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• 271. [Image] Geology, hydrothermal petrology, stable isotope geochemistry, and fluid inclusion geothermometry of LASL geothermal test well C/T-1 (Mesa 31-1), East Mesa, Imperial Valley, California, USA

  	Borehole Mesa 31-1 (LASL C/T-1) is an 1899-m (6231-ft) deep well located in the northwestern part of the East Mesa Geothermal Field. Mesa 31-1 is the first Calibration/Test Well (C/T-1) in the Los Alamos ...
  	Citation × Citation Citation Abstract Copy Title: Geology, hydrothermal petrology, stable isotope geochemistry, and fluid inclusion geothermometry of LASL geothermal test well C/T-1 (Mesa 31-1), East Mesa, Imperial Valley, California, USA Author: Miller, K.R Year: 1980 Borehole Mesa 31-1 (LASL C/T-1) is an 1899-m (6231-ft) deep well located in the northwestern part of the East Mesa Geothermal Field. Mesa 31-1 is the first Calibration/Test Well (C/T-1) in the Los Alamos Scientific Laboratory (LASL), Geothermal Log Interpretation Program. The purpose of this study is to provide a compilation of drillhole data, drill cuttings, well lithology, and formation petrology that will serve to support the use of well LASL C/T-1 as a calibration/test well for geothermal logging. In addition, reviews of fluid chemistry, stable isotope studies, isotopic and fluid inclusion geothermometry, and the temperature log data are presented. This study provides the basic data on the geology and hydrothermal alteration of the rocks in LASL C/T-1 as background for the interpretation of wireline logs.; LA-8515-MS Title: Geology, hydrothermal petrology, stable isotope geochemistry, and fluid inclusion geothermometry of LASL geothermal test well C/T-1 (Mesa 31-1), East Mesa, Imperial Valley, California, USA Author: Miller, K.R Year: 1980 Borehole Mesa 31-1 (LASL C/T-1) is an 1899-m (6231-ft) deep well located in the northwestern part of the East Mesa Geothermal Field. Mesa 31-1 is the first Calibration/Test Well (C/T-1) in the Los Alamos Scientific Laboratory (LASL), Geothermal Log Interpretation Program. The purpose of this study is to provide a compilation of drillhole data, drill cuttings, well lithology, and formation petrology that will serve to support the use of well LASL C/T-1 as a calibration/test well for geothermal logging. In addition, reviews of fluid chemistry, stable isotope studies, isotopic and fluid inclusion geothermometry, and the temperature log data are presented. This study provides the basic data on the geology and hydrothermal alteration of the rocks in LASL C/T-1 as background for the interpretation of wireline logs.; LA-8515-MS Close

• 272. [Image] Utilization of geothermal energy for methane production for J. A. Albertson Land and Cattle Company

  	To utilize the geothermal energy in the area of its 30,000-head cattle feedlot, J.A. Albertson Land and Cattle Co. is considering the development of an integrated geothermal/bioconversion system that would ...
  	Citation × Citation Citation Abstract Copy Title: Utilization of geothermal energy for methane production for J. A. Albertson Land and Cattle Company Author: Bissell, R.R. Year: 1980 To utilize the geothermal energy in the area of its 30,000-head cattle feedlot, J.A. Albertson Land and Cattle Co. is considering the development of an integrated geothermal/bioconversion system that would use the cattle manure as a feedstock for an anaerobic-digestion plant to produce methane plus a digester-residue cattle-feed supplement. The feedlot lies within a high-temperature gradient and heat-flow area associated with the Western Snake River basin in Malheur Co., Oregon. The three digesters designed for the process will operate mesophilically (at 98/sup 0/F) with a 20-day retention time. To make up the digesters' heat losses, the geothermal water source will need to be about 135/sup 0/F and have a flow rate of 120-240 gpm, depending on the size ultimately selected for the facility. If the digester residue replaces alfalfa hay in the cattle's current rations, its value will amount to $1.15 million/yr. Burning the methane in engine/generator sets would produce 985-1970 kW of electric power that could be either sold or used as a day-to-day substitute for the geothermal heat. An economic analysis of the system is presented; DOE/ET/27230-T2 Title: Utilization of geothermal energy for methane production for J. A. Albertson Land and Cattle Company Author: Bissell, R.R. Year: 1980 To utilize the geothermal energy in the area of its 30,000-head cattle feedlot, J.A. Albertson Land and Cattle Co. is considering the development of an integrated geothermal/bioconversion system that would use the cattle manure as a feedstock for an anaerobic-digestion plant to produce methane plus a digester-residue cattle-feed supplement. The feedlot lies within a high-temperature gradient and heat-flow area associated with the Western Snake River basin in Malheur Co., Oregon. The three digesters designed for the process will operate mesophilically (at 98/sup 0/F) with a 20-day retention time. To make up the digesters' heat losses, the geothermal water source will need to be about 135/sup 0/F and have a flow rate of 120-240 gpm, depending on the size ultimately selected for the facility. If the digester residue replaces alfalfa hay in the cattle's current rations, its value will amount to $1.15 million/yr. Burning the methane in engine/generator sets would produce 985-1970 kW of electric power that could be either sold or used as a day-to-day substitute for the geothermal heat. An economic analysis of the system is presented; DOE/ET/27230-T2 Close

