MATHEMATICAL MODEL OF FREEZING OF ROCKS SATURATED WITH SALT SOLUTION TAKING INTO ACCOUNT THE INFLUENCE OF OSMOSIS
- 作者: Ramazanov M.1, Bulgakova N.1, Lobkovsky L.2,3
-
隶属关系:
- Institute for Geothermal Research and Renewable Energy (Branch of the Joint Institute for High Temperatures, Russian Academy of Sciences)
- P.P.Shirshov Institute of Oceanology of the Russian Academy of Science
- Moscow Institute of Physics and Technology (State University)
- 期: 卷 23, 编号 5 (2023)
- 页面: ES5007
- 栏目: Articles
- URL: https://journals.rcsi.science/1681-1208/article/view/259647
- DOI: https://doi.org/10.2205/2023ES000857
- EDN: https://elibrary.ru/bycury
- ID: 259647
如何引用文章
全文:
作者简介
M. Ramazanov
Institute for Geothermal Research and Renewable Energy (Branch of the Joint Institute for High Temperatures, Russian Academy of Sciences)
Email: mukamay-ipg@mail.ru
ORCID iD: 0000-0002-2468-1272
N. Bulgakova
Institute for Geothermal Research and Renewable Energy (Branch of the Joint Institute for High Temperatures, Russian Academy of Sciences)
Email: mukamay-ipg@mail.ru
ORCID iD: 0000-0002-4224-1246
L. Lobkovsky
P.P.Shirshov Institute of Oceanology of the Russian Academy of Science; Moscow Institute of Physics and Technology (State University)
编辑信件的主要联系方式.
Email: mukamay-ipg@mail.ru
ORCID iD: 0000-0002-8033-8452
参考
- Chuvilin, E. M. (1999), Migration of ions of chemical elements in freezing and frozen soils, Polar Record, 35(192), 59–66, https://doi.org/10.1017/s0032247400026346.
- Kemper, W. D. (1961), Movement of Water as Effected by Free Energy and Pressure Gradients: II. Experimental Analysis of Porous Systems in Which Free Energy and Pressure Gradients Act in Opposite Directions, Soil Science Society of America Journal, 25(4), 260–265, https://doi.org/10.2136/sssaj1961.03615995002500040010x.
- Landau, L. D., and E. M. Lifshitz (1976), Theoretical Physics: Volume 5, Nauka, Moscow (in Russian).
- Lobkovskii, L. I., and M. M. Ramazanov (2018), Front Regime of Heat and Mass Transfer in a Gas Hydrate Reservoir under the Negative Temperature Conditions, Fluid Dynamics, 53(4), 517–530, https://doi.org/10.1134/s0015462818040092.
- Ramazanov, M. M., A. V. Karakin, and L. I. Lobkovskiy (2019), Mathematical Model for the Motion of Solutions Taking into Account the Osmotic Effect, Doklady Earth Sciences, 489(1), 1306–1309, https://doi.org/10.1134/s1028334x19110060
- Ramazanov, M. M., N. S. Bulgakova, and L. I. Lobkovskiy (2022), Osmotic Convection, Doklady Physics, 67(5), 153–158, https://doi.org/10.1134/s1028335822040061.
- Shakhova, N., I. Semiletov, O. Gustafsson, V. Sergienko, L. Lobkovsky, O. Dudarev, V. Tumskoy, M. Grigoriev, A. Mazurov, A. Salyuk, R. Ananiev, A. Koshurnikov, D. Kosmach, A. Charkin, N. Dmitrevsky, V. Karnaukh, A. Gunar, A. Meluzov, and D. Chernykh (2017), Current rates and mechanisms of subsea permafrost degradation in the East Siberian Arctic Shelf, Nature Communications, 8(1), https://doi.org/10.1038/ncomms15872.
- Tsypkin, G. G. (2009), Flows with phase transitions in porous media, Fizmatlit, Moscow (in Russian)
- Yakushev, V. S. (2009), Natural gas and gas hydrates in permafrost, VNIIGAZ, Moscow (in Russian)
补充文件
