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1

Z-Axis Tipper Electromagnetics | Open Energy Information  

Open Energy Info (EERE)

Z-Axis Tipper Electromagnetics Z-Axis Tipper Electromagnetics Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Z-Axis Tipper Electromagnetics Details Activities (2) Areas (2) Regions (0) NEPA(1) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Magnetotelluric Techniques Information Provided by Technique Lithology: Stratigraphic/Structural: Hydrological: Thermal: Cost Information Low-End Estimate (USD): 4,827.00482,700 centUSD 4.827 kUSD 0.00483 MUSD 4.827e-6 TUSD / mile Median Estimate (USD): 6,206.14620,614 centUSD 6.206 kUSD 0.00621 MUSD 6.20614e-6 TUSD / mile High-End Estimate (USD): 17,239.291,723,929 centUSD 17.239 kUSD 0.0172 MUSD 1.723929e-5 TUSD / mile Dictionary.png

2

Magnetotelluric measurements  

SciTech Connect

The ideas of flux quantization and Josephson tunneling are reviewed, and the operation of the dc SQUID as a magnetometer is described. The SQUID currently used for magnetotellurics has a sensitivity of 10/sup -14/ T Hz/sup -1/2/, a dynamic range at 10/sup 7/ in a 1 Hz bandwidth, a frequency response from 0 to 40 kHz, and a slewing rate of 5 x 10/sup -5/T s/sup -1/. Recent improvements in sensitivity are discussed: SQUIDS are rapidly approaching the limit imposed by the uncertainty principle. The essential ideas of magnetotelluric (MT) measurements are outlined, and it is shown how the remote reference method can lead to major reductions in bias errors compared to more conventional schemes. The field techniques of the Berkeley group are described. The practical application of MT requires that amplitude and phase spectra of apparent resistivities be transformed into a geologically useful distribution of subsurface resistivities. In many areas where MT is being applied today, the technique may not provide the information needed because stations are too few and widely spaced, or because we are unable to interpret data influenced by complex 3-D resistivity features. The results of two surveys, one detailed, the other regional, over the Klamath Basin, Oregon, are examined. The detailed survey is able to resolve small (1 km wide) structural features that are missed or add a component of spatial aliasing to the regional data. On the other hand, the regional survey avoids truncation effects that may occur when the survey undersamples an area.

Clarke, J.; Goldstein, N.E.

1980-06-01T23:59:59.000Z

3

Magnetotellurics | Open Energy Information  

Open Energy Info (EERE)

Magnetotellurics Magnetotellurics Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Magnetotellurics Details Activities (39) Areas (36) Regions (5) NEPA(8) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Magnetotelluric Techniques Information Provided by Technique Lithology: Rock composition, mineral and clay content Stratigraphic/Structural: Detection of permeable pathways, fracture zones, faults Hydrological: Resistivity influenced by porosity, grain size distribution, permeability, fluid saturation, fluid type and phase state of the pore water Thermal: Resistivity influenced by temperature Cost Information Low-End Estimate (USD): 522.2252,222 centUSD

4

Ball nose milling cutter radius compensation in Z axis for CNC  

Science Journals Connector (OSTI)

A new AutoCAD/VisualLISP based method to substitute the 3D tool radius compensation in Z axis for CNC milling processes is here described. Specific features of VisualLISP programming language combined with AutoCAD facilities are used to gather the data ... Keywords: AutoCAD VisualLISP, CNC milling, Z axis compensation, complex shaped parts, tool radius compensation

Dragoi Mircea Viorel

2009-02-01T23:59:59.000Z

5

Category:Audio-Magnetotellurics | Open Energy Information  

Open Energy Info (EERE)

Audio-Magnetotellurics Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermalpower.jpg Looking for the Audio-Magnetotellurics page? For detailed information on...

6

Magnetotelluric Techniques | Open Energy Information  

Open Energy Info (EERE)

Magnetotelluric Techniques Magnetotelluric Techniques Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Magnetotelluric Techniques Details Activities (0) Areas (0) Regions (0) NEPA(2) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Electromagnetic Sounding Techniques Information Provided by Technique Lithology: Rock composition, mineral and clay content Stratigraphic/Structural: Detection of permeable pathways, fracture zones, faults Hydrological: Resistivity influenced by porosity, grain size distribution, permeability, fluid saturation, fluid type and phase state of the pore water Thermal: Resistivity influenced by temperature Dictionary.png Magnetotelluric Techniques:

7

Definition: Magnetotellurics | Open Energy Information  

Open Energy Info (EERE)

Magnetotellurics Magnetotellurics Jump to: navigation, search Dictionary.png Magnetotellurics Magnetotellurics (MT) is a natural-source (i.e., passive), electromagnetic method that measures the ratio of earth's naturally varying electric and magnetic fields over a wide range of frequencies to determine the resistivity structure of the subsurface (Reynolds, 1997). View on Wikipedia Wikipedia Definition Related Terms sustainability Ret LikeLike UnlikeLike You like this.Sign Up to see what your friends like. rieved from "http://en.openei.org/w/index.php?title=Definition:Magnetotellurics&oldid=502655" Category: Definitions What links here Related changes Special pages Printable version Permanent link Browse properties About us Disclaimers Energy blogs Linked Data Developer services

8

Magnetotelluric Methods | Open Energy Information  

Open Energy Info (EERE)

Magnetotelluric Methods Magnetotelluric Methods Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Magnetotelluric Methods Details Activities (0) Areas (0) Regions (0) NEPA(3) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Information Provided by Technique Lithology: Stratigraphic/Structural: Hydrological: Thermal: Dictionary.png Magnetotelluric Methods: No definition has been provided for this term. Add a Definition References No exploration activities found. Document # Analysis Type Applicant Geothermal Area Lead Agency District Office Field Office Mineral Manager Surface Manager Development Phase(s) Techniques DOI-BLM-NV-C010-2012-0070-CX CX US Navy Geothermal Program Office Dixie Valley Geothermal Area BLM BLM Carson City District Office BLM Stillwater Field Office BLM BLM Geothermal/Exploration Reflection Survey

9

PROJECT COMPLETION REPORT MAGNETOTELLURICS -APPLICATION TO RESOURCE  

E-Print Network (OSTI)

/LITHOSPHERE, IMPROVEMENT OF TECHNIQUES OF DATA ACQUISITION AND INTERPRETATION MLP-5103-28 (THN) NATIONAL GEOPHYSICALPROJECT COMPLETION REPORT MAGNETOTELLURICS - APPLICATION TO RESOURCE EXPLORATION, STUDIES OF CRUST;1 PROJECT COMPLETION REPORT Of MAGNETOTELLURICS ­ APPLICATION TO RESOURCE EXPLORATION, STUDIES OF CRUST

Harinarayana, T.

10

Definition: Magnetotelluric Techniques | Open Energy Information  

Open Energy Info (EERE)

Definition Definition Edit with form History Facebook icon Twitter icon » Definition: Magnetotelluric Techniques Jump to: navigation, search Dictionary.png Magnetotelluric Techniques Magnetotellurics is an electromagnetic geophysical method used to image the electrical resistivity structure of the subsurface through the measurement of electrical and magnetic fields at the earth's surface.[1] View on Wikipedia Wikipedia Definition Magnetotellurics (MT) is an electromagnetic geophysical method of imaging the earth's subsurface by measuring natural variations of electrical and magnetic fields at the Earth's surface. Investigation depth ranges from 300m below ground by recording higher frequencies down to 10,000m or deeper with long-period soundings. Developed in Russia and

11

Audio-Magnetotellurics | Open Energy Information  

Open Energy Info (EERE)

Audio-Magnetotellurics Audio-Magnetotellurics Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Audio-Magnetotellurics Details Activities (4) Areas (4) Regions (0) NEPA(1) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Magnetotelluric Techniques Information Provided by Technique Lithology: Rock composition, mineral and clay content Stratigraphic/Structural: Detection of permeable pathways, fracture zones, faults Hydrological: Resistivity influenced by porosity, grain size distribution, permeability, fluid saturation, fluid type and phase state of the pore water Thermal: Resistivity influenced by temperature Cost Information Low-End Estimate (USD): 1,118.26111,826 centUSD

12

Category:Magnetotelluric Techniques | Open Energy Information  

Open Energy Info (EERE)

Subcategories This category has the following 4 subcategories, out of 4 total. A Audio-Magnetotellurics 1 pages C Controlled Source Audio MT 1 pages M ...

13

Electrical, electromagnetic, and magnetotelluric methods | Open Energy  

Open Energy Info (EERE)

Electrical, electromagnetic, and magnetotelluric methods Electrical, electromagnetic, and magnetotelluric methods Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Electrical, electromagnetic, and magnetotelluric methods Abstract Application of electrical methods began with Robert W. Fox's 1830 observation of self potentials associated with copper vein deposits in Cornwall. Conrad Schlumberger introduced the direct current equal potential line resistivity method in 1912. Harry W. Conklin received the first patents on the electromagnetic (EM) method in 1917. From these beginnings, the history of the development of the resistivity induced-polarization (IP), magnetotelluric and EM methods are traced to the present time. It is of interest to note that application of electrical methods flourished from

14

Magnetotellurics At Glass Mountain Area (Cumming And Mackie,...  

Open Energy Info (EERE)

Area (Cumming And Mackie, 2007) Exploration Activity Details Location Glass Mountain Geothermal Area Exploration Technique Magnetotellurics Activity Date Usefulness useful...

15

Magnetotellurics At Valles Caldera - Redondo Area (Wilt & Haar, 1986) |  

Open Energy Info (EERE)

Magnetotellurics At Valles Caldera - Redondo Area (Wilt & Haar, 1986) Magnetotellurics At Valles Caldera - Redondo Area (Wilt & Haar, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Valles Caldera - Redondo Area (Wilt & Haar, 1986) Exploration Activity Details Location Valles Caldera - Redondo Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Magnetotelluric results indicate deep low resistivity at the western edge of the caldera which may be associated with deep hot fluids. On the basis of geophysical and well data, we make three estimates of reservoir dimensions. Telluric profiles, magnetotelluric sounding, dc resistivity, and electromagnetic sounding surveys were all performed over the caldera in hopes of outlining deep drilling targets (Group 7 Inc., 1972; McPhar, 1973;

16

Magnetotellurics At Long Valley Caldera Geothermal Area (Hermance...  

Open Energy Info (EERE)

Hermance, Et Al., 1988) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Long Valley Caldera Geothermal Area (Hermance, Et...

17

Magnetotellurics At Beowawe Hot Springs Area (Garg, Et Al., 2007...  

Open Energy Info (EERE)

Garg, Et Al., 2007) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Beowawe Hot Springs Area (Garg, Et Al., 2007) Exploration...

18

Audio-Magnetotellurics At Chena Geothermal Area (Holdmann, Et...  

Open Energy Info (EERE)

Chena Geothermal Area (Holdmann, Et Al., 2006) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Audio-Magnetotellurics At Chena Geothermal Area...

19

MAGNETOTELLURIC SURVEYING AND MONITORING AT THE COSO GEOTHERMAL...  

Open Energy Info (EERE)

changes in the underground resistivity properties in the vicinity of injection due to fracture porosity enhancement. To these ends, we are acquiring a dense grid of magnetotelluric...

20

Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood...  

Open Energy Info (EERE)

Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood & Mabey, 1978) Exploration...

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Magnetotellurics At Coso Geothermal Area (2006) | Open Energy Information  

Open Energy Info (EERE)

Magnetotellurics At Coso Geothermal Area (2006) Magnetotellurics At Coso Geothermal Area (2006) Exploration Activity Details Location Coso Geothermal Area Exploration Technique Magnetotellurics Activity Date 2006 Usefulness useful DOE-funding Unknown Exploration Basis Use magnetotelluric data to model the reservoir. Notes Magnetotelluric (MT) data from 101 tensor stations over the East Flank of the Coso geothermal field, southeastern California, were inverted on a PC using a 3-D Gauss-Newton regularization algorithm based on a staggered-grid, finite difference forward problem and jacobians. Static shifts at each MT site can be included as additional parameters and solved for simultaneously. Recent modifications to the algorithm developed here include the addition of an LU solver to calculate the model parameter

22

Magnetotellurics At Grass Valley Area (Morrison, Et Al., 1979) | Open  

Open Energy Info (EERE)

Grass Valley Area (Morrison, Et Al., 1979) Grass Valley Area (Morrison, Et Al., 1979) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Grass Valley Area (Morrison, Et Al., 1979) Exploration Activity Details Location Grass Valley Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes The attempt to carry out a detailed interpretation of a magnetotelluric survey has demonstrated some fundamental problems that must be addressed in future surveys and in future research. (see paper conclusions) References H. Frank Morrison, K i Ha Lee, Gary Oppliger, Abhi jit De (1979) Magnetotelluric Studies In Grass Valley, Nevada Retrieved from "http://en.openei.org/w/index.php?title=Magnetotellurics_At_Grass_Valley_Area_(Morrison,_Et_Al.,_1979)&oldid=387832"

23

DOI-BLM-NV-B020-2010-0106-CX | Open Energy Information  

Open Energy Info (EERE)

-0106-CX -0106-CX Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: DOI-BLM-NV-B020-2010-0106-CX CX at Alum Geothermal Area for Geothermal/Exploration {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CX Applicant Sierra Geothermal Power Geothermal Area Alum Geothermal Area Project Location California Project Phase Geothermal/Exploration Techniques Hyperspectral Imaging, Magnetic Techniques, Magnetotellurics, Slim Holes, Z-Axis Tipper Electromagnetics Comments airborne thermal survey Time Frame (days) Application Time 182 Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Battle Mountain Managing Field Office BLM Tonopah Field Office

24

A Target-Oriented Magnetotelluric Inversion Approach For Characterizing The  

Open Energy Info (EERE)

Target-Oriented Magnetotelluric Inversion Approach For Characterizing The Target-Oriented Magnetotelluric Inversion Approach For Characterizing The Low Enthalpy Gross Schonebeck Geothermal Reservoir Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Target-Oriented Magnetotelluric Inversion Approach For Characterizing The Low Enthalpy Gross Schonebeck Geothermal Reservoir Details Activities (0) Areas (0) Regions (0) Abstract: Electrical conductivity is a key parameter for the exploration and characterization of geothermal reservoirs as hot mineralized formation water of active geothermal areas usually exhibits significantly higher conductivity than the surrounding host rock. Here we present results of a magnetotelluric (MT) exploration experiment carried out in the vicinity of the Gross Schonebeck geothermal test site in Northern Germany, where a

25

Three-dimensional magnetotelluric characterization of the Coso geothermal  

Open Energy Info (EERE)

magnetotelluric characterization of the Coso geothermal magnetotelluric characterization of the Coso geothermal field Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Three-dimensional magnetotelluric characterization of the Coso geothermal field Details Activities (1) Areas (1) Regions (0) Abstract: A dense grid of 125 magnetotelluric (MT) stations plus a single line of contiguous bipole array profiling has been acquired over the east flank of the Coso geothermal system, CA, USA. Due to production related electromagnetic (EM) noise the permanent observatory at Parkfield, CA was used as a remote reference to suppress this cultural EM noise interference. These data have been inverted to a fully three-dimensional (3D) resistivity model. This model shows the controlling geological structures possibly

26

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

27

Magnetotellurics At Socorro Mountain Area (Owens, Et Al., 2005) | Open  

Open Energy Info (EERE)

Owens, Et Al., 2005) Owens, Et Al., 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Socorro Mountain Area (Owens, Et Al., 2005) Exploration Activity Details Location Socorro Mountain Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes magneto-telluric surveys are pending for the near future when geochemical and surface geophysical surveys are complete. Results of this survey should verify the occurrence of low-resisitivity fluids and alteration at depth. References Lara Owens, Richard Baars, David Norman, Harold Tobin (2005) New Methods In Exploration At The Socorro Peak Kgra- A Gred Iii Project Retrieved from "http://en.openei.org/w/index.php?title=Magnetotellurics_At_Socorro_Mountain_Area_(Owens,_Et_Al.,_2005)&oldid=388765

28

Magnetotellurics At Truckhaven Area (Layman Energy Associates, 2010) | Open  

Open Energy Info (EERE)

Magnetotellurics At Truckhaven Area (Layman Energy Magnetotellurics At Truckhaven Area (Layman Energy Associates, 2010) Exploration Activity Details Location Truckhaven Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes The area of coverage for the DOE-funded geophysical surveys is shown in Figure 9. The 95 magnetotelluric (MT) soundings cover a central area of about 80 square kilometers. The 126 gravity stations extend over a broader area of about 150 square kilometers, centered on the same area covered by the MT soundings. A detailed description of the instrumentation and data acquisition procedures used for both surveys is provided in GSY-USA, Inc. (2003a). References Layman Energy Associates Inc. (2006) Final Scientific - Technical Report, Geothermal Resource Exploration Program, Truckhaven Area, Imperial

29

Magnetotellurics At Raft River Geothermal Area (1977) | Open Energy  

Open Energy Info (EERE)

Magnetotellurics At Raft River Geothermal Area (1977) Magnetotellurics At Raft River Geothermal Area (1977) Exploration Activity Details Location Raft River Geothermal Area Exploration Technique Magnetotellurics Activity Date 1977 Usefulness useful DOE-funding Unknown Notes Magnetotelluric soundings along a profile extending from the Raft River geothermal area in southern Idaho in Yellowstone National Park in Wyoming reveal a highly anomalous crustal structure involving a conductive zone at depths that range from 18 km in the central part of the eastern Snake River Plain to 7 km beneath the Raft River thermal area and as little as 5 km in Yellowstone. Resistivities in this conductive zone are less than 10 ohm-m and at some sites than 1 ohm-m. References Stanley, W.D.; Boehl, J.E.; Bostick, F.X.; Smith, H.W. (10 June

30

An Audio-Magnetotelluric Investigation In Terceira Island (Azores) | Open  

Open Energy Info (EERE)

Audio-Magnetotelluric Investigation In Terceira Island (Azores) Audio-Magnetotelluric Investigation In Terceira Island (Azores) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: An Audio-Magnetotelluric Investigation In Terceira Island (Azores) Details Activities (0) Areas (0) Regions (0) Abstract: Ten audio-magnetotelluric soundings have been carried out along a profile crossing the Serra do Cume caldera in the eastern part of the Terceira Island (Azores). The main objectives of this investigation were to detect geoelectrical features related with tectonic structures and to characterize regional hydrological and hydrothermal aspects mainly those related to geothermal fluid dynamics. Three-dimensional numerical investigation showed that the data acquired at periods shorter than 1 s are not significantly affected by ocean effect. The data was analysed using the

31

Magnetotellurics At Coso Geothermal Area (2004) | Open Energy Information  

Open Energy Info (EERE)

Magnetotellurics At Coso Geothermal Area (2004) Magnetotellurics At Coso Geothermal Area (2004) Exploration Activity Details Location Coso Geothermal Area Exploration Technique Magnetotellurics Activity Date 2004 Usefulness not indicated DOE-funding Unknown Exploration Basis EGS potential of Coso Geothermal Region Notes A dense grid of magnetotelluric (MT) stations plus contiguous bipole array profiling centered over the east flank of the Coso geothermal system is being acquired. Acquiring good quality MT data in producing geothermal systems is a challenge due to production related electromagnetic (EM) noise and, in the case of Coso, due to proximity of a regional DC intertie power transmission line. To achieve good results, a remote reference completely outside the influence of the dominant source of EM noise must be

32

A Magnetotelluric Survey Of The Nissyros Geothermal Field (Greece) | Open  

Open Energy Info (EERE)

Magnetotelluric Survey Of The Nissyros Geothermal Field (Greece) Magnetotelluric Survey Of The Nissyros Geothermal Field (Greece) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Magnetotelluric Survey Of The Nissyros Geothermal Field (Greece) Details Activities (0) Areas (0) Regions (0) Abstract: A preliminary magnetotelluric study consisting of twenty measurements, in the frequency range 128-0.016 Hz, was undertaken on the active volcanic island of Nissyros. Two boreholes identify the existence of high enthalpy manifestations. The results correlate well with the borehole logs and delineate, in a 1-D approximation, the existence and symmetry of a possible geothermal reservoir. Some of the main faulting features were detected as well as an inferred highly conductive zone at the centre of the

33

Magnetotellurics At Valles Caldera - Sulphur Springs Area (Wilt & Haar,  

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 » Magnetotellurics At Valles Caldera - Sulphur Springs Area (Wilt & Haar, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Valles Caldera - Sulphur Springs Area (Wilt & Haar, 1986) Exploration Activity Details Location Valles Caldera - Sulphur Springs Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Magnetotelluric results indicate deep low resistivity at the western edge of the caldera which may be associated with deep hot fluids. On the basis of geophysical and well data, we make three estimates of reservoir

34

A Broadband Tensorial Magnetotelluric Study In The Travale Geothermal Field  

Open Energy Info (EERE)

Broadband Tensorial Magnetotelluric Study In The Travale Geothermal Field Broadband Tensorial Magnetotelluric Study In The Travale Geothermal Field Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Broadband Tensorial Magnetotelluric Study In The Travale Geothermal Field Details Activities (0) Areas (0) Regions (0) Abstract: As a contribution to the EEC study of the potential contribution of electric and electromagnetic techniques to geothermal exploration, magnetotelluric studies have been undertaken with a sounding bandwidth ranging from 2 to 7 decades of period at more than 30 sites within the chosen test area of Travale. This area must be one of the most unfavourable for the application of electrical techniques on account both of the thickness (up to 2 km) of conducting (< 1 ohm / m in some locations) cover

35

MAGNETOTELLURICS -APPLICATION TO RESOURCE EXPLORATION, STUDIES OF CRUST/LITHOSPHERE,  

E-Print Network (OSTI)

OF TECHNIQUES OF DATA ACQUISITION AND INTERPRETATION NATIONAL GEOPHYSICAL RESEARCH INSTITUTE (COUNCILMAGNETOTELLURICS - APPLICATION TO RESOURCE EXPLORATION, STUDIES OF CRUST/LITHOSPHERE, IMPROVEMENT: NGRI-2009-EXP- MAGNETOTELLURICS ­ APPLICATION TO RESOURCE EXPLORATION, STUDIES OF CRUST / LITHOSPHERE

Harinarayana, T.

36

Geothermal significance of magnetotelluric sounding in the eastern Snake  

Open Energy Info (EERE)

significance of magnetotelluric sounding in the eastern Snake significance of magnetotelluric sounding in the eastern Snake River Plain-Yellowstone Region Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: Geothermal significance of magnetotelluric sounding in the eastern Snake River Plain-Yellowstone Region Details Activities (1) Areas (1) Regions (0) Abstract: Magnetotelluric soundings along a profile extending from the Raft River geothermal area in southern Idaho in Yellowstone National Park in Wyoming reveal a highly anamalous crustal structure involving a conductive zone at depths that range from 18 km in the central part of the eastern Snake River Plain to 7 km beneath the Raft River thermal area and as little as 5 km in Yellowstone. Resistivities in this conductive zone are less than

37

Further Analysis of 3D Magnetotelluric Measurements Over the Coso  

Open Energy Info (EERE)

Further Analysis of 3D Magnetotelluric Measurements Over the Coso Further Analysis of 3D Magnetotelluric Measurements Over the Coso Geothermal Field Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Proceedings: Further Analysis of 3D Magnetotelluric Measurements Over the Coso Geothermal Field Details Activities (1) Areas (1) Regions (0) Abstract: At last year's GRC annual meeting we presented initial results of a 3D investigation of the Coso Geothermal field utilizing a dense grid of magnetotelluric (MT) stations plus a single line of contiguous bipole array profiling over the east flank of the field (Newman et al., 2005). Motivation for this study is that electrical resistivity/ conductivity mapping can contribute to better improved understanding of enhanced geothermal systems (EGS) by imaging the geometry, bounds and controlling

38

New approaches to estimation of magnetotelluric parameters  

SciTech Connect

Fully efficient robust data processing procedures were developed and tested for single station and remote reference magnetotelluric (Mr) data. Substantial progress was made on development, testing and comparison of optimal procedures for single station data. A principal finding of this phase of the research was that the simplest robust procedures can be more heavily biased by noise in the (input) magnetic fields, than standard least squares estimates. To deal with this difficulty we developed a robust processing scheme which combined the regression M-estimate with coherence presorting. This hybrid approach greatly improves impedance estimates, particularly in the low signal-to-noise conditions often encountered in the dead band'' (0.1--0.0 hz). The methods, and the results of comparisons of various single station estimators are described in detail. Progress was made on developing methods for estimating static distortion parameters, and for testing hypotheses about the underlying dimensionality of the geological section.

Egbert, G.D.

