Loading…
Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability
Natural disasters such as landslides often occur on soil slopes in seasonally frozen areas that undergo freeze‒thaw cycling. Ecological slope protection is an effective way to prevent such disasters. To explore the change in the mechanical properties of soil under the influence of both root reinforc...
Saved in:
Published in: | PloS one 2024-04, Vol.19 (4), p.e0302409-e0302409 |
---|---|
Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | |
---|---|
cites | cdi_FETCH-LOGICAL-c590t-e77f77d845bd5789dd213dac46c579198e1792ff9a62df41c54251ac6fa1da63 |
container_end_page | e0302409 |
container_issue | 4 |
container_start_page | e0302409 |
container_title | PloS one |
container_volume | 19 |
creator | Wang, Ruihong Jing, Zexin Luo, Hao Bao, Shun Jia, Jingru Zhan, Xiaoyu |
description | Natural disasters such as landslides often occur on soil slopes in seasonally frozen areas that undergo freeze‒thaw cycling. Ecological slope protection is an effective way to prevent such disasters. To explore the change in the mechanical properties of soil under the influence of both root reinforcement and freeze‒thaw cycles and its influence on slope stability, the Baijiabao landslide in the Three Gorges Reservoir area was taken as an example. The mechanical properties of soil under different confining pressures, vegetation coverages (VCs) and numbers of freeze‒thaw cycles were studied via mechanical tests, such as triaxial compression tests, wave velocity tests and FLAC3D simulations. The results show that the shear strength of a root-soil composite increases with increasing confining pressure and VC and decreases with increasing number of freeze‒thaw cycles. Bermuda grass roots and confining pressure jointly improve the durability of soil under freeze‒thaw conditions. However, with an increase in the number of freeze‒thaw cycles, the resistance of root reinforcement to freeze‒thaw action gradually decreases. The observed effect of freeze‒thaw cycles on soil degradation was divided into three stages: a significant decrease in strength, a slight decrease in strength and strength stability. Freeze‒thaw cycles and VC mainly affect the cohesion of the soil and have little effect on the internal friction angle. Compared with that of a bare soil slope, the safety factor of a slope covered with plants is larger, the maximum displacement of a landslide is smaller, and it is less affected by freezing and thawing. These findings can provide a reference for research on ecological slope protection technology. |
doi_str_mv | 10.1371/journal.pone.0302409 |
format | article |
fullrecord | <record><control><sourceid>gale_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_8f132102e37d43b79545a1bb7977c6ba</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A791591969</galeid><doaj_id>oai_doaj_org_article_8f132102e37d43b79545a1bb7977c6ba</doaj_id><sourcerecordid>A791591969</sourcerecordid><originalsourceid>FETCH-LOGICAL-c590t-e77f77d845bd5789dd213dac46c579198e1792ff9a62df41c54251ac6fa1da63</originalsourceid><addsrcrecordid>eNqNks-KFDEQxhtR3HX1DUQaBNHDjEkn6XSflmVZdWBhwV28hur8mcmQ7rRJWh1PPoOP6JOYccZlBjxIDpVUfvVRVXxF8RyjOSYcv137KQzg5qMf9BwRVFHUPihOcUuqWV0h8vDgflI8iXGNECNNXT8uTrah4lV9WogrY7RMpTelCVp_179-_Ewr-FrKjXQ6ln4og_dpduutK6XvRx9t0mWv5QoGK8GVY_CjDslmGAZVRpefZUzQWWfT5mnxyICL-tk-nhV3767uLj_Mrm_eLy4vrmeStSjNNOeGc9VQ1inGm1apChMFktaS8Ra3jca8rYxpoa6UoVgyWjEMsjaAFdTkrFjsZJWHtRiD7SFshAcr_iR8WArIPeaRRGMwqTCqNOGKko63jDLAXb5wLusOstb5Tmucul4rqYcUwB2JHv8MdiWW_ovAGFGGa5oVXu8Vgv886ZhEb6PUzsGg_RQFQZS3lKFmi77coUvIvdnB-Cwpt7i4yIOzPHvdZmr-DyofpXsrswGMzfmjgjdHBZlJ-ltawhSjWNx-_H_25tMx--qAXWlwaRW9m5L1QzwG6Q6UwccYtLnfH0Zi61-x96_Y-lfs_ZvLXhzu_r7or2HJb4jJ7kw</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3047945084</pqid></control><display><type>article</type><title>Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability</title><source>Publicly Available Content Database</source><source>PubMed Central</source><creator>Wang, Ruihong ; Jing, Zexin ; Luo, Hao ; Bao, Shun ; Jia, Jingru ; Zhan, Xiaoyu</creator><contributor>Qaidi, Shaker</contributor><creatorcontrib>Wang, Ruihong ; Jing, Zexin ; Luo, Hao ; Bao, Shun ; Jia, Jingru ; Zhan, Xiaoyu ; Qaidi, Shaker</creatorcontrib><description>Natural disasters such as landslides often occur on soil slopes in seasonally frozen areas that undergo freeze‒thaw cycling. Ecological slope protection is an effective way to prevent such disasters. To explore the change in the mechanical properties of soil under the influence of both root reinforcement and freeze‒thaw cycles and its influence on slope stability, the Baijiabao landslide in the Three Gorges Reservoir area was taken as an example. The mechanical properties of soil under different confining pressures, vegetation coverages (VCs) and numbers of freeze‒thaw cycles were studied via mechanical tests, such as triaxial compression tests, wave velocity tests and FLAC3D simulations. The results show that the shear strength of a root-soil composite increases with increasing confining pressure and VC and decreases with increasing number of freeze‒thaw cycles. Bermuda grass roots and confining pressure jointly improve the durability of soil under freeze‒thaw conditions. However, with an increase in the number of freeze‒thaw cycles, the resistance of root reinforcement to freeze‒thaw action gradually decreases. The observed effect of freeze‒thaw cycles on soil degradation was divided into three stages: a significant decrease in strength, a slight decrease in strength and strength stability. Freeze‒thaw cycles and VC mainly affect the cohesion of the soil and have little effect on the internal friction angle. Compared with that of a bare soil slope, the safety factor of a slope covered with plants is larger, the maximum displacement of a landslide is smaller, and it is less affected by freezing and thawing. These findings can provide a reference for research on ecological slope protection technology.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0302409</identifier><identifier>PMID: 38662726</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Biology and Life Sciences ; Earth Sciences ; Engineering research ; Freezing ; Landslides ; Physical Sciences ; Plant Roots - physiology ; Soil - chemistry ; Soil mechanics ; Soil temperature ; Soils ; Thermal properties</subject><ispartof>PloS one, 2024-04, Vol.19 (4), p.e0302409-e0302409</ispartof><rights>Copyright: © 2024 Wang et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</rights><rights>COPYRIGHT 2024 Public Library of Science</rights><rights>2024 Wang et al 2024 Wang et al</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c590t-e77f77d845bd5789dd213dac46c579198e1792ff9a62df41c54251ac6fa1da63</cites><orcidid>0000-0001-6318-0369</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC11045164/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC11045164/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,27924,27925,37013,53791,53793</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/38662726$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><contributor>Qaidi, Shaker</contributor><creatorcontrib>Wang, Ruihong</creatorcontrib><creatorcontrib>Jing, Zexin</creatorcontrib><creatorcontrib>Luo, Hao</creatorcontrib><creatorcontrib>Bao, Shun</creatorcontrib><creatorcontrib>Jia, Jingru</creatorcontrib><creatorcontrib>Zhan, Xiaoyu</creatorcontrib><title>Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability</title><title>PloS one</title><addtitle>PLoS One</addtitle><description>Natural disasters such as landslides often occur on soil slopes in seasonally frozen areas that undergo freeze‒thaw cycling. Ecological slope protection is an effective way to prevent such disasters. To explore the change in the mechanical properties of soil under the influence of both root reinforcement and freeze‒thaw cycles and its influence on slope stability, the Baijiabao landslide in the Three Gorges Reservoir area was taken as an example. The mechanical