field Tobias Paul Thomas R. Krogstad Jan Tommy Gravdahl  

E-Print Network [OSTI]

UAV Formation Flight using 3D Potential Field Tobias Paul Thomas R. Krogstad Jan Tommy Gravdahl ESG aerial vehicles (UAVs). Based on a virtual leader approach, combined with an extended local potential a group of UAVs based on a simplified small-scale helicopter, which is simulated in MATLABTM /Simulink

Gravdahl, Jan Tommy

378

Stroke amplifier for deformable mirrors Robert H. Webb, Marc J. Albanese, Yaopeng Zhou, Thomas Bifano, and  

E-Print Network [OSTI]

Stroke amplifier for deformable mirrors Robert H. Webb, Marc J. Albanese, Yaopeng Zhou, Thomas stroke of a deformable mirror. By arranging for the wavefront to traverse the deformable mirror more than to produce lower- cost mirrors. Unfortunately, most commercial MEMS mirrors have only a limited stroke

379

Top Stroke Rehabil 2013;20(4):299307 2013 Thomas Land Publishers, Inc.  

E-Print Network [OSTI]

299 Top Stroke Rehabil 2013;20(4):299­307 © 2013 Thomas Land Publishers, Inc. www stimulation (NMES) for recovery of hand function after stroke are not known. This clinical pilot study thenar muscles of 16 persons with chronic stroke. Participants were identified a priori as having a low

Griffin, Lisa

380

Meter Any Wire, Anywhere by Virtualizing the Voltage Channel Thomas Schmid, David Culler, Prabal Dutta  

E-Print Network [OSTI]

Meter Any Wire, Anywhere by Virtualizing the Voltage Channel Thomas Schmid, David Culler, Prabal}@eecs.umich.edu culler@cs.berkeley.edu Abstract AC power meters require both voltage and current to be sampled physical proximity and fed into a single power metering de- vice. In this paper, we explore the viability

Dutta, Prabal

Note: This page contains sample records for the topic "rift area thomas" 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

The Java Machine Learning Library Thomas Abeel, Yvan Saeys and Yves Van de Peer  

E-Print Network [OSTI]

The Java Machine Learning Library Thomas Abeel, Yvan Saeys and Yves Van de Peer Department of Plant.abeel@psb.ugent.be What is Java-ML? Motivation Code & Documentation Applications 1. Machine learning techniques: · 18 style, no GUI 6. Open Source · Lack of a (good) machine learning library: · Reference implementations

Gent, Universiteit

382

INVERTIBLE FILTER BANKS ON THE 2-SPHERE B.T. Thomas Yeo Wanmei Ou Polina Golland  

E-Print Network [OSTI]

INVERTIBLE FILTER BANKS ON THE 2-SPHERE B.T. Thomas Yeo Wanmei Ou Polina Golland Computer Science to the sphere, many key challenges remain. In this paper, we develop conditions for the invertibility be incorpo- rated into the design of self-invertible axis-symmetric wavelets. Self- invertibility

Golland, Polina

383

ALTIMETER DATA FOR OPERATIONAL USE IN THE MARINE ENVIRONMENT Susan Digby, Thomas Antczak  

E-Print Network [OSTI]

ALTIMETER DATA FOR OPERATIONAL USE IN THE MARINE ENVIRONMENT Susan Digby, Thomas Antczak Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California Robert Leben, George Born, Mississippi Nick Shay University of Miami, Rosentiel School of Marine and Atmospheric Science, Miami, Florida

384

Biomass, Condition of Western Lake Erie Dreissenids Primary Investigator: Thomas Nalepa -NOAA GLERL (Emeritus)  

E-Print Network [OSTI]

Biomass, Condition of Western Lake Erie Dreissenids Primary Investigator: Thomas Nalepa - NOAA of dreissenid biomass but there are no current, accurate estimates of biomass in this portion of the lake. Biomass is calculated from abundances, size- frequencies, and length-weights. The goal of this project

385

Zero electron kinetic energy spectroscopy of the ArCl anion Thomas Lenzer,a)  

E-Print Network [OSTI]

and the neutral complexes are observed in the ZEKE spectra. From our spectroscopic data we construct modelZero electron kinetic energy spectroscopy of the ArCl anion Thomas Lenzer,a) Ivan Yourshaw, Berkeley, California 94720 Received 19 January 1999; accepted 23 February 1999 Zero electron kinetic energy

Neumark, Daniel M.

386

Zero electron kinetic energy spectroscopy of the XeCl Thomas Lenzer,a)  

E-Print Network [OSTI]

measurements for the neutral state we construct a Morse­Morse-switching­van der Waals model potential functionZero electron kinetic energy spectroscopy of the XeCl? anion Thomas Lenzer,a) Ivan Yourshaw, Berkeley, California 94720 Received 9 November 2001; accepted 21 December 2001 Zero electron kinetic energy

Neumark, Daniel M.

387

Preempting Uncertain Regulatory Threats Thomas P. Lyon and John W. Maxwelly  

E-Print Network [OSTI]

Preempting Uncertain Regulatory Threats Thomas P. Lyon and John W. Maxwelly September 15, 2004 assume certainty regarding the likelihood of the regulatory threat. We examine industry voluntary self and credible regulatory threat is needed to induce industry to take voluntary self-regulatory actions. 1

Lyon, Thomas P.

388

Impact of EPS on Digestion of Waste Activate Sludge Thomas Gostanian  

E-Print Network [OSTI]

Impact of EPS on Digestion of Waste Activate Sludge Thomas Gostanian Faculty Mentor: Professor Chul of WAS is the make-up of the Extracellular Polymeric Substances (EPS) surrounding the cells, which acts as a glue/inorganics in influent, temperature, reactor flow types, etc). Certain EPS complexes are vulnerable to specific

Mountziaris, T. J.

389

Fraunhofer FOKUSCompetence Center NGNI Prof. Dr.-Ing. habil Thomas Magedanz  

E-Print Network [OSTI]

Fraunhofer FOKUSCompetence Center NGNI Overview ?berblick 1 Prof. Dr.-Ing. habil Thomas Magedanz Berlin, Germany Internet: www.av.tu-berlin.de Email: tm@cs.tu-berlin.de #12;Fraunhofer FOKUSCompetence and IT is fueling the innovation in Service Delivery Platforms and underlying networking infrastructures · IP

Wichmann, Felix

390

OPTIMAL INVESTMENT POLICIES FOR THE HORSE RACE MODEL Thomas S. Ferguson and C. Zachary Gilstein  

E-Print Network [OSTI]

OPTIMAL INVESTMENT POLICIES FOR THE HORSE RACE MODEL Thomas S. Ferguson and C. Zachary Gilstein UCLA and Bell Communications May 1985, revised 2004 Abstract. Optimal investment policies for maximizing the expected value of the utility of an investor's fortune are presented for investment models

Ferguson, Thomas S.

391

A GENERAL INVESTMENT MODEL Thomas S. Ferguson and C. Zachary Gilstein  

E-Print Network [OSTI]

A GENERAL INVESTMENT MODEL Thomas S. Ferguson and C. Zachary Gilstein UCLA and Bell Communications Revised May 1985 Abstract. A Bayesian approach to a general investment model is proposed based on knowledge of the probability distributions of possible investment re- turns (future market events

Ferguson, Thomas S.

392

SYMMETRIC ITERATED BETTI NUMBERS ERIC BABSON, ISABELLA NOVIK, AND REKHA THOMAS  

E-Print Network [OSTI]

SYMMETRIC ITERATED BETTI NUMBERS ERIC BABSON, ISABELLA NOVIK, AND REKHA THOMAS Abstract. We de#12 Betti numbers of I. We prove that for I , the Stanley-Reisner ideal of a simplicial complex , these numbers are the symmetric counterparts of the exterior iterated Betti numbers of introduced by Duval

Novik, Isabella

393

Friction, Frontogenesis, and the Stratification of the Surface Mixed Layer LEIF THOMAS*  

E-Print Network [OSTI]

Friction, Frontogenesis, and the Stratification of the Surface Mixed Layer LEIF THOMAS* Department restratification resulting from frontogenesis in regions of confluent flow. Frictional forces acting of friction versus frontogenesis in the restratification of the mixed layer and are tested using numerical

Thompson, Andrew

394

Fiber coupling with adaptive optics for free-space optical communication Thomas Weyraucha  

E-Print Network [OSTI]

Fiber coupling with adaptive optics for free-space optical communication Thomas Weyraucha , Mikhail, Department of Manufacturing Engineering, Brookline, MA 02446 ABSTRACT We describe an adaptive optical fiber coupling system for free-space optical communication comprising a micro- electromechanical deformable

395

Self-assembling DNA Nanostructures for Patterned Molecular Assembly Thomas H. LaBeana  

E-Print Network [OSTI]

1 Self-assembling DNA Nanostructures for Patterned Molecular Assembly Thomas H. LaBeana , Kurt V@cs.duke.edu; Tel: (919)660-65685 Abstract The Chapter describes the use of DNA for molecular-scale self-assembly with a discussion of DNA-nanostructures, starting with the self-assembly of various building-blocks known as DNA

Reif, John H.

