version 00, 12 Sept. 2003
Data Download and Documentation Page
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This database contains fluid geochemical data from low to moderate temperature (up to 150°C) wells and thermal springs in the Great Basin. The Great Basin subset includes portions of the following states that fall within an expanded buffered boundary of the Great Basin: Arizona, California, Idaho, Nevada, Oregon, Utah, and Wyoming. In addition to geochemical analyses, the database contains information on hole depth (for wells), flow rate, references, and geothermometer and charge balance calculations.
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Acknowledgment of source data:
GEO-HEAT CENTER GEOCHEMICAL DATABASE
The original database was compiled by the Geo-Heat Center, Klamath Falls, OR. in February 2002 with the help of organizations in 16 western states that contributed data (click here for acknowledgments of source data for the Great Basin states). The full version of the Geo-Heat Center databases includes a database of direct use applications, a listing of geothermal resources lying near communities, and fluid geochemical data for many western states outside the Great Basin. Funding for this compilation was provided by United States Department of Energy grant DE-FG07-99ID13827 (Geo-Heat Center). The full database is available from the Geo-Heat center on CD at a modest price at:
Geo-Heat Center
Oregon Institute of Technology
3201 Campus Drive
Klamath Falls, OR 97601
(541) 885-1750
RECOMPILATION by GREAT BASIN CENTER FOR GEOTHERMAL ENERGY
The recompiled Great Basin database was created by merging portions of 21 files from the original Geo-Heat database into a single spreadsheet (3 files from each state in the buffered Great Basin boundary). Merging was accomplished using Microsoft Access and Excel. Geothermometer temperature estimates and a charge balance calculation have been added. Funding for this recompilation was provided by United States Department of Energy grant DE-FG07-99ID13827 (Geo-Heat Center) and DE-FG36-02ID14311 (Great Basin Center for Geothermal Energy).
The Great Basin database files:
This is a spreadsheet of well and thermal spring geochemical analyses, including coordinates and a key to references. Geochemical elements with reported values of “<x.xx” (with the “less than” symbol) have been left “as is” in this database. Abbreviated references contained in this spreadsheet correspond (in most cases) to complete references contained in the “GeoHeat Great Basin References.pdf” file.
This is a comma-delimited ASCII text file equivalent to “GeoHeat_GB.xls”.
This is an ArcView and ArcGIS-compatible shapefile of the database (Lambert projection). Missing geochemical data are represented by “-1”. Geochemical data with “less-than” (<) symbols have been converted to one-half the detection limit value, with the exception of arsenic data, for which all entrees with “less than” symbols have been converted to “-1” (no data).
This is a list of references for the Geo-Heat database, listed by state. Short references contained in the geochemical spreadsheet and shapefile can be used to look up the full reference in this file.
DESCRIPTIONS OF GREAT BASIN GEO-HEAT CENTER DATA FILES:
This is a spreadsheet of well and thermal spring geochemical analyses, including coordinates and references. Geochemical elements with reported values of “<x.xx” (with the “less than” symbol) have been left “as is” in this database. Abbreviated references contained in this spreadsheet correspond (in most cases) to complete references contained in the “GeoHeat Great Basin References.pdf” file.
Description of columns (fields) in the spreadsheet:
State: Two-letter abbreviation for state.
Site_ID: Site identification number or name. Represented as text, not a number, because some states have alphanumeric codes for this field.
SampleNo: Sample number. Available only for Arizona.
Date: Date. Format varies from state to state.
Name: Site name.
Type: Type of sample site: CLT = commercial low-temperature; INJ = injection well; M = mine; NLT = non-commercial low temperature; OIL = petroleum well; S = spring, SP = spring, SW = well drilled to control spring; TG = temperature gradient well; W = well; WW = well; X = type not confirmed.
Depth_m: Depth of well in meters. “-1” values indicate no data.
Flow_lpm: Flow rate in liters per minute. “-1” values indicate no data.
Latitude: Decimal degrees of latitude.
Longitude: Decimal degrees of longitude.
Reference: Abbreviated reference, which can be used to look up the full reference in the file “GeoHeat_GB_References_v0.pdf”.
Temp_C: Temperature in degrees centigrade.
