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Detailed Reference Information |
Rosanne, M., Paszkuta, M., Thovert, J.-F. and Adler, P.M. (2004). Electro-osmotic coupling in compact clays. Geophysical Research Letters 31: doi: 10.1029/2004GL020770. issn: 0094-8276. |
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Electro-osmotic coefficients are determined experimentally and compared to numerical data. The numerical model assumes random packings of grains of various shapes; the prediction corresponds to a modified analytical solution. A special set up was designed to measure all relevant properties independently as functions of the porosity and electrolyte concentration. Two model clays and a compact natural clay were used. Good agreement was found between experimental and numerical results, indicating that the electro-osmotic coefficient can be predicted from conductivity and permeability. |
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Abstract |
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Keywords
Electromagnetics, Measurement and standards, Electromagnetics, Numerical methods, Electromagnetics, Random media and rough surfaces, Physical Properties of Rocks, Magnetic and electrical properties, Physical Properties of Rocks, Permeability and porosity |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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