396

ASSESSMENT OF AUDIO FEATURES FOR AUTOMATIC COUGH DETECTION Thomas Drugman, Jerome Urbain, Thierry Dutoit  

E-Print Network [OSTI]

ASSESSMENT OF AUDIO FEATURES FOR AUTOMATIC COUGH DETECTION Thomas Drugman, Jerome Urbain, Thierry://tcts.fpms.ac.be/drugman/ ABSTRACT This paper addresses the issue of cough detection using only audio recordings, with the ultimate. 1. INTRODUCTION For children as well as for adults, cough is in pneumology the commonest syndrom

Dupont, Stéphane

397

Arduino Remote Infrared Network Adapter Rene Neff, Thomas Trimborn and Matthias Wubbeling  

E-Print Network [OSTI]

ARINA: Arduino Remote Infrared Network Adapter Ren´e Neff, Thomas Trimborn and Matthias W}@cs.uni-bonn.de Abstract In this paper we present ARINA, a light-weight Arduino based system for forwarding infrared signals via Ethernet. Short introductions on infrared communication and Arduino as a development platform

Behnke, Sven

398

Relationship between protein folding thermodynamics and the energy landscape Jaegil Kim,* Thomas Keyes,  

E-Print Network [OSTI]

Relationship between protein folding thermodynamics and the energy landscape Jaegil Kim,* Thomas Received 23 September 2008; published 4 March 2009 The origin of protein folding thermodynamics is examined.15.Cc, 05.70. a, 87.15.A Protein folding--i.e., how a polypeptide chain reaches a unique native state

Straub, John E.

399

The Agile Research Penultimatum Thomas Way, Sandhya Chandrasekhar and Arun Murthy  

E-Print Network [OSTI]

thomas.way@villanova.edu Abstract - Agile software development is a widely used and successful Unified Process, Rational Unified Process, Agile Modeling, and most recently, Lean Software Development methodology for organizing and managing software product development in an industry setting. For academic

Way, Thomas

400

Rewriting Shakespeare: Thomas Otway's Venice Preserv'd and Edward Young's The Revenge  

E-Print Network [OSTI]

the early eighteenth century. Thomas Otway's Venice Preserv'd, first performed in 1682, is an example of the approach taken by most Restoration adapters of Shakespeare. Otway took from Shakespeare that which he wanted to use and discarded the rest. Edward...

Lovan, Gary Eugene

1996-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "rift area thomas" 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

Taking Control of Green Speed Thomas A. Nikolai, Ph.D.  

E-Print Network [OSTI]

to know about green speed A lot of green speed misinformation Poor communication cited #1 problem GreenTaking Control of Green Speed Thomas A. Nikolai, Ph.D. The Doctor of Green Speed nikolait finds when requesting green speed help are.... #12;The 3 most common answers a superintendent finds when

402

A connectionist model of spatial learning in the rat Thomas Strosslin  

E-Print Network [OSTI]

A connectionist model of spatial learning in the rat Thomas Str¨osslin April 14, 2004 #12. In subsequent visits, they can recall this information and thus avoid dangerous places or find again a food". In the late 1940s, theoretical considerations have led researchers to the conclusion that rats establish

Gerstner, Wulfram

403

Understanding open source in an industrial context Sven Ziemer, yvind Hauge and Thomas sterlie  

E-Print Network [OSTI]

of software development that will revolution- ize the software industry [2]. A recent addition to the onUnderstanding open source in an industrial context Sven Ziemer, ?yvind Hauge and Thomas ?sterlie source in an industrial context. Building a grounded theory from an industry-driven R&D project, our

404

The Nachos Instructional Operating System Wayne A. Christopher, Steven J. Procter, and Thomas E. Anderson  

E-Print Network [OSTI]

The Nachos Instructional Operating System Wayne A. Christopher, Steven J. Procter, and Thomas E operating systems at an undergraduate level, it is very important to provide a project that is realistic enough to show how real operating systems work, yet simple enough that the students can understand

Anderson, Tom

405

STAMP-Based Analysis of a Refinery Overflow Accident Nancy Leveson, Margaret Stringfellow, and John Thomas  

E-Print Network [OSTI]

1 STAMP-Based Analysis of a Refinery Overflow Accident Nancy Leveson, Margaret Stringfellow, and John Thomas As an example of STAMP, we have taken an accident report produced for a real refinery failures and operator actions (or missing actions) related to the loss. But stopping after identifying

Leveson, Nancy

406

A Multi-HMM Approach to ECG Segmentation Julien Thomas, Cedric Rose and Francois Charpillet  

E-Print Network [OSTI]

A Multi-HMM Approach to ECG Segmentation Julien Thomas, C´edric Rose and Franc¸ois Charpillet INRIA studies require to analyze thousands of ECGs in order to evaluate the side effects of a new drug. In this paper we present a new approach to automatic ECG segmentation based on hierarchic continuous density hid

Boyer, Edmond

407

On the computational power of photosynthesis Niall Murphy, Damien Woods and Thomas J. Naughton  

E-Print Network [OSTI]

On the computational power of photosynthesis Niall Murphy, Damien Woods and Thomas J. Naughton County Kildare, Ireland #12;Abstract We describe a simplified explanation of photosynthesis. We charac- terise the complexity of photosynthesis by interpreting its chemical equa- tion as a language acceptance

Murphy, Niall

408

Microsoft Word - Omak-Area-3G-CX.doc  

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

9, 2011 9, 2011 REPLY TO ATTN OF: KEC-4 SUBJECT: Environmental Clearance Memorandum Roger Thomas Project Manager - TECT-CSB-1 Proposed Action: Omak Area 3G Radio Site Upgrades Budget Information: Work Orders 197229, 197230, & 197231; Task 03 Categorical Exclusion Applied (from Subpart D, 10 C.F.R. Part 1021): B1.19 "Siting, construction, and operation of microwave and radio communication towers and associated facilities..." Location: Okanogan and Douglas counties, Washington Proposed by: Bonneville Power Administration (BPA) Description of the Proposed Action: BPA proposes to upgrade communication equipment at three existing BPA facilities in Okanogan and Douglas counties, Washington. The work would occur at two

409

Southeast Idaho Area Links  

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

Area Attractions and Events Area Geography Area History Area Links Driving Directions Idaho Falls Attractions and Events INL History INL Today Research Park Sagebrush Steppe...

410

Day 2 - Thurs Plenary 3 - Dave Thomas.ppt  

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

DEAD IN 7 MINUTES DEAD IN 7 MINUTES "But, it can't happen to me." TAKE-AWAY MINDFULNESS IS A "PRACTICAL" TOOL IN FOREST FIREFIGHTING OBJECTIVES v Mindfulness v Up's and down's v Practical Tips South Canyon Fatality Area, August 1994 Shame & Stupidity WEICK & SUTCLIFFE Disconfirm Expectations If we just follow our procedures, checklists, plans, events will unfold as we think they should. "H2 would not be a great risk...light fuels & rocky areas in Cache Bar..." 1. Preoccupation with failure "Any lapse is seen as symptom that something could be wrong with the larger system." Weick/Sutcliffe 2. Reluctance to Simplify Relentless attack on simplification. 3. Sensitivity to Operations Seeing what is actually going on: the "Big Picture"

411

F-Race and Iterated F-Race: An Overview Mauro Birattari, Zhi Yuan, Prasanna Balaprakash, and Thomas Sttzle  

E-Print Network [OSTI]

Chapter 13 F-Race and Iterated F-Race: An Overview Mauro Birattari, Zhi Yuan, Prasanna Balaprakash search algorithms in Mauro Birattari · Zhi Yuan · Prasanna Balaprakash · Thomas Stützle IRIDIA, Co

Birattari, Mauro

412

Review of Natural Phenomena Hazards (NPH) Requirements Currently Applied to the Thomas Jefferson National Accelerator Facility (TJNAF)  

Broader source: Energy.gov [DOE]

Review of Natural Phenomena Hazards (NPH) Requirements Currently Applied to the Thomas Jefferson National Accelerator Facility (TJNAF) By: Integrated NPH Team: David Luke, Lead, TJSO Rusty Sprouse, JSA Michael A. Epps, TJSO Richard Korynta, TJSO

413

Strontium Substitution for Calcium in Lithogenesis Sarah D. Blaschko, Thomas Chi, Joe Miller, Lawrence Flechner, Sirine Fakra,  

E-Print Network [OSTI]

Strontium Substitution for Calcium in Lithogenesis Sarah D. Blaschko, Thomas Chi, Joe Miller, AK), Novato, California Purpose: Strontium has chemical similarity to calcium, which enables the replace- ment of calcium by strontium in biomineralization processes. Incorporating stron- tium into human

414

Geophysical Setting of the Blue Mountain Geothermal Area, North-Central  

Open Energy Info (EERE)

Setting of the Blue Mountain Geothermal Area, North-Central Setting of the Blue Mountain Geothermal Area, North-Central Nevada and Its Relationship to a Crustal-Scale Fracture Associated with the Inception of the Yellowstone Hotspot Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Geophysical Setting of the Blue Mountain Geothermal Area, North-Central Nevada and Its Relationship to a Crustal-Scale Fracture Associated with the Inception of the Yellowstone Hotspot Abstract The Blue Mountain geothermal field, located about 35 km northwest of Winnemucca, Nevada, is situated along a prominent crustal-scale fracture interpreted from total intensity aeromagnetic and gravity data. Aeromagnetic data indicate that this feature is related to the intrusion of mafic dikes, similar to the Northern Nevada Rift (Zoback et al.,1994), and

415

Questions and Answers - What did Thomas Jefferson do as a scientist?  