1991-01-01T23:59:59.000Z

39

Initial Results of Magnetotelluric Array Surveying at the Dixie Valley  

Open Energy Info (EERE)

Initial Results of Magnetotelluric Array Surveying at the Dixie Valley Initial Results of Magnetotelluric Array Surveying at the Dixie Valley Geothermal Area, with Implications for Structural Controls and Hydrothermal Alteration Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Initial Results of Magnetotelluric Array Surveying at the Dixie Valley Geothermal Area, with Implications for Structural Controls and Hydrothermal Alteration Abstract A new generation MT array measurement system was applied in a contiguous bipole deployment at the Dixie Valley thermal area. Basic goals of the survey area are 1), resolve a fundamental structural ambiguity at the Dixie Valley thermal area (single range front fault versus shallower, stepped pediment; 2) delineate fault zones which have experienced fluid flux as

40

Magnetotellurics At Northern Basin & Range Region (Pritchett, 2004) | Open  

Open Energy Info (EERE)

Magnetotellurics At Northern Basin & Range Region Magnetotellurics At Northern Basin & Range Region (Pritchett, 2004) Exploration Activity Details Location Northern Basin and Range Geothermal Region Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes NOTE: These are theoretical/computer simulation tests of various methods on eight hypothetical 'model' basing-and-range geothermal systems. "The 300-meter heat flow holes are essentially useless for finding the "hidden" reservoirs. Clearly, the best results are obtained from the SP and MT surveys, with DC resistivity a close third. It is concluded that the best way to find "hidden" basin and range geothermal resources of this general type is to carry out simultaneous SP and low-frequency MT surveys, and then

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Magnetotellurics At Stillwater Area (Laney, 2005) | Open Energy Information  

Open Energy Info (EERE)

Magnetotellurics At Stillwater Area (Laney, 2005) Magnetotellurics At Stillwater Area (Laney, 2005) Exploration Activity Details Location Stillwater Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Structural Controls, Alteration, Permeability and Thermal Regime of Dixie Valley from New-Generation Mt/Galvanic Array Profiling, Phillip Wannamaker. A new-generation MT/DC array resistivity measurement system was applied at the Dixie Valley thermal area. Basic goals of the survey are 1), resolve a fundamental structural ambiguity at the Dixie Valley thermal area (single rangefront fault versus shallower, stepped pediment; 2), delineate fault zones which have experienced fluid flux as indicated by low resistivity; 3), image the disposition of resistive, possible reservoir formations in

42

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

43

Magnetotellurics At Salt Wells Area (Bureau of Land Management, 2009) |  

Open Energy Info (EERE)

Salt Wells Area (Bureau of Land Management, 2009) Salt Wells Area (Bureau of Land Management, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Salt Wells Area (Bureau of Land Management, 2009) Exploration Activity Details Location Salt Wells Geothermal Area Exploration Technique Magnetotellurics Activity Date 2008 - 2008 Usefulness not indicated DOE-funding Unknown Exploration Basis Vulcan increased exploration efforts in the summer and fall of 2008, during which time the company drilled two temperature gradient holes (86-15 O on Pad 1 and 17-16 O on Pad 3); conducted seismic, gravity and magnetotelluric surveys; and drilled deep exploration wells at Pads 6 and 8 and binary wells at Pads 1, 2, 4, and 7. Notes Data from these wells is proprietary, and so were unavailable for inclusion

44

3D Magnetotelluric Characterization Of The Geothermal Anomaly In The  

Open Energy Info (EERE)

Magnetotelluric Characterization Of The Geothermal Anomaly In The Magnetotelluric Characterization Of The Geothermal Anomaly In The Llucmajor Aquifer System (Majorca, Spain) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: 3D Magnetotelluric Characterization Of The Geothermal Anomaly In The Llucmajor Aquifer System (Majorca, Spain) Details Activities (0) Areas (0) Regions (0) Abstract: In the Llucmajor aquifer system (Majorca Island, Spain) some geothermal evidences have appeared. This phenomenon is not isolated to Majorca and it is present in other areas, where it can be associated with structural conditions, especially to the extensional event suffered by the island after the Alpine Orogeny. However, the origin of this anomaly in Llucmajor is not well known, and there is no surface geological evidence of

45

Schlumberger soundings, audio-magnetotelluric soundings and telluric  

Open Energy Info (EERE)

soundings, audio-magnetotelluric soundings and telluric soundings, audio-magnetotelluric soundings and telluric mapping in and around the Coso Range, California Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Report: Schlumberger soundings, audio-magnetotelluric soundings and telluric mapping in and around the Coso Range, California Details Activities (4) Areas (2) Regions (0) Abstract: Results of geophysical surveys in and around the Coso Range, and in particular in the area surrounding Coso Hot Springs are reported. Electrical properties of rocks associated with thermal phenomena of the Devil's Kitchen-Coso Hot Springs area in the Coso rhyolite dome field and the large arcuate fracture system previously postulated to represent a stage of incipient caldera formation were studied. Six individual plates

46

Magnetotellurics At Truckhaven Area (Warpinski, Et Al., 2004) | Open Energy  

Open Energy Info (EERE)

Magnetotellurics At Truckhaven Area (Warpinski, Et Magnetotellurics At Truckhaven Area (Warpinski, Et Al., 2004) Exploration Activity Details Location Truckhaven Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes The Truckhaven project, which is located on the west flank of the Salton Trough in southern California, is north and west of several existing geothermal power generation facilities in the trough. An extensive shallow geothermal anomaly is known to exist in this area and this region corresponds to a gravity high, which has been further delineated by the drilling of numerous shallow temperature gradient wells and one deep, abandoned, test well. Layman Energy Associates has performed Phase I exploration tasks to further constrain the anomaly, including a detailed

47

Magnetotelluric Studies In Grass Valley, Nevada | Open Energy Information  

Open Energy Info (EERE)

Studies In Grass Valley, Nevada Studies In Grass Valley, Nevada Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Reference Material: Magnetotelluric Studies In Grass Valley, Nevada Details Activities (1) Areas (1) Regions (0) Abstract: A program of detail magnetotelluric soundings was initiated in 1974 in Green Valley, Nevada, as part of the Lawrence Berkeley Laboratory's major study of techniques for geothermal exploration in north central Nevada. The magnetotelluric program had three main goals; the determination of resistivity distribution at depths greater than that conveniently measured with other techniques; a comparison of the interpreted resistivity at shallow depth with the results of the other techniques ; and the evaluation of the SQUID or Josephson effect magnetometer i n practical

48

Magnetotellurics At Dixie Valley Geothermal Field Area (Laney, 2005) | Open  

Open Energy Info (EERE)

2005) 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Dixie Valley Geothermal Field Area (Laney, 2005) Exploration Activity Details Location Dixie Valley Geothermal Field Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Structural Controls, Alteration, Permeability and Thermal Regime of Dixie Valley from New-Generation Mt/Galvanic Array Profiling, Phillip Wannamaker. A new-generation MT/DC array resistivity measurement system was applied at the Dixie Valley thermal area. Basic goals of the survey are 1), resolve a fundamental structural ambiguity at the Dixie Valley thermal area (single rangefront fault versus shallower, stepped pediment; 2), delineate fault

49

Magnetotellurics At International Geothermal Area, Indonesia (Laney, 2005)  

Open Energy Info (EERE)

(Laney, 2005) (Laney, 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At International Geothermal Area Indonesia (Laney, 2005) Exploration Activity Details Location International Geothermal Area Indonesia Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Improving Exploration Models of Andesite-Hosted Geothermal Systems, Allis, Browne, Bruton, Christensen, Hulen, Lutz, Mindenhall, Nemcok, Norman, Powell and Stimac. The approach we are using is to characterize the petrology, geochemistry and fractures in core and cuttings samples and then integrate these data with measured downhole temperatures and pressures and with the compositions of the reservoir fluids. Our investigations represent

50

Magnetotellurics At Akutan Fumaroles Area (Kolker, Et Al., 2010) | Open  

Open Energy Info (EERE)

Akutan Fumaroles Area (Kolker, Et Al., 2010) Akutan Fumaroles Area (Kolker, Et Al., 2010) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Akutan Fumaroles Area (Kolker, Et Al., 2010) Exploration Activity Details Location Akutan Fumaroles Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes "The 2009 MT survey detects a resistivity pattern typical of most economically viable geothermal reservoirs where a low resistivity, low permeability hydrothermal smectite alteration layer caps a higher temperature, permeable geothermal reservoir. The MT resistivity pattern indicates that a hydrothermally altered clay cap exists near the fumarole and probably overlies an outflow connection from the fumarole to the

51

Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural Analysis to Identify Hidden, High Enthalpy, Extensional Geothermal Systems  

Energy.gov (U.S. Department of Energy (DOE))

Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural Analysis to Identify Hidden, High Enthalpy, Extensional Geothermal Systems presentation at the April 2013 peer review meeting held in Denver, Colorado.

52

3D MAGNETOTELLURIC CHARACTERIZATION OF THE COSO GEOTHERMAL FIELD | Open  

Open Energy Info (EERE)

CHARACTERIZATION OF THE COSO GEOTHERMAL FIELD CHARACTERIZATION OF THE COSO GEOTHERMAL FIELD Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Proceedings: 3D Magnetotelluric characterization of the COSO Geothermal Field Details Activities (0) Areas (0) Regions (0) Abstract: Knowledge of the subsurface electrical resistivity/conductivity can contribute to a better understanding of complex hydrothermal systems, typified by Coso geothermal field, through mapping the geometry (bounds and controlling structures) over existing production. Three-dimensional magnetotelluric (MT) inversion is now an emerging technology for characterizing the resistivity structures of complex geothermal systems. The method appears to hold great promise, but histories exploiting truly 3D inversion that demonstrate the advantages that can be gained by acquiring

53

Audio-Magnetotellurics At Coso Geothermal Area (1977) | Open Energy  

Open Energy Info (EERE)

Coso Geothermal Area (1977) Coso Geothermal Area (1977) Exploration Activity Details Location Coso Geothermal Area Exploration Technique Audio-Magnetotellurics Activity Date 1977 Usefulness not indicated DOE-funding Unknown Exploration Basis To investigate electrical properties of rocks associated with thermal phenomena of the Devil's Kitchen-Coso Hot Springs area Notes Audio-magnetotelluric geophysical surveys determined that the secondary low in the geothermal area, best defined by the 7.5-Hz AMT map and dc soundings, is caused by a shallow conductive zone (5--30 ohm m) interpreted to be hydrothermally altered Sierra Nevada basement rocks containing saline water of a hot water geothermal system. This zone of lowest apparent resistivities over the basement rocks lies within a closed contour of a

54

Magnetotellurics At Walker-Lane Transitional Zone Region (Pritchett, 2004)  

Open Energy Info (EERE)

Walker-Lane Transitional Zone Region (Pritchett, 2004) Walker-Lane Transitional Zone Region (Pritchett, 2004) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Walker-Lane Transitional Zone Region (Pritchett, 2004) Exploration Activity Details Location Walker-Lane Transition Zone Geothermal Region Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes NOTE: These are theoretical/computer simulation tests of various methods on eight hypothetical 'model' basing-and-range geothermal systems. "The 300-meter heat flow holes are essentially useless for finding the "hidden" reservoirs. Clearly, the best results are obtained from the SP and MT surveys, with DC resistivity a close third. It is concluded that the best

55

Magnetotellurics At Central Nevada Seismic Zone Region (Pritchett, 2004) |  

Open Energy Info (EERE)

Pritchett, 2004) Pritchett, 2004) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Central Nevada Seismic Zone Region (Pritchett, 2004) Exploration Activity Details Location Central Nevada Seismic Zone Geothermal Region Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes NOTE: These are theoretical/computer simulation tests of various methods on eight hypothetical 'model' basing-and-range geothermal systems. "The 300-meter heat flow holes are essentially useless for finding the "hidden" reservoirs. Clearly, the best results are obtained from the SP and MT surveys, with DC resistivity a close third. It is concluded that the best way to find "hidden" basin and range geothermal resources of this general

56

Audio-magnetotellurics (AMT) for steeply-dipping mineral targets: importance of multi-component measurements at each site  

E-Print Network (OSTI)

Audio-magnetotellurics (AMT) for steeply-dipping mineral targets: importance of multi- component-dipping mineralized bodies present a particular problem for audio-magnetotelluric (AMT) exploration. Such targets have-source audio- magnetotelluric (AMT) method becomes an attractive tool. AMT has advanced significantly since

Jones, Alan G.

57

MAGNETOTELLURIC INVESTIGATIONS IN THE GEOTHERMAL FIELDS OF SATLUJ-SPITI, BEAS-PARBATI VALLEYS IN  

E-Print Network (OSTI)

Although, many countries are utiliszing the geothermal energy for power generation, India is yet to joinMAGNETOTELLURIC INVESTIGATIONS IN THE GEOTHERMAL FIELDS OF SATLUJ-SPITI, BEAS- PARBATI VALLEYS.NGRI-2008-EXP-637 MAGNETOTELLURIC INVESTIGATIONS IN GEOTHERMAL FIELDS OF SATLUJ-SPITI, BEAS- PARBATI VALLEYS

Harinarayana, T.

58

2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets-  

Open Energy Info (EERE)

D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth Details Activities (0) Areas (0) Regions (0) Abstract: With the aim of investigating the possibilities of magnetotelluric methods for the exploration of potential Enhanced Geothermal System (EGS) sites in the Upper Rhine valley, a 2-D magnetotelluric (MT) survey has been carried out on a 13 km long profile across the thermal anomaly in the area of the geothermal power plant of Soultz-sous-Forets in the winter 2007/08. Despite strong artificial noise, processing using remote referencing and Sutarno phase consistent smoothing

59

Audio-Magnetotellurics At Chena Area (Erkan, Et. Al., 2008) | Open Energy  

Open Energy Info (EERE)

Chena Geothermal Area Chena Geothermal Area (Erkan, Et. Al., 2008) Exploration Activity Details Location Chena Geothermal Area Exploration Technique Audio-Magnetotellurics Activity Date Usefulness not useful DOE-funding Unknown Notes An audio-magnetotelluric (AMT) survey was also carried out in August 2005 covering about 3 km_3 km around the CHS. Using controlled-source audio-magnetotelluric (CSAMT) and natural-source audio-magnetotelluric (NSAMT) methods, 1D and 2D inversions of the data were subsequently performed (Reed and Liu, 2006). The AMT results did not show an obvious low-resistivity anomaly in the vicinity of the hot springs. References Kamil Erkan, Gwen Holdmann, Walter Benoit, David Blackwell (2008) Understanding The Chena Hot Springs, Alaska, Geothermal System Using

60

Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood & Mabey,  

Open Energy Info (EERE)

Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood & Mabey, Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood & Mabey, 1978) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Audio-Magnetotellurics At Baltazor Hot Springs Area (Isherwood & Mabey, 1978) Exploration Activity Details Location Baltazor Hot Springs Area Exploration Technique Audio-Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes The 27 Hz AMT map (Fig. 5a) defines a resistivity low near the hot spring with minimum values of 2.5 ohm-m; the deeper probing 7.5 Hz map (Fig. 5b) defines a similar low with minimum values of 1.6 ohm-m. Both maps show a second low to the south apparently associated with the low-density Cenozoic sediments. Three telluric profiles across the KGRA also define a low of

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61

3-D Interpretation Of Magnetotelluric Data At The Bajawa Geothermal Field,  

Open Energy Info (EERE)

3-D Interpretation Of Magnetotelluric Data At The Bajawa Geothermal Field, 3-D Interpretation Of Magnetotelluric Data At The Bajawa Geothermal Field, Indonesia Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Paper: 3-D Interpretation Of Magnetotelluric Data At The Bajawa Geothermal Field, Indonesia Details Activities (0) Areas (0) Regions (0) Abstract: Three-dimensional (3-D) interpretation was carried out for the magnetotelluric (MT) data obtained in a geothermal area in Indonesia. The inversion scheme was based on the linearized leastsquares method with smoothness regularization. In addition to the subsurface resistivity structure, static shifts were also included as unknown parameters in the inversion. Forward modeling was by the finite difference scheme. The sensitivity matrix was computed once for a homogeneous half space and used

62

Magnetotellurics At U.S. West Region (Aiken & Ander, 1981) | Open Energy  

Open Energy Info (EERE)

Aiken & Ander, 1981) Aiken & Ander, 1981) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At U.S. West Region (Aiken & Ander, 1981) Exploration Activity Details Location U.S. West Region Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes Arizona, New Mexico, and southern Colorado 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=Magnetotellurics_At_U.S._West_Region_(Aiken_%26_Ander,_1981)&oldid=389969" Category: Exploration Activities What links here Related changes Special pages Printable version Permanent link Browse properties

63

A Closely-Spaced Magnetotelluric Study Of The Ahuachapan-Chipilapa  

Open Energy Info (EERE)

Closely-Spaced Magnetotelluric Study Of The Ahuachapan-Chipilapa Closely-Spaced Magnetotelluric Study Of The Ahuachapan-Chipilapa Geothermal Field, El Salvador Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Closely-Spaced Magnetotelluric Study Of The Ahuachapan-Chipilapa Geothermal Field, El Salvador Details Activities (0) Areas (0) Regions (0) Abstract: The distribution of electrical conductivity beneath the Ahuachapan-Chipilapa geothermal area was simulated using 2-D models based on 126 closely-spaced magnetotelluric (MT) measurements. The observed MT response was interpreted as being produced by the superposition of two orthogonal geological structural systems: an approximately E-W regional trend associated with the Central Graben structure, which affects the longer period response, and a local and younger N-S fault system that is

64

2D Joint Inversion Of Dc And Scalar Audio-Magnetotelluric Data In The  

Open Energy Info (EERE)

Joint Inversion Of Dc And Scalar Audio-Magnetotelluric Data In The Joint Inversion Of Dc And Scalar Audio-Magnetotelluric Data In The Evaluation Of Low Enthalpy Geothermal Fields Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: 2D Joint Inversion Of DC And Scalar Audio-Magnetotelluric Data In The Evaluation Of Low Enthalpy Geothermal Fields Details Activities (0) Areas (0) Regions (0) Abstract: Audio-magnetotelluric (AMT) and resistivity (dc) surveys are often used in environmental, hydrological and geothermal evaluation. The separate interpretation of those geophysical data sets assuming two-dimensional models frequently produces ambiguous results. The joint inversion of AMT and dc data is advocated by several authors as an efficient method for reducing the ambiguity inherent to each of those

65

Station location map and audio-magnetotelluric data log for Rye...  

Open Energy Info (EERE)

location map and audio-magnetotelluric data log for Rye Patch known geothermal resource area Jump to: navigation, search OpenEI Reference LibraryAdd to library Map: Station...

66

A Five-Component Magneto-Telluric Method In Geothermal Exploration...  

Open Energy Info (EERE)

Article: A Five-Component Magneto-Telluric Method In Geothermal Exploration- The Mt-5-Ex Abstract The present paper describes a new method designed both at recording and...

67

Three-Dimensional Inversion of Magnetotelluric Data on a PC, Methodology  

Open Energy Info (EERE)

Dimensional Inversion of Magnetotelluric Data on a PC, Methodology Dimensional Inversion of Magnetotelluric Data on a PC, Methodology and Applications to the Coso Geothermal Field Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Proceedings: Three-Dimensional Inversion of Magnetotelluric Data on a PC, Methodology and Applications to the Coso Geothermal Field Details Activities (1) Areas (1) Regions (0) Abstract: We describe here efforts in technology development to invert magnetotelluric (MT) data collected in geothermal settings for three-dimensional resistivity models using desktop PC's or small clusters. A finite difference scheme is utilized for the forward problem, with various options to compute the parameter Jacobians, and parameter step estimates are defined using an explicit Gauss-Newton step. The paper

68

Application Of 3D Inversion To Magnetotelluric Data In The Ogiri Geothermal  

Open Energy Info (EERE)

Of 3D Inversion To Magnetotelluric Data In The Ogiri Geothermal Of 3D Inversion To Magnetotelluric Data In The Ogiri Geothermal Area, Japan Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Paper: Application Of 3D Inversion To Magnetotelluric Data In The Ogiri Geothermal Area, Japan Details Activities (0) Areas (0) Regions (0) Abstract: A stable inversion technique has been developed for threedimensional (3D) interpretation of magnetotelluric (MT) data. The inversion method is based on the Gauss-Newton (linearized least-squares) method with smoothness regularization. Static shifts are also treated as unknown parameters in the inversion. The forward modeling is done by using the staggered-grid finite difference method. A Bayesian criterion ABIC is applied to searching for the optimum trade-off among the minimization of

69

Application Of 3D Inversion To Magnetotelluric Data In The Ogiri...  

Open Energy Info (EERE)

Of 3D Inversion To Magnetotelluric Data In The Ogiri Geothermal Area, Japan Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Application Of 3D...

70

MAGNETOTELLURIC SURVEYING AND MONITORING AT THE COSO GEOTHERMAL AREA,  

Open Energy Info (EERE)

SURVEYING AND MONITORING AT THE COSO GEOTHERMAL AREA, SURVEYING AND MONITORING AT THE COSO GEOTHERMAL AREA, CALIFORNIA, IN SUPPORT OF THE ENHANCED GEOTHERMAL SYSTEMS CONCEPT: SURVEY PARAMETERS AND INITIAL RESULTS Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Proceedings: MAGNETOTELLURIC SURVEYING AND MONITORING AT THE COSO GEOTHERMAL AREA, CALIFORNIA, IN SUPPORT OF THE ENHANCED GEOTHERMAL SYSTEMS CONCEPT: SURVEY PARAMETERS AND INITIAL RESULTS Details Activities (1) Areas (1) Regions (0) Abstract: Electrical resistivity may contribute to progress in enhanced geothermal systems (EGS) by imaging the geometry, bounds and controlling structures in existing production, and by monitoring changes in the underground resistivity properties in the vicinity of injection due to fracture porosity enhancement. To these ends, we are acquiring a dense grid

71

A Five-Component Magneto-Telluric Method In Geothermal Exploration- The  

Open Energy Info (EERE)

Five-Component Magneto-Telluric Method In Geothermal Exploration- The Five-Component Magneto-Telluric Method In Geothermal Exploration- The Mt-5-Ex Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Five-Component Magneto-Telluric Method In Geothermal Exploration- The Mt-5-Ex Details Activities (1) Areas (1) Regions (0) Abstract: The present paper describes a new method designed both at recording and processing levels for a practical solution of the overall problem of the Earth electromagnetism, in geophysics. Up to now, the random character of the natural signals prevented any measurement of reliable values of the phase shift between the various electromagnetic components at a given place. Hence it is impossible numerically to solve the general linear relations binding these components simply by using the processes of

72

Audio-Magnetotellurics At Raft River Geothermal Area (1978) | Open Energy  

Open Energy Info (EERE)

Audio-Magnetotellurics At Raft River Geothermal Area Audio-Magnetotellurics At Raft River Geothermal Area (1978) Exploration Activity Details Location Raft River Geothermal Area Exploration Technique Audio-Magnetotellurics Activity Date 1978 Usefulness not indicated DOE-funding Unknown Exploration Basis To infer the structure and the general lithology underlying the valley Notes An area of low apparent resistivity values defined by the audiomagnetotelluric (AMT) survey appears to outline the extent of the geothermal reservoir even though the reservoir is deeper than the penetration of the survey. Self-potential anomalies relate to near surface hydrology. Upward leakage from the reservoir produces shallower effects that were measured by the AMT survey. References Mabey, D.R.; Hoover, D.B.; O'Donnell, J.E.; Wilson, C.W. (1

73

Magnetotellurics At Nw Basin & Range Region (Pritchett, 2004) | Open Energy  

Open Energy Info (EERE)

Magnetotellurics At Nw Basin & Range Region Magnetotellurics At Nw Basin & Range Region (Pritchett, 2004) Exploration Activity Details Location Northwest Basin and Range Geothermal Region Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes NOTE: These are theoretical/computer simulation tests of various methods on eight hypothetical 'model' basing-and-range geothermal systems. "The 300-meter heat flow holes are essentially useless for finding the "hidden" reservoirs. Clearly, the best results are obtained from the SP and MT surveys, with DC resistivity a close third. It is concluded that the best way to find "hidden" basin and range geothermal resources of this general type is to carry out simultaneous SP and low-frequency MT surveys, and then

74

3D Magnetotelluric characterization of the COSO GeothermalField  

SciTech Connect

Knowledge of the subsurface electrical resistivity/conductivity can contribute to a better understanding of complex hydrothermal systems, typified by Coso geothermal field, through mapping the geometry (bounds and controlling structures) over existing production. Three-dimensional magnetotelluric (MT) inversion is now an emerging technology for characterizing the resistivity structures of complex geothermal systems. The method appears to hold great promise, but histories exploiting truly 3D inversion that demonstrate the advantages that can be gained by acquiring and analyzing MT data in three dimensions are still few in number. This project will address said issue, by applying 3D MT forward modeling and inversion to a MT data set acquired over the Coso geothermal field. The goal of the project is to provide the capability to image large geothermal reservoirs in a single self-consistent model. Initial analysis of the Coso MT data has been carried out using 2D MT imaging technology to construct an initial 3D resistivity model from a series of 2D resistivity images obtained using the inline electric field measurements (Zxy impedance elements) along different measurement transects. This model will be subsequently refined through a 3D inversion process. The initial 3D resistivity model clearly shows the controlling geological structures possibly influencing well production at Coso. The field data however, also show clear three dimensionality below 1 Hz, demonstrating the limitations of 2D resistivity imaging. The 3D MT predicted data arising from this starting model show good correspondence in dominant components of the impedance tensor (Zxy and Zyx) above 1Hz. Below 1 Hz there is significant differences between the field data and the 2D model data.

Newman, Gregory A.; Hoversten, Michael; Gasperikova, Erika; Wannamaker, Philip E.

2005-01-01T23:59:59.000Z

75

Innovative Computational Tools for Reducing Exploration Risk Through Integration of Water-Rock Interactions and Magnetotelluric Surveys  

Energy.gov (U.S. Department of Energy (DOE))

Innovative Computational Tools for Reducing Exploration Risk Through Integration of Water-Rock Interactions and Magnetotelluric Surveys presentation at the April 2013 peer review meeting held in Denver, Colorado.

76

Magnetotellurics At Cove Fort Area (Toksoz, Et Al, 2010) | Open Energy  

Open Energy Info (EERE)

Cove Fort Area (Toksoz, Et Al, 2010) Cove Fort Area (Toksoz, Et Al, 2010) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Magnetotellurics At Cove Fort Area (Toksoz, Et Al, 2010) Exploration Activity Details Location Cove Fort Geothermal Area Exploration Technique Magnetotellurics Activity Date Usefulness not indicated DOE-funding Unknown Notes We have collected various geophysical data around the geothermal field, including heat flow, gravity, MT, seismic surface wave phase and group velocity maps, seismic body wave travel time data and full seismic waveforms. All of these geophysical data sets have different strengths on characterizing subsurface structures and properties. Combining these data through a coordinated analysis and, when possible, by joint inversion

77

Magnetotellurics At Long Valley Caldera Area (Sorey, Et Al., 1991) | Open  

Open Energy Info (EERE)

Long Valley Caldera Area (Sorey, Long Valley Caldera Area (Sorey, Et Al., 1991) Exploration Activity Details Location Long Valley Caldera Area Exploration Technique Magnetotellurics Activity Date Usefulness useful DOE-funding Unknown Notes In 1986, Unocal Geothermal Division released results from 158 time-domain electromagnetic (TDEM) soundings and, with Chevron Resources, a total of 77 magnetotelluric (MT) stations. Reinterpretations of the Unocal and Chevron data (Park and Torres-Verdin, 1988 ) and the recent public-domain MT studies (e.g. Hermance et al., 1988) outline similar shallow low-resistivity regions. At shallow depths in the caldera References Michael L. Sorey, Gene A. Suemnicht, Neil C. Sturchio, Gregg A. Nordquist (1991) New Evidence On The Hydrothermal System In Long Valley

78

MT3D: a 3 dimensional magnetotelluric modeling program (user's guide and documentation for Rev. 1)  

SciTech Connect

MT3D.REV1 is a non-interactive computer program written in FORTRAN to do 3-dimensional magnetotelluric modeling. A 3-D volume integral equation has been adapted to simulate the MT response of a 3D body in the earth. An integro-difference scheme has been incorporated to increase the accuracy. This is a user's guide for MT3D.REV1 on the University of Utah Research Institute's (UURI) PRIME 400 computer operating under PRIMOS IV, Rev. 17.

