Stanford Geothermal Program Final Absorption Report

Adsorbed water on the rock surfaces in vapor-dominated geothermal fields has long been thought to provide a major source of fluid within the reservoir. Over the past several years, the Stanford Geothermal Program has conducted a series of investigations into the phenomena of water adsorption in geothermal systems, and their effects on reservoir performance. The results and conclusions of the most recent studies will be summarized here. Included are two reports and one

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 2013-03-20T13:01:00

Harvest Information

Original ID 50ec3aefb656b70647f32e38bc0232fc
Index Date 2013-06-11T19:40:02Z
Original Format ISO-USGIN
Original Version 1.2

Author

Position missing
Organization Stanford University, Stanford Geothermal Program, Dept. of Petroleum Engineering
Email horne@stanford.edu

Geographic Extent

North Bound 42.553080288955
South Bound 32.175612478498
East Bound -113.90625
West Bound -125.771484375