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

Who invented magnets? Who invented magnets? Previous Question (Who invented magnets?) Questions and Answers Main Index Next Question (Why does the U.S. use Fahrenheit instead of Celsius?) Why does the U.S. useFahrenheit instead of Celsius? What did Thomas Jefferson do as a scientist? It's true that Thomas Jefferson contributed some new knowledge directly to science and technology. But his main scientific contribution was as a statesman of science. For half a century in public office and in private life, he led the growth of American optimism about science, technology, and the future. Jefferson wished he could be a scientist all the time. When he was leaving the presidency in early 1809, he wrote, "Nature intended me for the tranquil pursuits of science, by rendering them my supreme delight." In

416

Wind Power Opportunities in St. Thomas, USVI: A Site-Specific Evaluation and Analysis  

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

Power Opportunities in Power Opportunities in St. Thomas, USVI: A Site-Specific Evaluation and Analysis E. Lantz, A. Warren, J.O. Roberts, and V. Gevorgian Technical Report NREL/TP-7A20-55415 September 2012 NREL is a national laboratory of the U.S. Department of Energy, Office of Energy Efficiency & Renewable Energy, operated by the Alliance for Sustainable Energy, LLC. National Renewable Energy Laboratory 15013 Denver West Parkway Golden, Colorado 80401 303-275-3000 * www.nrel.gov Contract No. DE-AC36-08GO28308 Wind Power Opportunities in St. Thomas, USVI: A Site-Specific Evaluation and Analysis E. Lantz, A. Warren, J.O. Roberts, and V. Gevorgian Prepared under Task No. IDVI.1020 Technical Report NREL/TP-7A20-55415 September 2012 NOTICE This report was prepared as an account of work sponsored by an agency of the United States government.

417

Thomas-Ehrman effect in a three-body model: $^{16}$Ne case  

E-Print Network [OSTI]

The dynamic mechanism of the Thomas-Ehrman shift is studied in three-cluster systems by example of $^{16}$Ne and $^{16}$C isobaric mirror partners. We predict configuration mixings for $0^+$ and $2^+$ states in $^{16}$Ne and $^{16}$C. Large isospin symmetry breaking on the level of wave function component weights is demonstrated for these states and discussed as three-body mechanism of Thomas-Ehrman shift. It is shown that the description of the Coulomb displacement energies requires a consistency among three parameters: the $^{16}$Ne decay energy $E_T$, the $^{15}$F ground state energy $E_r$, and the configuration mixing parameters for the $^{16}$Ne/$^{16}$C $0^+$ and $2^+$ states. Basing on this analysis we infer the $^{15}$F $1/2^+$ ground state energy to be $E_r=1.39-1.42$ MeV.

Grigorenko, L V; Zhukov, M V

2014-01-01T23:59:59.000Z

418

Thomas-Ehrman effect in a three-body model: $^{16}$Ne case  

E-Print Network [OSTI]

The dynamic mechanism of the Thomas-Ehrman shift is studied in three-cluster systems by example of $^{16}$Ne and $^{16}$C isobaric mirror partners. We predict configuration mixings for $0^+$ and $2^+$ states in $^{16}$Ne and $^{16}$C. Large isospin symmetry breaking on the level of wave function component weights is demonstrated for these states and discussed as three-body mechanism of Thomas-Ehrman shift. It is shown that the description of the Coulomb displacement energies requires a consistency among three parameters: the $^{16}$Ne decay energy $E_T$, the $^{15}$F ground state energy $E_r$, and the configuration mixing parameters for the $^{16}$Ne/$^{16}$C $0^+$ and $2^+$ states. Basing on this analysis we infer the $^{15}$F $1/2^+$ ground state energy to be $E_r=1.39-1.42$ MeV.

L. V. Grigorenko; T. A. Golubkova; M. V. Zhukov

2014-11-07T23:59:59.000Z

419

A review of "Verzeichnis der gedruckten Briefe deutscher Autoren des 17. Jahrhunderts" by Thomas Brger, ed.  

E-Print Network [OSTI]

jewels: Europe?s great cities. Thomas B?rger, ed. Verzeichnis der gedruckten Briefe deutscher Autoren des 17. Jahrhunderts. Teil 2: Drucke zwischen 1751 und 1980. 4 vols. Series: Repertorien zur Erforschung der fr?hen Neuzeit, Vol. 12.2. Wiesbaden... history studies of intellectual networks in Europe following the pioneering work in this regard by Wolfgang Reinhard. The primary utility of this tool, however, appears to be three-fold. First, it has the potential of providing a summary...

Susan R. Boettcher

2003-01-01T23:59:59.000Z

420

Accurate calculation of the solutions to the Thomas-Fermi equations  

E-Print Network [OSTI]

We obtain highly accurate solutions to the Thomas-Fermi equations for atoms and atoms in very strong magnetic fields. We apply the Pad\\'e-Hankel method, numerical integration, power series with Pad\\'e and Hermite-Pad\\'e approximants and Chebyshev polynomials. Both the slope at origin and the location of the right boundary in the magnetic-field case are given with unprecedented accuracy.

Paolo Amore; John P. Boyd; Francisco M. Fernndez

2012-05-08T23:59:59.000Z

Note: This page contains sample records for the topic "rift area thomas" 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

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

422

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

423

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

424

Thomas Jefferson National Accelerator Facility Site Tour - Accelerator Map  

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

Counting House Free Electron Accelerator Facility Machine Control Center Physics Storage Building North Linear Accelerator South Linear Accelerator VEPCO Substation Machine Control Center Annex Machine Control Center Annex II North Access Building South Access Building Central Helium Liquefier Injector Hall A Truck Ramp Hall B Truck Ramp Hall C Truck Ramp Experimental Hall A Experimental Hall B Experimental Hall C East Arc West Arc Counting House Free Electron Accelerator Facility Machine Control Center Physics Storage Building North Linear Accelerator South Linear Accelerator VEPCO Substation Machine Control Center Annex Machine Control Center Annex II North Access Building South Access Building Central Helium Liquefier Injector Hall A Truck Ramp Hall B Truck Ramp Hall C Truck Ramp Experimental Hall A Experimental Hall B Experimental Hall C East Arc West Arc Science Education Jefferson Lab Jefferson Lab Home Search Jefferson Lab Contact Jefferson Lab Science Education Home Teacher Resources Student Zone Games and Puzzles Science Cinema Programs and Events Search Education Privacy and Security Notice Jefferson Lab Site Tour Guided Tour Site Map Accelerator Area Map Administrative Area Map Tour Index

425

Dust acoustic solitary and shock excitations in a Thomas-Fermi magnetoplasma  

SciTech Connect (OSTI)

The linear and nonlinear properties of dust-acoustic waves are investigated in a collisionless Thomas-Fermi magnetoplasma, whose constituents are electrons, ions, and negatively charged dust particles. At dust time scale, the electron and ion number densities follow the Thomas-Fermi distribution, whereas the dust component is described by the classical fluid equations. A linear dispersion relation is analyzed to show that the wave frequencies associated with the upper and lower modes are enhanced with the variation of dust concentration. The effect of the latter is seen more strongly on the upper mode as compared to the lower mode. For nonlinear analysis, we obtain magnetized Korteweg-de Vries (KdV) and Zakharov-Kuznetsov (ZK) equations involving the dust-acoustic solitary waves in the framework of reductive perturbation technique. Furthermore, the shock wave excitations are also studied by allowing dissipation effects in the model, leading to the Korteweg-de Vries-Burgers (KdVB) and ZKB equations. The analysis reveals that the dust-acoustic solitary and shock excitations in a Thomas-Fermi plasma are strongly influenced by the plasma parameters, e.g., dust concentration, dust temperature, obliqueness, magnetic field strength, and dust fluid viscosity. The present results should be important for understanding the solitary and shock excitations in the environments of white dwarfs or supernova, where dust particles can exist.

Rahim, Z.; Qamar, A. [Institute of Physics and Electronics, University of Peshawar, Peshawar 25000 (Pakistan); National Center for Physics (NCP) at QAU Campus, Shahdra Valley Road, Islamabad 44000 (Pakistan); Ali, S. [National Center for Physics (NCP) at QAU Campus, Shahdra Valley Road, Islamabad 44000 (Pakistan)

2014-07-15T23:59:59.000Z

426

Site Monitoring Area Maps  

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

to the Site Monitoring Area (SMA) The Site Monitoring Area sampler Control measures (best management practices) installed at the Site Monitoring Area Structures such as...

427

On Some Computations of Higher Rank Refined Donaldson-Thomas Invariants  

E-Print Network [OSTI]

We present some computations of higher rank refined Donaldson-Thomas invariants on local curve geometries, corresponding to local D6-D2-D0 or D4-D2-D0 configurations. A refined wall-crossing formula for invariants with higher D6 or D4 ranks is derived and verified to agree with the existing formulas under the unrefined limit. Using the formula, refined invariants on the $(-1,-1)$ and $(-2,0)$ local rational curve with higher D6 or D4 ranks are computed.

Wu-yen Chuang; Chien-Hsun Wang

2014-09-08T23:59:59.000Z

428

Bakamjian-Thomas mass operator for the few-nucleon system from chiral dynamics  

E-Print Network [OSTI]

We present an exploratory study consisting in the formulation of a relativistic quantum mechanics to describe the few-nucleon system at low energy, starting from the quantum field theoretical chiral Lagrangian involving pions and nucleons. To this aim we construct a Bakamjian-Thomas mass operator and perform a truncation of the Fock space which respects at each stage the relativistic covariance. Such truncation is justified, at sufficiently low energy, in the framework of a systematic chiral expansion. As an illustration we discuss the bound state observables and low-energy phaseshifts of the nucleon-nucleon and pion-nucleon scattering at the leading order of our scheme.

L. Girlanda; W. H. Klink; M. Viviani

2007-02-07T23:59:59.000Z

429

On Raviart-Thomas and VMS formulations for flow in heterogeneous materials.  