Nutter, C.; Wannamaker, P.E.

1980-11-01T23:59:59.000Z

79

A data variance technique for automated despiking of magnetotelluric data with a remote reference  

SciTech Connect

The magnetotelluric method employs co-located surface measurements of electric and magnetic fields to infer the local electrical structure of the earth. The frequency-dependent 'apparent resistivity' curves can be inaccurate at long periods if input data are contaminated - even when robust remote reference techniques are employed. Data despiking prior to processing can result in significantly more reliable estimates of long period apparent resistivities. This paper outlines a two-step method of automatic identification and replacement for spike-like contamination of magnetotelluric data; based on the simultaneity of natural electric and magnetic field variations at distant sites. This simultaneity is exploited both to identify windows in time when the array data are compromised, and to generate synthetic data that replace observed transient noise spikes. In the first step, windows in data time series containing spikes are identified via intersite comparison of channel 'activity' - such as the variance of differenced data within each window. In the second step, plausible data for replacement of flagged windows is calculated by Wiener filtering coincident data in clean channels. The Wiener filters - which express the time-domain relationship between various array channels - are computed using an uncontaminated segment of array training data. Examples are shown where the algorithm is applied to artificially contaminated data, and to real field data. In both cases all spikes are successfully identified. In the case of implanted artificial noise, the synthetic replacement time series are very similar to the original recording. In all cases, apparent resistivity and phase curves obtained by processing the despiked data are much improved over curves obtained from raw data.

Kappler, K.

2011-02-15T23:59:59.000Z

80

MAGNETOTELLURIC MEASUREMENTS  

E-Print Network (OSTI)

pretation, Klamath Basin, Oregon Swan Lake and Klamath B i lline A-A', Swan Lake Valley, Klamath Comty, Oregon. A 2-D fA-A', Swan Lake Valley area, Mantath County, Oregon. For

Clarke, J.

2010-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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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81

MAGNETOTELLURIC MEASUREMENTS  

E-Print Network (OSTI)

Klamath Basin, Oregon Swan Lake and Klamath B i l l s Tuea,line A-A', Swan Lake Valley, Klamath Comty, Oregon. A 2-D fn the Swan Lake Valley area, Klamath Comty, Oregon. ? lgure

Clarke, J.

2010-01-01T23:59:59.000Z

82

MAGNETOTELLURIC MEASUREMENTS  

E-Print Network (OSTI)

line A-A', Swan Lake Valley, Klamath Comty, Oregon. A 2-D fn the Swan Lake Valley area, Klamath Comty, Oregon. ? lgure

Clarke, J.

2010-01-01T23:59:59.000Z

83

New approaches to estimation of magnetotelluric parameters. Final technical report, 1 August 1989--31 July 1991  

SciTech Connect

Fully efficient robust data processing procedures were developed and tested for single station and remote reference magnetotelluric (Mr) data. Substantial progress was made on development, testing and comparison of optimal procedures for single station data. A principal finding of this phase of the research was that the simplest robust procedures can be more heavily biased by noise in the (input) magnetic fields, than standard least squares estimates. To deal with this difficulty we developed a robust processing scheme which combined the regression M-estimate with coherence presorting. This hybrid approach greatly improves impedance estimates, particularly in the low signal-to-noise conditions often encountered in the ``dead band`` (0.1--0.0 hz). The methods, and the results of comparisons of various single station estimators are described in detail. Progress was made on developing methods for estimating static distortion parameters, and for testing hypotheses about the underlying dimensionality of the geological section.

Egbert, G.D.

1991-12-31T23:59:59.000Z

84

3-D Magnetotelluric Investigations for geothermal exploration in Martinique (Lesser Antilles). Characteristic Deep Resistivity Structures, and Shallow Resistivity Distribution Matching Heliborne TEM Results  

E-Print Network (OSTI)

Within the framework of a global French program oriented towards the development of renewable energies, Martinique Island (Lesser Antilles, France) has been extensively investigated (from 2012 to 2013) through an integrated multi-methods approach, with the aim to define precisely the potential geothermal ressources, previously highlighted (Sanjuan et al., 2003). Amongst the common investigation methods deployed, we carried out three magnetotelluric (MT) surveys located above three of the most promising geothermal fields of Martinique, namely the Anses d'Arlet, the Montagne Pel{\\'e}e and the Pitons du Carbet prospects. A total of about 100 MT stations were acquired showing single or multi-dimensional behaviors and static shift effects. After processing data with remote reference, 3-D MT inversions of the four complex elements of MT impedance tensor without pre-static-shift correction, have been performed for each sector, providing three 3-D resistivity models down to about 12 to 30 km depth. The sea coast effe...

Coppo, Nicolas; Girard, Jean-Franois; Wawrzyniak, Pierre; Hautot, Sophie; Tarits, Pascal; Jacob, Thomas; Martelet, Guillaume; Mathieu, Francis; Gadalia, Alain; Bouchot, Vincent; Traineau, Herv

2015-01-01T23:59:59.000Z

85

The Characteristic States of the Magnetotelluric Impedance Tensor: Construction, Analytic Properties and Utility in the Analysis of General Earth Conductivity Distributions  

E-Print Network (OSTI)

It is shown that the Magnetotelluric (MT) impedance tensor admits an anti-symmetric generalized eigenvalue - eigenstate decomposition consistent with the anti-symmetry of electric and magnetic fields referred to the same coordinate frame: this is achieved by anti-diagonalization through rotation by 2x2 complex operators of the SU(2) rotation group. The eigenstates comprise simple proportional relationships between linearly polarized eigenvalues of the input magnetic and output electric field along the locally resistive and conductive propagation path into the Earth, respectively mediated by the maximum and minimum characteristic values of the tensor (eigen-impedances). It is shown from first principles that the eigen-impedances are expected to be positive real (passive) functions, analytic in the entire lower-half complex frequency plane and with singularities confined on the positive imaginary frequency axis. Insofar as the impedance tensor is generated by isometric transformation of the eigen-impedances, it...

Tzanis, Andreas

2014-01-01T23:59:59.000Z

86

The magnetotelluric inverse problem  

E-Print Network (OSTI)

20, . . . Hz, the Schumann resonances. The sunlit side ofyears 10 million years Schumann resonances 1 minute 1 second

Medin, Ashley E.

2008-01-01T23:59:59.000Z

87

The Magnetotelluric Inverse Problem  

E-Print Network (OSTI)

20, . . . Hz, the Schumann resonances. The sunlit side ofyears 10 million years Schumann resonances 1 minute 1 second

Medin, Ashley E

2008-01-01T23:59:59.000Z

88

Robust smooth magnetotelluric transfer functions  

Science Journals Connector (OSTI)

......presented at 54th Annl. Int. Mtg, Soc. Excl. Geophys., Atlanta...jackknifed the entire robust process because of computational time...and the section weights. The process is stopped when the number of...presented at 54th Annl. Int. Mtg, SOC.Excl. Geophys., Atlanta......

Jimmy C. Larsen; Randall L. Mackie; Adele Manzella; Adolfo Fiordelisi; Shirley Rieven

1996-03-01T23:59:59.000Z

89

Submitted to Symposium on VLSI Circuits, June 2000 A Monolithic Surface Micromachined Z-Axis Gyroscope with Digital Output  

E-Print Network (OSTI)

is 1µm for 3V drive voltage. This corresponds to Qx=3.2. Separate feedback capacitors (Cfb+ = Cfb- = 1

Kraft, Michael

90

CX-008605: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

05: Categorical Exclusion Determination 05: Categorical Exclusion Determination CX-008605: Categorical Exclusion Determination Geothermal Technology Advancement for Rapid Development of Resources in the U.S. CX(s) Applied: A9, B3.2, B3.11 Date: 07/19/2012 Location(s): Texas Offices(s): Golden Field Office Bell Geospace, Inc. (BGI) would utilize DOE and cost share funds to (1) combine airborne full tensor gravity (FTG) and the z-axis tipper electromagnetic (ZTEM) deep penetrating, low frequency, passive electromagnetic exploration system onto one platform for simultaneous acquisition; (2) test the applicability of each of these technologies for geothermal exploration over a known geothermal deposit; (3) if the initial tests successfully show the usefulness of these combined technologies, test surveys would be acquired over a more "greenfield" area; and (4) use the

91

CX-007420: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

20: Categorical Exclusion Determination 20: Categorical Exclusion Determination CX-007420: Categorical Exclusion Determination Geothermal Technology Advancement for Rapid Development of Resources in the U.S. CX(s) Applied: A9, B3.2, B3.11 Date: 11/30/2011 Location(s): Texas Offices(s): Golden Field Office Bell Geospace, Inc. (BGI) would utilize DOE and cost share funds to (1) combine airborne full tensor gravity (FTG) and the z-axis tipper electromagnetic (ZTEM) deep penetrating, low frequency, passive electromagnetic exploration system onto one platform for simultaneous acquisition; (2) test the applicability of each of these technologies for geothermal exploration over a known geothermal deposit; (3) if the initial tests successfully show the usefulness of these combined technologies, test surveys would be acquired over a more "greenfield" area; and (4) use the

92

Robust magnetotelluric inversion1 Tetsuo Matsuno3  

E-Print Network (OSTI)

-3 Midoricho, Tachikawa, Tokyo 190-8518, Japan,4 +81-42-512-0762, matsuno.tetsuo@nipr.ac.jp5 Alan D. Chave6

Jones, Alan G.

93

Geothermal resources in Southwestern Utah: gravity and magnetotelluric investigations.  

E-Print Network (OSTI)

??Recent geothermal studies on sedimentary basins in Western Utah suggest the possibility of significant geothermal reservoirs at depths of 3 to 5 km. This research (more)

Hardwick, Christian Lynn

2013-01-01T23:59:59.000Z

94

Magneto-Telluric Experiments in Northern Ellesmere Island  

Science Journals Connector (OSTI)

......electromagneticinduction within an anisotropic plane sheet over a non-conductor...experiment. This inductive anisotropic model leads to approximate...mainly argillaceous limestone, shale and greywacke with minor but...is highly inhomogeneous or anisotropic and the electric field is......

K. Whitham; F. Andersen

1965-12-01T23:59:59.000Z

95

3D Magnetotelluric Characterization Of The Geothermal Anomaly...  

Open Energy Info (EERE)

(AMT) survey was carried out. The AMT data was processed using a Wavelet Transform-based scheme. Dimensionality analysis indicates that the geoelectrical structure is...

96

A magnetotelluric investigation of crustal structure in southeastern Arizona  

E-Print Network (OSTI)

was difficult to investigate because of ground water complications and because of the large amount of volcanics present in the region. Two known geothermal resource areas (KGRA's), the Clifton KGRA and the Gillard KGRA, lie along the MT profile. The KGRA... area is reflected in the resistivity model by a shallow, very conductive (5 ohm-m) anomaly. This is the only such anomaly detected along the NT profile, suggesting that only the Clifton-Norenci area is of geothermal interest. DEDICATION To my...

Parizek, Daniel Joseph

2012-06-07T23:59:59.000Z

97

One-Dimensional Magnetotelluric Inversion with Radiation Boundary Conditions  

E-Print Network (OSTI)

Department of Mathematics and Statistics University of Saskatchewan Saskatoon, Saskatchewan Raymond Spiteri Department of Computer Science University of Saskatchewan Saskatoon, Saskatchewan Jacek Szmigielski Department of Mathematics and Statistics University of Saskatchewan Saskatoon, Saskatchewan Abstract We

Spiteri, Raymond J.

98

Schlumberger soundings, audio-magnetotelluric soundings and telluric...  

Open Energy Info (EERE)

Kitchen-Coso Hot Springs area in the Coso rhyolite dome field and the large arcuate fracture system previously postulated to represent a stage of incipient caldera formation were...

99

Further Analysis of 3D Magnetotelluric Measurements Over the...  

Open Energy Info (EERE)

changes in the underground resistivity properties in the vicinity of injection due to fracture porosity enhancement. Initial analysis of the Coso MT data was carried out using 2D...

100

A Broadband Tensorial Magnetotelluric Study In The Travale Geothermal...  

Open Energy Info (EERE)

to 2 km) of conducting (< 1 ohm m in some locations) cover formations and of the intensity of the artificial disturbances from local power stations and distribution lines....

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Magnetotellurics At Roosevelt Hot Springs Geothermal Area (Ward...  

Open Energy Info (EERE)

MT data. References S. H. Ward, W. T. Parry, W. P. Nash, W. R. Sill, K. L. Cook, R. B. Smith, D. S. Chapman, F. H. Brown, J. A. Whelan, J. R. Bowman (1978) A Summary of the...

102

Geothermal significance of magnetotelluric sounding in the eastern...  

Open Energy Info (EERE)

and fitted to geologic models. Authors Stanley, W.D.; Boehl, J.E.; Bostick, F.X.; Smith and H.W. Published Journal J. Geophys. Res., 6101977 DOI Not Provided Check for DOI...

103

Three-dimensional magnetotelluric characterization of the Coso...  

Open Energy Info (EERE)

array profiling has been acquired over the east flank of the Coso geothermal system, CA, USA. Due to production related electromagnetic (EM) noise the permanent observatory at...

104

Fluid and deformation regime of an advancing subduction system at Marlborough, New Zealand  

Science Journals Connector (OSTI)

... field (tipper) data quality was good but degraded somewhat compared to impedance by unavoidable wind and thermal noise.

Philip E. Wannamaker; T. Grant Caldwell; George R. Jiracek; Virginie Maris; Graham J. Hill; Yasuo Ogawa; Hugh M. Bibby; Stewart L. Bennie; Wiebke Heise

2009-08-06T23:59:59.000Z

105

DETECTION OF GEOTHERMAL INTERFERENCE IN THE TUNNEL EXCAVATION USING MAGNETOTELLURICS TECHNIQUE  

E-Print Network (OSTI)

to the geo-engineers in order to devise safety measures suitable during construction of the tunnel of water and rock matrix heats the air in a tunnel that can make the working condition along. Hydropower generation has thus become a major source of power generation, especially in Himalayan region

Harinarayana, T.

106

On multifrequency magnetotelluric sounding over the Himalayan type colliding plate boundaries  

Science Journals Connector (OSTI)

......to incorporate dipping anisotropic subsurface conditions either...upper (namely, dipping anisotropic character of the top surfaces of the shales in the Himalayan region...thickness b is uniaxially anisotropic (such that the longitudinal......

P. D. Saraf; J. G. Negi

1983-09-01T23:59:59.000Z

107

Stochastic inversion of magnetotelluric data using a sharp boundary parameterization and application to a geothermal site  

E-Print Network (OSTI)

and application to a geothermal site Jinsong Chen1 , G. Michael Hoversten2 , Kerry Key3 , Gregg Nordquist4 case that mimics a geothermal exploration scenario. Our results demonstrated that the de- veloped on the estimates. We also applied the developed method to the field MT data collected from the Darajat geothermal

Chen, Jinsong

108

INTERPRETATION OF SHALLOW ELECTRICAL FEATURES FROM ELECTROMAGNETIC AND MAGNETOTELLURIC SURVEYS AT MOUNT HOOD, OREGON  

E-Print Network (OSTI)

INTRODUCTION As part of a geothermal energy assessment ofof Energy's Division of Geothermal Energy, Lawrence Berkeley

Wilt, M.

2010-01-01T23:59:59.000Z

109

Partial melting zones in the crust in southern Tibet from magnetotelluric results  

Science Journals Connector (OSTI)

... resistivity will reflect several thermally related processes. Indeed the Tibetan Plateau is characterized by strong geothermal activity4 with more than 600 hydrothermal areas, of which 70% are concentrated in southern ... areas, of which 70% are concentrated in southern Tibet in the so-called 'Himalayan geothermal belt' (HGB) along both sides of the YZS zone5. So far, 11 ...

Van Ngoc Pham; Danile Boyer; Pierre Therme; Xue Cheng Yuan; Li Li; Guo Yuan Jin

1986-01-23T23:59:59.000Z

110

A Closely-Spaced Magnetotelluric Study Of The Ahuachapan-Chipilapa...  

Open Energy Info (EERE)

and younger N-S fault system that is responsible for the short-to-intermediate period data. The MT response in the 0.02-10 s range period was used to simulate the conductivity...

111

A magnetotelluric investigation under the Williston Basin of southeastern Saskatchewan:1 Discussion2  

E-Print Network (OSTI)

Saskatchewan:1 Discussion2 ALAN G. JONES Geological Survey of Canada, 1 Observatory Crescent, Ottawa, Ont Saskatchewan; (ii) illustrating that based on the PanCanadian data no anomaly exists near 105°W longitude after the

Jones, Alan G.

112

E-Print Network 3.0 - audio-magnetotelluric station location...  

NLE Websites -- All DOE Office Websites (Extended Search)

;Questions: - How many stations are needed, and where should ... Source: DOE Office of Energy Efficiency and Renewable Energy, Hydrogen, Fuel Cells and Infrastructure Technologies...

113

Adaptive finite element modelling of two-dimensional magnetotelluric fields in general anisotropic media  

Science Journals Connector (OSTI)

......the error indicator is updated. This process is repeated until the required level of...after 16 grid refinement and the iteration process was terminated. The final mesh contains...induction problem, 71th Annual Internat. Mtg., Soc. Expl. Geophys. (Expanded......

Yuguo Li; Josef Pek

2008-12-01T23:59:59.000Z

114

Mapping offshore sedimentary structure using electromagnetic methods and terrain effects in marine magnetotelluric data  

Science Journals Connector (OSTI)

......temperature, which follows a geothermal gradient of 25.4 8...man-made source of energy is measured, are also...reconnaissance, a low-cost alternative to the use...the seafloor, at the cost of greater algorithmic...linear relationship and a geothermal gradient of 25.4 K......

Steven Constable; Kerry Key; Lisl Lewis

2009-02-01T23:59:59.000Z

115

Magma genesis and crustal spreading in the northern neovolcanic zone of Iceland: telluric-magnetotelluric constraints  

Science Journals Connector (OSTI)

......Constraints on temperature beneath Iceland...Symposium on the Development and Use of Geothermal...in the eastern Snake River Plain - Yellowstone...Constraints on temperature beneath Iceland...Symposium on the Development and Use of Geothermal...45,l-16. temperature, J. Geophys......

R. E. Thayer; A. Bjornsson; L. Alvarez; J. F. Hermance

1981-05-01T23:59:59.000Z

116

Structure and thermal regime beneath the South Pole region, East Antarctica, from magnetotelluric measurements  

Science Journals Connector (OSTI)

......Figure B2 Recordings of electric fields on parallel...a superposition of elementary volumes (e.g. Stratton...spherical distribution of electric charge over the Earth's...of electrode contact resistance on electric field measurements......

Philip E. Wannamaker; John A. Stodt; Louise Pellerin; Steven L. Olsen; Darrell B. Hall

2004-04-01T23:59:59.000Z

117

Area selection for diamonds using magnetotellurics: Examples from southern Africa Alan G. Jones a,  

E-Print Network (OSTI)

of the Witwatersrand, Jan Smuts Avenue, Johannesburg 2050, South Africa k ABB AB, HVDC, Ludvika, SE-77180, Sweden a b

Jones, Alan G.

118

A magnetotelluric survey on Manitoulin Island and Bruce Peninsula along GLIMPCE seismic line J: black shales mask the Grenville Front  

Science Journals Connector (OSTI)

......91, 7403-7416. Liberty B. A. , Bolton T...Oil shale assessment project drillholes for regional...by Beards (1967) and Liberty & Bolton (1971) amongst...91, 7403-7416. Liberty, B. A. & Bolton...Oil shale assessment project drillholes for regional......

M. Mareschal; R. D. Kurtz; M. Chouteau; R. Chakridi

1991-04-01T23:59:59.000Z

119

A magnetotelluric survey on Manitoulin Island and Bruce Peninsula along GLIMPCE seismic line J: black shales mask the Grenville Front  

Science Journals Connector (OSTI)

......Geological Survey, 1985. Oil shale assessment project drillholes...GLIMPCE seismic line J: black shales mask the Grenville Front M...highly conductive layer of black shales of limited extent, precludes...y believed to be caused by anisotropic effects associated with thick......

M. Mareschal; R. D. Kurtz; M. Chouteau; R. Chakridi

1991-04-01T23:59:59.000Z

120

A magnetotelluric survey on Manitoulin Island and Bruce Peninsula along GLIMPCE seismic line J: black shales mask the Grenville Front  

Science Journals Connector (OSTI)

......edsDawson J. B., et al. Ontario Geological Survey, 1985. Oil shale assessment project drillholes for regional correlations...Dawson, J. B. er al. Ontario Geological Survey, 1985. Oil shale assessment project drillholes for regional correlations......

M. Mareschal; R. D. Kurtz; M. Chouteau; R. Chakridi

1991-04-01T23:59:59.000Z

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Magnetotelluric 3-D inversiona review of two successful workshops on forward and inversion code testing and comparison  

Science Journals Connector (OSTI)

......more modelling reviews followed: one...algorithms are not yet standard tools for MT data...in section and plan view. Table-1...time. In the review paper by Siripunvaraporn...but also non-standard norms and measures...possibly even on a standard laptop. Figure-13...top) and a plan view (bottom......

Marion P. Miensopust; Pilar Queralt; Alan G. Jones; the 3D MT modellers

2013-01-01T23:59:59.000Z

122

Magnetotelluric characterization of a salt diapir: a case study on BicorbQuesa Diapir (Prebetic Zone, SE Spain)  

Science Journals Connector (OSTI)

...the adjacent synclines (Garca ZZQQhya-Rodrigo 1960; De Ruig 1992). Most of these anticlines...Mijnbow 59:155a 168. a Garca ZZQQhya-Rodrigo B. (1960) Sur la structure du Nord de...Mateus A., Pous J., Heise W., Santos F.M., Almeida E. (2008) Unraveling...

M. Rubinat; J. Ledo; E. Roca; O. Rosell; P. Queralt

123

Determination of a Geothermal Energy Field with Audio-Magnetotelluric (AMT) Data at the South of Manisa, Turkey  

Science Journals Connector (OSTI)

In this study, we present an investigation of the geothermal energy field and its energy potential at the south of Manisa in Turkey. The resistivities of the geothermal energy field have a key role in determining...

Hatice Karakilcik

2014-01-01T23:59:59.000Z

124

Decomposition analysis of the BEAR magnetotelluric data: implications for the upper mantle conductivity in the Fennoscandian Shield  

Science Journals Connector (OSTI)

......priori conductivity model of the crust, seawater and sediments of Fennoscandia established...Figure 2 Integrated conductance of seawater, sediments and uppermost crust (0-10...in olivine and implication for water storage in the mantle, Nature, 357,672-674......

I. Lahti; T. Korja; P. Kaikkonen; K. Vaittinen

2005-12-01T23:59:59.000Z

125

Reply to the 'Comments on: Concerning dispersion relations for the magnetotelluric impedance tensor' By G. D. Egbert  

Science Journals Connector (OSTI)

......the output (total) electric field from the actual...of the total output electric field. Consequently...a system composed of elementary linear rings of currents...current is associated a resistance R, a capacitance C...losses. The system of elementary linear ring currents......

E. Yee; K. V. Paulson

1990-07-01T23:59:59.000Z

126

Resistivity Log At Long Valley Caldera Geothermal Area (Nordquist...  

Open Energy Info (EERE)

Magnetotelluric and Magnetic Variation Interpretation Philip E. Wannamaker, P.M. Wright, Zhou Zi-xing, Li Xing-bin, Zhao Jing-xiang (1991) Magnetotelluric Transect of Long...

127

Geophysical Prospecting, 2013, 61 (Suppl. 1), 505532 doi: 10.1111/j.1365-2478.2012.01117.x Review paper: Instrumentation for marine magnetotelluric and  

E-Print Network (OSTI)

exploits the natural variations in the Earth's magnetic field that induce electric currents and fields CGeophysical Prospecting, 2013, 61 (Suppl. 1), 505­532 doi: 10.1111/j.1365-2478.2012.01117.x Review accepted June 2012 ABSTRACT We review and describe the electromagnetic transmitters and receivers used

Constable, Steve

128

Stochastic inversion of 2D magnetotelluric data using sharp boundary parameterization Jinsong Chen*, Lawrence Berkeley National Laboratory, Michael G. Hoversten, Chevron Energy  

E-Print Network (OSTI)

in computing power, especially parallel computing techniques, and the recent development of new numerical Institution of Oceanography, and Gregg Nordquist, Chevron Geothermal and Power Operations Summary Stochastic approaches for inverting geophysical data have many advantages over deterministic inversion methods in terms

Chen, Jinsong

129

The Cool Flame Combustion of Ethanol  

Science Journals Connector (OSTI)

...research-article The Cool Flame Combustion of Ethanol J. Brown C. F. H. Tipper The kinetics...products of the cool flame combustion of ethanol between about 280 and 330 C have been...much less for a 1 : 2 than for a 1 : 1 ethanol/oxygen mixture at constant T and varied...

1969-01-01T23:59:59.000Z

130

Running head: Crossmodal action representations1 Surface-based information mapping reveals crossmodal vision-action3  

E-Print Network (OSTI)

. Oosterhof1 7 Alison J. Wiggett1 8 Jörn Diedrichsen1,2 9 Steven P. Tipper1 10 Paul E. Downing1 11 12 1 School regions in which local voxel-wise patterns of activity can distinguish among40 different actions, across

Diedrichsen, Jörn

131

Time Resolved X-ray Fine Structures, Neutron Emission, and Ion Velocities in a Fast 1 kJ Plasma Focus  

Science Journals Connector (OSTI)

One to four (mostly 2) X-ray spot structures are present in hydrogen and deuterium along the z-axis during the dense pinch phase; approximately 4% argon is required for soft radiation pin hole photography. Spo...