• 273. [Image] Reservoir simulation studies: Wairakei Geothermal Field, New Zealand. Final report

  	Numerical reservoir simulation techniques were used to perform a history-match of the Wairakei geothermal system in New Zealand. First, a one-dimensional (vertical) model was chosen; realistic stratigraphy ...
  	Citation × Citation Citation Abstract Copy Title: Reservoir simulation studies: Wairakei Geothermal Field, New Zealand. Final report Author: Pritchett, J.W Year: 1980 Numerical reservoir simulation techniques were used to perform a history-match of the Wairakei geothermal system in New Zealand. First, a one-dimensional (vertical) model was chosen; realistic stratigraphy was incorporated and the known production history was imposed. The effects of surface and deep recharge were included. Good matches were obtained, both for the reservoir pressure decline history and changes in average discharge enthalpy with time. Next, multidimensional effects were incorporated by treating with a two-dimensional vertical section. Again, good history matches were obtained, although computed late-time discharge enthalpies were slightly high. It is believed that this disparity arises from inherently three-dimensional effects. Predictive calculations using the two-dimensional model suggest that continued future production will cause little additional reservoir pressure drop, but that thermal degradation will occur. Finally, ground subsidence data at Wairakei was examined. It was concluded that traditional elastic pore-collapse models based on classical soil-mechanics concepts are inadequate to explain the observed surface deformation. It is speculated that the measured subsidence may be due to structural effects such as aseismic slippage of a buried reservoir boundary fault.; LBL-11497; GREMP-11; SSS-R-80-4313 Title: Reservoir simulation studies: Wairakei Geothermal Field, New Zealand. Final report Author: Pritchett, J.W Year: 1980 Numerical reservoir simulation techniques were used to perform a history-match of the Wairakei geothermal system in New Zealand. First, a one-dimensional (vertical) model was chosen; realistic stratigraphy was incorporated and the known production history was imposed. The effects of surface and deep recharge were included. Good matches were obtained, both for the reservoir pressure decline history and changes in average discharge enthalpy with time. Next, multidimensional effects were incorporated by treating with a two-dimensional vertical section. Again, good history matches were obtained, although computed late-time discharge enthalpies were slightly high. It is believed that this disparity arises from inherently three-dimensional effects. Predictive calculations using the two-dimensional model suggest that continued future production will cause little additional reservoir pressure drop, but that thermal degradation will occur. Finally, ground subsidence data at Wairakei was examined. It was concluded that traditional elastic pore-collapse models based on classical soil-mechanics concepts are inadequate to explain the observed surface deformation. It is speculated that the measured subsidence may be due to structural effects such as aseismic slippage of a buried reservoir boundary fault.; LBL-11497; GREMP-11; SSS-R-80-4313 Close

• 274. [Image] Small-Scale Electric Systems Using Geothermal Energy: A Guide to Development