properties of soil under different confining pressures, vegetation coverages (VCs) and numbers of freeze‒thaw cycles were studied via mechanical tests, such as triaxial compression tests, wave velocity tests and FLAC3D simulations. The results show that the shear strength of a root-soil composite increases with increasing confining pressure and VC and decreases with increasing number of freeze‒thaw cycles. Bermuda grass roots and confining pressure jointly improve the durability of soil under freeze‒thaw conditions. However, with an increase in the number of freeze‒thaw cycles, the resistance of root reinforcement to freeze‒thaw action gradually decreases. The observed effect of freeze‒thaw cycles on soil degradation was divided into three stages: a significant decrease in strength, a slight decrease in strength and strength stability. Freeze‒thaw cycles and VC mainly affect the cohesion of the soil and have little effect on the internal friction angle. Compared with that of a bare soil slope, the safety factor of a slope covered with plants is larger, the maximum displacement of a landslide is smaller, and it is less affected by freezing and thawing. These findings can provide a reference for research on ecological slope protection technology.</description><subject>Biology and Life Sciences</subject><subject>Earth Sciences</subject><subject>Engineering research</subject><subject>Freezing</subject><subject>Landslides</subject><subject>Physical Sciences</subject><subject>Plant Roots - physiology</subject><subject>Soil - chemistry</subject><subject>Soil mechanics</subject><subject>Soil temperature</subject><subject>Soils</subject><subject>Thermal properties</subject><issn>1932-6203</issn><issn>1932-6203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNqNks-KFDEQxhtR3HX1DUQaBNHDjEkn6XSflmVZdWBhwV28hur8mcmQ7rRJWh1PPoOP6JOYccZlBjxIDpVUfvVRVXxF8RyjOSYcv137KQzg5qMf9BwRVFHUPihOcUuqWV0h8vDgflI8iXGNECNNXT8uTrah4lV9WogrY7RMpTelCVp_179-_Ewr-FrKjXQ6ln4og_dpduutK6XvRx9t0mWv5QoGK8GVY_CjDslmGAZVRpefZUzQWWfT5mnxyICL-tk-nhV3767uLj_Mrm_eLy4vrmeStSjNNOeGc9VQ1inGm1apChMFktaS8Ra3jca8rYxpoa6UoVgyWjEMsjaAFdTkrFjsZJWHtRiD7SFshAcr_iR8WArIPeaRRGMwqTCqNOGKko63jDLAXb5wLusOstb5Tmucul4rqYcUwB2JHv8MdiWW_ovAGFGGa5oVXu8Vgv886ZhEb6PUzsGg_RQFQZS3lKFmi77coUvIvdnB-Cwpt7i4yIOzPHvdZmr-DyofpXsrswGMzfmjgjdHBZlJ-ltawhSjWNx-_H_25tMx--qAXWlwaRW9m5L1QzwG6Q6UwccYtLnfH0Zi61-x96_Y-lfs_ZvLXhzu_r7or2HJb4jJ7kw</recordid><startdate>20240425</startdate><enddate>20240425</enddate><creator>Wang, Ruihong</creator><creator>Jing, Zexin</creator><creator>Luo, Hao</creator><creator>Bao, Shun</creator><creator>Jia, Jingru</creator><creator>Zhan, Xiaoyu</creator><general>Public Library of Science</general><general>Public Library of Science (PLoS)</general><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>IOV</scope><scope>ISR</scope><scope>7X8</scope><scope>5PM</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0001-6318-0369</orcidid></search><sort><creationdate>20240425</creationdate><title>Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability</title><author>Wang, Ruihong ; Jing, Zexin ; Luo, Hao ; Bao, Shun ; Jia, Jingru ; Zhan, Xiaoyu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c590t-e77f77d845bd5789dd213dac46c579198e1792ff9a62df41c54251ac6fa1da63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Biology and Life Sciences</topic><topic>Earth Sciences</topic><topic>Engineering research</topic><topic>Freezing</topic><topic>Landslides</topic><topic>Physical Sciences</topic><topic>Plant Roots - physiology</topic><topic>Soil - chemistry</topic><topic>Soil mechanics</topic><topic>Soil temperature</topic><topic>Soils</topic><topic>Thermal properties</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Ruihong</creatorcontrib><creatorcontrib>Jing, Zexin</creatorcontrib><creatorcontrib>Luo, Hao</creatorcontrib><creatorcontrib>Bao, Shun</creatorcontrib><creatorcontrib>Jia, Jingru</creatorcontrib><creatorcontrib>Zhan, Xiaoyu</creatorcontrib><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Gale