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| | 9.1 Potential Field Methods |
 | | Electrokinetic, or streaming, potential is due to the flow of a fluid with certain electrical properties passing through a pipe or porous medium with different electrical properties (figure 1). |
 | | Flow of gasses and fluids in pipes, leakage of a reservoir within the foundation or abutment of a dam, movement of ionic fluids to or within the groundwater, flow of geothermal fluids, and movement of water into or through a karst system can be the origin of streaming potentials. |
 | | Variation in the flow of fluid due to rainfall, reservoir elevation changes, channelization of flow, or change of surface elevation where measurements are obtained are sources of variation of streaming potential. |
| www.cflhd.gov /agm/geoApplications/SurfaceMethods/931SelfPotentialMethod.htm (1984 words) |
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