Phase Transitions of the Second Kind in Polycrystalline Compounds and Rocks under Pressure


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Abstract

The results from experimental studies on the effect hydrostatic pressure of up to 400 MPa has on the thermal conductivity of fluid-saturated sandstone samples are analyzed. It is shown that moisture saturation strongly affects the processes of heat transfer in the initial range of pressures. Hydrostatic pressure affects the volume and elastic parameters, resulting in a phase transition of the second kind.

About the authors

S. N. Emirov

Institute of Geothermal Problems, Dagestan Scientific Center, Russian Academy of Sciences

Author for correspondence.
Email: wemirov@mail.ru
Russian Federation, Makhachkala, Republic of Dagestan, 367030

A. E. Ramazanova

Institute of Geothermal Problems, Dagestan Scientific Center, Russian Academy of Sciences

Email: wemirov@mail.ru
Russian Federation, Makhachkala, Republic of Dagestan, 367030

A. I. Ibragimov

Dagestan State Technical University

Email: wemirov@mail.ru
Russian Federation, Makhachkala, Republic of Dagestan, 367026

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