Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process

Abstract The freezing of sulfate saline soil involves the coupling effect of heat and mass transfer and crystallization deformation. The influence of salt content and temperature on the crystallization of ice and salt was analyzed by using a one‐side freezing experiment. Based on the effect of solut...

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Published in:Permafrost and Periglacial Processes
Main Authors: Zhang, Jing, Lai, Yuanming, Zhao, Yanhu, Li, Shuangyang
Other Authors: National Key Research and Development Program of China, Foundation for Innovative Research Groups of the National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2020
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.2080
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spelling crwiley:10.1002/ppp.2080 2024-06-02T08:13:11+00:00 Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process Zhang, Jing Lai, Yuanming Zhao, Yanhu Li, Shuangyang National Key Research and Development Program of China National Key Research and Development Program of China Foundation for Innovative Research Groups of the National Natural Science Foundation of China 2020 http://dx.doi.org/10.1002/ppp.2080 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.2080 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2080 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.2080 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 32, issue 1, page 102-118 ISSN 1045-6740 1099-1530 journal-article 2020 crwiley https://doi.org/10.1002/ppp.2080 2024-05-03T10:56:37Z Abstract The freezing of sulfate saline soil involves the coupling effect of heat and mass transfer and crystallization deformation. The influence of salt content and temperature on the crystallization of ice and salt was analyzed by using a one‐side freezing experiment. Based on the effect of solute and temperature on water activity, a crystallization kinetics model of ice–water phase change in saline soil was established. The application of supersaturation in the crystallization kinetics model of solution–crystal phase change is improved with the Frezchem model. The calculated results are compared with experimental data to validate the effectiveness of the proposed model. the study shows that: (a) crystallization can be well illustrated by the proposed model based on the concepts of the formation factor of ice crystals and solution supersaturation; (b) convection and diffusion are the main means of salt redistribution, which cause the accumulation of salt above the freezing front and the formation of discontinuously distributed–layered salt crystal zones; and (c) the alternate crystallization of ice and salt increases variation i solute concentration and then increases crystallization pressure, which leads to the deformation of salt expansion. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 32 1 102 118
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The freezing of sulfate saline soil involves the coupling effect of heat and mass transfer and crystallization deformation. The influence of salt content and temperature on the crystallization of ice and salt was analyzed by using a one‐side freezing experiment. Based on the effect of solute and temperature on water activity, a crystallization kinetics model of ice–water phase change in saline soil was established. The application of supersaturation in the crystallization kinetics model of solution–crystal phase change is improved with the Frezchem model. The calculated results are compared with experimental data to validate the effectiveness of the proposed model. the study shows that: (a) crystallization can be well illustrated by the proposed model based on the concepts of the formation factor of ice crystals and solution supersaturation; (b) convection and diffusion are the main means of salt redistribution, which cause the accumulation of salt above the freezing front and the formation of discontinuously distributed–layered salt crystal zones; and (c) the alternate crystallization of ice and salt increases variation i solute concentration and then increases crystallization pressure, which leads to the deformation of salt expansion.
author2 National Key Research and Development Program of China
National Key Research and Development Program of China
Foundation for Innovative Research Groups of the National Natural Science Foundation of China
format Article in Journal/Newspaper
author Zhang, Jing
Lai, Yuanming
Zhao, Yanhu
Li, Shuangyang
spellingShingle Zhang, Jing
Lai, Yuanming
Zhao, Yanhu
Li, Shuangyang
Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
author_facet Zhang, Jing
Lai, Yuanming
Zhao, Yanhu
Li, Shuangyang
author_sort Zhang, Jing
title Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
title_short Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
title_full Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
title_fullStr Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
title_full_unstemmed Study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
title_sort study on the mechanism of crystallization deformation of sulfate saline soil during the unidirectional freezing process
publisher Wiley
publishDate 2020
url http://dx.doi.org/10.1002/ppp.2080
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.2080
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2080
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.2080
genre Permafrost and Periglacial Processes
genre_facet Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 32, issue 1, page 102-118
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.2080
container_title Permafrost and Periglacial Processes
container_volume 32
container_issue 1
container_start_page 102
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