SciTech Connect (OSTI)

It is well known that the continuous Galerkin method (in its standard form) is not locally conservative, yet many stabilized methods are constructed by augmenting the standard Galerkin weak form. In particular, the Variational Multiscale (VMS) method has achieved popularity for combating numerical instabilities that arise for mixed formulations that do not otherwise satisfy the LBB condition. Among alternative methods that satisfy local and global conservation, many employ Raviart-Thomas function spaces. The lowest order Raviart-Thomas finite element formulation (RT0) consists of evaluating fluxes over the midpoint of element edges and constant pressures within the element. Although the RT0 element poses many advantages, it has only been shown viable for triangular or tetrahedral elements (quadrilateral variants of this method do not pass the patch test). In the context of heterogenous materials, both of these methods have been used to model the mixed form of the Darcy equation. This work aims, in a comparative fashion, to evaluate the strengths and weaknesses of either approach for modeling Darcy flow for problems with highly varying material permeabilities and predominantly open flow boundary conditions. Such problems include carbon sequestration and enhanced oil recovery simulations for which the far-field boundary is typically described with some type of pressure boundary condition. We intend to show the degree to which the VMS formulation violates local mass conservation for these types of problems and compare the performance of the VMS and RT0 methods at boundaries between disparate permeabilities.

Turner, Daniel Zack

2010-11-01T23:59:59.000Z

430

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

431

Thomas Roser  

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

Roser Roser ! NSAC Subcommittee on Scientific Facilities ! February 15, 2013 ! eRHIC Project! ! ! Performance requirements! ! eRHIC design! ! R&D for eRHIC! ! Cost and schedule! 2 Performance requirements! ! ! Highly polarized (> 70%) electron, proton and neutron (He-3) beams! ! Ion beams from deuteron to the heaviest nuclei (uranium) ! ! Center of mass energy range: ~ 20 GeV to ~ 150 GeV ! ! Non-zero crossing angle to minimize synchrotron radiation background! ! Possibility to have multiple interaction regions ! ! High luminosity: 10 33 - 10 34 cm -2 s -1 ! ! First stage to reach CM energy of ≳ 70 GeV and luminosity of 
 10 32 - 10 34 cm -2 s -1 ! ! 3 RHIC! NSRL! LINAC! Booster! AGS! Tandems! STAR! 6:00 o'clock! PHENIX! 8:00 o'clock! 10:00 o'clock! Polarized Jet Target! 12:00 o'clock! RF! 4:00 o'clock!

432

Sustainability criteria for bioenergy systems: results from an expert survey Thomas Buchholz*, Valerie A. Luzadis, Timothy A. Volk  

E-Print Network [OSTI]

Sustainability criteria for bioenergy systems: results from an expert survey Thomas Buchholz in revised form 10 April 2009 Accepted 24 April 2009 Available online 9 May 2009 Keywords: Bioenergy and concerns about regional and national security are driving the development and use of biomass for bioenergy

Vermont, University of

433

Managing Plug-Loads for Demand Response within Buildings Thomas Weng, Bharathan Balaji, Seemanta Dutta, Rajesh Gupta, Yuvraj Agarwal  

E-Print Network [OSTI]

Managing Plug-Loads for Demand Response within Buildings Thomas Weng, Bharathan Balaji, Seemanta managers can per- form active energy management, especially during demand response situations that require, allowing them to deal with demand response situations through user- specified actuation policies. At its

Gupta, Rajesh

434

Adaptive Substrate for Enhanced Spatial Augmented Reality Contrast and Markus Broecker Ross T. Smith Bruce H. Thomas  

E-Print Network [OSTI]

Ross T. Smith Bruce H. Thomas Wearable Computer Lab University of South Australia ABSTRACT This paper employ hand-held displays or head-mounted displays with optical or video see through technologies for the appearance fidelity e-mail:Markus.Broecker@unisa.edu.au e-mail:ross@r-smith.net e-mail:Bruce

Thomas, Bruce

435

Hybrid Indoor and Outdoor Tracking for Mobile 3D Mixed Reality Wayne Piekarski, Ben Avery, Bruce H. Thomas, Pierre Malbezin  

E-Print Network [OSTI]

Hybrid Indoor and Outdoor Tracking for Mobile 3D Mixed Reality Wayne Piekarski, Ben Avery, Bruce H@tinmith.net, bruce.thomas@unisa.edu.au, pierre@tinmith.net Abstract This paper describes a new hybrid tracking system, in most cases an arrow navigation cue and a hand held World-in-Miniature model are used to provide

Thomas, Bruce

436

P~!ETRIC STUDY OF HEAT FLOW DURING RESISTANCE SPOT WELDING Euiwhan Kim and Thomas W. Eagar  

E-Print Network [OSTI]

pieces , electrical contact resistance, material properties, phase changes and heat dissipationi ...) P~!ETRIC STUDY OF HEAT FLOW DURING RESISTANCE SPOT WELDING Euiwhan Kim and Thomas W. Eagar Department of Materials Science and Engineering Hassachusetts Institute of Technology Cambridge, MA 02139

Eagar, Thomas W.

437

The Systems Science & Industrial Engineering (SSIE) Department and The Thomas J. Watson School of Engineering and Applied  

E-Print Network [OSTI]

The Systems Science & Industrial Engineering (SSIE) Department and The Thomas J. Watson School professionals, we will open the doors to demonstrate what industrial and systems engineers can contribute to any. We offer the BS degree in industrial and systems engineering (ISE), MEng degree in industrial

Suzuki, Masatsugu

438

Condition on the KohnSham kinetic energy and modern parametrization of the ThomasFermi density  

E-Print Network [OSTI]

; published online 20 January 2009 We study the asymptotic expansion of the neutral-atom energy as the atomic-correlation energy, EXC n , must be approximated. But a direct, orbital-free DFT could be constructed if onlyCondition on the Kohn­Sham kinetic energy and modern parametrization of the Thomas­Fermi density

Burke, Kieron

439

Airpath Control of a SI Engine with Variable Valve Timing Actuators Thomas Leroy, Jonathan Chauvin and Nicolas Petit  

E-Print Network [OSTI]

Airpath Control of a SI Engine with Variable Valve Timing Actuators Thomas Leroy, Jonathan Chauvin with Variable Valve Timing (VVT) actuators. VVT devices are used to produce internal exhaust gas recirculation actuators affect the fresh air charge in the cylinders. This has an impact on the torque output (leading

440

Manifold modeling for brain population analysis Samuel Gerber *, Tolga Tasdizen, P. Thomas Fletcher, Sarang Joshi, Ross Whitaker, and the Alzheimers  

E-Print Network [OSTI]

Manifold modeling for brain population analysis Samuel Gerber *, Tolga Tasdizen, P. Thomas Fletcher Brain MRI Manifold learning Computer aided clinical diagnosis a b s t r a c t This paper describes a method for building efficient representations of large sets of brain images. Our hypothesis

Utah, University of

Note: This page contains sample records for the topic "rift area thomas" 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

RECYCLING OF LATEX BASED PAINT AS POLYMER FEEDSTOCK MATERIALS Jennifer K. Lynch, Thomas J. Nosker, Robert Hamill, Richard L. Lehman  

E-Print Network [OSTI]

RECYCLING OF LATEX BASED PAINT AS POLYMER FEEDSTOCK MATERIALS Jennifer K. Lynch, Thomas J. Nosker investigates the recycling of used latex paints into non-paint products. Waste latex paint was collected, dried container cost for either recycling or hazardous waste disposal, is very high for the retailer. Much

442

NAME EMAIL SUPERVISOR NAME EMAIL SUPERVISOR Alrehaily, Leena lalrehai@uwo.ca JCW Gungor, Thomas tgungor@uwo.ca ERG  

E-Print Network [OSTI]

NAME EMAIL SUPERVISOR NAME EMAIL SUPERVISOR Alrehaily, Leena lalrehai@uwo.ca JCW Gungor, Thomas tgungor@uwo.ca ERG Armstrong, Erin earmstr6@uwo.ca MAK Guo, Dan dguo24@uwo.ca JCW Azizpoor Fard, Mahmood mazizpoo@uwo.ca JFC Guo, Jiacheng jguo52@uwo.ca KMB Barbon, Stephanie sbarbon@uwo.ca JBG Guo, Xiaoxuan xguo

Lennard, William N.

443

METAL COATING OF POROUS SILICON GAS SENSORS FOR IMPROVED SENSITIVITY & SELECTIVITY Thomas Osburn, Georgia Tech Physics, MSE SURF 2009 Fellow  

E-Print Network [OSTI]

METAL COATING OF POROUS SILICON GAS SENSORS FOR IMPROVED SENSITIVITY & SELECTIVITY Thomas Osburn Introduction Gas sensors on the market today have many limitations that prevent real world applications. The current standard, metal oxide sensors, are highly temperature dependant and work at high temperatures

Li, Mo

444

Supporting Systolic and Memory Communication in iWarp Shekhar Borkar, Robert Cohn, George Cox, Thomas Gross,  

E-Print Network [OSTI]

Supporting Systolic and Memory Communication in iWarp Shekhar Borkar, Robert Cohn, George Cox, Thomas Gross, H. T. Kung, Monica Lam, Margie Levine, Brian Moore, Wire Moore, Craig Peterson, Jim Susman/CMO under Contract MDA972­90­C­0035. Authors' affiliations: R. Cohn, T. Gross, H. T. Kung, and J. Webb

Shewchuk, Jonathan

445

Onset of Metallic Behavior in Magnesium Clusters Owen C. Thomas, Weijun Zheng, Shoujun Xu, and Kit H. Bowen, Jr.  