  	This comprehensive overview of small-scale [100 kilowatt - 10 megawatts (MW)] electric development using geothermal energy has been prepared primarily for financial investors as a guide to resource opportunities, ...
  	Citation × Citation Citation Abstract Copy Title: Small-Scale Electric Systems Using Geothermal Energy: A Guide to Development Author: McAuliffe, P. K. Year: 1983 This comprehensive overview of small-scale [100 kilowatt - 10 megawatts (MW)] electric development using geothermal energy has been prepared primarily for financial investors as a guide to resource opportunities, commercial technologies, and financial incentives. California's geothermal resource in the 180°F to 350°F temperature range has been estimated to contain enough energy to generate over 1,000 MW. To assist in economically developing these resources, the guide summarizes important siting considerations, including resource requirements. Discussed are the three technologies--flashed steam, Organic Rankine Cycle (ORC), and total flow--which can convert the available energy in geothermal resources into electricity. Of the three, small-scale ORC systems have the greatest potential for commercial development in the immediate future. The technology involved in ORC systems is well established and has been proven in industrial operations. The overall performance (efficiency) of geothermal ORC is a function of resource characteristics, plant design, working fluid selection, and numerous other considerations. The guide discusses overall performance in detail. Title: Small-Scale Electric Systems Using Geothermal Energy: A Guide to Development Author: McAuliffe, P. K. Year: 1983 This comprehensive overview of small-scale [100 kilowatt - 10 megawatts (MW)] electric development using geothermal energy has been prepared primarily for financial investors as a guide to resource opportunities, commercial technologies, and financial incentives. California's geothermal resource in the 180°F to 350°F temperature range has been estimated to contain enough energy to generate over 1,000 MW. To assist in economically developing these resources, the guide summarizes important siting considerations, including resource requirements. Discussed are the three technologies--flashed steam, Organic Rankine Cycle (ORC), and total flow--which can convert the available energy in geothermal resources into electricity. Of the three, small-scale ORC systems have the greatest potential for commercial development in the immediate future. The technology involved in ORC systems is well established and has been proven in industrial operations. The overall performance (efficiency) of geothermal ORC is a function of resource characteristics, plant design, working fluid selection, and numerous other considerations. The guide discusses overall performance in detail. Close

• 275. [Image] Geothermal Potential of the West Boise Area

  	With increased use being placed on natural gas, electricity, petroleum, and coal, alternative forms of energy have been sought to help release the pressures being placed on these resources. Geothermal ...
  	Citation × Citation Citation Abstract Copy Title: Geothermal Potential of the West Boise Area Author: Mink, L.L. Year: 1977 With increased use being placed on natural gas, electricity, petroleum, and coal, alternative forms of energy have been sought to help release the pressures being placed on these resources. Geothermal energy is one of the major alternative forms. In portions of Boise, geothermal resources have been utilized for many years for heating of homes and several state office buildings. Recent investigations in the Boise area have shown that hot water is abundant all along the Boise Foothills. This report discusses two areas showing good potential for future geothermal development. These areas are the Dry Creek Valley and the area between Pierce Gulch and Polecat Gulch. Both areas have water temperatures exceeding 37.8°C. In the Boise area it is found that zones of hot water are associated with some type of structural control. The hot water zones associated with the Dry Creek Valley and the Pierce-Polecat area were found to be located at or near the intersection of major linears mapped along the Boise Foothills. These linears reflect a zone of weakness at depth in the rock allowing warm water to migrate upward from the granitic rock of the Idaho batholith below. By mapping all known fault and linear patterns in the area, it is possible to correlate these zones of weakness with areas of hot water. At the intersection of two or more linears, where fracturing is greatest, the majority of geothermal water has been located Title: Geothermal Potential of the West Boise Area Author: Mink, L.L. Year: 1977 With increased use being placed on natural gas, electricity, petroleum, and coal, alternative forms of energy have been sought to help release the pressures being placed on these resources. Geothermal energy is one of the major alternative forms. In portions of Boise, geothermal resources have been utilized for many years for heating of homes and several state office buildings. Recent investigations in the Boise area have shown that hot water is abundant all along the Boise Foothills. This report discusses two areas showing good potential for future geothermal development. These areas are the Dry Creek Valley and the area between Pierce Gulch and Polecat Gulch. Both areas have water temperatures exceeding 37.8°C. In the Boise area it is found that zones of hot water are associated with some type of structural control. The hot water zones associated with the Dry Creek Valley and the Pierce-Polecat area were found to be located at or near the intersection of major linears mapped along the Boise Foothills. These linears reflect a zone of weakness at depth in the rock allowing warm water to migrate upward from the granitic rock of the Idaho batholith below. By mapping all known fault and linear patterns in the area, it is possible to correlate these zones of weakness with areas of hot water. At the intersection of two or more linears, where fracturing is greatest, the majority of geothermal water has been located Close

