Freezing Patterns in Saline Soils: Modeling with Regard to the Osmotic Effect

Freezing patterns in a porous soil saturated with a saline solution are investigated with regard to osmotic effects, using a model suggested previously by the authors but in a more general formulation. The results include a numerical and an approximate self-similar analytical solution to a nonlinear problem; description of typical freezing behavior in the presence of osmotic pressure. The modeling results agree well with experimental evidence on freezing of saline clay and sand. The model includes three porous domains with ice (I), thermodynamically equilibrated ice+solution (II), and a liquid saline solution (III) in the pores. The modeling is performed for a simplified case of domains II and III that share a mobile phase boundary where the solution freezes up partially, with heat release.

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Publication Details

Journal
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Published
2024-12-12
DOI
https://doi.org/10.2205/2024es000919
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
0.00

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article

Freezing Patterns in Saline Soils: Modeling with Regard to the Osmotic Effect

Evgeny Chuvilin, Natalia Shakhova, L. I. Lobkovsky, N. S. Bulgakova et al.
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Climate change and permafrost
article

Freezing Patterns in Saline Soils: Modeling with Regard to the Osmotic Effect

Evgeny Chuvilin, Natalia Shakhova, L. I. Lobkovsky, N. S. Bulgakova, S. R. Gadzhimagomedova, М. М. Рамазанов
article en

Abstract

Freezing patterns in a porous soil saturated with a saline solution are investigated with regard to osmotic effects, using a model suggested previously by the authors but in a more general formulation. The results include a numerical and an approximate self-similar analytical solution to a nonlinear problem; description of typical freezing behavior in the presence of osmotic pressure. The modeling results agree well with experimental evidence on freezing of saline clay and sand. The model includes three porous domains with ice (I), thermodynamically equilibrated ice+solution (II), and a liquid saline solution (III) in the pores. The modeling is performed for a simplified case of domains II and III that share a mobile phase boundary where the solution freezes up partially, with heat release.

Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Skolkovo Institute of Science and Technology (RU), National Research Tomsk State University (RU), Institute of Oceanology. PP Shirshov Russian Academy of Sciences (RU), Institute of Geosphere Dynamics (RU), V.I. Il'ichev Pacific Oceanological Institute (RU), Joint Institute for High Temperatures (RU)
Russian Science Foundation
Openalex Percentile: Top 74%
Climate change and permafrost
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