The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming
The temperature difference at the top and bottom of the crushed-rock layer can drive the heat convection inside. Based on this mechanism, crushed-rock structures with different forms are widely used in the construction and maintenance of the Qinghai-Tibet Railway as cooling measures in permafrost re...
Published in: | Frontiers in Earth Science |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media S.A.
2021
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Subjects: | |
Online Access: | https://doi.org/10.3389/feart.2021.795894 https://doaj.org/article/b3512671f03c48ce92f6eb9c068f7ed8 |
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author | Qihang Mei Bin Yang Ji Chen Jingyi Zhao Xin Hou Youqian Liu Jinchang Wang Shouhong Zhang Haiming Dang |
author_facet | Qihang Mei Bin Yang Ji Chen Jingyi Zhao Xin Hou Youqian Liu Jinchang Wang Shouhong Zhang Haiming Dang |
author_sort | Qihang Mei |
collection | Directory of Open Access Journals: DOAJ Articles |
container_title | Frontiers in Earth Science |
container_volume | 9 |
description | The temperature difference at the top and bottom of the crushed-rock layer can drive the heat convection inside. Based on this mechanism, crushed-rock structures with different forms are widely used in the construction and maintenance of the Qinghai-Tibet Railway as cooling measures in permafrost regions. To explore the stability of different forms of crushed-rock structure embankments under climate warming, the temperature and deformation data of a U-shaped crushed-rock embankment (UCRE) and a crushed-rock revetment embankment (CRRE) are analysed. The variations in temperature indicate that permafrost beneath the natural sites and embankments is degrading but at different rates. The thermal regime of ground under the natural site is only affected by climate warming, while that under embankment is also affected by embankment construction and the cooling effect of the crushed-rock structure. These factors make shallow permafrost degradation beneath the embankments slower than that beneath the natural sites and deep permafrost degradation faster than that beneath the natural sites. Moreover, the convection occurring in the crushed-rock base layer during the cold season makes the degradation of permafrost beneath the UCRE slower than that in the CRRE. The faster degradation of permafrost causes the accumulated deformation of the CRRE to be far greater than that of the UCRE, which may exceed the allowable value of the design code. The analysis shows that the stability of the UCRE meets the engineering requirements and the CRRE needs to be strengthened in warm and ice-rich permafrost regions under climate warming. |
format | Article in Journal/Newspaper |
genre | Ice permafrost |
genre_facet | Ice permafrost |
id | ftdoajarticles:oai:doaj.org/article:b3512671f03c48ce92f6eb9c068f7ed8 |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_doi | https://doi.org/10.3389/feart.2021.795894 |
op_relation | https://www.frontiersin.org/articles/10.3389/feart.2021.795894/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2021.795894 https://doaj.org/article/b3512671f03c48ce92f6eb9c068f7ed8 |
op_source | Frontiers in Earth Science, Vol 9 (2021) |
publishDate | 2021 |
publisher | Frontiers Media S.A. |
record_format | openpolar |
spelling | ftdoajarticles:oai:doaj.org/article:b3512671f03c48ce92f6eb9c068f7ed8 2025-01-16T22:21:41+00:00 The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming Qihang Mei Bin Yang Ji Chen Jingyi Zhao Xin Hou Youqian Liu Jinchang Wang Shouhong Zhang Haiming Dang 2021-12-01T00:00:00Z https://doi.org/10.3389/feart.2021.795894 https://doaj.org/article/b3512671f03c48ce92f6eb9c068f7ed8 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2021.795894/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2021.795894 https://doaj.org/article/b3512671f03c48ce92f6eb9c068f7ed8 Frontiers in Earth Science, Vol 9 (2021) permafrost crushed-rock structure embankment stability thermal regime settlement Science Q article 2021 ftdoajarticles https://doi.org/10.3389/feart.2021.795894 2022-12-31T07:24:06Z The temperature difference at the top and bottom of the crushed-rock layer can drive the heat convection inside. Based on this mechanism, crushed-rock structures with different forms are widely used in the construction and maintenance of the Qinghai-Tibet Railway as cooling measures in permafrost regions. To explore the stability of different forms of crushed-rock structure embankments under climate warming, the temperature and deformation data of a U-shaped crushed-rock embankment (UCRE) and a crushed-rock revetment embankment (CRRE) are analysed. The variations in temperature indicate that permafrost beneath the natural sites and embankments is degrading but at different rates. The thermal regime of ground under the natural site is only affected by climate warming, while that under embankment is also affected by embankment construction and the cooling effect of the crushed-rock structure. These factors make shallow permafrost degradation beneath the embankments slower than that beneath the natural sites and deep permafrost degradation faster than that beneath the natural sites. Moreover, the convection occurring in the crushed-rock base layer during the cold season makes the degradation of permafrost beneath the UCRE slower than that in the CRRE. The faster degradation of permafrost causes the accumulated deformation of the CRRE to be far greater than that of the UCRE, which may exceed the allowable value of the design code. The analysis shows that the stability of the UCRE meets the engineering requirements and the CRRE needs to be strengthened in warm and ice-rich permafrost regions under climate warming. Article in Journal/Newspaper Ice permafrost Directory of Open Access Journals: DOAJ Articles Frontiers in Earth Science 9 |
spellingShingle | permafrost crushed-rock structure embankment stability thermal regime settlement Science Q Qihang Mei Bin Yang Ji Chen Jingyi Zhao Xin Hou Youqian Liu Jinchang Wang Shouhong Zhang Haiming Dang The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title | The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title_full | The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title_fullStr | The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title_full_unstemmed | The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title_short | The Thermal and Settlement Characteristics of Crushed-Rock Structure Embankments of the Qinghai-Tibet Railway in Permafrost Regions Under Climate Warming |
title_sort | thermal and settlement characteristics of crushed-rock structure embankments of the qinghai-tibet railway in permafrost regions under climate warming |
topic | permafrost crushed-rock structure embankment stability thermal regime settlement Science Q |
topic_facet | permafrost crushed-rock structure embankment stability thermal regime settlement Science Q |
url | https://doi.org/10.3389/feart.2021.795894 https://doaj.org/article/b3512671f03c48ce92f6eb9c068f7ed8 |