K. H. Schoenbach; L. Michel; H. Krompholz

1976-01-01T23:59:59.000Z

132

Physical processes of the interaction of ion and plasma streams with a target surface in a dense plasma focus device  

Science Journals Connector (OSTI)

Dynamics of the interaction of powerful streams of high-temperature plasma and fast ions generated in a device of the Dense Plasma Focus (DPF) type has been studied for...Z...axis of the DPF chamber on its cath...

V. A. Gribkov; A. S. Demin; E. V. Demina; A. V. Dubrovsky

2012-12-01T23:59:59.000Z

133

Most Viewed Documents for Geosciences: September 2014 | OSTI...  

Office of Scientific and Technical Information (OSTI)

Los Alamos National Laboratory (2014) 24 Sloshing analysis of viscous liquid storage tanks Uras, R.Z. (1995) 22 Seismic and magneto-telluric imaging for geothermal exploration...

134

Hydrothermal Resources Fact Sheet  

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

Geophysics Potential fields methods (e.g. gravity, magnetics, magnetotellurics), heat flow mapping, and advanced seismic techniques along with improvements in interpreting...

135

Geophys. J. Int. (2009) 176, 431442 doi: 10.1111/j.1365-246X.2008.03975.x GJIGeomagnetism,rockmagnetismandpalaeomagnetism  

E-Print Network (OSTI)

a geothermal gradient of 25.4 ± 8 K km-1 . Key words: Electrical properties; Magnetotelluric; Marine to a man-made source of energy is measured, are also sometimes used (e.g. Gomez- Trevino & Edwards 1983; H form 2007 November 25 S U M M A R Y Marine magnetotelluric (MT) and marine controlled-source

Constable, Steve

136

Geophys. J. Int. (2009) 176, 431442 doi: 10.1111/j.1365-246X.2008.03975.x GJIGeomagnetism,rockmagnetismandpalaeomagnetism  

E-Print Network (OSTI)

a geothermal gradient of 25.4 ± 8 K km-1 . Key words: Electrical properties; Magnetotelluric; Marine to a man-made source of energy is measured, are also sometimes used (e.g. Gomez- Trevino & Edwards 1983; H form 2007 November 25 SUMMARY Marine magnetotelluric (MT) and marine controlled-source electromagnetic

Key, Kerry

137

Method and apparatuses for ion cyclotron spectrometry  

DOE Patents (OSTI)

An ion cyclotron spectrometer may include a vacuum chamber that extends at least along a z-axis and means for producing a magnetic field within the vacuum chamber so that a magnetic field vector is generally parallel to the z-axis. The ion cyclotron spectrometer may also include means for producing a trapping electric field within the vacuum chamber. The trapping electric field may comprise a field potential that, when taken in cross-section along the z-axis, includes at least one section that is concave down and at least one section that is concave up so that ions traversing the field potential experience a net magnetron effect on a cyclotron frequency of the ions that is substantially equal to zero. Other apparatuses and a method for performing ion cyclotron spectrometry are also disclosed herein.

Dahl, David A. (Idaho Falls, ID); Scott, Jill R. (Idaho Falls, ID); McJunkin, Timothy R. (Idaho Falls, ID)

2012-03-06T23:59:59.000Z

138

The CAFE experiment : a joint seismic and MT investigation of the Cascadia subduction system  

E-Print Network (OSTI)

In this thesis we present results from inversion of data using dense arrays of collocated seismic and magnetotelluric stations located in the Cascadia subduction zone region of central Washington. In the migrated seismic ...

McGary, R. Shane

2013-01-01T23:59:59.000Z

139

North American Central Plains conductivity anomaly within the Trans-Hudson orogen in northern Saskatchewan, Canada  

E-Print Network (OSTI)

Saskatchewan, Canada Alan G. Jones } James A. Craven Geological Survey of Canada, 1 Observatory Crescent Magnetotelluric data acquired across the Paleoproterozoic Trans-Hudson orogen, north- ern Saskatchewan, image one

Jones, Alan G.

140

Meteoritics & Planetary Science 39, Nr 6, 787790 (2004) Abstract available online at http://meteoritics.org  

E-Print Network (OSTI)

exploratory program by PEMEX with intermittent core recovery and, more recently, by the National University, magnetotelluric and offshore seismic surveys, pre-existing boreholes of PEMEX and UNAM programs, site conditions

Claeys, Philippe

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

3D Magnetotelluic characterization of the Coso Geothermal Field  

E-Print Network (OSTI)

and Neubauer, F. M. , 2003, 3D inversion of a scalar radio3D MAGNETOTELLURIC CHARACTERIZATION OF THE COSO GEOTHERMALMT imaging. An initial 3D conductivity model was constructed

Newman, Gregory A.; Hoversten, G. Michael; Wannamaker, Philip E.; Gasperikova, Erika

2008-01-01T23:59:59.000Z

142

RAPID/NEPA | Open Energy Information  

Open Energy Info (EERE)

Magnetotelluric Survey at Soda Lake CX Nevada Geothermal BLM Nevada State Office CX for Micro-Earthquake Survey at ?? Geothermal Area CX Geothermal BLM Nevada State Office CX for...

143

2010 Asia-Pacific International Symposium on Aerospace Technology Control-oriented Modeling for Hypersonic Vehicle Control  

E-Print Network (OSTI)

that viscous effect increase drag by about 32% and has little effect on pitch moment, lift, poles and zeros of the aircraft and z axis points downward. x0 and z0 are x and z direction distance from lip point to the origin the pressure distribution on the model's four regions. Region I is under the forebody, region II is under

Huang, Xun

144

3D NAVIGATION WITH AN INSECT-INSPIRED AUTOPILOT G.PORTELLI, J.SERRES, F.RUFFIER, and N.FRANCESCHINI  

E-Print Network (OSTI)

), is a dual OF regulator consisting of two interdependent feedback loops, each of which has its own OF set-point (only eight pixels) and it suffices to control the clearance from the four walls and the forward speed the sway Y-axis giving the side thrust S, and along the heave Z-axis giving the vertical lift L. (b

Paris-Sud XI, Université de

145

Digital in-line holography for biological applications  

Science Journals Connector (OSTI)

...particular photoelectron and LEED holography, indicates that improved z-axis...Applications , Halifax, NS, Canada ). 15 Kreuzer H J Fink...Engineering Research Council of Canada. The use of the Kirchhoff...Electron Diffraction (LEED) holography [see Heinz...University, Halifax, NS, Canada. | Journal Article Research...

Wenbo Xu; M. H. Jericho; I. A. Meinertzhagen; H. J. Kreuzer

2001-01-01T23:59:59.000Z

146

Z-Tiles: Building Blocks for Modular, Pressure-Sensing Floorspaces  

E-Print Network (OSTI)

Z-Tiles: Building Blocks for Modular, Pressure-Sensing Floorspaces Bruce Richardson, Krispin Leydon, University of Limerick, Limerick, Ireland {bruce.richardson | krispin.leydon | mikael.fernstrom}@ul.ie Joseph acting parallel to the z axis. Copyright is held by the author/owner(s). CHI 2004, April 24-29, 2004

147

6.4 Composition and invertibility of linear transformations  

E-Print Network (OSTI)

number of reflections is a reflection composed with a rotation. #12; Yaw: z-axis (up direction), pitch and ). See Example 5. Conversely, any rotation can be factored into yaw, pitch, roll rotations. #12; We wish=Ax given by a linear system as in (18). We have x=A-1y given by a linear system. We can obtain the second

Choi, Suhyoung

148

Structured H1 Command and Control-Loop Design for Unmanned Helicopters  

E-Print Network (OSTI)

(including wind gusts), excellent decoupling, andgood speed of response. Nomenclature A = system or plant-frame components R = control weighting matrix r = yaw rate in the body-frame components rfb = yaw-rate feedback U-loop output vector Z = inertial position z axis zt = performance output = system L2 gain in = L2 gain inner

Benmei, Chen

149

Design and Control of a Compact 6-Degree-of-Freedom Precision Positioner with Linux- Based Real-Time Control  

E-Print Network (OSTI)

to measure vertical, x-, and yrotation motions. Three 2-axis Hall-effect sensors are used to determine lateral motions and rotation motion about the z-axis by measuring the magnetic flux density generated by the magnet matrix. This positioning system has a...

Yu, Ho

2010-01-14T23:59:59.000Z

150

Uniform insulation applied-B ion diode  

DOE Patents (OSTI)

An applied-B field extraction ion diode has uniform insulation over an anode surface for increased efficiency. When the uniform insulation is accomplished with anode coils, and a charge-exchange foil is properly placed, the ions may be focused at a point on the z axis.

Seidel, David B. (Albuquerque, NM); Slutz, Stephen A. (Albuquerque, NM)

1988-01-01T23:59:59.000Z

151

Microsoft PowerPoint - 2009_04 ATF User's Meeting Talk.pptx  

NLE Websites -- All DOE Office Websites (Extended Search)

were ejected parallel to the laser axis - an off-z-axis (along x-direction) pop-in BPM, which is located ( g ) p p , at 12-cm from IP(1000 Z R ); - its intensity 0.2-Jcm 2...

152

Magnetic resonance imaging (MRI) of solid materials entails numerous problems from short longitudinal relaxation (T2) times to  

E-Print Network (OSTI)

. Solid-State STRAFI NMR Probe for Material Imaging of Quadrupolar Nuclei, J. Magn. Reson. httpMagnetic resonance imaging (MRI) of solid materials entails numerous problems from short for broadband tuning, sample translation along z-axis, and electrodes for in situ battery studies. An Alderman

Weston, Ken

153

Sensing mode atomic force microscope  

DOE Patents (OSTI)

An atomic force microscope utilizes a pulse release system and improved method of operation to minimize contact forces between a probe tip affixed to a flexible cantilever and a specimen being measured. The pulse release system includes a magnetic particle affixed proximate the probe tip and an electromagnetic coil. When energized, the electromagnetic coil generates a magnetic field which applies a driving force on the magnetic particle sufficient to overcome adhesive forces exhibited between the probe tip and specimen. The atomic force microscope includes two independently displaceable piezo elements operable along a Z-axis. A controller drives the first Z-axis piezo element to provide a controlled approach between the probe tip and specimen up to a point of contact between the probe tip and specimen. The controller then drives the first Z-axis piezo element to withdraw the cantilever from the specimen. The controller also activates the pulse release system which drives the probe tip away from the specimen during withdrawal. Following withdrawal, the controller adjusts the height of the second Z-axis piezo element to maintain a substantially constant approach distance between successive samples.

Hough, Paul V. C. (Port Jefferson, NY); Wang, Chengpu (Upton, NY)

2003-01-01T23:59:59.000Z

154

ASP Conference Series, Vol. **VOLUME**, **PUBLICATION YEAR** **EDITORS**  

E-Print Network (OSTI)

simulation with Schwarzschild black hole with a free falling corona. The initial sim- ulation results show of the general-relativistic effect below 3rS (rS is the Schwarzschild ra- dius), is strongly decelerated here were made assuming axisymmetry with re- spect to the z-axis and mirror symmetry with respect

Nishikawa, Ken-Ichi

155

A MODEL FOR POROUS-MEDIUM COMBUSTION  

Science Journals Connector (OSTI)

......usually taken from experiments; Vo is determined by the inlet gas velocity under consideration, and for the typical combustion processes where Vo is parallel to the z-axis in which we are interested it is natural to choose V3o~0-1 to 1-Oms......

J. NORBURY; A. M. STUART

1989-02-01T23:59:59.000Z

156

Possible Magmatic Input to the Dixie Valley Geothermal Field, and  

Open Energy Info (EERE)

Possible Magmatic Input to the Dixie Valley Geothermal Field, and Possible Magmatic Input to the Dixie Valley Geothermal Field, and Implications for District-Scale Resource Exploration, Inferred from Magnetotelluric (MT) Resistivity Surveying Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Possible Magmatic Input to the Dixie Valley Geothermal Field, and Implications for District-Scale Resource Exploration, Inferred from Magnetotelluric (MT) Resistivity Surveying Abstract Magnetotelluric (MT) profiling in northwestern Nevadais used to test hypotheses on the main sources of heat andhydrothermal fluid for the Dixie Valley-Central NevadaSeismic Belt area. The transect reveals families of resistivitystructures commonly dominated by steeply-dipping features,some of which may be of key geothermal significance. Mostnotably, 2-D inversion

157

A Regional Strategy For Geothermal Exploration With Emphasis On Gravity And  

Open Energy Info (EERE)

Strategy For Geothermal Exploration With Emphasis On Gravity And Strategy For Geothermal Exploration With Emphasis On Gravity And Magnetotellurics Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Regional Strategy For Geothermal Exploration With Emphasis On Gravity And Magnetotellurics Details Activities (4) Areas (2) Regions (0) Abstract: As part of the resource evaluation and exploration program conducted by Los Alamos Scientific Laboratory for the national Hot Dry Rock (HDR) Geothermal Program, a regional magnetotelluric (MT) survey of New Mexico and Arizona is being performed. The MT lines are being located in areas where the results of analysis of residual gravity anomaly maps of Arizona and New Mexico, integrated with other geologic and geophysical studies indicate the greatest potential for HDR resources. The residual

158

Definition: Controlled Source Audio MT | Open Energy Information  

Open Energy Info (EERE)

Definition Definition Edit with form History Facebook icon Twitter icon » Definition: Controlled Source Audio MT Jump to: navigation, search Dictionary.png Controlled Source Audio MT Controlled Source Audio-Magnetotellurics (CSAMT) is an active source application of a magnetotelluric survey aimed at providing a more reliable signal and rapid acquisition time relative to a natural source MT measurement.[1] View on Wikipedia Wikipedia Definition Magnetotellurics (MT) is an electromagnetic geophysical method of imaging the earth's subsurface by measuring natural variations of electrical and magnetic fields at the Earth's surface. Investigation depth ranges from 300m below ground by recording higher frequencies down to 10,000m or deeper with long-period soundings. Developed in Russia and

159

Property:DOI | Open Energy Information  

Open Energy Info (EERE)

DOI DOI Jump to: navigation, search Property Name DOI Property Type String Pages using the property "DOI" Showing 25 pages using this property. (previous 25) (next 25) 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + 10.1016/j.crte.2010.04.001 + 3 3-D Inversion Of Borehole-To-Surface Electrical Data Using A Back-Propagation Neural Network + 10.1016/j.jappgeo.2008.06.002 + 3D Magnetotelluric Characterization Of The Geothermal Anomaly In The Llucmajor Aquifer System (Majorca, Spain) + 10.1016/j.jappgeo.2008.05.006 + 4 40 Years Of Dogger Aquifer Management In Ile-De-France, Paris Basin, France + 10.1016/j.geothermics.2010.09.005 + A A Broadband Tensorial Magnetotelluric Study In The Travale Geothermal Field + 10.1016/0375-6505(85)90040-9 +

160

Electronic structure of dimetal bonded systems: ditungsten, dimolybdenum and diruthenium systems  

E-Print Network (OSTI)

with a 0.05 contour surface. The z axis is taken to be perpendicular to the plane defined by the tungsten atoms and ? -CO ligands.......24 5 Orbital correlation diagram for 1 illustrating the changes in energy of the four highest occupied (dashed... Page 1 Crystallographic Data for Tungsten Formamidinate Compounds................. 9 2 Bond Parameters (? or deg) for 1................................................................. 11 3 Bond Parameters (? or deg) for 2...

Villagran Martinez, Dino

2007-04-25T23:59:59.000Z

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


161

Category:Electromagnetic Sounding Techniques | Open Energy Information  

Open Energy Info (EERE)

Electromagnetic Sounding Techniques Electromagnetic Sounding Techniques Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Geothermalpower.jpg Looking for the Electromagnetic Sounding Techniques page? For detailed information on Electromagnetic Sounding Techniques, click here. Category:Electromagnetic Sounding Techniques Add.png Add a new Electromagnetic Sounding Techniques Technique Subcategories This category has only the following subcategory. M [×] Magnetotelluric Techniques‎ 1 pages Pages in category "Electromagnetic Sounding Techniques" The following 2 pages are in this category, out of 2 total. M Magnetotelluric Techniques T Time-Domain Electromagnetics Retrieved from "http://en.openei.org/w/index.php?title=Category:Electromagnetic_Sounding_Techniques&oldid=689837"

162

Vacuum electron acceleration by using two variable frequency laser pulses  

SciTech Connect

A method is proposed for producing a relativistic electron bunch in vacuum via direct acceleration by using two frequency-chirped laser pulses. We consider the linearly polarized frequency-chiped Hermit-Gaussian 0, 0 mode lasers with linear chirp in which the local frequency varies linearly in time and space. Electron motion is investigated through a numerical simulation using a three-dimensional particle trajectory code in which the relativistic Newton's equations of motion with corresponding Lorentz force are solved. Two oblique laser pulses with proper chirp parameters and propagation angles are used for the electron acceleration along the z-axis. In this way, an electron initially at rest located at the origin could achieve high energy, ?=319 with the scattering angle of 1.02{sup ?} with respect to the z-axis. Moreover, the acceleration of an electron in different initial positions on each coordinate axis is investigated. It was found that this mechanism has the capability of producing high energy electron microbunches with low scattering angles. The energy gain of an electron initially located at some regions on each axis could be greatly enhanced compared to the single pulse acceleration. Furthermore, the scattering angle will be lowered compared to the acceleration by using laser pulses propagating along the z-axis.

Saberi, H.; Maraghechi, B. [Department of Physics, Amirkabir University of Technology, 15875-4413 Tehran (Iran, Islamic Republic of)] [Department of Physics, Amirkabir University of Technology, 15875-4413 Tehran (Iran, Islamic Republic of)

2013-12-15T23:59:59.000Z

163

Volume 14, Number 4 5 April 2013  

E-Print Network (OSTI)

[1] Seismic velocity is a function of bulk vibrational properties of the media, whereas electrical Africa and the surrounding regions, and a new electrical image from magnetotelluric (MT) data recorded observations. The differences between the two demonstrate that the linear relationship between Vs

Jones, Alan G.

164

Preliminary interpretation of the upper crustal structure beneath Prince Edward Island  

E-Print Network (OSTI)

during 1983 to aid in the assessment of the geothermal energy potential of the province. At ten locations gravity anomaly in the region. Key words: magnetotelluric method, geothermal energy, Prince Edward Island of the geothermal energy potential of Atlantic Canada is now in its fifth year and has entered its final phase

Jones, Alan G.

165

Prof. Harinarayana, NGRI was felicitated by Andhra University, Visakhapatnam  

E-Print Network (OSTI)

and Bulgarian scientists under Indo-Bulgarian scientific co-operation to develop geothermal resources. Based in introducing a new geophysical technique ­ marine magnetotellurics - in India for oil exploration in Gulf, Hyderabad On the occasion of Diamond Jubilee celebrations (1949-2009) by the Department of Geophysics

Harinarayana, T.

166

Natural Hazards and Earth System Sciences (2004) 4: 641646 SRef-ID: 1684-9981/nhess/2004-4-641  

E-Print Network (OSTI)

storms, electrochemical noise due to change in the contact potential between electrodes and ground during is significantly stronger and embedded in noise. Furthermore, EEP signals vary in terms of duration and size making by noise (e.g. noise of magnetotelluric origin (Kauf- man and Keller, 1981) caused mainly by magnetic

Paris-Sud XI, Université de

167

Method for determining depth and shape of a sub-surface conductive object  

DOE Patents (OSTI)

The depth to and size of an underground object may be determined by sweeping a controlled source audio magnetotelluric (CSAMT) signal and locating a peak response when the receiver spans the edge of the object. The depth of the object is one quarter wavelength in the subsurface media of the frequency of the peak. 3 figures.

Lee, D.O.; Montoya, P.C.; Wayland, Jr.

1984-06-27T23:59:59.000Z

168

Optimal command generation for maneuvering the space station  

E-Print Network (OSTI)

with linearly appearing bounded controls. It was shown that on average, the run time for the control eliminated differential inclusion method was one-sixth that of the collocation method. ' One method y'ves a higher accuracy, while the other gives faster... and positive in the direction of vehicle motion. The z-axis points to the nadir, and the y-axis is normal to the orbit plane and completes the right-handed orthogonal system. 15 This can be seen in Figure 2. 2. The angular velocity of LVLH relative...

Bryson, Amy Louise

2012-06-07T23:59:59.000Z

169

Singular eigenfunctions for the three-dimensional radiative transport equation  

E-Print Network (OSTI)

Case's method obtains solutions to the radiative transport equation as superpositions of elementary solutions when the specific intensity depends on one spatial variable. In this paper, we find elementary solutions when the specific intensity depends on three spatial variables in three-dimensional space. By using the reference frame whose z-axis lies in the direction of the wave vector, the angular part of each elementary solution becomes the singular eigenfunction for the one-dimensional radiative transport equation. Thus Case's method is generalized.

Manabu Machida

2013-09-07T23:59:59.000Z

170

Fixture for supporting and aligning a sample to be analyzed in an x-ray diffraction apparatus  

DOE Patents (OSTI)

A fixture is provided for supporting and aligning small samples of material on a goniometer for x-ray diffraction analysis. A sample-containing capillary is accurately positioned for rotation in the x-ray beam by selectively adjusting the fixture to position the capillary relative to the x and y axes thereof to prevent wobble and position the sample along the z axis or the axis of rotation. By employing the subject fixture relatively small samples of materials can be analyzed in an x-ray diffraction apparatus previously limited to the analysis of much larger samples.

Green, L.A.; Heck, J.L. Jr.

1985-04-23T23:59:59.000Z

171

SU?E?I?41: Study On the CT Radiation Attenuation Characteristics of Human Body for Phantom Design Using Monte Carlo Simulations  

Science Journals Connector (OSTI)

Purpose: The CTDI values measured with standard PMMA phantoms were now being challenged due to the clinical application of new technologies such as automatic tube current modulation(TCM) the aim of this study is to simulate the CT radiation attenuation characteristics of human body along Z?axis which were the basic data of developing new phantoms used to evaluate TCM. Methods: The CT model used in this study has been modeled including the source energy spectrum the bow?tie filter as well and the beam shape. The voxel phantoms RPI Adult Male designed to match the ICRP anatomical references for average individuals were also selected in this study. MCNPX 2.5.0 was used to simulate the 120 kVp CT X?ray attenuation of voxel phantom along the z?axis. Averaged photon flux was tallied before and after it passed though the phantom separately simulations were also carried out using different thickness of PMMA plates instead of the voxel phantom. Results: The CT X?ray attenuation of PMMA and its thickness presents a significant negative exponential relationship with the r2=0.9975. The CT X?ray attenuation data of every 2cm along Z?axis direction of voxel phantom were obtained combined with characteristics of CT X?ray attenuation of PMMA the PMMA equivalent thickness of the voxel phantom torso along the Z?axis direction in terms of CT X?ray attenuation were calculated. The PMMA equivalent thickness ranges from 5.5cm to 30.1cm. The liver and spleen plane which contents substantive organs such as the liver and spleen and bone structure as ribs and the lumbar was the maximum attenuation plane. Conclusion: The trend of the overall attenuation characteristics of the human body in terms of CT X?ray was in accord with the anatomical structure these results could be used to develop new dose phantoms which were used to evaluate automatic tube current modulation with further study. This project was partially funded by National Institutes of Health (National Library of Medicine R01LM009362 and National Institute of Biomedical Imaging and Bioengineering R42EB010404)

h Liu

2013-01-01T23:59:59.000Z

172

Category:Reference Materials | Open Energy Information  

Open Energy Info (EERE)

Category Category Edit History Facebook icon Twitter icon » Category:Reference Materials (Redirected from Reference Materials) Jump to: navigation, search This is a deprecated subcategory. All Reference Materials will be converted to References. Pages in category "Reference Materials" The following 200 pages are in this category, out of 2,265 total. (previous 200) (next 200) 1 10 CFR § 1021 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits 238U Decay Series Systematics Of Young Lavas From Batur Volcano, Sunda Arc 2D Joint Inversion Of Dc And Scalar Audio-Magnetotelluric Data In The Evaluation Of Low Enthalpy Geothermal Fields

173

CX-001422: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

2: Categorical Exclusion Determination 2: Categorical Exclusion Determination CX-001422: Categorical Exclusion Determination A 3D-3C Reflection Seismic Survey and Data Integration to Identify the Seismic Response of Fractures and Permeable Zones Over a Known Geothermal Resource: Soda lake, Churchill County, Nevada CX(s) Applied: B3.1, A9 Date: 03/29/2010 Location(s): Soda Lake, Nevada Office(s): Energy Efficiency and Renewable Energy, Golden Field Office Magma Energy (United States) Corporation (Magma) would demonstrate the potential geothermal resource at the Soda Lake geothermal area in Churchill County, Nevada. In Phase I (exploration geophysics), Magma would collect and interpret resistivity data from both Magnetotelluric and Controlled-Source Audio-Magnetotelluric electrical surveys, and conduct

174

Intersecting Fault Trends and Crustal-Scale Fluid Pathways Below the Dixie  

Open Energy Info (EERE)

Intersecting Fault Trends and Crustal-Scale Fluid Pathways Below the Dixie Intersecting Fault Trends and Crustal-Scale Fluid Pathways Below the Dixie Valley Geothermal Area, Nevada, Inferred from 3d Magnetotelluric Surveying Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Intersecting Fault Trends and Crustal-Scale Fluid Pathways Below the Dixie Valley Geothermal Area, Nevada, Inferred from 3d Magnetotelluric Surveying Abstract Geothermal systems may occur in zones of structural dilatency which create the crustal plumbing that al-lows concentration of high-temperature fluids from surrounding volumes. While structural orientations of the U.S. Great Basin are dominated visually by the NNE-oriented horst-graben morphology, other alignments are apparent, perhaps principally a NNW-trending grain

175

A Preparation Zone For Volcanic Explosions Beneath Naka-Dake Crater, Aso  

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 » A Preparation Zone For Volcanic Explosions Beneath Naka-Dake Crater, Aso Volcano, As Inferred From Magnetotelluric Surveys Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Preparation Zone For Volcanic Explosions Beneath Naka-Dake Crater, Aso Volcano, As Inferred From Magnetotelluric Surveys Details Activities (0) Areas (0) Regions (0) Abstract: The 1st crater of Naka-dake, Aso volcano, is one of the most active craters in Japan, and known to have a characteristic cycle of activity that consists of the formation of a crater lake, drying-up of the

