Abstract
The macroscopic conductivity of fractures is determined for Gaussian and self-affine fractures by solving the three-dimensional Laplace equation. Results are discussed and compared with various analytical or two-dimensional approximations. They are shown to be in good agreement with some existing experimental data.
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VOLIK, S., MOURZENKO, V.V., THOVERT, JF. et al. Thermal Conductivity of a Single Fracture. Transport in Porous Media 27, 305–326 (1997). https://doi.org/10.1023/A:1006585510976
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DOI: https://doi.org/10.1023/A:1006585510976