E-Print Network [OSTI]

Onset of Metallic Behavior in Magnesium Clusters Owen C. Thomas, Weijun Zheng, Shoujun Xu, and Kit-selected magnesium cluster anions, Mgn ÿ , over the size range, n 3­35. Their s-p band gaps were observed to close in the finite size re- gime for the case of magnesium. Magnesium is a particu- larly instructive case because

Simons, Jack

446

On the ratio between shifts in the eddy-driven jet and the Hadley Paul W. Staten Thomas Reichler  

E-Print Network [OSTI]

On the ratio between shifts in the eddy-driven jet and the Hadley cell edge Paul W. Staten · Thomas and in the Hadley cell edge as depicted in models and reanalyses. We cal- culate an interannual shift ratio of approximately 1.5:1 between the eddy-driven jet and the Hadley cell edge over the Southern Hemisphere during

Reichler, Thomas

447

Bubble Dynamics, Shock Waves and Sonoluminescence Author(s): Claus-Dieter Ohl, Thomas Kurz, Reinhard Geisler, Olgert Lindau, Werner  

E-Print Network [OSTI]

Bubble Dynamics, Shock Waves and Sonoluminescence Author(s): Claus-Dieter Ohl, Thomas Kurz, Physical and Engineering Sciences. http://www.jstor.org #12;THE ROYAL SOCIETY Bubble dynamics, shock waves emission by bubbles is studied experimentally. Single bubbles kept in a bubble trap and single laser

Ohl, Claus-Dieter

448

CONTROLLED VARIABLES IN SENTENCE INTONATION* Carole E. Gelfer,t Katherine S. Harris,t and Thomas Haer  

E-Print Network [OSTI]

CONTROLLED VARIABLES IN SENTENCE INTONATION* Carole E. Gelfer,t Katherine S. Harris,t and Thomas realization (Atkinson, 1973; Collier, 1975; Gelfer, Harris, Collier, & Baer, 1985; Maeda, 1976). Unfortunately characteristics of utterances (Klatt, Stevens, & Mead, 1968). For example, because of the reduced airflow

449

Mechanical reorganization of cross-linked F-actin networks at the air-buffer Thomas Boatwright,a  

E-Print Network [OSTI]

Mechanical reorganization of cross-linked F-actin networks at the air-buffer interface Thomas compression is studied. We observe two distinct classes of behavior: a mechanically induced structural reorganization of the monolayer and a subsequent reversible, nonlinear mechanical response. Measurements

Dennin, Michael

450

Minimization of energy per particle among Bravais lattices in R2 Lennard-Jones and Thomas-Fermi cases  

E-Print Network [OSTI]

that the global min- imizer of the total energy is the triangular lattice of length one. His method was adapted. The problem is to find the configuration of the points which minimizes the total energy of interaction, calledMinimization of energy per particle among Bravais lattices in R2 : Lennard-Jones and Thomas

451

Field Mapping At Reese River Area (Henkle, Et Al., 2005) | Open Energy  

Open Energy Info (EERE)

Field Mapping At Reese River Area (Henkle, Et Al., Field Mapping At Reese River Area (Henkle, Et Al., 2005) Exploration Activity Details Location Reese River Area Exploration Technique Field Mapping Activity Date Usefulness useful DOE-funding Unknown References William R. Henkle Jr., Wayne C. Gundersen, Thomas D. Gundersen (2005) Mercury Geochemical, Groundwater Geochemical, And Radiometric Geophysical Signatures At Three Geothermal Prospects In Northern Nevada Retrieved from "http://en.openei.org/w/index.php?title=Field_Mapping_At_Reese_River_Area_(Henkle,_Et_Al.,_2005)&oldid=510756" Categories: Exploration Activities DOE Funded Activities What links here Related changes Special pages Printable version Permanent link Browse properties 429 Throttled (bot load) Error 429 Throttled (bot load) Throttled (bot load)

452

Bioavailable organic carbon in wetland soils across a broad climogeographic area  

E-Print Network [OSTI]

for the degree of MASTER OF SCIENCE Approved as to style and content by; David A. Zuberer (Co-Chair of Committee) Larry P. Wilding (Co-Chair of Committee) Thomas W. Boutton (Member) Mark A s ey (Head of Department) May 2002 Major Subject: Soil Science... ABSTRACT Bioavailable Organic Carbon in Wetland Soils Across a Broad Climogeographic Area. (May 2002) Andrew Dwight Baker, B. S. , Texas A&M University Co-Chairs of Advisory Committee. Dr. David A. Zuberer Dr. Larry P. Wilding Soils from a broad...

Baker, Andrew Dwight

2012-06-07T23:59:59.000Z

453

UNITED STATES DEPARTMENT OF ENERGY (DOE) THOMAS JEFFERSON NATIONAL ACCELERATOR FACILITY (JEFFERSON LAB)  

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

- 2014 JSAT Application Package - 2014 JSAT Application Package Page 1 of 6 UNITED STATES DEPARTMENT OF ENERGY (DOE) THOMAS JEFFERSON NATIONAL ACCELERATOR FACILITY (JEFFERSON LAB) JLAB SCIENCE ACTIVITIES FOR TEACHERS (JSAT) ATTENTION ALL 5 th , 6 th AND 8 th GRADE MIDDLE SCHOOL SCIENCE TEACHERS! THIS PROGRAM IS FOR YOU! What is it? JSAT is an after school program for 5 th , 6 th and 8 th grade science teachers designed to build teachers' skills in the physical sciences, funded by the Jefferson Science Associates Initiatives Fund. What will I do? The 2013-2014 program will include interactive activities to enhance physical science instruction at the middle school level and lectures by Jefferson Lab staff on the applications of science. And, yes, teachers WILL receive class sets of some activities!

454

CO2 EMISSION CALCULATIONS AND TRENDS Thomas A. Boden and Gregg Marland  

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

EMISSION CALCULATIONS AND TRENDS EMISSION CALCULATIONS AND TRENDS Thomas A. Boden and Gregg Marland Environmental Sciences Division Oak Ridge National Laboratory Oak Ridge, Tennessee 37830-6335 Robert J. Andres Institute of Northern Engineering School of Engineering University of Alaska-Fairbanks Fairbanks, Alaska 99775-5900 ABSTRACT FEB 05 ZS3 OSTI The submitted manuscript has been authored by a contractor of the U.S. Government under contract No. DE- ACO5-840R21400. Accordingly, the U.S. Government retains a nonexclusive, royalty-free license to publish or reproduce the published form of this contribution, or allow others to do so. for U.S. Government purposes." This paper describes the compilation, calculation, and availability of the most comprehensive CO2 emissions database currently available. The database offers global, regional, and national annual

455

MEMORANDUM FOR ELIZABETH MONTOYA TRANSITION TEAM FROM THOMAS N. PYKE, J  

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

^ g December 1, 200S ^ g December 1, 200S MEMORANDUM FOR ELIZABETH MONTOYA TRANSITION TEAM FROM THOMAS N. PYKE, J CHIEF INFORMATION OFFICER SUBJECT: Follow-up to our meeting this morning Carl Staton and I appreciated the opportunity to brief you this morning on our office's activities, including the cyber security issue. We noted four follow-up actions: 1. The breakdown ofOCIO Federal and contracting FTE at all of our sites is: Federal Contractor a. Forrestal 51 144 b. Germantown 85 213 c. Albuquerque 1 39 d. Pittsburgh 1 0 c. Linthicum, Maryland 0 8 f. Las Vegas 3 39 Total: 141 443 2. The number of Federal FTE in the OCIO cyber security office is 16. 3. We have some additional infbrmation about the detailee from NNSA that we mentioned. The detailee, Mr. Robbie Green, is in the process of being

456

Radiation Transport Thomas A. Brunner Joint Russian-American Five-Laboratory Conference on  

National Nuclear Security Administration (NNSA)

Forms of Approximate Forms of Approximate Radiation Transport Thomas A. Brunner Joint Russian-American Five-Laboratory Conference on Computational Mathematics/Physics 19-23 June 2005 Vienna, Austria Sandia is a multiprogram laboratory operated by Sandia Corporation, a Lockheed Martin Company, for the United States Department of Energy's National Nuclear Security Administration under contract DE-AC04-94AL85000. The Diffusion Approximation * Taylor Expand Intensity in Angle * Fast, robust, and accurate numerical solutions * Flux can be larger than energy density - More stuff moving than is there to move * Flux Limited Diffusion improves robustness - Limits flux so that it's not larger than energy density - Many different flux limiters Spherical Harmonics (PN) * Intensity expanded further in angle than diffusion

457

CRANE CO. 757 THIRD AVENUE NEW YORK. N.Y. THOMAS UNGERLAND ASSOCIATE GENERAL COUNSEL  

Office of Legacy Management (LM)

? ? z _ - c 0-e . CRANE CO. 757 THIRD AVENUE NEW YORK. N.Y. THOMAS UNGERLAND ASSOCIATE GENERAL COUNSEL December 14, 1987 James J. Fiore Director Office of Nuclear Energy Department of Energy Washington, D.C. Re: Crane - Indian Orchard Dear M r. Fiore: W e acknowledge receipt of your letter to Paul Hundt, dated September 29, 1987, which requests certain information about Crane's plant site in Indian Orchard, Massachusetts. The plant is not currently operating. Crane was unable to locate any records concerning the machining of uranium in the 1947-48 period for a customer, Brookhaven Labs, at the Indian Orchard, facility. It is believed that the records, which were kept on the second floor at 305 Hamshire Street, Indian Orchard, Massachusetts were moved ten or fifteen years ago