TDS: Total dissolved solids, milligrams per liter.
Field_pH: pH measured in field.
Lab_pH: pH measured in laboratory.
Conduct: Conductivity measured in field, in units of microseimens.
Na: Sodium, milligrams per liter.
K: Potassium, milligrams per liter.
Ca: Calcium, milligrams per liter.
Mg: Magnesium, milligrams per liter.
Fe: Iron, milligrams per liter.
Sr: Strontium, milligrams per liter.
Li: Lithium, milligrams per liter.
B: Boron, milligrams per liter.
SiO2: Silica, milligrams per liter.
HCO3: Bicarbonate, milligrams per liter.
SO4: Sulfate, milligrams per liter.
Cl: Chloride, milligrams per liter.
F: Fluoride, milligrams per liter.
As: Arsenic, milligrams per liter.
Calc_TDS: Calculated total dissolved solids, milligrams per liter.
NO3: Nitrate, milligrams per liter.
T_Na_K_Ca: Estimated reservoir temperature in degrees centigrade based on the sodium-potassium-calcium geothermometer, with a magnesium correction when a magnesium analysis is available. Values of “-1” indicate that insufficient data were available to estimate a temperature. Caution should be used in interpreting geothermometer temperature estimates, which don’t always accurately estimate reservoir temperatures. Geothermometer calculations are the same as those employed and documented by Mariner et al., 1983 (Mariner, R.H., Presser, T.S., and Evans, W.C., 1983, Geochemistry of active geothermal systems in the northern Basin and Range province: Geothermal Resources Council Special Report No. 13, p. 95-119.
T_SiO2: Estimated reservoir temperature in degrees centigrade based on the silica geothermometer. Values of “-1” indicate that insufficient data were available to estimate a temperature. Caution should be used in interpreting geothermometer temperature estimates, which don’t always accurately estimate reservoir temperatures. Geothermometer calculations are the same as those employed and documented by Mariner et al., 1983 (Mariner, R.H., Presser, T.S., and Evans, W.C., 1983, Geochemistry of active geothermal systems in the northern Basin and Range province: Geothermal Resources Council Special Report No. 13, p. 95-119.
Ave_Gtemp: Average of the Na-K-Ca-Mg and the silica geothermometer temperature estimates, in degrees centigrade.
Chg_Bal: A charge balance based on the analyses listed in the spreadsheet. The formula used is: 100 * (cations – anions)/[(cations + anions)/2]. Values of “-999” indicate insufficient data to calculate a charge balance.
This is an ArcView and ArcGIS-compatible shapefile of the database. Missing geochemical data are represented by “-1”. Geochemical data with “less-than” (<) symbols have been converted to one-half the detection limit value, with the exception of arsenic data, for which all entrees with “less than” symbols have been converted to “-1” (no data).
Lambert, Central Meridian = -117,
Central Parallel = 0,
Standard Parallel 1 = 33,
Standard Parallel 2 = 45;
False Easting and False Northing = 0,
Datum = NAD27
Description of columns (fields) in the attribute table of the shape file:
State: Two-letter abbreviation for state.
Site_ID: Site identification number or name. Represented as text, not a number, because some states have alphanumeric codes for this field.
SampleNo: Sample number. Available only for Arizona.
Date: Date. Format varies from state to state.
Name: Site name.
Type: Type of sample site: CLT = commercial low-temperature; INJ = injection well; M = mine; NLT = non-commercial low temperature; OIL = petroleum well; S = spring, SP = spring, SW = well drilled to control spring; TG = temperature gradient well; W = well; WW = well; X = type not confirmed.
Depth_m: Depth of well in meters. “-1” values indicate no data.
Flow_lpm: Flow rate in liters per minute. “-1” values indicate no data.
Latitude: Decimal degrees of latitude.
Longitude: Decimal degrees of longitude.
Reference: Abbreviated reference, which can be used to look up the full reference in the file “GeoHeat_GB_References_v0.pdf”.
Temp_C: Temperature in degrees centigrade.
TDS: Total dissolved solids, milligrams per liter.
Field_pH: pH measured in field.
Lab_pH: pH measured in laboratory.
Conduct: Conductivity measured in field, in units of microseimens.
Na: Sodium, milligrams per liter.
