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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Main Authors: Xingming Li, Kaiming Cao, Shaoping Huang, Ruiming Xing, Yuanhai Yang
Format: Article
Language:English
Published: MDPI AG 2023-05-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/13/11/6596
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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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AT ruimingxing developmentpatternoftopplingdeformationslopesinwesternchina
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