Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling

Purpose It is of great significance to study the influence of subgrade filling on permafrost temperature field in permafrost area for the smooth construction and safe operation of railway. Design/methodology/approach The paper builds up the model for the hydrothermal coupling calculation of permafro...

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Published in:Railway Sciences
Main Authors: Wang, Yunjia, Zhang, Qianli
Format: Article in Journal/Newspaper
Language:English
Published: Emerald 2023
Subjects:
Online Access:http://dx.doi.org/10.1108/rs-04-2023-0016
https://www.emerald.com/insight/content/doi/10.1108/RS-04-2023-0016/full/xml
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spelling cremerald:10.1108/rs-04-2023-0016 2024-06-09T07:48:57+00:00 Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling Wang, Yunjia Zhang, Qianli 2023 http://dx.doi.org/10.1108/rs-04-2023-0016 https://www.emerald.com/insight/content/doi/10.1108/RS-04-2023-0016/full/xml https://www.emerald.com/insight/content/doi/10.1108/RS-04-2023-0016/full/html en eng Emerald https://www.emerald.com/insight/site-policies Railway Sciences volume 2, issue 2, page 179-196 ISSN 2755-0907 2755-0915 journal-article 2023 cremerald https://doi.org/10.1108/rs-04-2023-0016 2024-05-15T13:23:28Z Purpose It is of great significance to study the influence of subgrade filling on permafrost temperature field in permafrost area for the smooth construction and safe operation of railway. Design/methodology/approach The paper builds up the model for the hydrothermal coupling calculation of permafrost using finite element software COMSOL to study how permafrost temperature field changes in the short term after subgrade filling, on which basis it proposes the method of calculation for the concave distortion of freezing front in the subgrade-covered area. Findings The results show that the freezing front below the subgrade center sinks due to the thermal effect of subgrade filling, which will trigger hydrothermal erosion in case of sufficient moisture inflows, leading to the thawing settlement or the cracking of the subgrade, etc. The heat output of soil will be hindered the most in case of July filling, in which case the sinking and the distortion of the freezing front is found to be the most severe, which the recovery of the permafrost temperature field, the slowest, constituting the most unfavorable working condition. The concave distortion of the freezing front in the subgrade area increases with the increase in temperature difference between the filler and ground surface, the subgrade height, the subgrade width and the volumetric thermal capacity of filler, while decreases with the increase of the thermal conductivity of filler. Therefore, the filler chose for engineering project shall be of small volumetric thermal capacity, low initial temperature and high thermal conductivity whenever possible. Originality/value The concave distortion of the freezing front under different working conditions at different times after filling can be calculated using the method proposed. Article in Journal/Newspaper permafrost Emerald Railway Sciences
institution Open Polar
collection Emerald
op_collection_id cremerald
language English
description Purpose It is of great significance to study the influence of subgrade filling on permafrost temperature field in permafrost area for the smooth construction and safe operation of railway. Design/methodology/approach The paper builds up the model for the hydrothermal coupling calculation of permafrost using finite element software COMSOL to study how permafrost temperature field changes in the short term after subgrade filling, on which basis it proposes the method of calculation for the concave distortion of freezing front in the subgrade-covered area. Findings The results show that the freezing front below the subgrade center sinks due to the thermal effect of subgrade filling, which will trigger hydrothermal erosion in case of sufficient moisture inflows, leading to the thawing settlement or the cracking of the subgrade, etc. The heat output of soil will be hindered the most in case of July filling, in which case the sinking and the distortion of the freezing front is found to be the most severe, which the recovery of the permafrost temperature field, the slowest, constituting the most unfavorable working condition. The concave distortion of the freezing front in the subgrade area increases with the increase in temperature difference between the filler and ground surface, the subgrade height, the subgrade width and the volumetric thermal capacity of filler, while decreases with the increase of the thermal conductivity of filler. Therefore, the filler chose for engineering project shall be of small volumetric thermal capacity, low initial temperature and high thermal conductivity whenever possible. Originality/value The concave distortion of the freezing front under different working conditions at different times after filling can be calculated using the method proposed.
format Article in Journal/Newspaper
author Wang, Yunjia
Zhang, Qianli
spellingShingle Wang, Yunjia
Zhang, Qianli
Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
author_facet Wang, Yunjia
Zhang, Qianli
author_sort Wang, Yunjia
title Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
title_short Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
title_full Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
title_fullStr Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
title_full_unstemmed Numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
title_sort numerical analysis for permafrost temperature field in the short term of permafrost subgrade filling
publisher Emerald
publishDate 2023
url http://dx.doi.org/10.1108/rs-04-2023-0016
https://www.emerald.com/insight/content/doi/10.1108/RS-04-2023-0016/full/xml
https://www.emerald.com/insight/content/doi/10.1108/RS-04-2023-0016/full/html
genre permafrost
genre_facet permafrost
op_source Railway Sciences
volume 2, issue 2, page 179-196
ISSN 2755-0907 2755-0915
op_rights https://www.emerald.com/insight/site-policies
op_doi https://doi.org/10.1108/rs-04-2023-0016
container_title Railway Sciences
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