Analytical estimates of permeability and possible convective heat transfer in compact porous fluid–saturated rocks
- Авторлар: Volkov D.P.1, Zarichnyak Y.P.1, Ramazanova A.E.2, Emirov S.N.2
-
Мекемелер:
- St. Petersburg National Research University of Information Technologies, Mechanics, and Optics
- Institute of Geothermal Problems, Dagestan Scientific Center
- Шығарылым: Том 80, № 6 (2016)
- Беттер: 702-706
- Бөлім: Proceedings of the Interdisciplinary Symposium “Ordering in Minerals and Alloys” OMA-18 and Proceedings of the International Interdisciplinary Symposium “Order, Disorder, and Properties of Oxides” ODPO-18
- URL: https://journals.rcsi.science/1062-8738/article/view/184551
- DOI: https://doi.org/10.3103/S1062873816060411
- ID: 184551
Дәйексөз келтіру
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
Қосымша файлдар
