Abstract
The effective thermal conductivity of secondary rocks (sandstone, dolomite, aleurolite) is studied under high pressures of up to 400 MPa and temperatures of 273–523 K. It is established that the temperature and baric functions of thermal conductivity depend substantially on the degree of crystallization and the mosaicity of rock-forming compounds.
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Original Russian Text © A.E. Ramazanova, S.N. Emirov, 2012, published in Izvestiya Rossiiskoi Akademii Nauk. Seriya Fizicheskaya, 2012, Vol. 76, No. 10, pp. 1283–1287.
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Ramazanova, A.E., Emirov, S.N. Baric and temperature dependences for the thermal conductivity of sedimentary rocks. Bull. Russ. Acad. Sci. Phys. 76, 1152–1156 (2012). https://doi.org/10.3103/S1062873812100103
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DOI: https://doi.org/10.3103/S1062873812100103