176

DOI-BLM-NV-C010-2009-0051-CX | Open Energy Information  

Open Energy Info (EERE)

DOI-BLM-NV-C010-2009-0051-CX DOI-BLM-NV-C010-2009-0051-CX Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: DOI-BLM-NV-C010-2009-0051-CX CX at Soda Lake Geothermal Area for Geothermal/Exploration, Magnetotelluric Survey at Soda Lake General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CX Applicant Global Magma Energy Group Geothermal Area Soda Lake Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Magnetotelluric Techniques Comments The Bureau of Reclamation has deferred surface management authority to the BLM for this project. Time Frame (days) Application Time 27 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Carson City

177

CX-001731: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

31: Categorical Exclusion Determination 31: Categorical Exclusion Determination CX-001731: Categorical Exclusion Determination Recovery Act: Application of a New Structural Model and Exploration Technologies to Define a Blind Geothermal System: A Viable Alternative to Grid-Drilling for Geothermal Exploration: McCoy, Churchill County, Nevada CX(s) Applied: B3.1, A9 Date: 04/16/2010 Location(s): Churchill County, Nevada Office(s): Energy Efficiency and Renewable Energy, Golden Field Office Magma Energy (United States) Corporation (MEC) would demonstrate the potential geothermal resource at the McCoy geothermal area in Churchill County, Nevada (NV). In Phase 1 (exploration geophysics), Magma would collect and interpret resistivity data from both Magnetotelluric (MT) and Controlled-Source Audio-Magnetotelluric (CSAMT) electrical surveys, and

178

CX-001423: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

3: Categorical Exclusion Determination 3: Categorical Exclusion Determination CX-001423: Categorical Exclusion Determination Application of a New Structural Model and Exploration Technologies to Define a Blind Geothermal System: An Alternative to Grid-Drilling for Geothermal Exploration, McCoy, Churchill County, Nevada CX(s) Applied: B3.1, A9 Date: 03/29/2010 Location(s): McCoy, Nevada Office(s): Energy Efficiency and Renewable Energy, Golden Field Office Magma Energy (United States) Corporation (Magma) would demonstrate the potential geothermal resource at the McCoy geothermal area in Churchill County, Nevada. In Phase I (exploration geophysics), Magma would collect and interpret resistivity data from both Magnetotelluric and Controlled-Source Audio-Magnetotelluric electrical surveys, and conduct

179

CX-007430: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

30: Categorical Exclusion Determination 30: Categorical Exclusion Determination CX-007430: Categorical Exclusion Determination Innovative Computational Tools for Reducing Exploration Risk Through Integration of Water-rock Interactions and Magnetotelluric Surveys CX(s) Applied: A9, B3.6 Date: 12/01/2011 Location(s): Utah Offices(s): Golden Field Office The University of Utah would utilize DOE and cost share funds to develop the framework and procedures required to relate reservoir permeabilities (from indicators of water-rock ratios), degree and type of clay alteration, and temperature to the electrical resistivities of geothermal systems as recorded by magnetotelluric (MT) surveys. Laboratory work would be conducted in the X-ray diffraction and fluid inclusion laboratories located at the Energy and Geoscience Institute (EGI ), 423 Wakara Way, Research

180

A Numerical Evaluation Of Electromagnetic Methods In Geothermal Exploration  

Open Energy Info (EERE)

GEOTHERMAL ENERGYGeothermal Home GEOTHERMAL ENERGYGeothermal Home Journal Article: A Numerical Evaluation Of Electromagnetic Methods In Geothermal Exploration Details Activities (0) Areas (0) Regions (0) Abstract: The size and low resistivity of the clay cap associated with a geothermal system create a target well suited for electromagnetic (EM) methods and also make electrical detection of the underlying geothermal reservoir a challenge. Using 3-D numerical models, we evaluate four EM techniques for use in geothermal exploration: magnetotellurics (MT), controlled-source audio magnetotellurics (CSAMT), long-offset time-domain EM (LOTEM), and short-offset time-domain EM (TEM). Our results show that all of these techniques can delineate the clay cap, but none can be said to unequivocally detect the reservoir. We do find, however, that the EM

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Property:Abstract | Open Energy Information  

Open Energy Info (EERE)

Abstract Abstract Jump to: navigation, search This is a property of type Text. Pages using the property "Abstract" Showing 25 pages using this property. (previous 25) (next 25) 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + With the aim of investigating the possibilities of magnetotelluric methods for the exploration of potential Enhanced Geothermal System (EGS) sites in the Upper Rhine valley, a 2-D magnetotelluric (MT) survey has been carried out on a 13 km long profile across the thermal anomaly in the area of the geothermal power plant of Soultz-sous-Forets in the winter 2007/08. Despite strong artificial noise, processing using remote referencing and Sutarno phase consistent smoothing revealed significant results from 10 out of 16 sites. Indication for 1-D structures was found in the shortest periods, 2-D effects in the periods up to 40 s, and 3-D effects in the long period range. Since 3-D effects were found in the longer periods, 2-D inversion was carried out for periods smaller than 40 s. The results of the inversion are consistent with the geology of the geothermal site and distinguish well the sediments from the granitic basement including the structures given by the faults. A conductive anomaly with a resistivity of about 3 Ωm has been found at a depth down to 2000 m in the area of the Soultz and Kutzenhausen faults, which is attributed to geothermal processes.

182

Half-Monopole in the Weinberg-Salam Model  

E-Print Network (OSTI)

We present new axially symmetric half-monopole configuration of the SU(2)$\\times$U(1) Weinberg-Salam model of electromagnetic and weak interactions. The half-monopole configuration possesses net magnetic charge $2\\pi/e$ which is half the magnetic charge of a Cho-Maison monopole. The electromagnetic gauge potential is singular along the negative $z$-axis. However the total energy is finite and increases only logarithmically with increasing Higgs field self-coupling constant $\\lambda^{1/2}$ at $\\sin^2\\theta_W=0.2312$. In the U(1) magnetic field, the half-monopole is just a one dimensional finite length line magnetic charge extending from the origin $r=0$ and lying along the negative $z$-axis. In the SU(2) 't Hooft magnetic field, it is a point magnetic charge located at $r=0$. The half-monopole possesses magnetic dipole moment that decreases exponentially fast with increasing Higgs field self-coupling constant $\\lambda^{1/2}$ at $\\sin^2\\theta_W=0.2312$.

Rosy Teh; Ban-Loong Ng; Khai-Ming Wong

2014-06-04T23:59:59.000Z

183

Time-optimal synthesis of SU(2) transformations for a spin-1/2 system  

Science Journals Connector (OSTI)

We consider a quantum control problem involving a spin-1/2 particle in a magnetic field. The magnitude of the field is held constant, and the direction of the field, which is constrained to lie in the xy plane, serves as a control parameter that can be varied to govern the evolution of the system. We analytically solve for the time dependence of the control parameter that will synthesize a given target SU(2) transformation in the least possible amount of time, and we show that the time-optimal solutions have a simple geometric interpretation in terms of the fiber bundle structure of SU(2). We also generalize our time-optimal solutions to a control problem that includes a constant bias field along the z? axis and to the case of inhomogeneous control, in which a single control parameter governs the evolution of an ensemble of spin-1/2 systems.

A. D. Boozer

2012-01-19T23:59:59.000Z

184

Parallelization of the Red-Black Algorithm on Solving the Second-Order PN Transport Equation with the Hybrid Finite Element Method  

SciTech Connect

The Red-Black algorithm has been successfully applied on solving the second-order parity transport equation with the PN approximation in angle and the Hybrid Finite Element Method (HFEM) in space, i.e., the Variational Nodal Method (VNM) [1,2,3,4,5]. Any transport solving techniques, including the Red-Black algorithm, need to be parallelized in order to take the advantage of the development of supercomputers with multiple processors for the advanced modeling and simulation. To our knowledge, an attempt [6] was done to parallelize it, but it was devoted only to the z axis plans in three-dimensional calculations. General parallelization of the Red-Black algorithm with the spatial domain decomposition has not been reported in the literature. In this summary, we present our implementation of the parallelization of the Red-Black algorithm and its efficiency results.

Yaqi Wang; Cristian Rabiti; Giuseppe Palmiotti

2011-06-01T23:59:59.000Z

185

3-D GRMHD Simulations of Generating Jets  

E-Print Network (OSTI)

We have performed a first fully 3-D GRMHD simulation with Schwarzschild black hole with a free falling corona. The initial simulation results show that a jet is created as in the previous simulations using the axisymmetric geometry with the mirror symmetry at the equator. However, the time to generate the jet is longer than in the 2-D axisymmetric simulations. We expect that due to the additional freedom in the azimuthal dimension without axisymmetry with respect to the z axis and reflection symmetry with respect to the equatorial plane, the dynamics of jet formation can be modified. Further simulations are required for the study of instabilities along the azimuthal direction such as accretion-eject instability

Nishikawa, K I; Shibata, K; Kudoh, T; Sol, H

2002-01-01T23:59:59.000Z

186

3-D GRMHD Simulations of Generating Jets  

E-Print Network (OSTI)

We have performed a first fully 3-D GRMHD simulation with Schwarzschild black hole with a free falling corona. The initial simulation results show that a jet is created as in the previous simulations using the axisymmetric geometry with the mirror symmetry at the equator. However, the time to generate the jet is longer than in the 2-D axisymmetric simulations. We expect that due to the additional freedom in the azimuthal dimension without axisymmetry with respect to the z axis and reflection symmetry with respect to the equatorial plane, the dynamics of jet formation can be modified. Further simulations are required for the study of instabilities along the azimuthal direction such as accretion-eject instability

K. -I. Nishikawa; S. Koide; K. Shibata; T. Kudoh; H. Sol

2002-08-05T23:59:59.000Z

187

Current initiation in low-density foam z-pinch plasmas  

Science Journals Connector (OSTI)

Low density agar and aerogel foams were tested as z-pinch loads on the Saturn accelerator to study current flow initiation. In these first experiments we studied the initial plasma conditions by measuring the visible emission at early times with a framing camera and a streaked one-dimensional imaging system. Later near the stagnation when the plasma is hotter x-ray imaging and spectraldiagnostics were used to characterize the plasma.Filamentation and arcing at the current contacts were observed. Bright implosion features were also observed. Increasing the early time conductivity by coating the target with a high-z layer and by providing a low-current prepulse is the most important factor in obtaining good coupling to the machine. None of the pinches were uniform along the z axis. The prime causes of these problems are believed to be the electrode contacts and the current return configuration. Solutions are discussed.

M. S. Derzon; T. J. Nash; G. O. Allshouse; A. J. Antolak; M. Hurst; J. S. McGurn; D. J. Muron; J. F. Seaman; J. MacFarlane; T. Demiris; L. Hrubesh; H. Lewis; D. Ryutov; T. Barber; T. Gilliland; D. Jobe; S. Lazier

1997-01-01T23:59:59.000Z

188

Polarized-neutron reflectometry : recent developments and perspectives.  

SciTech Connect

Polarized neutron reflectometry (PNR) has an important role in solving non-collinear magnetic structures in thin films. In principle PNR provides the unambiguous determination of multi-axial magnetic depth profiles in systems of scientific and technological importance. However, only a limited number of problems have been solved unimpeachably, because the magnetic depth profiles were obtained by fitting procedures yielding solutions whose main features were not evident in the raw data. A recent formulation of reflectometry, and the concurrent development of 'total polarimetry; are now stimulating the design of neutron polarization and polarization analysis geometries capable of determining directly if and how a magnetic system contains a non-collinear structure in the film (x-y) plane. In the simplest of these geometries the neutrons are polarized and analyzed along the z-axis perpendicular to the film plane.

Felcher, G. P.; te Velthuis, S. G. E.; Ruhm, A.; Donner, W.; Materials Science Division; PNS

2001-03-01T23:59:59.000Z

189

Modular low aspect ratio-high beta torsatron  

DOE Patents (OSTI)

A fusion reactor device in which the toroidal magnetic field and at least a portion of the poloidal magnetic field are provided by a single set of modular coils. The coils are arranged on the surface of a low aspect ratio toroid in planes having the cylindrical coordinate relationship .phi.=.phi..sub.i +kz where k is a constant equal to each coil's pitch and .phi..sub.i is the toroidal angle at which the i'th coil intersects the z=o plane. The device may be described as a modular, high beta torsation whose screw symmetry is pointed along the systems major (z) axis. The toroid defined by the modular coils preferably has a racetrack minor cross section. When vertical field coils and preferably a toroidal plasma current are provided for magnetic field surface closure within the toroid, a vacuum magnetic field of racetrack shaped minor cross section with improved stability and beta valves is obtained.

Sheffield, George V. (Hopewell, NJ); Furth, Harold P. (Princeton, NJ)

1984-02-07T23:59:59.000Z

190

Property:References | Open Energy Information  

Open Energy Info (EERE)

References References Jump to: navigation, search This is a property of type Text. Subproperties This property has the following 43 subproperties: A Active Seismic Techniques Aeromagnetic Survey Airborne Gravity Survey Audio-Magnetotellurics C Chemical Logging Compound and Elemental Analysis Controlled Source Audio MT Controlled Source Frequency-Domain Magnetics D DC Resistivity Survey (Dipole-Dipole Array) DC Resistivity Survey (Mise-Á-La-Masse) DC Resistivity Survey (Pole-Dipole Array) DC Resistivity Survey (Schlumberger Array) DC Resistivity Survey (Wenner Array) Direct-Current Resistivity Survey D cont. Downhole Techniques E Electrical Profiling Configurations Electrical Techniques Electromagnetic Techniques F Frequency-Domain Electromagnetic Survey G Geodetic Survey Geophysical Techniques

191

Controlled Source Audio MT | Open Energy Information  

Open Energy Info (EERE)

Controlled Source Audio MT Controlled Source Audio MT Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Technique: Controlled Source Audio MT Details Activities (5) Areas (5) Regions (0) NEPA(0) Exploration Technique Information Exploration Group: Geophysical Techniques Exploration Sub Group: Electrical Techniques Parent Exploration Technique: Magnetotelluric Techniques Information Provided by Technique Lithology: Rock composition, mineral and clay content Stratigraphic/Structural: Detection of permeable pathways, fracture zones, faults Hydrological: Resistivity influenced by porosity, grain size distribution, permeability, fluid saturation, fluid type and phase state of the pore water Thermal: Resistivity influenced by temperature Cost Information Low-End Estimate (USD): 1,866.44186,644 centUSD

192

NVN-087930 | Open Energy Information  

Open Energy Info (EERE)

Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087930 CU at Desert Queen Geothermal Area for Geothermal/Exploration, {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Magma Energy Geothermal Area Desert Queen Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Magnetotelluric Methods Comments MT Survey Time Frame (days) Application Time 7 Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates Application Date 2009/09/09 Application Document Type NOI

193

NVN-086286 | Open Energy Information  

Open Energy Info (EERE)

6 6 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-086286 CU at Desert Queen Geothermal Area for Geothermal/Exploration, Magma Energy Action Plan for Geophysical and Vibroseis Surveys General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Magma Energy Consultant RMT, Inc. Geothermal Area Desert Queen Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Comments Desert Queen and Leach Hot Springs Time Frame (days) Application Time 31 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM

194

NVN-086761 | Open Energy Information  

Open Energy Info (EERE)

1 1 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-086761 CU at {{{GeothermalArea}}} for Geothermal/Exploration, {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Colado Project, LLC Geothermal Area {{{GeothermalArea}}}"{{{GeothermalArea}}}" cannot be used as a page name in this wiki. Project Location Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 5 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates Application Date 2009/02/19

195

Property:ExplorationSubGroup | Open Energy Information  

Open Energy Info (EERE)

ExplorationSubGroup ExplorationSubGroup Jump to: navigation, search Property Name ExplorationSubGroup Property Type Page Description Exploration sub groups for exploration activities Pages using the property "ExplorationSubGroup" Showing 25 pages using this property. (previous 25) (next 25) 2 2-M Probe Survey + Data Collection and Mapping + A Acoustic Logs + Well Log Techniques + Active Seismic Methods + Seismic Techniques + Active Seismic Techniques + Seismic Techniques + Active Sensors + Active Sensors + Aerial Photography + Passive Sensors + Aeromagnetic Survey + Magnetic Techniques + Airborne Electromagnetic Survey + Electrical Techniques + Airborne Gravity Survey + Gravity Techniques + Analytical Modeling + Modeling Techniques + Audio-Magnetotellurics + Electrical Techniques +

196

NVN-084629 | Open Energy Information  

Open Energy Info (EERE)

29 29 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-084629 CU at Patua Geothermal Area for Geothermal/Exploration, MT Survey at Patua Geothermal Project General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Vulcan Energy Geothermal Area Patua Geothermal Area Project Location Fernley, Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 13 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates Application Date 2008/01/22 Application Document Type NOI

197

NVN-087388 | Open Energy Information  

Open Energy Info (EERE)

NVN-087388 NVN-087388 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087388 CU at Salt Wells Geothermal Area for Geothermal/Exploration {{{NEPA_Name}}} General NEPA Document Info Environmental Analysis Type CU Applicant Enel North America Geothermal Area Salt Wells Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Audio-Magnetotellurics Comments Application via email with attached map and description of survey methodology and impacts. Time Frame (days) Application Time 1 Participating Agencies Lead Agency Stillwater Funding Agency none provided Managing District Office Carson City Managing Field Office Stillwater Funding Agencies none provided Surface Manager Stillwater Mineral Manager Stillwater

198

NVN-087811 | Open Energy Information  

Open Energy Info (EERE)

87811 87811 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087811 CU at New York Canyon Geothermal Area for Geothermal/Exploration, New York Canyon Geothermal Exploration and Development General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant TGP Dixie Development Co Geothermal Area New York Canyon Geothermal Area Project Location Lovelock, Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 21 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates

199

Program Description  

NLE Websites -- All DOE Office Websites (Extended Search)

Program Description Program Description SAGE, the Summer of Applied Geophysical Experience, is a unique educational program designed to introduce students in geophysics and related fields to "hands on" geophysical exploration and research. The program emphasizes both teaching of field methods and research related to basic science and a variety of applied problems. SAGE is hosted by the National Security Education Center and the Earth and Environmental Sciences Division of the Los Alamos National Laboratory. * teaches modern geophysical exploration techniques: seismic reflection and refraction, gravity and magnetics, electromagnetics (including magnetotellurics), and electrical resistivity * involves extensive hands-on field experience * integrates geophysical methods to solve real

200

Value of Information spreadsheet  

DOE Data Explorer (OSTI)

This spreadsheet represents the information posteriors derived from synthetic data of magnetotellurics (MT). These were used to calculate value of information of MT for geothermal exploration. Information posteriors describe how well MT was able to locate the "throat" of clay caps, which are indicative of hidden geothermal resources. This data is full explained in the peer-reviewed publication: Trainor-Guitton, W., Hoversten, G. M., Ramirez, A., Roberts, J., Jlusson, E., Key, K., Mellors, R. (Sept-Oct. 2014) The value of spatial information for determining well placement: a geothermal example, Geophysics.

Trainor-Guitton, Whitney

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Value of Information spreadsheet  

SciTech Connect

This spreadsheet represents the information posteriors derived from synthetic data of magnetotellurics (MT). These were used to calculate value of information of MT for geothermal exploration. Information posteriors describe how well MT was able to locate the "throat" of clay caps, which are indicative of hidden geothermal resources. This data is full explained in the peer-reviewed publication: Trainor-Guitton, W., Hoversten, G. M., Ramirez, A., Roberts, J., Jlusson, E., Key, K., Mellors, R. (Sept-Oct. 2014) The value of spatial information for determining well placement: a geothermal example, Geophysics.

Trainor-Guitton, Whitney

2014-05-12T23:59:59.000Z

202

NVN-086285 | Open Energy Information  

Open Energy Info (EERE)

5 5 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-086285 CU at Desert Peak Geothermal Area for Geothermal/Exploration, Magma Energy Action Plan for Geophysical and Vibroseis Surveys General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Magma Energy Geothermal Area Desert Peak Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 31 Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates Application Date 2008/10/31

203

NVN-087791 | Open Energy Information  

Open Energy Info (EERE)

NVN-087791 NVN-087791 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-087791 CU at New York Canyon Geothermal Area for Geothermal/Exploration, New York Canyon Geothermal Exploration and Development General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant TGP Dixie Development Company Geothermal Area New York Canyon Geothermal Area Project Location Lovelock, Nevada Project Phase Geothermal/Exploration Techniques Magnetotellurics Time Frame (days) Application Time 28 Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM Mineral Manager BLM

204

NVN-89306 | Open Energy Information  

Open Energy Info (EERE)

NVN-89306 NVN-89306 Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: NVN-89306 CU at {{{GeothermalArea}}} for Geothermal/Exploration, Spring Gulch MT Survey General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CU Applicant Terra Gen Dixie Valley Development Co Geothermal Area {{{GeothermalArea}}}"{{{GeothermalArea}}}" cannot be used as a page name in this wiki. Project Location Project Phase Geothermal/Exploration Techniques Magnetotellurics Comments MT Survey, Spring Gulch Project Time Frame (days) Participating Agencies Lead Agency Nevada Funding Agency none provided Managing District Office Winnemucca Managing Field Office Humboldt River Funding Agencies none provided Surface Manager BLM

205

Application of a New Structural Model and Exploration Technologies to  

Open Energy Info (EERE)

New Structural Model and Exploration Technologies to New Structural Model and Exploration Technologies to Define a Blind Geothermal System: A Viable Alternative to Grid-Drilling for Geothermal Exploration: McCoy, Churchill County, NV Geothermal Project Jump to: navigation, search Last modified on July 22, 2011. Project Title Application of a New Structural Model and Exploration Technologies to Define a Blind Geothermal System: A Viable Alternative to Grid-Drilling for Geothermal Exploration: McCoy, Churchill County, NV Project Type / Topic 1 Recovery Act: Geothermal Technologies Program Project Type / Topic 2 Validation of Innovative Exploration Technologies Project Description The structural model is based on the role of subsurface igneous dikes providing a buttressing effect in a regional strain field such that permeability is greatly enhanced. The basic thermal anomaly at McCoy was defined by substantial U.S. Department of Energy-funded temperature gradient drilling and geophysical studies conducted during the period 1978 to 1982. This database will be augmented with modern magnetotelluric, controlled-source audio-magnetotelluric, and 2D/3D reflection seismic surveys to define likely fluid up-flow plumes that will be drilled with slant-hole technology. Two sites for production-capable wells will be drilled in geothermally prospective areas identified in this manner. The uniqueness of this proposal lies in the use of a full suite of modern geophysical tools, use of slant-hole drilling, and the extensive technical database from previous DOE funding.

206

The influence of Zn vacancy on thermal conductivity of {beta}-Zn{sub 4}Sb{sub 3}: A molecular dynamics study  

SciTech Connect

The influence of Zn vacancy on lattice thermal conductivity of {beta}-Zn{sub 4}Sb{sub 3} is studied by non-equilibrium molecular dynamics approach. The lattice thermal conductivity of single-crystal bulk {beta}-Zn{sub 4}Sb{sub 3} decreases rapidly when there is Zn vacancy, and then when the vacancy grows, the lattice thermal conductivity decreases further but rather slowly, which suggests a scaling law of k{sub v}{approx}n{sub v}{sup -{alpha}} of Zn atom vacancy (n{sub v}) to lattice thermal conductivity (k{sub vac}). This phenomenon is attributed to the fact that the existence of vacancy scattering can significantly decrease the mean free path. When the Zn atom vacant proportion reaches 10%, that is the vacancy model of {beta}-Zn{sub 4}Sb{sub 3}, the lattice thermal conductivity is 1.32 W/mk along the x-axis and 1.62 W/mk along the z-axis, respectively, which drops by {approx}90% that of its full occupancy model. Therefore, our calculations show that the 10% Zn atom vacancy in {beta}-Zn{sub 4}Sb{sub 3} is the main reason for its exceptionally low thermal conductivity, and the interstitial Zn atoms have little effect on the thermal conductivity of single-crystal {beta}-Zn{sub 4}Sb{sub 3}. - Graphical abstract: The bulk thermal conductivity (k{sub pure}) is 11.88 W/mk along the x-axis and 20.00 W/mk the z-axis. When it is 10% vacancy, namely the vacancy model of {beta}-Zn{sub 4}Sb{sub 3}, the thermal conductivity of {beta}-Zn{sub 4}Sb{sub 3} is 1.32 W/mk along the x-axis and 1.62 W/mk along the z-axis, respectively, which reduces by {approx}90% that of its full occupancy model. Our calculations show that the 10% Zn atom vacancy in the crystal structure of {beta}-Zn{sub 4}Sb{sub 3} is the main reason for its exceptionally low thermal conductivity, and the interstitial Zn atoms have little effect on the thermal conductivity of single-crystal {beta}-Zn{sub 4}Sb{sub 3}. Highlights: Black-Right-Pointing-Pointer The lattice stability of {beta}-Zn{sub 4}Sb{sub 3} decreases remarkably with the growing vacancy. Black-Right-Pointing-Pointer 10% Zn vacancy leads to its low thermal conductivity and structural instability. Black-Right-Pointing-Pointer Interstitial Zn atoms in {beta}-Zn{sub 4}Sb{sub 3} mainly stabilize the crystal structure.

