Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development
A three-phase model capable of predicting the heat transfer and moisture migration for soil freezing process was developed based on the Shen-Chen model and the mechanisms of heat and mass transfer in unsaturated soil freezing. The pre-melted film was taken into consideration, and the relationship be...
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doaj-5377be3049cb4889b66ef0d3ef24fe5a2021-09-05T13:59:35ZengDe GruyterOpen Physics2391-54712018-04-01161758310.1515/phys-2018-0014phys-2018-0014Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model developmentXu Fei0Zhang Yaning1Jin Guangri2Li Bingxi3Kim Yong-Song4Xie Gongnan5Fu Zhongbin6School of Energy Science and Engineering, Harbin Institute of Technology, Harbin, ChinaSchool of Energy Science and Engineering, Harbin Institute of Technology, Harbin, ChinaSchool of Mechanical Engineering, Hanyang University, Seoul, Republic of KoreaSchool of Energy Science and Engineering, Harbin Institute of Technology, Harbin, ChinaSchool of Energy Science and Engineering, Harbin Institute of Technology, Harbin, ChinaSchool of Marine Science and Technology, Northwestern Polytechnical University, Xi’an, ChinaSchool of Energy Science and Engineering, Harbin Institute of Technology, Harbin, ChinaA three-phase model capable of predicting the heat transfer and moisture migration for soil freezing process was developed based on the Shen-Chen model and the mechanisms of heat and mass transfer in unsaturated soil freezing. The pre-melted film was taken into consideration, and the relationship between film thickness and soil temperature was used to calculate the liquid water fraction in both frozen zone and freezing fringe. The force that causes the moisture migration was calculated by the sum of several interactive forces and the suction in the pre-melted film was regarded as an interactive force between ice and water. Two kinds of resistance were regarded as a kind of body force related to the water films between the ice grains and soil grains, and a block force instead of gravity was introduced to keep balance with gravity before soil freezing. Lattice Boltzmann method was used in the simulation, and the input variables for the simulation included the size of computational domain, obstacle fraction, liquid water fraction, air fraction and soil porosity. The model is capable of predicting the water content distribution along soil depth and variations in water content and temperature during soil freezing process.https://doi.org/10.1515/phys-2018-0014lattice boltzmannunsaturated soil freezingthree phase modelwater content44.30.+v |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xu Fei Zhang Yaning Jin Guangri Li Bingxi Kim Yong-Song Xie Gongnan Fu Zhongbin |
spellingShingle |
Xu Fei Zhang Yaning Jin Guangri Li Bingxi Kim Yong-Song Xie Gongnan Fu Zhongbin Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development Open Physics lattice boltzmann unsaturated soil freezing three phase model water content 44.30.+v |
author_facet |
Xu Fei Zhang Yaning Jin Guangri Li Bingxi Kim Yong-Song Xie Gongnan Fu Zhongbin |
author_sort |
Xu Fei |
title |
Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development |
title_short |
Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development |
title_full |
Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development |
title_fullStr |
Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development |
title_full_unstemmed |
Three phase heat and mass transfer model for unsaturated soil freezing process: Part 1 - model development |
title_sort |
three phase heat and mass transfer model for unsaturated soil freezing process: part 1 - model development |
publisher |
De Gruyter |
series |
Open Physics |
issn |
2391-5471 |
publishDate |
2018-04-01 |
description |
A three-phase model capable of predicting the heat transfer and moisture migration for soil freezing process was developed based on the Shen-Chen model and the mechanisms of heat and mass transfer in unsaturated soil freezing. The pre-melted film was taken into consideration, and the relationship between film thickness and soil temperature was used to calculate the liquid water fraction in both frozen zone and freezing fringe. The force that causes the moisture migration was calculated by the sum of several interactive forces and the suction in the pre-melted film was regarded as an interactive force between ice and water. Two kinds of resistance were regarded as a kind of body force related to the water films between the ice grains and soil grains, and a block force instead of gravity was introduced to keep balance with gravity before soil freezing. Lattice Boltzmann method was used in the simulation, and the input variables for the simulation included the size of computational domain, obstacle fraction, liquid water fraction, air fraction and soil porosity. The model is capable of predicting the water content distribution along soil depth and variations in water content and temperature during soil freezing process. |
topic |
lattice boltzmann unsaturated soil freezing three phase model water content 44.30.+v |
url |
https://doi.org/10.1515/phys-2018-0014 |
work_keys_str_mv |
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