• 276. [Image] Geological and Geophysical Study of the Origin of the Warm Springs in Bath County, Virginia. Final Report, June 1, 1975--April 30, 1976

  	A study was made to determine the origin of the warm springs and to evaluate the geothermal resource potential of the area in the vicinity of the Warm Springs anticline in Bath and Alleghany Counties, ...
  	Citation × Citation Citation Abstract Copy Title: Geological and Geophysical Study of the Origin of the Warm Springs in Bath County, Virginia. Final Report, June 1, 1975--April 30, 1976 Author: Costain, J.K. Year: 1976 A study was made to determine the origin of the warm springs and to evaluate the geothermal resource potential of the area in the vicinity of the Warm Springs anticline in Bath and Alleghany Counties, Virginia. Phase 1 of the study was the compilation of a geologic map based on published maps and supported by reconnaissance geologic mapping in areas where published maps were not available. Phase II consisted of a regional bipole-dipole electric resistivity survey made in order to detect the presence of resistivity lows that might be associated with a geothermal system at depth. Phase III involved the drilling of a single hole to a depth of approximately 300 m to obtain a heat flow value that is representative of the area. The above data were used to arrive at a model that unambiguously explains the origin of thermal springs. It is concluded that the warm springs constitute a geothermal resource for low temperature application such as space heating (LBS) Title: Geological and Geophysical Study of the Origin of the Warm Springs in Bath County, Virginia. Final Report, June 1, 1975--April 30, 1976 Author: Costain, J.K. Year: 1976 A study was made to determine the origin of the warm springs and to evaluate the geothermal resource potential of the area in the vicinity of the Warm Springs anticline in Bath and Alleghany Counties, Virginia. Phase 1 of the study was the compilation of a geologic map based on published maps and supported by reconnaissance geologic mapping in areas where published maps were not available. Phase II consisted of a regional bipole-dipole electric resistivity survey made in order to detect the presence of resistivity lows that might be associated with a geothermal system at depth. Phase III involved the drilling of a single hole to a depth of approximately 300 m to obtain a heat flow value that is representative of the area. The above data were used to arrive at a model that unambiguously explains the origin of thermal springs. It is concluded that the warm springs constitute a geothermal resource for low temperature application such as space heating (LBS) Close

• 277. [Image] Planning, Drilling, Logging, and Testing of Energy Extraction Hole EE-1, Phases I and II

  	Energy Extraction Hole No. 1 (EE-1) is the second deep hole drilled into the Precambrian-age granitic rocks of the Jemez Mountains of north-central New Mexico. EE-1 was drilled to intersect a hydraulic ...
  	Citation × Citation Citation Abstract Copy Title: Planning, Drilling, Logging, and Testing of Energy Extraction Hole EE-1, Phases I and II Author: Pettitt, R.A. Year: 1977 Energy Extraction Hole No. 1 (EE-1) is the second deep hole drilled into the Precambrian-age granitic rocks of the Jemez Mountains of north-central New Mexico. EE-1 was drilled to intersect a hydraulic fracture extending outward from near the bottom of previously drilled hole GT-2, thus completing the underground circulation loop required for the hot dry rock geothermal energy extraction experiment. Directional drilling techniques were used to intersect the fracture zone. In addition, high-temperature instrumentation and equipment development, hydraulic fracturing experiments, pressure-flow testing of the fracture systems, and fracture mapping and borehole-ranging technique activities were conducted. The drilling, logging, and testing operations in EE-1 are described Title: Planning, Drilling, Logging, and Testing of Energy Extraction Hole EE-1, Phases I and II Author: Pettitt, R.A. Year: 1977 Energy Extraction Hole No. 1 (EE-1) is the second deep hole drilled into the Precambrian-age granitic rocks of the Jemez Mountains of north-central New Mexico. EE-1 was drilled to intersect a hydraulic fracture extending outward from near the bottom of previously drilled hole GT-2, thus completing the underground circulation loop required for the hot dry rock geothermal energy extraction experiment. Directional drilling techniques were used to intersect the fracture zone. In addition, high-temperature instrumentation and equipment development, hydraulic fracturing experiments, pressure-flow testing of the fracture systems, and fracture mapping and borehole-ranging technique activities were conducted. The drilling, logging, and testing operations in EE-1 are described Close