458

Thomas Mason Oak Ridge National Lab July 10 2012 SB Summit  

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

National Laboratory Presented to the DOE/NNSA Regional Small Business Summit Thomas E. Mason Director, Oak Ridge National Laboratory Knoxville, Tennessee July 10, 2012 2 Managed by UT-Battelle for the U.S. Department of Energy RegionalSummit_1207 ORNL is DOE's largest science and energy laboratory 2 Managed by UT-Battelle for the U.S. Department of Energy $1.65B budget World's most intense neutron source 4,400 employees World-class research reactor 3,000 research guests annually $500M modernization investment Nation's largest materials research portfolio Most powerful open scientific computing facility Nation's most diverse energy portfolio Managing billion-dollar U.S. ITER project 3 Managed by UT-Battelle for the U.S. Department of Energy RegionalSummit_1207

459

Microphysics of Neutron Star Outer Envelopes in the Periodized, Magnetic Thomas-Fermi Model  

E-Print Network [OSTI]

Observations of several types of neutron stars indicate surface temperature inhomogeneities. In recent years magneto-thermal simulations have supported the idea that the magnetic field and anisotropic heat conduction play important roles in generating these inhomogeneities. Simulations rely on crustal microphysics input heretofore calculated at the level of a plasma model -- neglecting lattice structure and electron polarizability. We focus on the low density outer envelope, treating both of these elements by a proper periodization of the magnetic Thomas-Fermi model. Our solution method involves a novel domain decomposition and we describe a scalable implementation using \\textit{Hypre}. The method may be seen as a prototype for the general class of problems involving nonlinear charge screening of periodic, quasi-low-dimensionality structures, e.g. liquid crystals. Findings include low density $c'<0$ elastic instabilities for both bcc and fcc lattices, reminiscent of the situation in some light actinides, a...

Engstrom, Tyler A; Owen, Benjamin J; Brannick, James; Hu, Xiaozhe

2014-01-01T23:59:59.000Z

460

Statistical and Realistic Numerical Model Investigations of Anthropogenic and Climatic Factors that Influence Hypoxic Area Variability in the Gulf of Mexico  

E-Print Network [OSTI]

, Steven DiMarco George Jackson Committee Members, Robert Hetland Thomas Bianchi Piers Chapman Steven Davis Head of Department, Piers Chapman May 2012 Major Subject: Oceanography iii ABSTRACT Statistical and Realistic Numerical Model... Investigations of Anthropogenic and Climatic Factors that Influence Hypoxic Area Variability in the Gulf of Mexico. (May 2012) Yang Feng, B. S., Ocean University of China; M.S., Ocean University of China Co?Chairs of Advisory Committee: Dr. Steven Di...

Feng, Yang

2012-07-16T23:59:59.000Z

Note: This page contains sample records for the topic "rift area thomas" 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

Radiometrics At Reese River Area (Henkle, Et Al., 2005) | Open...  

Open Energy Info (EERE)

References William R. Henkle Jr., Wayne C. Gundersen, Thomas D. Gundersen (2005) Mercury Geochemical, Groundwater Geochemical, And Radiometric Geophysical Signatures At Three...

462

Handbook of Drug Metabolism Edited by Thomas F. Woolf. Marcel Dekker Inc.:? New York. 1999. xi + 596 pp. $225.00. ISBN 0-8247-0229-8.  

Science Journals Connector (OSTI)

Handbook of Drug Metabolism Edited by Thomas F. Woolf. ... Part 1 (Fundamentals of Drug Metabolism) lays the foundations from kinetic and physiological viewpoints, with thorough chapters on the pharmacokinetics of drug metabolites and on hepatic morphology, respectively. ...

Kevin S. Currie

1999-10-21T23:59:59.000Z

463

Dept. No. Dept. Name Analyst Dept. No. Dept. Name Analyst 107 Anthropology Franchesca Kim 375 Papers of Thomas Jefferson Maidul Begum  

E-Print Network [OSTI]

Papers of Thomas Jefferson Maidul Begum 108 Center for African American Studies Ami Patel 395 PPPL Contract Wendy Fang 109 Applied & Comp. Math Brad Johnson 396 PPPL Wendy Fang 110 Architecture Franchesca

Rowley, Clarence W.

464

Thomas W. Lester, Ph. D., is Dean of the College of Engineering; Richard J. Sweigard, Ph.D., is Associate Dean  

E-Print Network [OSTI]

Thomas W. Lester, Ph. D., is Dean of the College of Engineering; Richard J. Sweigard, Ph Programs; Bruce L. Walcott is Associate Dean for Economic Development and Innovations Management. The College of Engineering offers programs leadingtoundergraduateandgraduatedegreesin

MacAdam, Keith

465

Material Disposal Areas  

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

Material Disposal Areas Material Disposal Areas Material Disposal Areas Material Disposal Areas, also known as MDAs, are sites where material was disposed of below the ground surface in excavated pits, trenches, or shafts. Contact Environmental Communication & Public Involvement P.O. Box 1663 MS M996 Los Alamos, NM 87545 (505) 667-0216 Email Material Disposal Areas at LANL The following are descriptions and status updates of each MDA at LANL. To view a current fact sheet on the MDAs, click on LA-UR-13-25837 (pdf). MDA A MDA A is a Hazard Category 2 nuclear facility comprised of a 1.25-acre, fenced, and radiologically controlled area situated on the eastern end of Delta Prime Mesa. Delta Prime Mesa is bounded by Delta Prime Canyon to the north and Los Alamos Canyon to the south.

466

Public Meeting on Oversight of Complex, High Hazard Nuclear Operations - Statement of Thomas P. DAgostino - May 12, 2010  

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

of Thomas P. D'Agostino of Thomas P. D'Agostino Administrator, National Nuclear Security Administration Defense Nuclear Facilities Safety Board Public Hearing on Line and Independent Oversight May 12, 2010 Mr. Chairman, members of the Board, thank you for this opportunity to meet with you in this public forum to discuss effective oversight of our nuclear facilities. You provided written lines of inquiry prior to this meeting, and my formal response is organized around them. Of course, I will also be happy to answer any additional questions you may have. Let me begin by describing our overall oversight approach as it currently exists. I will discuss its effectiveness, point out both its strengths and weaknesses, and use it as a basis for describing the changes we are considering. I will then discuss our approach to

467

area | OpenEI  

Open Energy Info (EERE)

area area Dataset Summary Description These estimates are derived from a composite of high resolution wind resource datasets modeled for specific countries with low resolution data originating from the National Centers for Environmental Prediction (United States) and the National Center for Atmospheric Research (United States) as processed for use in the IMAGE model. The high resolution datasets were produced by the National Renewable Energy Laboratory (United States), Risø DTU National Laboratory (Denmark), the National Institute for Space Research (Brazil), and the Canadian Wind Energy Association. The data repr Source National Renewable Energy Laboratory Date Released Unknown Date Updated Unknown Keywords area capacity clean energy international National Renewable Energy Laboratory

468

NSTB Summarizes Vulnerable Areas  

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

NSTB Summarizes Vulnerable Areas NSTB Summarizes Vulnerable Areas Commonly Found in Energy Control Systems Experts at the National SCADA Test Bed (NSTB) discovered some common areas of vulnerability in the energy control systems assessed between late 2004 and early 2006. These vulnerabilities ranged from conventional IT security issues to specific weaknesses in control system protocols. The paper "Lessons Learned from Cyber Security Assessments of SCADA and Energy Management Systems" describes the vulnerabilities and recommended strategies for mitigating them. It should be of use to asset owners and operators, control system vendors, system integrators, and third-party vendors interested in enhancing the security characteristics of current and future products.

469

Neutron Science Research Areas | ORNL  

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

Home | Science & Discovery | Neutron Science | Research Areas SHARE Research Areas Neutron scattering research at ORNL covers four broad research areas: biology and soft...

470

Western Area Power Administration  

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

Loveland Area Projects November 29-30, 2011 2 Agenda * Overview of Western Area Power Administration * Post-1989 Loveland Area Projects (LAP) Marketing Plan * Energy Planning and Management Program * Development of the 2025 PMI Proposal * 2025 PMI Proposal * 2025 PMI Comment Period & Proposal Information * Questions 3 Overview of Western Area Power Administration (Western) * One of four power marketing administrations within the Department of Energy * Mission: Market and deliver reliable, renewable, cost-based Federal hydroelectric power and related services within a 15-state region of the central and western U.S. * Vision: Provide premier power marketing and transmission services Rocky Mountain Region (RMR) is one of five regional offices 4 Rocky Mountain Region

471

Decontamination & decommissioning focus area  

SciTech Connect (OSTI)

In January 1994, the US Department of Energy Office of Environmental Management (DOE EM) formally introduced its new approach to managing DOE`s environmental research and technology development activities. The goal of the new approach is to conduct research and development in critical areas of interest to DOE, utilizing the best talent in the Department and in the national science community. To facilitate this solutions-oriented approach, the Office of Science and Technology (EM-50, formerly the Office of Technology Development) formed five Focus AReas to stimulate the required basic research, development, and demonstration efforts to seek new, innovative cleanup methods. In February 1995, EM-50 selected the DOE Morgantown Energy Technology Center (METC) to lead implementation of one of these Focus Areas: the Decontamination and Decommissioning (D & D) Focus Area.

NONE

1996-08-01T23:59:59.000Z

472

Honey Lake Geothermal Area  

Broader source: Energy.gov [DOE]

The Honey Lake geothermal area is located in Lassen County, California and Washoe County, Nevada. There are three geothermal projects actively producing electrical power. They are located at Wendel...

473

AREA 5 RWMS CLOSURE  

National Nuclear Security Administration (NNSA)

153 CLOSURE STRATEGY NEVADA TEST SITE AREA 5 RADIOACTIVE WASTE MANAGEMENT SITE Revision 0 Prepared by Under Contract No. DE-AC52-06NA25946 March 2007 DISCLAIMER Reference herein to...

