Thermo-mechanical coupling analysis and software development

In order to quickly and accurately grasp the law of freeze-thaw reaction of permafrost slopes, based on the hydro-thermal-mechanical coupling theory, relying on MATLto compile a finite element program that can reflect the multi-field coupling mechanism of the soil. This test is in good agreement wit...

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Published in:Thermal Science
Main Authors: Chai Jianwei, Ai Hua, Liu Ting
Format: Article in Journal/Newspaper
Language:English
Published: VINCA Institute of Nuclear Sciences 2021
Subjects:
Online Access:https://doi.org/10.2298/TSCI2104199C
https://doaj.org/article/8b87f43c45d74fa2b8b9b6d79ab4b791
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spelling ftdoajarticles:oai:doaj.org/article:8b87f43c45d74fa2b8b9b6d79ab4b791 2023-05-15T17:56:59+02:00 Thermo-mechanical coupling analysis and software development Chai Jianwei Ai Hua Liu Ting 2021-01-01T00:00:00Z https://doi.org/10.2298/TSCI2104199C https://doaj.org/article/8b87f43c45d74fa2b8b9b6d79ab4b791 EN eng VINCA Institute of Nuclear Sciences http://www.doiserbia.nb.rs/img/doi/0354-9836/2021/0354-98362104199C.pdf https://doaj.org/toc/0354-9836 https://doaj.org/toc/2334-7163 0354-9836 2334-7163 doi:10.2298/TSCI2104199C https://doaj.org/article/8b87f43c45d74fa2b8b9b6d79ab4b791 Thermal Science, Vol 25, Iss 4 Part B, Pp 3199-3208 (2021) numerical calculation software development permafrost slope hydro-thermal-mechanical coupling freezing and thawing Mechanical engineering and machinery TJ1-1570 article 2021 ftdoajarticles https://doi.org/10.2298/TSCI2104199C 2022-12-31T10:22:45Z In order to quickly and accurately grasp the law of freeze-thaw reaction of permafrost slopes, based on the hydro-thermal-mechanical coupling theory, relying on MATLto compile a finite element program that can reflect the multi-field coupling mechanism of the soil. This test is in good agreement with the classic test, which verifies the reliability of the program. Based on this, the paper developed a set of water-thermal-mechanical coupling analysis software for permafrost slopes that can run independently and is easy to operate. The software’s functions and development process are introduced. The response characteristics of frozen soil slopes under freezing and thawing are analyzed in combination with the example papers. The results show that the slope temperature, moisture, stress and displacement are obviously different at different times. The maximum shear stress band appears at the freezing-thawing interface of the slope. The horizontal displacement of the slope is basically the same along the slope when the freezing is completed. At the end of the thawing period, the upper part and the lower part are large. The horizontal displacement and unfrozen water content of the slope during the thawing period are larger than those during the freezing period, but the maximum shear stress is small and the stability of permafrost in the warm season is poor. It has important application value for freeze-thaw calculation of frozen soil slope engineering. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Thermal Science 25 4 Part B 3199 3208
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic numerical calculation
software development
permafrost slope
hydro-thermal-mechanical coupling
freezing and thawing
Mechanical engineering and machinery
TJ1-1570
spellingShingle numerical calculation
software development
permafrost slope
hydro-thermal-mechanical coupling
freezing and thawing
Mechanical engineering and machinery
TJ1-1570
Chai Jianwei
Ai Hua
Liu Ting
Thermo-mechanical coupling analysis and software development
topic_facet numerical calculation
software development
permafrost slope
hydro-thermal-mechanical coupling
freezing and thawing
Mechanical engineering and machinery
TJ1-1570
description In order to quickly and accurately grasp the law of freeze-thaw reaction of permafrost slopes, based on the hydro-thermal-mechanical coupling theory, relying on MATLto compile a finite element program that can reflect the multi-field coupling mechanism of the soil. This test is in good agreement with the classic test, which verifies the reliability of the program. Based on this, the paper developed a set of water-thermal-mechanical coupling analysis software for permafrost slopes that can run independently and is easy to operate. The software’s functions and development process are introduced. The response characteristics of frozen soil slopes under freezing and thawing are analyzed in combination with the example papers. The results show that the slope temperature, moisture, stress and displacement are obviously different at different times. The maximum shear stress band appears at the freezing-thawing interface of the slope. The horizontal displacement of the slope is basically the same along the slope when the freezing is completed. At the end of the thawing period, the upper part and the lower part are large. The horizontal displacement and unfrozen water content of the slope during the thawing period are larger than those during the freezing period, but the maximum shear stress is small and the stability of permafrost in the warm season is poor. It has important application value for freeze-thaw calculation of frozen soil slope engineering.
format Article in Journal/Newspaper
author Chai Jianwei
Ai Hua
Liu Ting
author_facet Chai Jianwei
Ai Hua
Liu Ting
author_sort Chai Jianwei
title Thermo-mechanical coupling analysis and software development
title_short Thermo-mechanical coupling analysis and software development
title_full Thermo-mechanical coupling analysis and software development
title_fullStr Thermo-mechanical coupling analysis and software development
title_full_unstemmed Thermo-mechanical coupling analysis and software development
title_sort thermo-mechanical coupling analysis and software development
publisher VINCA Institute of Nuclear Sciences
publishDate 2021
url https://doi.org/10.2298/TSCI2104199C
https://doaj.org/article/8b87f43c45d74fa2b8b9b6d79ab4b791
genre permafrost
genre_facet permafrost
op_source Thermal Science, Vol 25, Iss 4 Part B, Pp 3199-3208 (2021)
op_relation http://www.doiserbia.nb.rs/img/doi/0354-9836/2021/0354-98362104199C.pdf
https://doaj.org/toc/0354-9836
https://doaj.org/toc/2334-7163
0354-9836
2334-7163
doi:10.2298/TSCI2104199C
https://doaj.org/article/8b87f43c45d74fa2b8b9b6d79ab4b791
op_doi https://doi.org/10.2298/TSCI2104199C
container_title Thermal Science
container_volume 25
container_issue 4 Part B
container_start_page 3199
op_container_end_page 3208
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