Diffusion Coupled (electrochemical) Self-Potential Effects in Geothermal Areas

Previous studies of self-potential anomalies across geothermal systems; scope of paper; effective mobilities of cations and anions in electrolytic solutions; mathematical calculations describing electrochemical concentrations; equations used to describe flux of solute ions and total electric current; pure ambipolar diffusion equations and potential gradient equation; equations describing electrical effects generated by the diffusion of ions and the divergence conditions; application of mathematical calculations to non-lineargeothermal problems; ranges of diffusion potential of 20 rock samples; equations relating permeability and pore size to surface conductivity; electrical conductivity measurements at Roosevelt Hot Springs; results of mathematical modeling at Roosevelt.

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 1982-01-01T00:00:00

Harvest Information

Original ID 6b3eaee7b49162fc7f1835a79e0a735c
Index Date 2013-08-26T20:30:22Z
Original Format ISO-USGIN
Original Version 1.2

Author

Name W.R. Sill
Position missing
Organization Department of Geology & Geophysics, University of Utah
Email gg@utah.edu

Geographic Extent

North Bound 42
South Bound 37
East Bound -109.0452
West Bound -114.04883