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- W1978985103 abstract "A theoretical model is presented for the prediction of the thermal conductivity of fluid-saturated rocks. Rock is idealized as being composed of a connected mineral phase permeated with non-intersecting oblate spheroidal pores. The pores are assumed to be completely saturated with a single-phase fluid. An effective medium theory is used to predict the overall conductivity in terms of the conductivities of the solid and fluid phases, the porosity, and an average aspect ratio of the spheroidal pores. In the limiting case where the pores are thin cracks, the predicted conductivity coincides with the known (Hashin-Shtrikman) lower bound, while the limiting case of spherical pores reproduces the upper bound. The theory is tested against the experimental data from various sedimentary and crystalline rocks, and it is shown to allow the prediction of liquid-saturated conductivities based on gas-saturated measurements, without the need for any arbitrary parameters. The model also provides a link to other petrophysical properties that depend on pore structure, such as compressibility." @default.
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- W1978985103 date "1989-11-01" @default.
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- W1978985103 title "Thermal conductivity of fluid-saturated rocks" @default.
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- W1978985103 doi "https://doi.org/10.1016/0920-4105(89)90019-3" @default.
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