Development Pattern of Toppling Deformation Slopes in Western China
Controlled by regional geological background, and affected by human activity and weathering, toppling deformation slopes occur in different regions in China. Based on statistics about domestic toppling deformation slopes and their distribution, the regional geological susceptibility zonation area of...
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MDPI AG
2023-05-01
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author | Xingming Li Kaiming Cao Shaoping Huang Ruiming Xing Yuanhai Yang |
author_facet | Xingming Li Kaiming Cao Shaoping Huang Ruiming Xing Yuanhai Yang |
author_sort | Xingming Li |
collection | DOAJ |
description | Controlled by regional geological background, and affected by human activity and weathering, toppling deformation slopes occur in different regions in China. Based on statistics about domestic toppling deformation slopes and their distribution, the regional geological susceptibility zonation area of toppling deformation slopes was determined. Firstly, a regional geological susceptibility evaluation was conducted according to these toppling deformation slopes, choosing landform, stratigraphic age, seismic intensity and tectonic stress distribution, and the study area was divided into very low, low, medium, high and very high susceptibility areas. Secondly, a geographic position susceptibility evaluation was conducted aimed at different sections of typical rivers in western China and the toppling deformation slopes related to them, and the study area was divided into upstream, midstream and downstream of 11 rivers that were respectively classified into very low, low, high and very high susceptibility areas. Thirdly, based on the results, associations between the toppling deformation factors (lithology, slope height, elevation, horizontal depth and vertical depth) and the distribution of deformation slopes were revealed. Finally, the development regularity was analyzed comprehensively. The results show that the toppling deformation slopes of hydropower projects are more developed in Sichuan, Qinghai and Yunnan provinces of China. With regard to regional geography, besides the Yellow River, both the Lancang River and the Yalong River flow through areas with toppling deformation that are classified as highly susceptible geological zones in all levels. The results of this study can be used as references for site selection plans in hydropower projects. |
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spelling | doaj.art-06042537070a428c970ec38b04cbefa62023-11-18T07:34:12ZengMDPI AGApplied Sciences2076-34172023-05-011311659610.3390/app13116596Development Pattern of Toppling Deformation Slopes in Western ChinaXingming Li0Kaiming Cao1Shaoping Huang2Ruiming Xing3Yuanhai Yang4School of Environment and Engineering, Hubei Land Resources Vocational College, Wuhan 430090, ChinaSchool of Civil Architectural and Environmental Engineering, Hubei University of Technology, Wuhan 430068, ChinaSchool of Civil Architectural and Environmental Engineering, Hubei University of Technology, Wuhan 430068, ChinaSchool of Civil Architectural and Environmental Engineering, Hubei University of Technology, Wuhan 430068, ChinaSchool of Civil Architectural and Environmental Engineering, Hubei University of Technology, Wuhan 430068, ChinaControlled by regional geological background, and affected by human activity and weathering, toppling deformation slopes occur in different regions in China. Based on statistics about domestic toppling deformation slopes and their distribution, the regional geological susceptibility zonation area of toppling deformation slopes was determined. Firstly, a regional geological susceptibility evaluation was conducted according to these toppling deformation slopes, choosing landform, stratigraphic age, seismic intensity and tectonic stress distribution, and the study area was divided into very low, low, medium, high and very high susceptibility areas. Secondly, a geographic position susceptibility evaluation was conducted aimed at different sections of typical rivers in western China and the toppling deformation slopes related to them, and the study area was divided into upstream, midstream and downstream of 11 rivers that were respectively classified into very low, low, high and very high susceptibility areas. Thirdly, based on the results, associations between the toppling deformation factors (lithology, slope height, elevation, horizontal depth and vertical depth) and the distribution of deformation slopes were revealed. Finally, the development regularity was analyzed comprehensively. The results show that the toppling deformation slopes of hydropower projects are more developed in Sichuan, Qinghai and Yunnan provinces of China. With regard to regional geography, besides the Yellow River, both the Lancang River and the Yalong River flow through areas with toppling deformation that are classified as highly susceptible geological zones in all levels. The results of this study can be used as references for site selection plans in hydropower projects.https://www.mdpi.com/2076-3417/13/11/6596toppling deformationsregional geologywestern hydropower projectsgeographical positionsusceptibilitydevelopment regularity |
spellingShingle | Xingming Li Kaiming Cao Shaoping Huang Ruiming Xing Yuanhai Yang Development Pattern of Toppling Deformation Slopes in Western China Applied Sciences toppling deformations regional geology western hydropower projects geographical position susceptibility development regularity |
title | Development Pattern of Toppling Deformation Slopes in Western China |
title_full | Development Pattern of Toppling Deformation Slopes in Western China |
title_fullStr | Development Pattern of Toppling Deformation Slopes in Western China |
title_full_unstemmed | Development Pattern of Toppling Deformation Slopes in Western China |
title_short | Development Pattern of Toppling Deformation Slopes in Western China |
title_sort | development pattern of toppling deformation slopes in western china |
topic | toppling deformations regional geology western hydropower projects geographical position susceptibility development regularity |
url | https://www.mdpi.com/2076-3417/13/11/6596 |
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