Long-term stability calculation of reservoir bank slope considering water-rock interaction

Early warning and forecast have always been the key points for landslide research because the disaster caused by landslide leads to enormous life and property loss. This article applies the transformed degradation results of rock to rock mass to calculate the stability and failure mode changes of la...

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Main Authors: Liang-Peng Wan, Mei-Ling Zhou, Subin Desar
Format: Article
Language:English
Published: Faculty of Mechanical Engineering in Slavonski Brod, Faculty of Electrical Engineering in Osijek, Faculty of Civil Engineering in Osijek 2017-01-01
Series:Tehnički Vjesnik
Subjects:
Online Access:https://hrcak.srce.hr/file/257891
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spelling doaj-ad89bb8ca380450ca805d84eaeabcbeb2020-11-24T21:43:41ZengFaculty of Mechanical Engineering in Slavonski Brod, Faculty of Electrical Engineering in Osijek, Faculty of Civil Engineering in Osijek Tehnički Vjesnik1330-36511848-63392017-01-01241283289Long-term stability calculation of reservoir bank slope considering water-rock interactionLiang-Peng Wan0Mei-Ling Zhou1Subin Desar2School of Water Resources and Hydropower Engineering, Wuhan University, Bayi road No. 299, Wuchang district in Wuhan of Hubei, ChinaChina Three Gorges University, Daxue road No. 8, Xiling district in Yichang of Hubei, ChinaChina Three Gorges University, Daxue road No. 8, Xiling district in Yichang of Hubei, ChinaEarly warning and forecast have always been the key points for landslide research because the disaster caused by landslide leads to enormous life and property loss. This article applies the transformed degradation results of rock to rock mass to calculate the stability and failure mode changes of landslide over time, and to guide engineering through experiment based on hydro-fluctuation belt water-rock interaction of Three Gorges Reservoir area. The results showed that until the rock mass degrades to a certain extent, the sliding zone export gets rise, the slip plane moves to surface, the back edge crack surface gets down, and the sliding mass gradually narrows down. As the ability of hydro-fluctuation belt to resist upper rock mass load reduces, the hydro-fluctuation belt collapses at the first, and then causes the back edge crack resulting in huge amount of rock mass slip. The contribution of each parameter in different stratum to landslide stability is studied through sensitivity analysis. Based on this, the comprehensive strength parameter can be evaluated and calculated combined with continuous deterioration of hydro-fluctuation belt. The comprehensive strength parameter can reflect comprehensive disaster resist capacity of landslide. The research results provide a reference for actual project, and the research methods provide a new way for landslide early warning and forecast.https://hrcak.srce.hr/file/257891comprehensive strengthdeteriorating rulefailure modereservoir bank slopestability analysiswater-rock interaction
collection DOAJ
language English
format Article
sources DOAJ
author Liang-Peng Wan
Mei-Ling Zhou
Subin Desar
spellingShingle Liang-Peng Wan
Mei-Ling Zhou
Subin Desar
Long-term stability calculation of reservoir bank slope considering water-rock interaction
Tehnički Vjesnik
comprehensive strength
deteriorating rule
failure mode
reservoir bank slope
stability analysis
water-rock interaction
author_facet Liang-Peng Wan
Mei-Ling Zhou
Subin Desar
author_sort Liang-Peng Wan
title Long-term stability calculation of reservoir bank slope considering water-rock interaction
title_short Long-term stability calculation of reservoir bank slope considering water-rock interaction
title_full Long-term stability calculation of reservoir bank slope considering water-rock interaction
title_fullStr Long-term stability calculation of reservoir bank slope considering water-rock interaction
title_full_unstemmed Long-term stability calculation of reservoir bank slope considering water-rock interaction
title_sort long-term stability calculation of reservoir bank slope considering water-rock interaction
publisher Faculty of Mechanical Engineering in Slavonski Brod, Faculty of Electrical Engineering in Osijek, Faculty of Civil Engineering in Osijek
series Tehnički Vjesnik
issn 1330-3651
1848-6339
publishDate 2017-01-01
description Early warning and forecast have always been the key points for landslide research because the disaster caused by landslide leads to enormous life and property loss. This article applies the transformed degradation results of rock to rock mass to calculate the stability and failure mode changes of landslide over time, and to guide engineering through experiment based on hydro-fluctuation belt water-rock interaction of Three Gorges Reservoir area. The results showed that until the rock mass degrades to a certain extent, the sliding zone export gets rise, the slip plane moves to surface, the back edge crack surface gets down, and the sliding mass gradually narrows down. As the ability of hydro-fluctuation belt to resist upper rock mass load reduces, the hydro-fluctuation belt collapses at the first, and then causes the back edge crack resulting in huge amount of rock mass slip. The contribution of each parameter in different stratum to landslide stability is studied through sensitivity analysis. Based on this, the comprehensive strength parameter can be evaluated and calculated combined with continuous deterioration of hydro-fluctuation belt. The comprehensive strength parameter can reflect comprehensive disaster resist capacity of landslide. The research results provide a reference for actual project, and the research methods provide a new way for landslide early warning and forecast.
topic comprehensive strength
deteriorating rule
failure mode
reservoir bank slope
stability analysis
water-rock interaction
url https://hrcak.srce.hr/file/257891
work_keys_str_mv AT liangpengwan longtermstabilitycalculationofreservoirbankslopeconsideringwaterrockinteraction
AT meilingzhou longtermstabilitycalculationofreservoirbankslopeconsideringwaterrockinteraction
AT subindesar longtermstabilitycalculationofreservoirbankslopeconsideringwaterrockinteraction
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