Analytical estimates of permeability and possible convective heat transfer in compact porous fluid–saturated rocks


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The possible occurrence of convection in fine-grained (low-porous <15%) fluid-saturated (argon, water) rocks under hydrostatic pressures of up to 100 MPa is studied. Calculations of the Rayleigh filtration number and the Darcy number are presented. It is shown that the convective motion of fluid does not occur in pore-saturating fluids within the considered range of pressure variation, pore sizes, and temperature differences.

作者简介

D. Volkov

St. Petersburg National Research University of Information Technologies, Mechanics, and Optics

Email: zarich4@gmail.com
俄罗斯联邦, St. Petersburg, 197101

Yu. Zarichnyak

St. Petersburg National Research University of Information Technologies, Mechanics, and Optics

编辑信件的主要联系方式.
Email: zarich4@gmail.com
俄罗斯联邦, St. Petersburg, 197101

A. Ramazanova

Institute of Geothermal Problems, Dagestan Scientific Center

Email: zarich4@gmail.com
俄罗斯联邦, Makhachkala, 367030

S. Emirov

Institute of Geothermal Problems, Dagestan Scientific Center

Email: zarich4@gmail.com
俄罗斯联邦, Makhachkala, 367030

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