Zhai, Pengcheng [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China) [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China); State Key Laboratory of Advanced Technology of Materials Synthesis and Processing, Wuhan University of Technology, Wuhan 430070 (China); Li, Guodong; Wen, Pengfei [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China)] [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China); Li, Yao, E-mail: liyao06@126.com [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China)] [Department of Engineering Structure and Mechanics, Wuhan University of Technology, Wuhan 430070 (China); Zhang, Qingjie; Liu, Lisheng [State Key Laboratory of Advanced Technology of Materials Synthesis and Processing, Wuhan University of Technology, Wuhan 430070 (China)] [State Key Laboratory of Advanced Technology of Materials Synthesis and Processing, Wuhan University of Technology, Wuhan 430070 (China)

2012-09-15T23:59:59.000Z

207

Spontaneous Potential At Fort Bidwell Area (Laney, 2005) | Open Energy  

Open Energy Info (EERE)

Spontaneous Potential At Fort Bidwell Area (Laney, 2005) Spontaneous Potential At Fort Bidwell Area (Laney, 2005) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Spontaneous Potential Well Log At Fort Bidwell Area (Laney, 2005) Exploration Activity Details Location Fort Bidwell Area Exploration Technique Spontaneous Potential Well Log 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

208

Property:DataAcquisition | Open Energy Information  

Open Energy Info (EERE)

DataAcquisition DataAcquisition Jump to: navigation, search Property Name DataAcquisition Property Type Text Description Information on acquisition, including both collection and lists of data repositories. Subproperties This property has the following 27 subproperties: A Active Seismic Techniques Aeromagnetic Survey C Controlled Source Frequency-Domain Magnetics Core Analysis D Direct-Current Resistivity Survey E Electrical Techniques F FLIR FMI Log Frequency-Domain Electromagnetic Survey G Ground Gravity Survey Ground Magnetics H Hand-held X-Ray Fluorescence (XRF) I Isotopic Analysis- Fluid Isotopic Analysis- Rock M Magnetotellurics Mud Logging P PSInSAR R Radar Reflection Survey R cont. Refraction Survey S SRT Self Potential Step-out Well Stereo Satellite Imagery T Telluric Survey Time-Domain Electromagnetics

209

Category:Geothermal References | 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 Category Edit History Facebook icon Twitter icon » Category:Geothermal References Jump to: navigation, search Add a new Reference Pages in category "Geothermal References" The following 200 pages are in this category, out of 323 total. (previous 200) (next 200) 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth 2007 Annual Report A A Case History of Injection Through 1991 at Dixie Valley, Nevada A Coordinated Exploration Program for Geothermal Sources on the Island of Hawaii A geochemical model of the Kilauea east rift zone A model for the shallow thermal regime at Dixie Valley geothermal field

210

DOI-BLM-NV-CO1000-2010-0021-CX | Open Energy Information  

Open Energy Info (EERE)

DOI-BLM-NV-CO1000-2010-0021-CX DOI-BLM-NV-CO1000-2010-0021-CX Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: DOI-BLM-NV-CO1000-2010-0021-CX CX at Coyote Canyon Geothermal Area for Geothermal/Exploration, {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CX Applicant TGP Dixie Development LLC Geothermal Area Coyote Canyon Geothermal Area Project Location Churchill County, NV, Churchill County, NV Project Phase Geothermal/Exploration Techniques Magnetotelluric Methods Time Frame (days) Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Carson City Managing Field Office Stillwater Funding Agencies none provided Surface Manager Nevada Mineral Manager BLM

211

Direct-Current Resistivity Survey At Valles Caldera - Sulphur Springs Area  

Open Energy Info (EERE)

Wilt & Haar, 1986) Wilt & Haar, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Valles Caldera - Sulphur Springs Area (Wilt & Haar, 1986) Exploration Activity Details Location Valles Caldera - Sulphur Springs Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Telluric profiles, magnetotelluric sounding, dc resistivity, and electromagnetic sounding surveys were all performed over the caldera in hopes of outlining deep drilling targets (Group 7 Inc., 1972; McPhar, 1973; Geonomics Inc., 1976). These data are used to help define the electrical structure in the reservoir region. Some of the data were reinterpreted using computer models, and interpretations from the various surveys were

212

Thermal Gradient Holes At Salt Wells Area (Bureau of Land Management, 2009)  

Open Energy Info (EERE)

Thermal Gradient Holes At Salt Wells Area (Bureau of Land Management, 2009) Thermal Gradient Holes At Salt Wells Area (Bureau of Land Management, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Thermal Gradient Holes At Salt Wells Area (Bureau of Land Management, 2009) Exploration Activity Details Location Salt Wells Geothermal Area Exploration Technique Thermal Gradient Holes Activity Date 2008 - 2008 Usefulness not indicated DOE-funding Unknown Exploration Basis Vulcan increased exploration efforts in the summer and fall of 2008, during which time the company drilled two temperature gradient holes (86-15 O on Pad 1 and 17-16 O on Pad 3); conducted seismic, gravity and magnetotelluric surveys; and drilled deep exploration wells at Pads 6 and 8 and binary wells at Pads 1, 2, 4, and 7. Notes

213

Single-Well and Cross-Well Seismic At Salt Wells Area (Bureau of Land  

Open Energy Info (EERE)

Single-Well and Cross-Well Seismic At Salt Wells Area (Bureau of Land Single-Well and Cross-Well Seismic At Salt Wells Area (Bureau of Land Management, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Single-Well and Cross-Well Seismic At Salt Wells Area (Bureau of Land Management, 2009) Exploration Activity Details Location Salt Wells Geothermal Area Exploration Technique Single-Well And Cross-Well Seismic Activity Date 2008 - 2008 Usefulness not indicated DOE-funding Unknown Exploration Basis Vulcan increased exploration efforts in the summer and fall of 2008, during which time the company drilled two temperature gradient holes (86-15 O on Pad 1 and 17-16 O on Pad 3); conducted seismic, gravity and magnetotelluric surveys; and drilled deep exploration wells at Pads 6 and 8 and binary

214

Property:Foaf/Page | Open Energy Information  

Open Energy Info (EERE)

Page Page Jump to: navigation, search Property Name Foaf/Page Property Type URL Description Link to an external page discussing the same topic. (URL) It is equivalent to the well-known foaf:page property. Pages using the property "Foaf/Page" Showing 25 pages using this property. (previous 25) (next 25) 1 10 CFR § 1021 + http://en.openei.org/wiki/File:10CFRPart1021.pdf + 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + http://www.sciencedirect.com/science/article/pii/S1631071310001070 + 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits + http://www.sciencedirect.com/science/article/B6VCS-48B5BV5-KK/2/a841cce0d247b754e5163bb62f72dc05 +

215

Exploration for Geothermal Resources in Dixie Valley, Nevada- Case History  

Open Energy Info (EERE)

in Dixie Valley, Nevada- Case History in Dixie Valley, Nevada- Case History Jump to: navigation, search OpenEI Reference LibraryAdd to library Journal Article: Exploration for Geothermal Resources in Dixie Valley, Nevada- Case History Abstract After several years of reconnaissance geology in Nevada, an exploration program to evaluate the geothermal resource potential of Dixie Valley was begun in 1974. Between 1974 and 1978 Sunoco Energy Development Co. conducted two heat-flow drilling programs, a resistivity survey, a seismic emission study, a ground noise survey, two magnetotelluric surveys, a hydrology study, and a surface geology survey. The synthesis of the data resulting from these projects into the regional geologic framework led to the acquisition of geothermal resource leases from fee property owners,

216

DOI-BLM-NV-CO1000-2010-0022-CX | Open Energy Information  

Open Energy Info (EERE)

DOI-BLM-NV-CO1000-2010-0022-CX DOI-BLM-NV-CO1000-2010-0022-CX Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home NEPA Document Collection for: DOI-BLM-NV-CO1000-2010-0022-CX CX at Coyote Canyon Geothermal Area for Geothermal/Exploration, {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CX Applicant Terra-Gen Power LLC Geothermal Area Coyote Canyon Geothermal Area Project Location Churchill County, NV, Churchill County, NV Project Phase Geothermal/Exploration Techniques Electromagnetic Techniques, Magnetotelluric Techniques, Seismic Techniques Time Frame (days) Application Time 213 Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Carson City Managing Field Office Stillwater Funding Agencies none provided

217

CX-004109: Categorical Exclusion Determination | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

109: Categorical Exclusion Determination 109: Categorical Exclusion Determination CX-004109: Categorical Exclusion Determination Phase 2 - A 3D-3C Reflection Seismic Survey and Data Integration to Identify the Seismic Response of Fractures and Permeable Zones over a Known Geothermal Resource: Soda Lake, Churchill County, Nevada CX(s) Applied: B3.1, B3.7 Date: 09/29/2010 Location(s): Soda Lake, Nevada Office(s): Energy Efficiency and Renewable Energy, Golden Field Office Magma Energy Corporation would demonstrate the potential geothermal resource at the Soda Lake geothermal area in Churchill County, Nevada. In Phase 1 (exploration geophysics), Magma collected and interpreted resistivity data from both Magnetotelluric and Controlled-Source Audio-Magnotelluric electrical surveys, and conduct detailed geologic

218

Category:Reference Materials | 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 Category Edit History Facebook icon Twitter icon » Category:Reference Materials Jump to: navigation, search This is a deprecated subcategory. All Reference Materials will be converted to References. Pages in category "Reference Materials" The following 200 pages are in this category, out of 2,265 total. (previous 200) (next 200) 1 10 CFR § 1021 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits 238U Decay Series Systematics Of Young Lavas From Batur Volcano, Sunda Arc

219

Exploratory Well At Salt Wells Area (Bureau of Land Management, 2009) |  

Open Energy Info (EERE)

Exploratory Well At Salt Wells Area (Bureau of Land Management, 2009) Exploratory Well At Salt Wells Area (Bureau of Land Management, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Exploratory Well At Salt Wells Area (Bureau of Land Management, 2009) Exploration Activity Details Location Salt Wells Geothermal Area Exploration Technique Exploratory Well Activity Date 2008 - 2008 Usefulness not indicated DOE-funding Unknown Exploration Basis Vulcan increased exploration efforts in the summer and fall of 2008, during which time the company drilled two temperature gradient holes (86-15 O on Pad 1 and 17-16 O on Pad 3); conducted seismic, gravity and magnetotelluric surveys; and drilled deep exploration wells at Pads 6 and 8 and binary wells at Pads 1, 2, 4, and 7. Notes Data from these wells is proprietary, and so were unavailable for inclusion

220

Direct-Current Resistivity Survey At Valles Caldera - Redondo Area (Wilt &  

Open Energy Info (EERE)

Wilt & Wilt & Haar, 1986) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Direct-Current Resistivity Survey At Valles Caldera - Redondo Area (Wilt & Haar, 1986) Exploration Activity Details Location Valles Caldera - Redondo Area Exploration Technique Direct-Current Resistivity Survey Activity Date Usefulness not indicated DOE-funding Unknown Notes Telluric profiles, magnetotelluric sounding, dc resistivity, and electromagnetic sounding surveys were all performed over the caldera in hopes of outlining deep drilling targets (Group 7 Inc., 1972; McPhar, 1973; Geonomics Inc., 1976). These data are used to help define the electrical structure in the reservoir region. Some of the data were reinterpreted using computer models, and interpretations from the various surveys were

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Time-Domain Electromagnetics At Long Valley Caldera Area (Sorey, Et Al.,  

Open Energy Info (EERE)

1991) 1991) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Time-Domain Electromagnetics At Long Valley Caldera Area (Sorey, Et Al., 1991) Exploration Activity Details Location Long Valley Caldera Area Exploration Technique Time-Domain Electromagnetics Activity Date Usefulness useful DOE-funding Unknown Notes In 1986, Unocal Geothermal Division released results from 158 time-domain electromagnetic (TDEM) soundings and, with Chevron Resources, a total of 77 magnetotelluric (MT) stations. Reinterpretations of the Unocal and Chevron data (Park and Torres-Verdin, 1988 ) and the recent public-domain MT studies (e.g. Hermance et al., 1988) outline similar shallow low-resistivity regions. At shallow depths in the caldera References Michael L. Sorey, Gene A. Suemnicht, Neil C. Sturchio, Gregg A.

222

A Portable Elf-Mt System For Shallow Resistivity Sounding | 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 » A Portable Elf-Mt System For Shallow Resistivity Sounding Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: A Portable Elf-Mt System For Shallow Resistivity Sounding Details Activities (0) Areas (0) Regions (0) Abstract: In view of recent extensive investigation of shallow resistivity structure for active fault studies and geothermal exploration, we developed a portable magnetotelluric (MT) system for the extremely low frequency (ELF) range. The system aims primarily at making real-time analyses of MT data at the so-called Schumann resonance frequencies of ~ 8, 14 and 20 Hz.

223

Property:FieldProcedures | Open Energy Information  

Open Energy Info (EERE)

FieldProcedures FieldProcedures Jump to: navigation, search Property Name FieldProcedures Property Type Text Description Description of actions, equipment and footprint of the exploration activity Subproperties This property has the following 39 subproperties: A Active Seismic Techniques Airborne Gravity Survey Audio-Magnetotellurics C Controlled Source Audio MT Cross-Dipole Acoustic Log D DC Resistivity Survey (Dipole-Dipole Array) DC Resistivity Survey (Mise-Á-La-Masse) DC Resistivity Survey (Pole-Dipole Array) DC Resistivity Survey (Schlumberger Array) DC Resistivity Survey (Wenner Array) Development Drilling Direct-Current Resistivity Survey Drilling Techniques E Earth Tidal Analysis Electrical Profiling Configurations Electromagnetic Techniques Exploration Drilling F FMI Log Frequency-Domain Electromagnetic Survey

224

Ground Gravity Survey At Truckhaven Area (Layman Energy Associates, 2009) |  

Open Energy Info (EERE)

Truckhaven Area (Layman Energy Associates, 2009) Truckhaven Area (Layman Energy Associates, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Truckhaven Area (Layman Energy Associates, 2009) Exploration Activity Details Location Truckhaven Area Exploration Technique Ground Gravity Survey Activity Date Usefulness useful DOE-funding Unknown Notes The area of coverage for the DOE-funded geophysical surveys is shown in Figure 9. The 95 magnetotelluric (MT) soundings cover a central area of about 80 square kilometers. The 126 gravity stations extend over a broader area of about 150 square kilometers, centered on the same area covered by the MT soundings. A detailed description of the instrumentation and data acquisition procedures used for both surveys is provided in GSY-USA, Inc.

225

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

226

Airborne electromagnetic surveys as a reconnaissance technique for  

Open Energy Info (EERE)

electromagnetic surveys as a reconnaissance technique for electromagnetic surveys as a reconnaissance technique for geothermal exploration Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Conference Proceedings: Airborne electromagnetic surveys as a reconnaissance technique for geothermal exploration Details Activities (1) Areas (1) Regions (0) Abstract: INPUT airborne electromagnetic (AEM) surveys were conducted during 1979 in five Known Geothermal Resource Areas (KGRA's). AEM work has not been significantly utilized in the past for geothermal purposes because it was thought that a shallow exploration technique would not be effective. Extensive audio-magnetotelluric (AMT) work by the USGS in KGRA's showed that many geothermal systems do have a near-surface electrical signature which should be detectable by an AEM system. INPUT responses in the form of

227

Airborne Electromagnetic Survey At Raft River Geothermal Area (1979) | Open  

Open Energy Info (EERE)

Electromagnetic Survey At Raft River Electromagnetic Survey At Raft River Geothermal Area (1979) Exploration Activity Details Location Raft River Geothermal Area Exploration Technique Airborne Electromagnetic Survey Activity Date 1979 Usefulness not indicated DOE-funding Unknown Exploration Basis To show that AEM methods can be useful in exploration for and defining geothermal systems Notes Extensive audio-magnetotelluric (AMT) work by the USGS in KGRA's showed that many geothermal systems do have a near-surface electrical signature which should be detectable by an AEM system. References Christopherson, K.R.; Long, C.L.; Hoover, D.B. (1 September 1980) Airborne electromagnetic surveys as a reconnaissance technique for geothermal exploration Retrieved from "http://en.openei.org/w/index.php?title=Airborne_Electromagnetic_Survey_At_Raft_River_Geothermal_Area_(1979)&oldid=510231

228

Property:Document type | Open Energy Information  

Open Energy Info (EERE)

Document type Document type Jump to: navigation, search Property Name Document type Property Type String Description The type of document as a string. This property is used by a variety of concepts including Reference Materials and may contain document types appropriate for multiple concepts. Allows Values Book;Book Review;Book Section;Conference Paper;Conference Proceedings;General;Info Graphic/Map/Chart;Journal Article;Legal;Memorandum;Periodical;Personal Communication;Poster;Report;Thesis/Dissertation;Web Site Pages using the property "Document type" Showing 25 pages using this property. (previous 25) (next 25) 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + Journal Article + 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits + Journal Article +

229

Cryptic Faulting and Multi-Scale Geothermal Fluid Connections in the Dixie  

Open Energy Info (EERE)

Cryptic Faulting and Multi-Scale Geothermal Fluid Connections in the Dixie Cryptic Faulting and Multi-Scale Geothermal Fluid Connections in the Dixie Valley-Central Nevada Seismic Belt Area- Implications from Mt Resistivity Surveying Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Cryptic Faulting and Multi-Scale Geothermal Fluid Connections in the Dixie Valley-Central Nevada Seismic Belt Area- Implications from Mt Resistivity Surveying Abstract Extended magnetotelluric (MT) profiling results over the Dixie Valley-Central Nevada Seismic Belt area were recently completed to explore the hypothesis that fluid circulation to depths of 10 km or more is generating well temperatures in the field >280 C.This transect has revealed families of resistivity structures commonly dominated by high-angle

230

DOI-BLM-NV-C010-2012-0070-CX | Open Energy Information  

Open Energy Info (EERE)

C010-2012-0070-CX C010-2012-0070-CX CX at Dixie Valley Geothermal Area for Geothermal/Exploration {{{NEPA_Name}}} General NEPA Document Info Energy Sector Geothermal energy Environmental Analysis Type CX Applicant US Navy Geothermal Program Office Geothermal Area Dixie Valley Geothermal Area Project Location Nevada Project Phase Geothermal/Exploration Techniques Magnetotelluric Methods, Reflection Survey Time Frame (days) Application Time 115 Participating Agencies Lead Agency BLM Funding Agency none provided Managing District Office Carson City Managing Field Office Stillwater Funding Agencies none provided Surface Manager BLM Mineral Manager BLM Selected Dates Application Date 4/30/2012 Revised Application Date 7/27/2012 Decision Document Date 8/23/2012 Relevant Numbers

231

Page not found | Department of Energy  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

91 - 24800 of 26,764 results. 91 - 24800 of 26,764 results. Download CX-007430: Categorical Exclusion Determination Innovative Computational Tools for Reducing Exploration Risk Through Integration of Water-rock Interactions and Magnetotelluric Surveys CX(s) Applied: A9, B3.6 Date: 12/01/2011 Location(s): Utah Offices(s): Golden Field Office http://energy.gov/nepa/downloads/cx-007430-categorical-exclusion-determination Download CX-007748: Categorical Exclusion Determination Integration of the Farm Power Misty Meadows Generating Facility CX(s) Applied: B1.7 Date: 01/11/2012 Location(s): Oregon Offices(s): Bonneville Power Administration http://energy.gov/nepa/downloads/cx-007748-categorical-exclusion-determination Download CX-007862: Categorical Exclusion Determination Northeast Photovoltaic Regional Training Provider

232

Information needs for characterization of high-level waste repository sites in six geologic media. Volume 2. Appendices  

SciTech Connect

Volume II contains appendices for the following: (1) remote sensing and surface mapping techniques; (2) subsurface mapping methods for site characterization; (3) gravity technique; (4) audio-frequency magnetotelluric technique; (5) seismic refraction technique; (6) direct-current electrical resistivity method; (7) magnetic technique; (8) seismic reflection technique; (9) seismic crosshole method; (10) mechanical downhole seismic velocity survey method; (11) borehole geophysical logging techniques; (12) drilling and coring methods for precharacterization studies; (13) subsurface drilling methods for site characterization; (14) geomechanical/thermomechanical techniques for precharacterization studies; (15)geomechanical/thermal techniques for site characterization studies; (16) exploratory geochemical techniques for precharacterization studies; (17) geochemical techniques for site characterization; (18) hydrologic techniques for precharacterization studies; (19) hydrologic techniques for site characterization; and (20) seismological techniques.

NONE

1985-05-01T23:59:59.000Z

233

Geological interpretation of Mount Ciremai geothermal system from remote sensing and magneto-teluric analysis  

E-Print Network (OSTI)

The exploration of geothermal system at Mount Ciremai has been started since the early 1980s and has just been studied carefully since the early 2000s. Previous studies have detected the potential of geothermal system and also the groundwater mechanism feeding the system. This paper will discuss the geothermal exploration based on regional scale surface temperature analysis with Landsat image to have a more detail interpretation of the geological setting and magneto-telluric or MT survey at prospect zones, which identified by the previous method, to have a more exact and in depth local scale structural interpretation. Both methods are directed to pin point appropriate locations for geothermal pilot hole drilling and testing. We used four scenes of Landsat Enhanced Thematic Mapper or ETM+ data to estimate the surface manifestation of a geothermal system. Temporal analysis of Land Surface Temperature or LST was applied and coupled with field temperature measurement at seven locations. By combining the TTM with ...

Sumintadireja, Prihadi; Irawan, Dasapta E; Irawan, Diky; Fadillah, Ahmad

2015-01-01T23:59:59.000Z

234

Instrumentation and process control development for in situ coal gasification  

SciTech Connect

This report describes (1) the results of calculations made to determine the influence of various permeability structures on reverse combustion linkage for UCG, and (2) the results of heavy oil fireflood mapping by the Controlled Source Audio Magnetotelluric (CSAMT) method proposed for UCG process mapping. A two-phase, two-dimension reservoir model called RESEV was used for the permeability effects work; the results indicate that high permeability horizontal zones, well completion and separation, and orthotropic permeability all have significant influence on the success of reverse combustion linkage. Specific conclusions are made which emphasize the need for careful site characterization and for proper well completions. Regarding the second activity, CSAMT-derived resistivity maps provided good descriptions of the progress of the fireflood, which is being conducted by BETC near Bartlette, KS. The combustion front apparently did not proceed in a uniform, radial manner.

Love, S.L. (ed.)

1981-03-01T23:59:59.000Z

235

DC Resistivity Survey (Schlumberger Array) At Coso Geothermal Area (1977) |  

Open Energy Info (EERE)

DC Resistivity Survey (Schlumberger Array) At Coso DC Resistivity Survey (Schlumberger Array) At Coso Geothermal Area (1977) Exploration Activity Details Location Coso Geothermal Area Exploration Technique DC Resistivity Survey (Schlumberger Array) Activity Date 1977 Usefulness not indicated DOE-funding Unknown Exploration Basis To investigate electrical properties of rocks associated with thermal phenomena of the Devil's Kitchen-Coso Hot Springs area Notes 18 USGS Schlumberger soundings and 6 Schlumberger soundings by Furgerson (1973) were plotted and automatically processed and interpreted References Jackson, D.B. ODonnell, J.E.; Gregory, D. I. (1 January 1977) Schlumberger soundings, audio-magnetotelluric soundings and telluric mapping in and around the Coso Range, California Retrieved from "http://en.openei.org/w/index.php?title=DC_Resistivity_Survey_(Schlumberger_Array)_At_Coso_Geothermal_Area_(1977)&oldid=591389

236

u.s. DEPARTMENT OF ENERGY EERE PROJECT MANAGEMENT CENTER NEPA DETERMINATION  

Energy.gov (U.S. Department of Energy (DOE)) Indexed Site

{~." ,.~ I {~." ,.~ I u.s. DEPARTMENT OF ENERGY EERE PROJECT MANAGEMENT CENTER NEPA DETERMINATION REClPIENT: University of Utah Page 1 of2 STATE: UT PROJECT TITLE: Innovative Computational Tools for Reducing Exploration Risk T hrough Integration of Water-rock Interactions and Magnetotelluric Surveys Funding Opportunity Announcement Number DE-FOA-OOOOS22 Procurement Instrument Number NEPA Control Number CID Number DE-EEOOO5S2 1 GFO-OOO5521-OO1 a Based on my review ofthe information concerning the proposed action, as NEPA Compliance Officer (authorized under DOE Order4SI.IA), I have made the following determination: ex, EA, EIS APPENDIX AND NU MBER: Description: A91nformation gathering, analysis, and d issemination Information gathering (including, but not limited to, literature surveys, inventories, site visits, and audits), data analysis

237

Ground Gravity Survey At Salt Wells Area (Bureau of Land Management, 2009)  

Open Energy Info (EERE)

Salt Wells Area (Bureau of Land Management, 2009) Salt Wells Area (Bureau of Land Management, 2009) Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Exploration Activity: Ground Gravity Survey At Salt Wells Area (Bureau of Land Management, 2009) Exploration Activity Details Location Salt Wells Geothermal Area Exploration Technique Ground Gravity Survey Activity Date 2008 - 2008 Usefulness not indicated DOE-funding Unknown Exploration Basis Vulcan increased exploration efforts in the summer and fall of 2008, during which time the company drilled two temperature gradient holes (86-15 O on Pad 1 and 17-16 O on Pad 3); conducted seismic, gravity and magnetotelluric surveys; and drilled deep exploration wells at Pads 6 and 8 and binary wells at Pads 1, 2, 4, and 7. Notes Data from these wells is proprietary, and so were unavailable for inclusion

238

Property:Author | Open Energy Information  

Open Energy Info (EERE)

Property Property Edit with form History Facebook icon Twitter icon » Property:Author Jump to: navigation, search Property Name Author Property Type String Description The author of a document, resource, reference material or tool. Pages using the property "Author" Showing 25 pages using this property. (previous 25) (next 25) 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + Johannes Geiermann +, Eva Schill + 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits + Peter W. Lipman +, O. A. Bogatikov +, A. A. Tsvetkov +, ... 2007 Annual Report + Enel + 238U Decay Series Systematics Of Young Lavas From Batur Volcano, Sunda Arc + K. H. Rubin +, G. E. Wheller +, M. O. Tanzer +, ...