In Context: Opposing Viewpoints</collection><collection>Gale In Context: Science</collection><collection>MEDLINE - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><collection>Directory of Open Access Journals (Open Access)</collection><jtitle>PloS one</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Ruihong</au><au>Jing, Zexin</au><au>Luo, Hao</au><au>Bao, Shun</au><au>Jia, Jingru</au><au>Zhan, Xiaoyu</au><au>Qaidi, Shaker</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2024-04-25</date><risdate>2024</risdate><volume>19</volume><issue>4</issue><spage>e0302409</spage><epage>e0302409</epage><pages>e0302409-e0302409</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>Natural disasters such as landslides often occur on soil slopes in seasonally frozen areas that undergo freeze‒thaw cycling. Ecological slope protection is an effective way to prevent such disasters. To explore the change in the mechanical properties of soil under the influence of both root reinforcement and freeze‒thaw cycles and its influence on slope stability, the Baijiabao landslide in the Three Gorges Reservoir area was taken as an example. The mechanical properties of soil under different confining pressures, vegetation coverages (VCs) and numbers of freeze‒thaw cycles were studied via mechanical tests, such as triaxial compression tests, wave velocity tests and FLAC3D simulations. The results show that the shear strength of a root-soil composite increases with increasing confining pressure and VC and decreases with increasing number of freeze‒thaw cycles. Bermuda grass roots and confining pressure jointly improve the durability of soil under freeze‒thaw conditions. However, with an increase in the number of freeze‒thaw cycles, the resistance of root reinforcement to freeze‒thaw action gradually decreases. The observed effect of freeze‒thaw cycles on soil degradation was divided into three stages: a significant decrease in strength, a slight decrease in strength and strength stability. Freeze‒thaw cycles and VC mainly affect the cohesion of the soil and have little effect on the internal friction angle. Compared with that of a bare soil slope, the safety factor of a slope covered with plants is larger, the maximum displacement of a landslide is smaller, and it is less affected by freezing and thawing. These findings can provide a reference for research on ecological slope protection technology.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>38662726</pmid><doi>10.1371/journal.pone.0302409</doi><tpages>e0302409</tpages><orcidid>https://orcid.org/0000-0001-6318-0369</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1932-6203 |
ispartof | PloS one, 2024-04, Vol.19 (4), p.e0302409-e0302409 |
issn | 1932-6203 1932-6203 |
language | eng |
recordid | cdi_doaj_primary_oai_doaj_org_article_8f132102e37d43b79545a1bb7977c6ba |
source | Publicly Available Content Database; PubMed Central |
subjects | Biology and Life Sciences Earth Sciences Engineering research Freezing Landslides Physical Sciences Plant Roots - physiology Soil - chemistry Soil mechanics Soil temperature Soils Thermal properties |
title | Effect of freeze‒thaw cycles on root-Soil composite mechanical properties and slope stability |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T22%3A21%3A58IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Effect%20of%20freeze%E2%80%92thaw%20cycles%20on%20root-Soil%20composite%20mechanical%20properties%20and%20slope%20stability&rft.jtitle=PloS%20one&rft.au=Wang,%20Ruihong&rft.date=2024-04-25&rft.volume=19&rft.issue=4&rft.spage=e0302409&rft.epage=e0302409&rft.pages=e0302409-e0302409&rft.issn=1932-6203&rft.eissn=1932-6203&rft_id=info:doi/10.1371/journal.pone.0302409&rft_dat=%3Cgale_doaj_%3EA791591969%3C/gale_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c590t-e77f77d845bd5789dd213dac46c579198e1792ff9a62df41c54251ac6fa1da63%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=3047945084&rft_id=info:pmid/38662726&rft_galeid=A791591969&rfr_iscdi=true |