Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions

The object of the study is the soil susceptible to cryogenic cracking during freezing. The formation of cracks creates the problems in the development of mineral deposits in northern regions with sharply continental climates in Europe, Asia and North America. The destructive effects of cracks on the...

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Main Author: Stetjukha, Vladimir
Format: Report
Language:English
Published: Magazine of Civil Engineering 2021
Subjects:
Online Access:https://dx.doi.org/10.34910/mce.104.5
http://engstroy.spbstu.ru/en/article/2021.104.05/
id ftdatacite:10.34910/mce.104.5
record_format openpolar
spelling ftdatacite:10.34910/mce.104.5 2023-05-15T17:57:49+02:00 Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions Stetjukha, Vladimir 2021 pdf https://dx.doi.org/10.34910/mce.104.5 http://engstroy.spbstu.ru/en/article/2021.104.05/ en eng Magazine of Civil Engineering frost cracks frozen soil temperature drop deformation freezing heat transfer Text research paper article-journal ScholarlyArticle 2021 ftdatacite https://doi.org/10.34910/mce.104.5 2021-11-05T12:55:41Z The object of the study is the soil susceptible to cryogenic cracking during freezing. The formation of cracks creates the problems in the development of mineral deposits in northern regions with sharply continental climates in Europe, Asia and North America. The destructive effects of cracks on the construction of roads and linear structures require the prediction of cryogenic cracks. The developed mathematical model and the method of its use provide the prediction of the processes of frost cracks formation in harsh climates. The calculation algorithm realizes the procedures for the step-by-step solution of the spatial strength problem for a fragment of a soil mass taking into account changes in temperature fields and physical and mechanical properties of frozen soils over time. The given example demonstrates the results of predicting of cryogenic cracking of the soil in the form of graphs of stress distribution in the freezing massif. The calculation results illustrate the ability to predict the formation of frost cracks, the ability to determine the main parameters and periods of cracking. The research results can be used in the design of objects in the conditions of propagation of soils subjected to cracking. : The object of the study is the soil susceptible to cryogenic cracking during freezing. The formation of cracks creates the problems in the development of mineral deposits in northern regions with sharply continental climates in Europe, Asia and North America. The destructive effects of cracks on the construction of roads and linear structures require the prediction of cryogenic cracks. The developed mathematical model and the method of its use provide the prediction of the processes of frost cracks formation in harsh climates. The calculation algorithm realizes the procedures for the step-by-step solution of the spatial strength problem for a fragment of a soil mass taking into account changes in temperature fields and physical and mechanical properties of frozen soils over time. The given example demonstrates the results of predicting of cryogenic cracking of the soil in the form of graphs of stress distribution in the freezing massif. The calculation results illustrate the ability to predict the formation of frost cracks, the ability to determine the main parameters and periods of cracking. The research results can be used in the design of objects in the conditions of propagation of soils subjected to cracking. Report permafrost DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic frost cracks
frozen soil
temperature drop
deformation
freezing
heat transfer
spellingShingle frost cracks
frozen soil
temperature drop
deformation
freezing
heat transfer
Stetjukha, Vladimir
Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
topic_facet frost cracks
frozen soil
temperature drop
deformation
freezing
heat transfer
description The object of the study is the soil susceptible to cryogenic cracking during freezing. The formation of cracks creates the problems in the development of mineral deposits in northern regions with sharply continental climates in Europe, Asia and North America. The destructive effects of cracks on the construction of roads and linear structures require the prediction of cryogenic cracks. The developed mathematical model and the method of its use provide the prediction of the processes of frost cracks formation in harsh climates. The calculation algorithm realizes the procedures for the step-by-step solution of the spatial strength problem for a fragment of a soil mass taking into account changes in temperature fields and physical and mechanical properties of frozen soils over time. The given example demonstrates the results of predicting of cryogenic cracking of the soil in the form of graphs of stress distribution in the freezing massif. The calculation results illustrate the ability to predict the formation of frost cracks, the ability to determine the main parameters and periods of cracking. The research results can be used in the design of objects in the conditions of propagation of soils subjected to cracking. : The object of the study is the soil susceptible to cryogenic cracking during freezing. The formation of cracks creates the problems in the development of mineral deposits in northern regions with sharply continental climates in Europe, Asia and North America. The destructive effects of cracks on the construction of roads and linear structures require the prediction of cryogenic cracks. The developed mathematical model and the method of its use provide the prediction of the processes of frost cracks formation in harsh climates. The calculation algorithm realizes the procedures for the step-by-step solution of the spatial strength problem for a fragment of a soil mass taking into account changes in temperature fields and physical and mechanical properties of frozen soils over time. The given example demonstrates the results of predicting of cryogenic cracking of the soil in the form of graphs of stress distribution in the freezing massif. The calculation results illustrate the ability to predict the formation of frost cracks, the ability to determine the main parameters and periods of cracking. The research results can be used in the design of objects in the conditions of propagation of soils subjected to cracking.
format Report
author Stetjukha, Vladimir
author_facet Stetjukha, Vladimir
author_sort Stetjukha, Vladimir
title Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
title_short Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
title_full Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
title_fullStr Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
title_full_unstemmed Frost cracks formation in permafrost regions : Frost cracks formation in permafrost regions
title_sort frost cracks formation in permafrost regions : frost cracks formation in permafrost regions
publisher Magazine of Civil Engineering
publishDate 2021
url https://dx.doi.org/10.34910/mce.104.5
http://engstroy.spbstu.ru/en/article/2021.104.05/
genre permafrost
genre_facet permafrost
op_doi https://doi.org/10.34910/mce.104.5
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