K: Potassium, milligrams per liter.
Ca: Calcium, milligrams per liter.
Mg: Magnesium, milligrams per liter.
Fe: Iron, milligrams per liter.
Sr: Strontium, milligrams per liter.
Li: Lithium, milligrams per liter.
B: Boron, milligrams per liter.
SiO2: Silica, milligrams per liter.
HCO3: Bicarbonate, milligrams per liter.
SO4: Sulfate, milligrams per liter.
Cl: Chloride, milligrams per liter.
F: Fluoride, milligrams per liter.
As: Arsenic, milligrams per liter.
Calc_TDS: Calculated total dissolved solids, milligrams per liter.
NO3: Nitrate, milligrams per liter.
T_Na_K_Ca: Estimated reservoir temperature in degrees centigrade based on the sodium-potassium-calcium geothermometer, with a magnesium correction when a magnesium analysis is available. Values of “-1” indicate that insufficient data were available to estimate a temperature. Caution should be used in interpreting geothermometer temperature estimates, which don’t always accurately estimate reservoir temperatures. Geothermometer calculations are the same as those employed and documented by Mariner et al., 1983 (Mariner, R.H., Presser, T.S., and Evans, W.C., 1983, Geochemistry of active geothermal systems in the northern Basin and Range province: Geothermal Resources Council Special Report No. 13, p. 95-119.
T_SiO2: Estimated reservoir temperature in degrees centigrade based on the silica geothermometer. Values of “-1” indicate that insufficient data were available to estimate a temperature. Caution should be used in interpreting geothermometer temperature estimates, which don’t always accurately estimate reservoir temperatures. Geothermometer calculations are the same as those employed and documented by Mariner et al., 1983 (Mariner, R.H., Presser, T.S., and Evans, W.C., 1983, Geochemistry of active geothermal systems in the northern Basin and Range province: Geothermal Resources Council Special Report No. 13, p. 95-119.
Ave_Gtemp: Average of the Na-K-Ca-Mg and the silica geothermometer temperature estimates, in degrees centigrade.
Chg_Bal: A charge balance based on the analyses listed in the spreadsheet. The formula used is: 100 * (cations – anions)/[(cations + anions)/2]. Values of “-999” indicate insufficient data to calculate a charge balance.
The full database can be obtained from the Geo-Heat Center, Oregon Institute of Technology, 3201 Campus Drive, Klamath Falls, OR. 97601 tel: (541)885-1750; geoheat@oit.edu; http://geoheat.oit.edu.
Acknowledgments for individual state compilations are as follows:
Arizona: “Geothermal Resource Database - Arizona” by James C. Witcher from Southwest Technology Development Institute, Las Cruces, NM.
California: “California Low-Temperature Geothermal Resources Update - 1993" by Les Youngs, Department of Conservation, Division of Mines and Geology, Sacramento, CA.
Idaho: “Overview of Geothermal Investigations in Idaho, 1989 to 1993" by William J. Dansart, John D. Kauffman and Leland L. Mink, University of Idaho, Moscow, ID.
Nevada: “Nevada Low Temperature Geothermal Resource Assessment: 1994" by Larry J. Garside, Nevada Bureau of Mines and Geology, University of Nevada, Reno.
Oregon: “Open-File Report 0-94-9 Low-Temperature Geothermal Database for Oregon” by Gerald Black, Oregon Department of Geology and Mineral Industries, Portland, OR.
Utah: “Low-Temperature Geothermal Water in Utah: A Compilation of Data for Thermal Wells and Springs Through 1993" - Open File Report 311, Utah Geological Survey by Robert E. Blackett.
Wyoming: The well and spring information came from the original GEOTHERM database which was provided by Henry Heasler, University of Wyoming, Special Data and Visualization Center, Laramie, WY.
This data has been assembled together “as is” into a Great Basin data set. No
further editing for errors has been done beyond that already completed as part
of the original Geo-Heat database construction. Caution should be used in
interpreting geothermometer temperature estimates, which don’t always accurately
estimate reservoir temperatures.
Please contact us if you have questions, comments, or suggestions concerning the posting and availability of this database. Mark Coolbaugh: mfc@unr.nevada.edu; tel: (775) 784-1415.