• 278. [Image] Feasibility of a Geothermal Heating System for Oakridge, Oregon

  	Geological and geophysical data indicate that Oakridge is underlain by geothermal waters. The strongest evidence is from the geothermal gradient, the increase of temperature with depth, in a 400' well ...
  	Citation × Citation Citation Abstract Copy Title: Feasibility of a Geothermal Heating System for Oakridge, Oregon Author: Bowen, R.C. Year: 1979 Geological and geophysical data indicate that Oakridge is underlain by geothermal waters. The strongest evidence is from the geothermal gradient, the increase of temperature with depth, in a 400' well on the south edge of the City. Although this well shows signs of disturbance by ground water, the geothermal gradient appears to be similar to the gradient from a well near McCredie Hot Springs seven miles to the east. Additional evidence is a salt spring, just south of the City, that may represent a fossil geothermal system that has become sealed and is no longer flowing hot water. A third line of direct evidence is the presence of a warm spring about three miles southeast of the City that is now covered by Hills Creek Reservoir. Indirect geophysical evidence is a high gravity gradient from west to east near Oakridge. This gradient relates closely to the region of increasing geothermal gradient and heat flow of the Cascade Geothermal Anomaly. Indications of intersection of regional fault patterns could provide the subsurface fracturing and permeability necessary for a geothermal reservoir. The results of this study indicate that water sufficiently hot to be useful can be located by drilling to depths of three to four thousand feet at Oakridge. Three sites are proposed for shallow geothermal gradient holes to test the proposed model. Title: Feasibility of a Geothermal Heating System for Oakridge, Oregon Author: Bowen, R.C. Year: 1979 Geological and geophysical data indicate that Oakridge is underlain by geothermal waters. The strongest evidence is from the geothermal gradient, the increase of temperature with depth, in a 400' well on the south edge of the City. Although this well shows signs of disturbance by ground water, the geothermal gradient appears to be similar to the gradient from a well near McCredie Hot Springs seven miles to the east. Additional evidence is a salt spring, just south of the City, that may represent a fossil geothermal system that has become sealed and is no longer flowing hot water. A third line of direct evidence is the presence of a warm spring about three miles southeast of the City that is now covered by Hills Creek Reservoir. Indirect geophysical evidence is a high gravity gradient from west to east near Oakridge. This gradient relates closely to the region of increasing geothermal gradient and heat flow of the Cascade Geothermal Anomaly. Indications of intersection of regional fault patterns could provide the subsurface fracturing and permeability necessary for a geothermal reservoir. The results of this study indicate that water sufficiently hot to be useful can be located by drilling to depths of three to four thousand feet at Oakridge. Three sites are proposed for shallow geothermal gradient holes to test the proposed model. Close

• 279. [Image] Downhole Heat Exchanger for Shallow Geothermal Systems: Performance, Economics and Applicability