474

Geographic Area Month  

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

Fuels by PAD District and State (Cents per Gallon Excluding Taxes) - Continued Geographic Area Month No. 1 Distillate No. 2 Distillate a No. 4 Fuel b Sales to End Users Sales for...

475

Operational Area Monitoring Plan  

Office of Legacy Management (LM)

' ' SECTION 11.7B Operational Area Monitoring Plan for the Long -Term H yd rol og ical M o n i to ri ng - Program Off The Nevada Test Site S . C. Black Reynolds Electrical & Engineering, Co. and W. G. Phillips, G. G. Martin, D. J. Chaloud, C. A. Fontana, and 0. G. Easterly Environmental Monitoring Systems Laboratory U. S. Environmental Protection Agency October 23, 1991 FOREWORD This is one of a series of Operational Area Monitoring Plans that comprise the overall Environmental Monitoring Plan for the DOE Field Office, Nevada (DOEINV) nuclear and non- nuclear testing activities associated with the Nevada Test Site (NTS). These Operational Area Monitoring Plans are prepared by various DOE support contractors, NTS user organizations, and federal or state agencies supporting DOE NTS operations. These plans and the parent

476

Bay Area | Open Energy Information  

Open Energy Info (EERE)

Bay Area Bay Area Jump to: navigation, search Contents 1 Clean Energy Clusters in the Bay Area 1.1 Products and Services in the Bay Area 1.2 Research and Development Institutions in the Bay Area 1.3 Networking Organizations in the Bay Area 1.4 Investors and Financial Organizations in the Bay Area 1.5 Policy Organizations in the Bay Area Clean Energy Clusters in the Bay Area Products and Services in the Bay Area Loading map... {"format":"googlemaps3","type":"ROADMAP","types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"limit":500,"offset":0,"link":"all","sort":[""],"order":[],"headers":"show","mainlabel":"","intro":"","outro":"","searchlabel":"\u2026

477

Texas Area | Open Energy Information  

Open Energy Info (EERE)

Area Area Jump to: navigation, search Contents 1 Clean Energy Clusters in the Texas Area 1.1 Products and Services in the Texas Area 1.2 Research and Development Institutions in the Texas Area 1.3 Networking Organizations in the Texas Area 1.4 Investors and Financial Organizations in the Texas Area 1.5 Policy Organizations in the Texas Area Clean Energy Clusters in the Texas Area Products and Services in the Texas Area Loading map... {"format":"googlemaps3","type":"ROADMAP","types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"limit":500,"offset":0,"link":"all","sort":[""],"order":[],"headers":"show","mainlabel":"","intro":"","outro":"","searchlabel":"\u2026

478

Rockies Area | Open Energy Information  

Open Energy Info (EERE)

Rockies Area Rockies Area Jump to: navigation, search Contents 1 Clean Energy Clusters in the Rockies Area 1.1 Products and Services in the Rockies Area 1.2 Research and Development Institutions in the Rockies Area 1.3 Networking Organizations in the Rockies Area 1.4 Investors and Financial Organizations in the Rockies Area 1.5 Policy Organizations in the Rockies Area Clean Energy Clusters in the Rockies Area Products and Services in the Rockies Area Loading map... {"format":"googlemaps3","type":"ROADMAP","types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"limit":500,"offset":0,"link":"all","sort":[""],"order":[],"headers":"show","mainlabel":"","intro":"","outro":"","searchlabel":"\u2026

479

OLED area illumination source  

DOE Patents [OSTI]

The present invention relates to an area illumination light source comprising a plurality of individual OLED panels. The individual OLED panels are configured in a physically modular fashion. Each OLED panel comprising a plurality of OLED devices. Each OLED panel comprises a first electrode and a second electrode such that the power being supplied to each individual OLED panel may be varied independently. A power supply unit capable of delivering varying levels of voltage simultaneously to the first and second electrodes of each of the individual OLED panels is also provided. The area illumination light source also comprises a mount within which the OLED panels are arrayed.

Foust, Donald Franklin (Scotia, NY); Duggal, Anil Raj (Niskayuna, NY); Shiang, Joseph John (Niskayuna, NY); Nealon, William Francis (Gloversville, NY); Bortscheller, Jacob Charles (Clifton Park, NY)

2008-03-25T23:59:59.000Z

480

MEASUREMENT OF BUILDING AREAS MEASUREMENT OF BUILDING AREAS  

E-Print Network [OSTI]

) Common Use Areas All floored areas in the building for circulation and standard facilities provided and the like. These are extracts of NWPC standard method of measurement of building areas with an addition fromSection S ANNEXURE 4 MEASUREMENT OF BUILDING AREAS MEASUREMENT OF BUILDING AREAS 1. GROSS BUILDING

Wang, Yan

Note: This page contains sample records for the topic "rift area thomas" 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

Subsurface contaminants focus area  

SciTech Connect (OSTI)

The US Department of Enregy (DOE) Subsurface Contaminants Focus Area is developing technologies to address environmental problems associated with hazardous and radioactive contaminants in soil and groundwater that exist throughout the DOE complex, including radionuclides, heavy metals; and dense non-aqueous phase liquids (DNAPLs). More than 5,700 known DOE groundwater plumes have contaminated over 600 billion gallons of water and 200 million cubic meters of soil. Migration of these plumes threatens local and regional water sources, and in some cases has already adversely impacted off-site rsources. In addition, the Subsurface Contaminants Focus Area is responsible for supplying technologies for the remediation of numerous landfills at DOE facilities. These landfills are estimated to contain over 3 million cubic meters of radioactive and hazardous buried Technology developed within this specialty area will provide efective methods to contain contaminant plumes and new or alternative technologies for development of in situ technologies to minimize waste disposal costs and potential worker exposure by treating plumes in place. While addressing contaminant plumes emanating from DOE landfills, the Subsurface Contaminants Focus Area is also working to develop new or alternative technologies for the in situ stabilization, and nonintrusive characterization of these disposal sites.

NONE

1996-08-01T23:59:59.000Z

482

Functional Area Dean's Office  

E-Print Network [OSTI]

Functional Area Dean's Office 1101 Ag & Resource Economics 1172 Animal Sciences 1171 Bio Ag Science and Pest Mgmt 1177 Hort & Landscape Architecture 1173 Soil & Crop Science 1170 Ag Colo Res Ctr 3046 Fiscal Officers Jessi Fuentes 1 1931 Val Parker 1 6953 Linda Moller 1 1441 Paula

483

Plutonium focus area  

SciTech Connect (OSTI)

To ensure research and development programs focus on the most pressing environmental restoration and waste management problems at the U.S. Department of Energy (DOE), the Assistant Secretary for the Office of Environmental Management (EM) established a working group in August 1993 to implement a new approach to research and technology development. As part of this new approach, EM developed a management structure and principles that led to the creation of specific Focus Areas. These organizations were designed to focus the scientific and technical talent throughout DOE and the national scientific community on the major environmental restoration and waste management problems facing DOE. The Focus Area approach provides the framework for intersite cooperation and leveraging of resources on common problems. After the original establishment of five major Focus Areas within the Office of Technology Development (EM-50, now called the Office of Science and Technology), the Nuclear Materials Stabilization Task Group (EM-66) followed the structure already in place in EM-50 and chartered the Plutonium Focus Area (PFA). The following information outlines the scope and mission of the EM, EM-60, and EM-66 organizations as related to the PFA organizational structure.

NONE

1996-08-01T23:59:59.000Z

484

A review of "The Ends of Life: Roads to Fulfilment in Early Modern England" by Keith Thomas  

E-Print Network [OSTI]

reviews 59 future of the humanities in general and seventeenth-century studies in particular, H?fer?s study reaffirms the centrality of the grand si?cle through a timely return to a larger concept of the humanities, before that other... of Life: Roads to Fulfilment in Early Modern England. Oxford and New York: Oxford University Press, 2009. xvi + 393 pp. + 14 illus. $60.00. Review by catherine patterson, university of houston In this wide-ranging and engaging book, Keith Thomas brings...

Patterson, Catherine

2010-01-01T23:59:59.000Z

485

A review of "Thomas and Rebecca Vaughans Aqua Vit: Non Vitis" by Donald R. Dickson, ed.  

E-Print Network [OSTI]

to contemporary Anglican sufferings, is an important contribution to understanding. Donald R. Dickson, ed. Thomas and Rebecca Vaughan?s Aqua Vit?: Non Vitis (British Library MS, Sloane 1741). Tempe: Arizona Center for Medieval and Renaissance Studies, 2001..., and the present reviewer. I am writing these words on April 17, the date on which Tho- mas Vaughan?s wife, Rebecca, died: ?My most deare wife sickened on Friday in the Evening, being the 16 of April, and dyed the Saturday following in the Evening, being the 17...

