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


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Аннотация

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.

Авторлар туралы

D. Volkov

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

Email: zarich4@gmail.com
Ресей, St. Petersburg, 197101

Yu. Zarichnyak

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

Хат алмасуға жауапты Автор.
Email: zarich4@gmail.com
Ресей, St. Petersburg, 197101

A. Ramazanova

Institute of Geothermal Problems, Dagestan Scientific Center

Email: zarich4@gmail.com
Ресей, Makhachkala, 367030

S. Emirov

Institute of Geothermal Problems, Dagestan Scientific Center

Email: zarich4@gmail.com
Ресей, Makhachkala, 367030

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