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Baric and temperature dependences for the thermal conductivity of sedimentary rocks

  • Proceedings of the International Simposium “Ordering in Minerals and Alloys” OMA-14
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Bulletin of the Russian Academy of Sciences: Physics Aims and scope

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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Correspondence to S. N. Emirov.

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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

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