Alan Rudrum

2003-01-01T23:59:59.000Z

486

EA-1177: Salvage/Demolition of 200 West Area, 200 East Area, and 300 Area  

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

7: Salvage/Demolition of 200 West Area, 200 East Area, and 7: Salvage/Demolition of 200 West Area, 200 East Area, and 300 Area Steam Plants, Richland, Washington EA-1177: Salvage/Demolition of 200 West Area, 200 East Area, and 300 Area Steam Plants, Richland, Washington SUMMARY This EA evaluates the environmental impacts for the proposal to salvage and demolish the 200 West Area, 200 East Area, and 300 Area steam plants and their associated steam distribution piping equipment, and ancillary facilities at the U.S. Department of Energy Hanford Site in Richland, Washington. PUBLIC COMMENT OPPORTUNITIES None available at this time. DOCUMENTS AVAILABLE FOR DOWNLOAD October 21, 1996 EA-1177: Finding of No Significant Impact Salvage/Demolition of 200 West Area, 200 East Area, and 300 Area Steam Plants October 21, 1996 EA-1177: Final Environmental Assessment

487

Focus Area Summary  

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

information provided was consolidated from the original five focus areas for the EM information provided was consolidated from the original five focus areas for the EM Corporate QA Board. The status of QAP/QIP approvals etc. was accurate at the time of posting; however, additional approvals may have been achieved since that time. If you have any questions about the information provided, please contact Bob Murray at robert.murray@em.doe.gov Task # Task Description Status 1.1 Develop a brief questionnaire to send out to both commercial and EM contractors to describe their current approach for identifying the applicable QA requirements for subcontractors, tailoring the requirements based upon risk, process for working with procurement to ensure QA requirements are incorporated into subcontracts, and implementing verification of requirement flow-down by their

488

Focus Area 3 Deliverables  

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

3 - Commercial Grade item and Services 3 - Commercial Grade item and Services Dedication Implementation and Nuclear Services Office of Environmental Management And Energy Facility Contractors Group Quality Assurance Improvement Project Plan Project Focus Area Task # and Description Deliverable Project Area 3-Commercial Grade Item and Services Dedication 3.1-Complete a survey of selected EM contractors to identify the process and basis for their CGI dedication program including safety classification of items being dedicated for nuclear applications within their facilities Completed Survey Approvals: Yes/No/NA Project Managers: S. Waisley, D. Tuttel Yes Executive Committee: D. Chung, J. Yanek, N. Barker, D. Amerine No EM QA Corporate Board: No Energy Facility Contractors Group

489

Argonne area restaurants  

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

area restaurants area restaurants Amber Cafe 13 N. Cass Ave. Westmont, IL 60559 630-515-8080 www.ambercafe.net Argonne Guest House Building 460 Argonne, IL 60439 630-739-6000 www.anlgh.org Ballydoyle Irish Pub & Restaurant 5157 Main Street Downers Grove, IL 60515 630-969-0600 www.ballydoylepub.com Bd's Mongolian Grill The Promenade Shopping Center Boughton Rd. & I-355 Bolingbrook, IL 60440 630-972-0450 www.gomongo.com Branmor's American Grill 300 Veterans Parkway Bolingbrook, IL 60440 630-226-9926 www.branmors.com Buca di Beppo 90 Yorktown Convenience Center Lombard, IL 60148 630-932-7673 www.bucadibeppo.com California Pizza Kitchen 551 Oakbrook Center Oak Brook, IL 60523 630-571-7800 www.cpk.com Capri Ristorante 5101 Main Street Downers Grove, IL 60516 630-241-0695 www.capriristorante.com Carrabba's Italian Grill

490

borrow_area.cdr  

Office of Legacy Management (LM)

information information at Weldon Spring, Missouri. This site is managed by the U.S. Department of Energy Office of Legacy Management. developed by the former WSSRAP Community Relations Department to provide comprehensive descriptions of key activities that took place throughout the cleanup process The Missouri Department of Conservation (MDC) approved a plan on June 9, 1995, allowing the U.S. Department of Energy (DOE) at the Weldon Spring Site Remedial Action Project (WSSRAP) to excavate nearly 2 million cubic yards of clay material from land in the Weldon Spring Conservation Area. Clay soil from a borrow area was used to construct the permanent disposal facility at the Weldon Spring site. Clay soil was chosen to construct the disposal facility because it has low permeability when

491

Discussion on the energy content of the galactic dark matter Bose-Einstein condensate halo in the Thomas-Fermi approximation  

E-Print Network [OSTI]

We show that the galactic dark matter halo, considered composed of an axionlike particles Bose-Einstein condensate \\cite{pir12} trapped by a self-graviting potential \\cite{boh07}, may be stable in the Thomas-Fermi approximation since appropriate choices for the dark matter particle mass and scattering length are made. The demonstration is performed by means of the calculation of the potential, kinetic and self-interaction energy terms of a galactic halo described by a Boehmer-Harko density profile. We discuss the validity of the Thomas-Fermi approximation for the halo system, and show that the kinetic energy contribution is indeed negligible.

J. C. C. de Souza; M. O. C. Pires

2014-01-23T23:59:59.000Z

492

Geothermal Areas | Open Energy Information  

Open Energy Info (EERE)

Geothermal Areas Geothermal Areas Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermal Areas Geothermal Areas are specific locations of geothermal potential (e.g., Coso Geothermal Area). The base set of geothermal areas used in this database came from the 253 geothermal areas identified by the USGS in their 2008 Resource Assessment.[1] Additional geothermal areas were added, as needed, based on a literature search and on projects listed in the GTP's 2011 database of funded projects. Add.png Add a new Geothermal Resource Area Map of Areas List of Areas Loading map... {"format":"googlemaps3","type":"ROADMAP","types":["ROADMAP","SATELLITE","HYBRID","TERRAIN"],"limit":2500,"offset":0,"link":"all","sort":[""],"order":[],"headers":"show","mainlabel":"","intro":"","outro":"","searchlabel":"\u2026

493

Western Area Power Administration  

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

v*Zy- i , . v*Zy- i , . r ,v * -i S # Af [, (e- . - o -A tl }r- 0 v-" l^~4~S J l ^-)^ I^U^ck iM clti ^ Area Power Administration Follow-up to Nov. 25, 2008 Transition Meeting Undeveloped Transmission Right-of-Way Western has very little undeveloped transmission right-of-way. There is a 7-mile right- of-way between Folsom, CA and Roseville, CA where Western acquired a 250' wide right-of-way but is only using half of it. Another line could be built parallel to Western's line to relieve congestion in the Sacramento area. In addition, Western has rights-of- way for many transmission lines that could be rebuilt to increase transmission capacity. For example, Western's Tracy-Livermore 230-kV line is a single circuit line but the existing towers could support a double circuit line. These rights-of-way would have to

494

Conceptual Model At Dixie Valley Geothermal Area (Thompson, Et...  

Open Energy Info (EERE)

1984. References George A. Thompson, Laurent J. Meister, Alan T. Herring, Thomas E. Smith, Dennis B. Burke, Robert L. Kovach, Robert O. Burford, Iraj A. Salehi, M. Darroll Wood...

495

CAVERN: The CAVE Research Network Andrew E. Johnson, Jason Leigh, Thomas A. DeFanti, Maxine D. Brown, and Daniel J. Sandin  

E-Print Network [OSTI]

CAVERN: The CAVE Research Network Andrew E. Johnson, Jason Leigh, Thomas A. DeFanti, Maxine D CAVERN, the CAVE Research Network, is an alliance of industrial and research institutions equipped, to at least six in 1997 , so now EVL turns its attention to the design and implementation of CAVERN, the CAVE

Johnson, Andrew

496

The Use of Commingled Plastic Lumber as Construction Materials Thomas J. Nosker, Ph.D., Richard W. Renfree, Ph.D.  

E-Print Network [OSTI]

The Use of Commingled Plastic Lumber as Construction Materials Thomas J. Nosker, Ph.D., Richard W at avoiding land filling post-industrial and post-consumer plastics. This has resulted in creating a supply of impure plastics at much reduced prices with respect to virgin plastics. The possibility exists to clean

497

The limits of feed-forward processing in visual object recognition Gabriel Kreiman1,2, Thomas Serre3 and Tomaso Poggio3  

E-Print Network [OSTI]

The limits of feed-forward processing in visual object recognition Gabriel Kreiman1,2, Thomas Serre) The visual architecture includes forward and back-projections - There are massive back explain many physiological observations 2.1 A hierarchical feed-forward object recognition model (Felleman

Kreiman, Gabriel

498

Contribution to Thomas D. & G. S. Dieckmann (eds.): SEA ICE -AN INTRODUCTION TO ITS PHYSICS, BIOLOGY , CHEMISTRY AND GEOLOGY, Blackwell Science, London, 2003, pp. 22-81  

E-Print Network [OSTI]

1 Contribution to Thomas D. & G. S. Dieckmann (eds.): SEA ICE - AN INTRODUCTION TO ITS PHYSICS to the macroscopic to the regional scale: Growth, microstructure and properties of sea ice1 Hajo Eicken 2 of the importance of sea ice over a wide range of scales in time and space. Considering the degree to which the ice

Eicken, Hajo

499

Office of Purchasing 213 Thomas Boyd Hall -Baton Rouge -Louisiana -70803-3001 -225/578-2176 -FAX 225/578-2292  

E-Print Network [OSTI]

Office of Purchasing 213 Thomas Boyd Hall - Baton Rouge - Louisiana - 70803-3001 - 225 the Purchasing Office; payments will be made through the Office of Accounting Services. Attached is a certificate stands behind our transactions. Our chief business officer is Dr. Jerry J. Baudin, Vice Chancellor

Harms, Kyle E.

500

A GIS-LIKE TRAINING ALGORITHM FOR LOG-LINEAR MODELS WITH HIDDEN Georg Heigold, Thomas Deselaers, Ralf Schluter, and Hermann Ney  

E-Print Network [OSTI]

A GIS-LIKE TRAINING ALGORITHM FOR LOG-LINEAR MODELS WITH HIDDEN VARIABLES Georg Heigold, Thomas with Generalized Iterative Scal- ing (GIS). GIS offers, upon others, the immediate advantages that it is locally convergent, completely parameter free, and guarantees an improvement of the criterion in each step. GIS

Deselaers, Thomas