  	Heat exchangers located within the wellbore of shallow geothermal resources are presently being used at several locations in the U.S. These heat exchangers are referred to as downhole heat exchangers. ...
  	Citation × Citation Citation Abstract Copy Title: Downhole Heat Exchanger for Shallow Geothermal Systems: Performance, Economics and Applicability Author: Reistad, G. M. Heat exchangers located within the wellbore of shallow geothermal resources are presently being used at several locations in the U.S. These heat exchangers are referred to as downhole heat exchangers. Such installations can have thermal energy output capacities as high as 1 MW for space heating with source water temperature of 90 to 100°C. This work reports on the performance and economics of downhole heat exchangers relative to the alternative geothermal system which pumps the fluid out of the ground and uses heat exchangers located at the earth's surface. Results indicate that the downhole heat exchange systems for capacity requirements less than about 500 to 100 kW are in general more desirable than the surface heat exchange systems for low capacity (less than about 500 to 1000 kW) requirements and shallow geothermal resources. For higher capacities the surface heat exchange systems become more economical. Furthermore, for large depths, the high capacities available from the surface systems are required in order to make the geothermal energy competitive with other sources Title: Downhole Heat Exchanger for Shallow Geothermal Systems: Performance, Economics and Applicability Author: Reistad, G. M. Heat exchangers located within the wellbore of shallow geothermal resources are presently being used at several locations in the U.S. These heat exchangers are referred to as downhole heat exchangers. Such installations can have thermal energy output capacities as high as 1 MW for space heating with source water temperature of 90 to 100°C. This work reports on the performance and economics of downhole heat exchangers relative to the alternative geothermal system which pumps the fluid out of the ground and uses heat exchangers located at the earth's surface. Results indicate that the downhole heat exchange systems for capacity requirements less than about 500 to 100 kW are in general more desirable than the surface heat exchange systems for low capacity (less than about 500 to 1000 kW) requirements and shallow geothermal resources. For higher capacities the surface heat exchange systems become more economical. Furthermore, for large depths, the high capacities available from the surface systems are required in order to make the geothermal energy competitive with other sources Close

• 280. [Image] Klamath Falls Geothermal Heating District

  	The City of Klamath Falls is proposing to construct a geothermal district heating project. Initially, the system will heat 14 government buildings (Phase I) in the downtown area, subsequently expanded ...
  	Citation × Citation Citation Abstract Copy Title: Klamath Falls Geothermal Heating District Author: Lund, J. W. Year: 1979 The City of Klamath Falls is proposing to construct a geothermal district heating project. Initially, the system will heat 14 government buildings (Phase I) in the downtown area, subsequently expanded to heat 11 blocks (Phase II), and then to heat the entire 54 block central business district (Phase III). Production wells will be drilled along the east boundary of the City, estimated to supply over 220°F water. A primary 8 inch diameter insulated steel pipeline placed in a concrete tunnel will supply geothermal fluid to a central heat exchange facility at the County Museum Building. Two plate heat exchangers will provide the necessary load for the initial 14 buildings. An injection well is located next to this facility. A closed loop secondary pipeline will supply heat to the 14 buildings at 200°F. This line will consist of buried insulated fiberglass reinforced pipe. The capital cost of the systems (Phase I) will be $1.4 million giving an equivalent annual capital, operation, and maintenance cost over a 20 year period of $150,000. Phase II cost of geothermal energy is estimated at $0.29 per therm, whereas the equivalent annual fossil fuel cost is estimated at $0.94 per therm Title: Klamath Falls Geothermal Heating District Author: Lund, J. W. Year: 1979 The City of Klamath Falls is proposing to construct a geothermal district heating project. Initially, the system will heat 14 government buildings (Phase I) in the downtown area, subsequently expanded to heat 11 blocks (Phase II), and then to heat the entire 54 block central business district (Phase III). Production wells will be drilled along the east boundary of the City, estimated to supply over 220°F water. A primary 8 inch diameter insulated steel pipeline placed in a concrete tunnel will supply geothermal fluid to a central heat exchange facility at the County Museum Building. Two plate heat exchangers will provide the necessary load for the initial 14 buildings. An injection well is located next to this facility. A closed loop secondary pipeline will supply heat to the 14 buildings at 200°F. This line will consist of buried insulated fiberglass reinforced pipe. The capital cost of the systems (Phase I) will be $1.4 million giving an equivalent annual capital, operation, and maintenance cost over a 20 year period of $150,000. Phase II cost of geothermal energy is estimated at $0.29 per therm, whereas the equivalent annual fossil fuel cost is estimated at $0.94 per therm Close