239

3D Magnetotelluic characterization of the Coso Geothermal Field | Open  

Open Energy Info (EERE)

Magnetotelluic characterization of the Coso Geothermal Field Magnetotelluic characterization of the Coso Geothermal Field Jump to: navigation, search GEOTHERMAL ENERGYGeothermal Home Journal Article: 3D Magnetotelluic characterization of the Coso Geothermal Field Details Activities (1) Areas (1) Regions (0) Abstract: Electrical resistivity may contribute to progress in understanding geothermal systems by imaging the geometry, bounds and controlling structures in existing production, and thereby perhaps suggesting new areas for field expansion. To these ends, a dense grid of magnetotelluric (MT) stations plus a single line of contiguous bipole array profiling has been acquired over the east flank of the Coso geothermal system. Acquiring good quality MT data in producing geothermal systems is a challenge due to production related electromagnetic (EM) noise and, in the

240

Density of defects and the scaling law of the entanglement entropy in quantum phase transition of one-dimensional spin systems induced by a quench  

SciTech Connect

We have studied quantum phase transition induced by a quench in different one-dimensional spin systems. Our analysis is based on the dynamical mechanism which envisages nonadiabaticity in the vicinity of the critical point. This causes spin fluctuation which leads to the random fluctuation of the Berry phase factor acquired by a spin state when the ground state of the system evolves in a closed path. The two-point correlation of this phase factor is associated with the probability of the formation of defects. In this framework, we have estimated the density of defects produced in several one-dimensional spin chains. At the critical region, the entanglement entropy of a block of L spins with the rest of the system is also estimated which is found to increase logarithmically with L. The dependence on the quench time puts a constraint on the block size L. It is also pointed out that the Lipkin-Meshkov-Glick model in point-splitting regularized form appears as a combination of the XXX model and Ising model with magnetic field in the negative z axis. This unveils the underlying conformal symmetry at criticality which is lost in the sharp point limit. Our analysis shows that the density of defects as well as the scaling behavior of the entanglement entropy follows a universal behavior in all these systems.

Basu, Banasri; Bandyopadhyay, Pratul; Majumdar, Priyadarshi [Physics and Applied Mathematics Unit, Indian Statistical Institute, Kolkata 700 108 (India); Jyotinagar Bidyasree Niketan H.S. School, 41 Jyotinagar, Kolkata 700 108 (India)

2011-03-15T23:59:59.000Z

Note: This page contains sample records for the topic "magnetotellurics z-axis tipper" 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

Application of Goubau Surface Wave Transmission Line for Improved Bench Testing of Diagnostic Beamline Elements  

SciTech Connect

In-air test fixtures for beamline elements typically utilize an X-Y positioning stage, and a wire antenna excited by an RF source. In most cases, the antenna contains a standing wave, and is useful only for coarse alignment measurements in CW mode. A surface-wave (SW) based transmission line permits RF energy to be launched on the wire, travel through the beamline component, and then be absorbed in a load. Since SW transmission lines employ travelling waves, the RF energy can be made to resemble the electron beam, limited only by ohmic losses and dispersion. Although lossy coaxial systems are also a consideration, the diameter of the coax introduces large uncertainties in centroid location. A SW wire is easily constructed out of 200 micron magnet wire, which more accurately approximates the physical profile of the electron beam. Benefits of this test fixture include accurate field mapping, absolute calibration for given beam currents, Z-axis independence, and temporal response measurements of sub-nanosecond pulse structures. Descriptions of the surface wave launching technique, transmission line, and instrumentation are presented, along with measurement data.

John Musson, Keith Cole, Sheldon Rubin

2009-05-01T23:59:59.000Z

242

Generalized Jacobi elliptic n-monopole type A  

Science Journals Connector (OSTI)

Recently a new type of classical generalized Jacobi elliptic one monopole solutions of the SU(2) Yang-Mills-Higgs theory are constructed with the Higgs field in the adjoint representation. In this paper we will extend the numerical work done on Jacobi elliptic monopoles by solving the Yang-Mills-Higgs equations with higher ?-winding number n=1 2 3 4 5 when the Higgs potential is non-vanishing (?=0.5 1). We calculated that all these solutions possess the same total energy as the generalized t Hooft-Polyakov monopole. We noticed that when the parameter q of the generalized Jacobi elliptic functions is a half integer the Jacobi elliptic monopoles are distorted and the center of mass are shifted away from origin. Due to the distortion the monopoles exhibit magnetic dipole moment. When the ?-winding number n=1 the Higgs modulus possess a point zero however as n increases the number of zeroes of the Higgs modulus increases in the direction perpendicular to the z-axis.

2013-01-01T23:59:59.000Z

243

Decomposition of Diagonal Hermitian Quantum Gates Using Multiple-Controlled Pauli Z Gates  

E-Print Network (OSTI)

Quantum logic decomposition refers to decomposing a given quantum gate to a set of physically implementable gates. An approach has been presented to decompose arbitrary diagonal quantum gates to a set of multiplexed-rotation gates around z axis. In this paper, a special class of diagonal quantum gates, namely diagonal Hermitian quantum gates, is considered and a new perspective to the decomposition problem with respect to decomposing these gates is presented. It is first shown that these gates can be decomposed to a set that solely consists of multiple-controlled Z gates. Then a binary representation for the diagonal Hermitian gates is introduced. It is shown that the binary representations of multiple-controlled Z gates form a basis for the vector space that is produced by the binary representations of all diagonal Hermitian quantum gates. Moreover, the problem of decomposing a given diagonal Hermitian gate is mapped to the problem of writing its binary representation in the specific basis mentioned above. Moreover, CZ gate is suggested to be the two-qubit gate in the decomposition library, instead of previously used CNOT gate. Experimental results show that the proposed approach can lead to circuits with lower costs in comparison with the previous ones.

Mahboobeh Houshmand; Morteza Saheb Zamani; Mehdi Sedighi; Mona Arabzadeh

2014-05-26T23:59:59.000Z

244

Hybrid Quantum Computation  

E-Print Network (OSTI)

We present a hybrid model of the unitary-evolution-based quantum computation model and the measurement-based quantum computation model. In the hybrid model part of a quantum circuit is simulated by unitary evolution and the rest by measurements on star graph states, thereby combining the advantages of the two standard quantum computation models. In the hybrid model, a complicated unitary gate under simulation is decomposed in terms of a sequence of single-qubit operations, the controlled-Z gates, and multi-qubit rotations around the z-axis. Every single-qubit- and the controlled-Z gate are realized by a respective unitary evolution, and every multi-qubit rotation is executed by a single measurement on a required star graph state. The classical information processing in our model only needs an information flow vector and propagation matrices. We provide the implementation of multi-control gates in the hybrid model. They are very useful for implementing Grover's search algorithm, which is studied as an illustrating example.

Arun Sehrawat; Daniel Zemann; Berthold-Georg Englert

2010-08-06T23:59:59.000Z

245

MAP, MAC, and Vortex-rings Configurations in the Weinberg-Salam Model  

E-Print Network (OSTI)

We report on the presence of new axially symmetric monopoles, antimonopoles and vortex-rings solutions of the SU(2)$\\times$U(1) Weinberg-Salam model of electromagnetic and weak interactions. When the $\\phi$-winding number $n=1$, and 2, the configurations are monopole-antimonopole pair (MAP) and monopole-antimonopole chain (MAC) with poles of alternating sign magnetic charge arranged along the $z$-axis. Vortex-rings start to appear from the MAP and MAC configurations when the winding number $n=3$. The MAP configurations possess zero net magnetic charge whereas the MAC configurations possess net magnetic charge of $4\\pi n/e$. In the MAP configurations, the monopole-antimonopole pair is bounded by the ${\\cal Z}^0$ field flux string and there is an electromagnetic current loop encircling it. The monopole and antimonopole possess magnetic charges $\\pm\\frac{2\\pi n}{e}$ respectively. In the MAC configurations there is no string connecting the monopole and the adjacent antimonopole and they possess magnetic charges $\\pm\\frac{4\\pi n}{e}$ respectively. The MAC configurations possess infinite total energy and zero magnetic dipole moment whereas the MAP configurations which are actually sphalerons possess finite total energy and magnetic dipole moment. The configurations were investigated for varying value of Higgs boson mass $0\\leq M_H^2\\leq 80$ at Weinberg angle $\\theta_W=\\frac{\\pi}{4}$.

Rosy Teh; Ban-Loong Ng; Khai-Ming Wong

2014-08-20T23:59:59.000Z

246

Complex instruction set computing architecture for performing accurate quantum $Z$ rotations with less magic  

E-Print Network (OSTI)

We present quantum protocols for executing arbitrarily accurate $\\pi/2^k$ rotations of a qubit about its $Z$ axis. Reduced instruction set computing (\\textsc{risc}) architectures typically restrict the instruction set to stabilizer operations and a single non-stabilizer operation, such as preparation of a "magic" state from which $T = Z(\\pi/4)$ gates can be teleported. Although the overhead required to distill high-fidelity copies of this magic state is high, the subsequent quantum compiling overhead to realize $Z$ rotations in a \\textsc{risc} architecture can be much greater. We develop a complex instruction set computing (\\textsc{cisc}) architecture whose instruction set includes stabilizer operations and preparation of magic states from which $Z(\\pi/2^k)$ gates can be teleported, for $2 \\leq k \\leq k_{\\text{max}}$. This results in a substantial overall reduction in the number of gates required to achieve a desired gate accuracy for $Z$ rotations. The key to our construction is a family of shortened quantum Reed-Muller codes of length $2^{k+2}-1$, whose magic-state distillation threshold shrinks with $k$ but is greater than 0.85% for $k \\leq 6$.

Andrew J. Landahl; Chris Cesare

2013-10-15T23:59:59.000Z

247

2D-network of inorganic-organic hybrid material built on Keggin type polyoxometallate and amino acid: [L-C{sub 2}H{sub 6}NO{sub 2}]{sub 3}[(PO{sub 4})Mo{sub 12}O{sub 36}].5H{sub 2}O  

SciTech Connect

A new inorganic-organic hybrid material based on polyoxometallate, [L-C{sub 2}H{sub 6}NO{sub 2}]{sub 3}[(PO{sub 4})Mo{sub 12}O{sub 36}].5H{sub 2}O, has been successfully synthesized and characterized by single-crystal X-ray analysis, elemental analysis, infrared and ultraviolet spectroscopy, proton nuclear magnetic resonance and differential thermal analysis techniques. The title compound crystallizes in the monoclinic space group, P2{sub 1}/c{sub ,} with a = 12.4938 (8) A, b = 19.9326 (12) A, c = 17.9270 (11) A, {beta} = 102.129 (1){sup o}, V = 4364.8 (5) A{sup 3}, Z = 4 and R{sub 1}(wR{sub 2}) = 0.0513, 0.0877. The most remarkable structural feature of this hybrid can be described as two-dimensional inorganic infinite plane-like (2D/{infinity} [(PO{sub 4})Mo{sub 12}O{sub 36}]{sup 3-}) which forming via weak Van der Waals interactions along the z axis. The characteristic band of the Keggin anion [(PO{sub 4})Mo{sub 12}O{sub 36}]{sup 3-} appears at 210 nm in the UV spectrum. Thermal analysis indicates that the Keggin anion skeleton begins to decompose at 520 deg. C.

Alizadeh, M.H. [Department of Chemistry, School of Sciences, Ferdowsi University, Mashhad 91779-1436 (Iran, Islamic Republic of)], E-mail: mhalizadehg@yahoo.com; Mirzaei, M. [Department of Chemistry, School of Sciences, Ferdowsi University, Mashhad 91779-1436 (Iran, Islamic Republic of); Razavi, H. [Department of Chemistry, Georgetown University, Washington, DC 20057 (United States)

2008-03-04T23:59:59.000Z

248

Architecture and operation of the Z Pulsed Power Facility vacuum system.  

SciTech Connect

The Z Pulsed Power Facility at Sandia National Laboratories in Albuquerque, New Mexico, USA is one of the world's premier high energy density physics facilities. The Z Facility derives its name from the z-pinch phenomena which is a type of plasma confinement system that uses the electrical current in the plasma to generate a magnetic field that compresses it. Z refers to the direction of current flow, the z axis in a three dimensional Cartesian coordinate system. The multiterawatt, multimegajoule electrical pulse the Facility produces is 100-400 nanoseconds in time. Research and development programs currently being conducted on the Z Facility include inertial confinement fusion, dynamic material properties, laboratory astrophysics and radiation effects. The Z Facility vacuum system consists of two subsystems, center section and load diagnostics. Dry roughing pumps and cryogenic high vacuum pumps are used to evacuate the 40,000 liter, 200 square meter center section of the facility where the experimental load is located. Pumping times on the order of two hours are required to reduce the pressure from atmospheric to 10{sup -5} Torr. The center section is cycled from atmosphere to high vacuum for each experiment. The facility is capable of conducting one to two experiments per day. Numerous smaller vacuum pumping systems are used to evacuate load diagnostics. The megajoules of energy released during an experiment causes damage to the Facility that presents numerous challenges for reliable operation of the vacuum system.

Riddle, Allen Chauncey; Petmecky, Don; Weed, John Woodruff

2010-11-01T23:59:59.000Z

249

Displacement current phenomena in the magnetically insulated transmission lines of the refurbished Z accelerator  

Science Journals Connector (OSTI)

Experimental data is presented that illustrates important displacement current phenomena in the magnetically insulated transmission lines (MITLs) of the refurbished Z accelerator [D.?V. Rose et al., Phys. Rev. ST Accel. Beams 13, 010402 (2010)]. Specifically, we show how displacement current in the MITLs causes significant differences between the accelerator current measured at the vacuum-insulator stack (at a radial position of about 1.6m from the Z axis of symmetry) and the accelerator current measured at the load (at a radial position of about 6cm from the Z axis of symmetry). The importance of accounting for these differences was first emphasized by Jennings etal. [C.?A. Jennings et al., IEEE Trans. Plasma Sci. 38, 529 (2010)], who calculated them using a full transmission-line-equivalent model of the four-level MITL system. However, in the data presented by Jennings etal., many of the interesting displacement current phenomena were obscured by parasitic current losses that occurred between the vacuum-insulator stack and the load (e.g., electron flow across the anode-cathode gap). By contrast, the data presented herein contain very little parasitic current loss, and thus for these low-loss experiments we are able to demonstrate that the differences between the current measured at the stack and the current measured at the load are due primarily to the displacement current that results from the shunt capacitance of the MITLs (about 8.41nF total). Demonstrating this is important because displacement current is an energy storage mechanism, where energy is stored in the MITL electric fields and can later be used by the system. Thus, even for higher-loss experiments, the differences between the current measured at the stack and the current measured at the load are often largely due to energy storage and subsequent release, as opposed to being due solely to some combination of measurement error and current loss in the MITLs and/or double post-hole convolute. Displacement current also explains why the current measured downstream of the MITLs (i.e., the load current) often exceeds the current measured upstream of the MITLs (i.e., the stack current) at various times in the power pulse (this particular phenomenon was initially thought to be due to timing and/or calibration errors). To facilitate a better understanding of these phenomena, we also introduce and analyze a simple LC circuit model of the MITLs. This model is easily implemented as a simple drive circuit in simulation codes, which has now been done for the LASNEX code [G.?B. Zimmerman and W.?L. Kruer, Comments Plasma Phys. Controlled Fusion 2, 51 (1975)] at Sandia, as well as for simpler MATLAB-based codes at Sandia. An example of this LC model used as a drive circuit will also be presented.

R. D. McBride; C. A. Jennings; R. A. Vesey; G. A. Rochau; M. E. Savage; W. A. Stygar; M. E. Cuneo; D. B. Sinars; M. Jones; K. R. LeChien; M. R. Lopez; J. K. Moore; K. W. Struve; T. C. Wagoner; E. M. Waisman

2010-12-27T23:59:59.000Z

250

Silver Peak Innovative Exploration Project Geothermal Project | Open Energy  

Open Energy Info (EERE)

Innovative Exploration Project Geothermal Project Innovative Exploration Project Geothermal Project Jump to: navigation, search Last modified on July 22, 2011. Project Title Silver Peak Innovative Exploration Project Project Type / Topic 1 Recovery Act: Geothermal Technologies Program Project Type / Topic 2 Validation of Innovative Exploration Technologies Project Description The scope of this three phase project includes tasks to validate a variety of innovative exploration and drilling technologies which aim to accurately characterize the geothermal site and thereby reduce project risk. Phase 1 exploration will consist of two parts: 1) surface and near surface investigations and 2) subsurface geophysical surveys and modeling. The first part of Phase 1 includes: a hyperspectral imaging survey (to map thermal anomalies and geothermal indicator minerals), shallow temperature probe measurements, and drilling of temperature gradient wells to depths of 1000 feet. In the second part of Phase 1, 2D & 3D geophysical modeling and inversion of gravity, magnetic, and magnetotelluric datasets will be used to image the subsurface. This effort will result in the creation of a 3D model composed of structural, geological, and resistivity components. The 3D model will then be combined with the temperature data to create an integrated model that will be used to prioritize drill target locations.

251

Property:Link | Open Energy Information  

Open Energy Info (EERE)

Link Link Jump to: navigation, search This is a property of type URL. Pages using the property "Link" Showing 25 pages using this property. (previous 25) (next 25) 1 10 CFR § 1021 + http://en.openei.org/wiki/File:10CFRPart1021.pdf + 2 2-D Magnetotellurics At The Geothermal Site At Soultz-Sous-Forets- Resistivity Distribution To About 3000 M Depth + http://www.sciencedirect.com/science/article/pii/S1631071310001070 + 2.8-Ma Ash-Flow Caldera At Chegem River In The Northern Caucasus Mountains (Russia), Contemporaneous Granites, And Associated Ore Deposits + http://www.sciencedirect.com/science/article/B6VCS-48B5BV5-KK/2/a841cce0d247b754e5163bb62f72dc05 + 2007 Annual Report + https://www.enel.com/en-GB/investors/financial_reports/annual/ + 238U Decay Series Systematics Of Young Lavas From Batur Volcano, Sunda Arc + http://www.sciencedirect.com/science/article/B6VCS-48B0DW7-F/2/8e2bc55d34022c3d13f71c2dd57cd45b +

252

A field test of electromagnetic geophysical techniques for locating simulated in situ mining leach solution  

SciTech Connect

The US Bureau of Mines, The University of Arizona, Sandia National Laboratories, and Zonge Engineering and Research Organization, Inc., conducted cooperative field tests of six electromagnetic (EM) geophysical methods to compare their effectiveness in locating a brine solution simulating in situ leach solution or a high-conductivity plume of contamination. The brine was approximately 160 m below the surface. The testsite was the University's San Xavier experimental mine near Tucson, AZ. Geophysical surveys using surface and surface-borehole, time-domain electromagnetic (TEM) induction; surface controlled-source audiofrequency magnetotellurics (CSAMT); surface-borehole, frequency-domain electromagnetic (FEM) induction; crosshole FEM; and surface magnetic field ellipticity were conducted before and during brine injection. The surface TEM data showed a broad decrease in resistivity. CSAMT measurements with the conventional orientation did not detect the brine, but measurements with another orientation indicated some decrease in resistivity. The surface-borehole and crosshole methods located a known fracture and other fracture zones inferred from borehole induction logs. Surface magnetic field ellipticity data showed a broad decrease in resistivity at depth following brine injection.

Tweeton, D.R.; Hanson, J.C.; Friedel, M.J.; Sternberg, B.K.; Dahl, L.J.

1994-01-01T23:59:59.000Z

253

Major results of geophysical investigations at Yucca Mountain and vicinity, southern Nevada  

SciTech Connect

In the consideration of Yucca Mountain as a possible site for storing high level nuclear waste, a number of geologic concerns have been suggested for study by the National Academy of Sciences which include: (1) natural geologic and geochemical barriers, (2) possible future fluctuations in the water table that might flood a mined underground repository, (3) tectonic stability, and (4) considerations of shaking such as might be caused by nearby earthquakes or possible volcanic eruptions. This volume represents the third part of an overall plan of geophysical investigation of Yucca Mountain, preceded by the Site Characterization Plan (SCP; dated 1988) and the report referred to as the Geophysical White Paper, Phase 1, entitled Status of Data, Major Results, and Plans for Geophysical Activities, Yucca Mountain Project (Oliver and others, 1990). The SCP necessarily contained uncertainty about applicability and accuracy of methods then untried in the Yucca Mountain volcano-tectonic setting, and the White Paper, Phase 1, focused on summarization of survey coverage, data quality, and applicability of results. For the most part, it did not present data or interpretation. The important distinction of the current volume lies in presentation of data, results, and interpretations of selected geophysical methods used in characterization activities at Yucca Mountain. Chapters are included on the following: gravity investigations; magnetic investigations; regional magnetotelluric investigations; seismic refraction investigations; seismic reflection investigations; teleseismic investigations; regional thermal setting; stress measurements; and integration of methods and conclusions. 8 refs., 60 figs., 2 tabs.

Oliver, H.W.; Ponce, D.A. [eds.] [Geological Survey, Menlo Park, CA (United States); Hunter, W.C. [ed.] [Geological Survey, Denver, CO (United States). Yucca Mountain Project Branch

1995-12-31T23:59:59.000Z

254

In-situ combustion project at Bartlett, Kansas. Final report  

SciTech Connect

As part of an ongoing research program for enhanced oil recovery, the Bartlesville Energy Technology Center, US Department of Energy, is in the process of developing petroleum-recovery techcniques for shallow, low-productivity, heavy-oil deposits in southeastern Kansas, southwestern Missouri and northeastern Oklahoma. Personnel at BETC designed and conducted an in-situ combustion experiment on the Link Lease in Labette County, near Bartlett, Kansas. The Nelson-McNeil calculation method was used to calculate oil recovery and predict production time for a 1.25 acre inverted five-spot. Two attempts to ignite the formation are described. The well completion methods, hydraulic fracturing, injection of air, workovers, production techniques, and well-monitoring methods of the process are described. Production results are shown for both combustion attempts. The progression of the burn and the final extent of the burn front were evaluated by the following methods: (1) controlled source audio-frequency magnetotelluric technique (CSAMT), (2) thermogravimetric analysis (TGA), (3) burn-front model, (4)geophysical log analysis, and (5) computer model study. 26 figures, 8 tables.

Miller, J.S.; Spence, K.L.

1983-04-01T23:59:59.000Z

255

Measurements for the BETC in-situ combustion experiment. [Post test surveys  

SciTech Connect

The Bartlesville Energy Technology Center (BETC) in situ combustion pilot project near Bartlette, Kansas, was studied using controlled source audio-magnetotelluric (CSAMT) mapping, thermal gravimetric analysis (TGA), conventional geophysical logging and modeling of the fireflood. Measurements of formation resistivity changes induced by in situ combustion indicate that CSAMT resistivity maps should show an increase in apparent resistivity. The substantial decrease of apparent resistivity measured within the five spot pattern indicated a complex sequence of events. Using the results from the CSAMT surveys the fire front was located and posttest core samples were obtained. The posttest core samples were examined using TGA techniques, and using information from combustion tube runs as standards, the location of the fire front in the core samples from the posttest holes was inferred. Models of the reservoir in situ combustion process were developed to help analyze the field results. The combustion kinematics, when used in conjunction with CSAMT and TGA techniques, indicated that considerable bypass of injected air occurred with an influx of brine into previously burned zones. This experiment offered an opportunity to integrate several new techniques into a systematic study of a difficult problem.

Wayland, J.R.; Bartel, L.C.

1982-11-01T23:59:59.000Z

256

Geothermal potential on Kirtland Air Force Base lands, Bernalillo County, New Mexico  

SciTech Connect

Extensive sampling and geochemical analysis of groundwater in and near the base disclosed no significant geothermal parameters. However, structural conditions and current hydrologic regimes strongly suggest that thermal waters would be masked by near surface, low temperature meteoric water originating as rain and snowfall in the nearby mountains. Controlled source audio-magnetotelluric (CSAMT) electromagnetic techniques, refraction seismic experiments, and gravity traverses were utilized on the base. These, together with published geohysical information that presents evidence for a shallow magma body beneath the Albuquerque Basin; favorable terrestrial heat flow, water chemistry, and shallow temperature gradient holes on the nearby mesa west of the Rio Grande; interpretation of regional gravity data; and geological data from nearby deep wells tend to confirm structural, stratigraphic, and hydrologic conditions favorable for developing an extensive intermediate to high-temperature hydrothermal regime on portions of Kirtland AFB lands where intensive land use occurs. Two possible exploration and development scenarios are presented. One involves drilling a well to a depth of 3000 to 5000 ft (914 to 1524 m) to test the possibility of encountering higher than normal water temperatures on the basinward side of the faults underlying the travertine deposits. The other is to conduct limited reflection seismograph surveys in defined areas on the base to determine the depth to basement (granite) and thickness of the overyling, unconfined, water filled, relatively unconsolidated sand and gravel aquifer.

Grant, P.R. Jr.

1981-10-01T23:59:59.000Z

257

Controlled-source electromagnetic survey at Soda Lakes geothermal area, Nevada  

SciTech Connect

The EM-60 system, a large-moment frequency-domain electromagnetic loop prospecting system, was operated in the Soda Lakes geothermal area, Nevada. Thirteen stations were occupied at distances ranging from 0.5-3.0 km from two transmitter sites. These yielded four sounding curves--the normalized amplitudes and phases of the vertical and radial magnetic fields as a function of frequency--at each station. In addition, two polarization ellipse parameters, ellipticity and tilt angle, were calculated at each frequency. The data were interpreted by means of a least-squares inversion procedure which fits a layered resistivity model to the data. A three-layer structure is indicated, with a near-surface 20 ohm-m layer of 100-400 m thickness, a middle 2 ohm-m layer of approximately 1 km thickness, and a basement of greater than 10 ohm-m. The models indicate a northwesterly structural strike; the top and middle layers seem to thicken from northeast to southwest. The results agree quite well with previous results of dipole-dipole and magnetotelluric (MT) surveys. The EM-60 survey provided greater depth penetration (1 to 1.5 km) than dipole-dipole, but MT far surpassed both in its depth of exploration. One advantage of EM in this area is its ease and speed of operation. Another advantage, its relative insensitivity to lateral inhomogeneities, is not as pronounced here as it would be in areas of more complex geology.

Stark, M.; Wilt, M.; Haught, J.R.; Goldstein, N.

1980-07-01T23:59:59.000Z

258

Geothermal energy resource investigations in the Eastern Copper River Basin, Alaska  

SciTech Connect

This report consists of a review of the geological, geochemical and geophysical data available for the Eastern Copper River basin with emphasis on the mud volcanoes, and the results of geophysical and geochemical studies carried out in the summers of 1982 and 1984. The purpose was to determine if there are geothermal energy resources in the Copper River Basin. The Eastern Copper River basin is situated on the flanks of a major volcano, Mt. Drum, which was active as late as 200,000 years ago and which is thought to have retained significant amounts of residual heat at high levels. Mt. Wrangell, farther to the east, has been volcanically active up to the present time. The 1982 geophysical and geochemical surveys located three principal areas of possible geothermal interest, one near Tazlina and two near the Klawasi mud volcanoes. The intensive survey work of 1984 was concentrated on those areas. We have integrated the results of soil helium, soil mercury, gravity, aeromagnetic, electrical, self-potential, and controlled-source audio magnetotelluric (CSAMT) surveys to evaluate the geothermal potential of the areas studied. 36 figs.

Wescott, E.M.; Turner, D.L.

1985-06-01T23:59:59.000Z

259

Geothermal-resource assessment of the Steamboat-Routt Hot Springs area, Colorado. Resources Series 22  

SciTech Connect

An assessment of the Steamboat Springs region in northwest Colorado was initiated and carried out in 1980 and 1981. The goal of this program was to delineate the geological features controlling the occurrence of the thermal waters (temperatures in excess of 68/sup 0/F (20/sup 0/C)) in this area at Steamboat Springs and 8 miles (12.8 km) north at Routt Hot Springs. Thermal waters from Heart Spring, the only developed thermal water source in the study area, are used in the municipal swimming pool in Steamboat Springs. The assessment program was a fully integrated program consisting of: dipole-dipole, Audio-magnetotelluric, telluric, self potential and gravity geophysical surveys, soil mercury and soil helium geochemical surveys; shallow temperature measurements; and prepartion of geological maps. The investigation showed that all the thermal springs appear to be fault controlled. Based on the chemical composition of the thermal waters it appears that Heart Spring in Steamboat Springs is hydrologically related to the Routt Hot Springs. This relationship was further confirmed when it was reported that thermal waters were encountered during the construction of the new high school in Strawberry Park on the north side of Steamboat Springs. In addition, residents stated that Strawberry Park appears to be warmer than the surrounding country side. Geological mapping has determined that a major fault extends from the Routt Hot Springs area into Strawberry Park.

Pearl, R.H.; Zacharakis, T.G.; Ringrose, C.D.

1983-01-01T23:59:59.000Z

260

Fuel Pond Sludge - Lessons Learned from Initial De-sludging of Sellafield's Pile Fuel Storage Pond - 12066  

SciTech Connect

The Pile Fuel Storage Pond (PFSP) at Sellafield was built and commissioned between the late 1940's and early 1950's as a storage and cooling facility for irradiated fuel and isotopes from the two Windscale Pile reactors. The pond was linked via submerged water ducts to each reactor, where fuel and isotopes were discharged into skips for transfer along the duct to the pond. In the pond the fuel was cooled then de-canned underwater prior to export for reprocessing. The plant operated successfully until it was taken out of operation in 1962 when the First Magnox Fuel Storage Pond took over fuel storage and de-canning operations on the site. The pond was then used for storage of miscellaneous Intermediate Level Waste (ILW) and fuel from the UK's Nuclear Programme for which no defined disposal route was available. By the mid 1970's the import of waste ceased and the plant, with its inventory, was placed into a passive care and maintenance regime. By the mid 1990s, driven by the age of the facility and concern over the potential challenge to dispose of the various wastes and fuels being stored, the plant operator initiated a programme of work to remediate the facility. This programme is split into a number of key phases targeted at sustained reduction in the hazard associated with the pond, these include: - Pond Preparation: Before any remediation work could start the condition of the pond had to be transformed from a passive store to a plant capable of complex retrieval operations. This work included plant and equipment upgrades, removal of redundant structures and the provision of a effluent treatment plant for removing particulate and dissolved activity from the pond water. - Canned Fuel Retrieval: Removal of canned fuel, including oxide and carbide fuels, is the highest priority within the programme. Handling and export equipment required to remove the canned fuel from the pond has been provided and treatment routes developed utilising existing site facilities to allow the fuel to be reprocessed or conditioned for long term storage. - Sludge Retrieval: In excess of 300 m{sup 3} of sludge has accumulated in the pond over many years and is made up of debris arising from fuel and metallic corrosion, wind blown debris and bio-organic materials. The Sludge Retrieval Project has provided the equipment necessary to retrieve the sludge, including skip washer and tipper machines for clearing sludge from the pond skips, equipment for clearing sludge from the pond floor and bays, along with an 'in pond' corral for interim storage of retrieved sludge. Two further projects are providing new plant processing routes, which will initially store and eventually passivate the sludge. - Metal Fuel Retrieval: Metal Fuel from early Windscale Pile operations and various other sources is stored within the pond; the fuel varies considerably in both form and condition. A retrieval project is planned which will provide fuel handling, conditioning, sentencing and export equipment required to remove the metal fuel from the pond for export to on site facilities for interim storage and disposal. - Solid Waste Retrieval: A final retrieval project will provide methods for handling, retrieval, packaging and export of the remaining solid Intermediate Level Waste within the pond. This includes residual metal fuel pieces, fuel cladding (Magnox, aluminium and zircaloy), isotope cartridges, reactor furniture, and miscellaneous activated and contaminated items. Each of the waste streams requires conditioning to allow it to be and disposed of via one of the site treatment plants. - Pond Dewatering and Dismantling: Delivery of the above projects will allow operations to progressively remove the radiological inventory, thereby reducing the hazard/risk posed by the plant. This will then allow subsequent dewatering of the pond and dismantling of the structure. (authors)

Carlisle, Derek; Adamson, Kate [Sellafield Ltd, Sellafield, Cumbria (United Kingdom)

2012-07-01T23:59:59.000Z

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261

AFC-1 Fuel Rodlet Fission Power Deposition Validation in ATR  

SciTech Connect

One of the viable options of long-term geological disposal of the nuclear power reactors generated spent fuel is to extract plutonium, the minor actinides (MA) and potentially long-lived fission products from the spent fuel and transmute them into short-lived or stable radionuclides in an appropriate reactor for the reduction of the radiological toxicity of the nuclear waste stream. An important component of that technology will be a non-fertile / low-fertile actinide transmutation fuel form containing the plutonium, neptunium, americium (and possibly curium) isotopes to be transmuted. Such advanced fuel forms, especially ones enriched in the long-life minor actinide (LLMA) elements (i.e., Np, Am, Cm), have minimal irradiation performance data available from which to establish a transmutation fuel form design. Recognizing these needs, an Advanced Fuel Cycle test series-1 (AFC-1) irradiation test on a variety of candidate fuel forms is now being conducted in Advanced Test Reactor (ATR) at the Idaho National Laboratory (INL). The first advanced fuel experiment (AFC-1) has been finalized and the test assembly analyzed for insertion and irradiation in ATR. The ATR core consists of a serpentine and rotationally symmetric fuel assembly about the z-axis of the core center. The plan view of the ATR core configuration is shown in Fig. 5, in Ref. 1. A cadmium filter with a 0.178 cm (0.045") thickness and 121.5 cm (48") in length, is currently used in the actinide-fuel capsule design for the East Flux Trap (EFT) position in ATR, to depress the linear heat generation rate (LHGR) lower than the projects 330 W/cm limit for the experimental fuel rodlets. The LHGR is proportional to the fission power deposited in the fuel rodlets from the neutron fissions. The fraction of the fission power generated from the neutron fission reactions deposited in the fuel rodlet is an important parameter for test assembly thermal analysis, which will be validated in this summary.

G. S. Chang; M. A. Lillo; D. J. Utterbeck

2008-11-01T23:59:59.000Z

262

A new correction method serving to eliminate the parabola effect of flatbed scanners used in radiochromic film dosimetry  

SciTech Connect

Purpose: The purpose of this study is the correction of the lateral scanner artifact, i.e., the effect that, on a large homogeneously exposed EBT3 film, a flatbed scanner measures different optical densities at different positions along thex axis, the axis parallel to the elongated light source. At constant dose, the measured optical densitiy profiles along this axis have a parabolic shape with significant dose dependent curvature. Therefore, the effect is shortly called the parabola effect. The objective of the algorithm developed in this study is to correct for the parabola effect. Any optical density measured at given position x is transformed into the equivalent optical density c at the apex of the parabola and then converted into the corresponding dose via the calibration of c versus dose. Methods: For the present study EBT3 films and an Epson 10000XL scanner including transparency unit were used for the analysis of the parabola effect. The films were irradiated with 6 MV photons from an Elekta Synergy accelerator in a RW3 slab phantom. In order to quantify the effect, ten film pieces with doses graded from 0 to 20.9 Gy were sequentially scanned at eight positions along thex axis and at six positions along the z axis (the movement direction of the light source) both for the portrait and landscape film orientations. In order to test the effectiveness of the new correction algorithm, the dose profiles of an open square field and an IMRT plan were measured by EBT3 films and compared with ionization chamber and ionization chamber array measurement. Results: The parabola effect has been numerically studied over the whole measuring field of the Epson 10000XL scanner for doses up to 20.9 Gy and for both film orientations. The presented algorithm transforms any optical density at positionx into the equivalent optical density that would be measured at the same dose at the apex of the parabola. This correction method has been validated up to doses of 5.2 Gy all over the scanner bed with 2D dose distributions of an open square photon field and an IMRT distribution. Conclusions: The algorithm presented in this study quantifies and corrects the parabola effect of EBT3 films scanned in commonly used commercial flatbed scanners at doses up to 5.2 Gy. It is easy to implement, and no additional work steps are necessary in daily routine film dosimetry.

Poppinga, D., E-mail: daniela.poppinga@uni-oldenburg.de; Schoenfeld, A. A.; Poppe, B. [Medical Radiation Physics, Carl v. Ossietzky University, Oldenburg 26127, Germany and Department for Radiation Oncology, Pius Hospital, Oldenburg 26121 (Germany)] [Medical Radiation Physics, Carl v. Ossietzky University, Oldenburg 26127, Germany and Department for Radiation Oncology, Pius Hospital, Oldenburg 26121 (Germany); Doerner, K. J. [Radiotherapy Department, General Hospital, Celle 29223 (Germany)] [Radiotherapy Department, General Hospital, Celle 29223 (Germany); Blanck, O. [CyberKnife Center Northern Germany, Gstrow 18273, Germany and Department for Radiation Oncology, University Clinic Schleswig-Holstein, Lbeck 23562 (Germany)] [CyberKnife Center Northern Germany, Gstrow 18273, Germany and Department for Radiation Oncology, University Clinic Schleswig-Holstein, Lbeck 23562 (Germany); Harder, D. [Medical Physics and Biophysics, Georg-August-University, Gttingen 37073 (Germany)] [Medical Physics and Biophysics, Georg-August-University, Gttingen 37073 (Germany)

2014-02-15T23:59:59.000Z

263

Engineering scale demonstration of a prospective Cast Stone process  

SciTech Connect

This report documents an engineering-scale demonstration with non-radioactive simulants that was performed at SRNL using the Scaled Continuous Processing Facility (SCPF) to fill an 8.5 ft container with simulated Cast Stone grout. The Cast Stone formulation was chosen from the previous screening tests. Legacy salt solution from previous Hanford salt waste testing was adjusted to correspond to the average composition generated from the Hanford Tank Waste Operation Simulator (HTWOS). The dry blend materials, ordinary portland cement (OPC), Class F fly ash, and ground granulated blast furnace slag (GGBFS or BFS), were obtained from Lafarge North America in Pasco, WA. Over three days, the SCPF was used to fill a 1600 gallon container, staged outside the facility, with simulated Cast Stone grout. The container, staged outside the building approximately 60 ft from the SCPF, was instrumented with x-, y-, and z-axis thermocouples to monitor curing temperature. The container was also fitted with two formed core sampling vials. For the operation, the targeted grout production rate was 1.5 gpm. This required a salt solution flow rate of approximately 1 gpm and a premix feed rate of approximately 580 lb/h. During the final day of operation, the dry feed rate was increased to evaluate the ability of the system to handle increased throughput. Although non-steady state operational periods created free surface liquids, no bleed water was observed either before or after operations. The final surface slope at a fill height of 39.5 inches was 1-1.5 inches across the 8.5 foot diameter container, highest at the final fill point and lowest diametrically opposed to the fill point. During processing, grout was collected in cylindrical containers from both the mixer discharge and the discharge into the container. These samples were stored in a humid environment either in a closed box proximal to the container or inside the laboratory. Additional samples collected at these sampling points were analyzed for rheological properties and density. Both the rheological properties (plastic viscosity and yield strength) and density were consistent with previous and later SCPF runs.

Cozzi, A.; Fowley, M.; Hansen, E.; Fox, K.; Miller, D.; Williams, M.

2014-09-30T23:59:59.000Z

264

Alum Innovative Exploration Project Geothermal Project | Open Energy  

Open Energy Info (EERE)

Innovative Exploration Project Geothermal Project Innovative Exploration Project Geothermal Project Jump to: navigation, search Last modified on July 22, 2011. Project Title Alum Innovative Exploration Project Project Type / Topic 1 Recovery Act: Geothermal Technologies Program Project Type / Topic 2 Validation of Innovative Exploration Technologies Project Description Phase 1 exploration will consist of two parts: 1) surface and near surface investigations and 2) subsurface geophysical surveys and modeling. The first part of Phase 1 includes: a hyperspectral imaging survey (to map thermal anomalies and geothermal indicator minerals), shallow (6 ft) temperature probe measurements, and drilling of temperature gradient wells to depths of 1000 feet. In the second part of Phase 1, 2D & 3D geophysical modeling and inversion of gravity, magnetic, and magnetotelluric datasets will be used to image the subsurface. This effort will result in the creation of a 3D model composed of structural, geological, and resistivity components. The 3D model will then be combined with the temperature and seismic data to create an integrated model that will be used to prioritize drill target locations. Four geothermal wells will be drilled and geologically characterized in Phase 2. The project will use a coiled-tube rig to test this drilling technology at a geothermal field for the first time. Two slimwells and two production wells will be drilled with core collected and characterized in the target sections of each well. In Phase 3, extended flow tests will be conducted on the producible wells to confirm the geothermal resource followed by an overall assessment of the productivity of the Alum geothermal area. Finally, Phase 3 will evaluate the relative contribution of each exploration technique in reducing risk during the early stages of the geothermal project.

265

The Momotombo Geothermal Field, Nicaragua: Exploration and development case history study  

SciTech Connect

This case history discusses the exploration methods used at the Momotombo Geothermal Field in western Nicaragua, and evaluates their contributions to the development of the geothermal field models. Subsequent reservoir engineering has not been synthesized or evaluated. A geothermal exploration program was started in Nicaragua in 1966 to discover and delineate potential geothermal reservoirs in western Nicaragua. Exploration began at the Momotombo field in 1970 using geological, geochemical, and geophysical methods. A regional study of thermal manifestations was undertaken and the area on the southern flank of Volcan Momotombo was chosen for more detailed investigation. Subsequent exploration by various consultants produced a number of geotechnical reports on the geology, geophysics, and geochemistry of the field as well as describing production well drilling. Geological investigations at Momotombo included photogeology, field mapping, binocular microscope examination of cuttings, and drillhole correlations. Among the geophysical techniques used to investigate the field sub-structure were: Schlumberger and electromagnetic soundings, dipole mapping and audio-magnetotelluric surveys, gravity and magnetic measurements, frequency domain soundings, self-potential surveys, and subsurface temperature determinations. The geochemical program analyzed the thermal fluids of the surface and in the wells. This report presents the description and results of exploration methods used during the investigative stages of the Momotombo Geothermal Field. A conceptual model of the geothermal field was drawn from the information available at each exploration phase. The exploration methods have been evaluated with respect to their contributions to the understanding of the field and their utilization in planning further development. Our principal finding is that data developed at each stage were not sufficiently integrated to guide further work at the field, causing inefficient use of resources.

None

1982-07-01T23:59:59.000Z

266

Geologic research of conventional and unconventional hydrocarbon resources. Quarterly report, October 1, 1992--March 1, 1993  

SciTech Connect

This report covers the period from October 1, 1992 to March 1, 1993. The overall goals of the program task are to provide a final synthesis of six deep seismic reflection profiles and other geological and geophysical data from the southern Washington Cascades region where a probable extensive deep sedimentary basin has been discovered. This deep sedimentary basin is hypothesized from geological, regional magnetotelluric (MT), gravity, magnetic , and seismic reflection data as described in the American Association of Petroleum Geologists (AAPG) article by Stanley and others (1992). This report analyzed three seismic reflection profiles acquired by the Morgantown Energy Technology Centers in combination with the extensive MT and other data to outline a probable geological model for a thick conductive section of rocks in the southern Washington Cascades (called the Southern Washington Cascades conductor, SWCC). Earlier MT models suggested that the section consisted of an east-dipping package that extended to depths of as much as 20 km but appeared to surface in the Bear Canyon area near Morton, Washington and along the axis of the Carbon River and Morton anticlines. Interpretation of the first three DOE seismic reflection approximately confirmed the MT interpretation and added new information on anticlinal structures and detailed stratigraphy. In this quarterly report, we summarize the progress over the first two quarters of the program for FY93, and project the possible findings during the remainder of the project. A milestone chart for the first two quarters has been submitted separately, along with cost reports, but a copy of these items are attached for completeness.

Not Available

1993-03-02T23:59:59.000Z

267

Contribution of Geophysical Prospecting to Geohazard Evaluation  

SciTech Connect

The physical properties of the subsoil are studied using geophysical methods. These studies are always indirect, such as gravimetric, magnetometric, magnetotelluric or reflection-refraction seismic surveys and are often combined to obtain more accurate and reliable results. With these tools the oil industry commonly investigates the sedimentary basins to localize structures that may favor the accumulation of hydrocarbons. Above all, seismic prospecting allow the understanding of the underground geology, defining boundaries of the geological formations as well as mechanical and physical properties of the rocks. New cutting-edge techniques allow high quality data to be obtained in almost all geological contexts and make reflection seismic the most powerful tool in subsurface observations. The seismic method was utilized in geothermal resources investigation, research of water strategic resources, volcanic risks assessment, etc. The refraction method was the first to be used in the exploration of oil reservoirs. At present the industry employs mainly refraction seismics to study shallow formations. Conversely, university researchers have applied wide-angle reflection-refraction surveys to localize deep crustal interfaces analyzing the high amplitudes of the wide-angle reflections and the velocities obtained from the refracted signals. Moho discontinuity and velocity distribution within the crust were mapped out, indicating thickness and boundary conditions in different geological settings. The maps have been used in the analysis of geodynamical behavior and of active movements within the crust, useful for seismotectonic investigations. The further addition of the seismic reflection imaging, with deep penetration and long transects, completed multidisciplinary programs to unravel the structure of the crust with clear seismic images and models. High-resolution application of seismic has a central role in the identification and characterization of seismotectonic and seismogenetic zones and of the related capable faults. The earthquakes represent an important external risk for key constructions and nuclear power plants and capable faults cause near-surface displacements being considered to be the more critical for site safety. A close cooperation among geophysicists, geologists and seismologists is recommended in the hazards evaluation, alike in macrozoning for location of seismic sources and in microzoning for the measure of terrains mechanical properties and dynamic responses. Here I present and discuss the results of integrated multidisciplinary studies to unravel the peculiarity of the crustal structures and seismicity in Southern Tuscany, Italy.

Nicolich, Rinaldo [Department of Civil Engineering, University of Trieste, via Valerio 10, I-34127 Trieste (Italy)

2006-03-23T23:59:59.000Z

268

TECTONIC VERSUS VOLCANIC ORIGIN OF THE SUMMIT DEPRESSION AT MEDICINE LAKE VOLCANO, CALIFORNIA  

SciTech Connect

Medicine Lake Volcano is a Quaternary shield volcano located in a tectonically complex and active zone at the transition between the Basin and Range Province and the Cascade Range of the Pacific Province. The volcano is topped by a 7x12 km elliptical depression surrounded by a discontinuous constructional ring of basaltic to rhyolitic lava flows. This thesis explores the possibility that the depression may have formed due to regional extension (rift basin) or dextral shear (pull-apart basin) rather than through caldera collapse and examines the relationship between regional tectonics and localized volcanism. Existing data consisting of temperature and magnetotelluric surveys, alteration mineral studies, and core logging were compiled and supplemented with additional core logging, field observations, and fault striae studies in paleomagnetically oriented core samples. These results were then synthesized with regional fault data from existing maps and databases. Faulting patterns near the caldera, extension directions derived from fault striae P and T axes, and three-dimensional temperature and alteration mineral models are consistent with slip across arcuate ring faults related to magma chamber deflation during flank eruptions and/or a pyroclastic eruption at about 180 ka. These results are not consistent with a rift or pull-apart basin. Limited subsidence can be attributed to the relatively small volume of ash-flow tuff released by the only known major pyroclastic eruption and is inconsistent with the observed topographic relief. The additional relief can be explained by constructional volcanism. Striae from unoriented and oriented core, augmented by striae measurements in outcrop suggest that Walker Lane dextral shear, which can be reasonably projected from the southeast, has probably propagated into the Medicine Lake area. Most volcanic vents across Medicine Lake Volcano strike north-south, suggesting they are controlled by crustal weakness related to Basin and Range extension. Interaction of dextral shear, Basin and Range extension, and the zone of crustal weakness expressed as the Mount Shasta-Medicine Lake volcanic highland controlled the location and initiation of Medicine Lake Volcano at about 500 ka.

Mark Leon Gwynn

2010-05-01T23:59:59.000Z

269

Tectonic versus volcanic origin of the summit depression at Medicine Lake Volcano, California  

SciTech Connect

Medicine Lake Volcano is a Quaternary shield volcano located in a tectonically complex and active zone at the transition between the Basin and Range Province and the Cascade Range of the Pacific Province. The volcano is topped by a 7x12 km elliptical depression surrounded by a discontinuous constructional ring of basaltic to rhyolitic lava flows. This thesis explores the possibility that the depression may have formed due to regional extension (rift basin) or dextral shear (pull-apart basin) rather than through caldera collapse and examines the relationship between regional tectonics and localized volcanism. Existing data consisting of temperature and magnetotelluric surveys, alteration mineral studies, and core logging were compiled and supplemented with additional core logging, field observations, and fault striae studies in paleomagnetically oriented core samples. These results were then synthesized with regional fault data from existing maps and databases. Faulting patterns near the caldera, extension directions derived from fault striae P and T axes, and three-dimensional temperature and alteration mineral models are consistent with slip across arcuate ring faults related to magma chamber deflation during flank eruptions and/or a pyroclastic eruption at about 180 ka. These results are not consistent with a rift or pull-apart basin. Limited subsidence can be attributed to the relatively small volume of ash-flow tuff released by the only known major pyroclastic eruption and is inconsistent with the observed topographic relief. The additional relief can be explained by constructional volcanism. Striae from unoriented and oriented core, augmented by striae measurements in outcrop suggest that Walker Lane dextral shear, which can be reasonably projected from the southeast, has probably propagated into the Medicine Lake area. Most volcanic vents across Medicine Lake Volcano strike north-south, suggesting they are controlled by crustal weakness related to Basin and Range extension. Interaction of dextral shear, Basin and Range extension, and the zone of crustal weakness expressed as the Mount Shasta-Medicine Lake volcanic highland controlled the location and initiation of Medicine Lake Volcano at about 500 ka.

Mark Leon Gwynn

2010-05-01T23:59:59.000Z

270

Dixie Valley Engineered Geothermal System Exploration Methodology Project, Baseline Conceptual Model Report  

SciTech Connect

The Engineered Geothermal System (EGS) Exploration Methodology Project is developing an exploration approach for EGS through the integration of geoscientific data. The Project chose the Dixie Valley Geothermal System in Nevada as a field laboratory site for methodology calibration purposes because, in the public domain, it is a highly characterized geothermal system in the Basin and Range with a considerable amount of geoscience and most importantly, well data. The overall project area is 2500km2 with the Calibration Area (Dixie Valley Geothermal Wellfield) being about 170km2. The project was subdivided into five tasks (1) collect and assess the existing public domain geoscience data; (2) design and populate a GIS database; (3) develop a baseline (existing data) geothermal conceptual model, evaluate geostatistical relationships, and generate baseline, coupled EGS favorability/trust maps from +1km above sea level (asl) to -4km asl for the Calibration Area at 0.5km intervals to identify EGS drilling targets at a scale of 5km x 5km; (4) collect new geophysical and geochemical data, and (5) repeat Task 3 for the enhanced (baseline + new ) data. Favorability maps were based on the integrated assessment of the three critical EGS exploration parameters of interest: rock type, temperature and stress. A complimentary trust map was generated to compliment the favorability maps to graphically illustrate the cumulative confidence in the data used in the favorability mapping. The Final Scientific Report (FSR) is submitted in two parts with Part I describing the results of project Tasks 1 through 3 and Part II covering the results of project Tasks 4 through 5 plus answering nine questions posed in the proposal for the overall project. FSR Part I presents (1) an assessment of the readily available public domain data and some proprietary data provided by Terra-Gen Power, LLC, (2) a re-interpretation of these data as required, (3) an exploratory geostatistical data analysis, (4) the baseline geothermal conceptual model, and (5) the EGS favorability/trust mapping. The conceptual model presented applies to both the hydrothermal system and EGS in the Dixie Valley region. FSR Part II presents (1) 278 new gravity stations; (2) enhanced gravity-magnetic modeling; (3) 42 new ambient seismic noise survey stations; (4) an integration of the new seismic noise data with a regional seismic network; (5) a new methodology and approach to interpret this data; (5) a novel method to predict rock type and temperature based on the newly interpreted data; (6) 70 new magnetotelluric (MT) stations; (7) an integrated interpretation of the enhanced MT data set; (8) the results of a 308 station soil CO2 gas survey; (9) new conductive thermal modeling in the project area; (10) new convective modeling in the Calibration Area; (11) pseudo-convective modeling in the Calibration Area; (12) enhanced data implications and qualitative geoscience correlations at three scales (a) Regional, (b) Project, and (c) Calibration Area; (13) quantitative geostatistical exploratory data analysis; and (14) responses to nine questions posed in the proposal for this investigation. Enhanced favorability/trust maps were not generated because there was not a sufficient amount of new, fully-vetted (see below) rock type, temperature, and stress data. The enhanced seismic data did generate a new method to infer rock type and temperature. However, in the opinion of the Principal Investigator for this project, this new methodology needs to be tested and evaluated at other sites in the Basin and Range before it is used to generate the referenced maps. As in the baseline conceptual model, the enhanced findings can be applied to both the hydrothermal system and EGS in the Dixie Valley region.

Iovenitti, Joe

2014-01-02T23:59:59.000Z