The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China

Rainfall and reservoir level fluctuation are two of the main factors contributing to reservoir landslides. However, in China’s Three Gorges Reservoir Area, when the reservoir water level fluctuates significantly, it comes at a time of abundant rainfall, which makes it difficult to distinguish which...

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Main Authors: Nenghao Zhao, Bin Hu, Qinglin Yi, Wenmin Yao, Chong Ma
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2017/3724867
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author Nenghao Zhao
Bin Hu
Qinglin Yi
Wenmin Yao
Chong Ma
author_facet Nenghao Zhao
Bin Hu
Qinglin Yi
Wenmin Yao
Chong Ma
author_sort Nenghao Zhao
collection DOAJ
description Rainfall and reservoir level fluctuation are two of the main factors contributing to reservoir landslides. However, in China’s Three Gorges Reservoir Area, when the reservoir water level fluctuates significantly, it comes at a time of abundant rainfall, which makes it difficult to distinguish which factor dominates the deformation of the landslide. This study focuses on how rainfall and reservoir water level decline affect the seepage and displacement field of Baijiabao landslide spatially and temporally during drawdown of reservoir water level in the Three Gorges Reservoir Area, thus exploring its movement mechanism. The monitoring data of the landslide in the past 10 years were analyzed, and the correlation between rainfall, reservoir water level decline, and landslide displacement was clarified. By the numerical simulation method, the deformation evolution mechanism of this landslide during drawdown of reservoir water level was revealed, respectively, under three conditions, namely, rainfall, reservoir water level decline, and coupling of the above two conditions. The results showed that the deformation of the Baijiabao landslide was the coupling effect of rainfall and reservoir water level decline, while the latter effect is more pronounced.
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institution Kabale University
issn 1468-8115
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language English
publishDate 2017-01-01
publisher Wiley
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series Geofluids
spelling doaj-art-070688ab1f3f4342910db8274de2a56c2025-02-03T06:00:10ZengWileyGeofluids1468-81151468-81232017-01-01201710.1155/2017/37248673724867The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, ChinaNenghao Zhao0Bin Hu1Qinglin Yi2Wenmin Yao3Chong Ma4Engineering Faculty, China University of Geosciences, Wuhan 430074, ChinaEngineering Faculty, China University of Geosciences, Wuhan 430074, ChinaCivil Engineering & Architecture Faculty, China Three Gorges University, Yichang 443002, ChinaEngineering Faculty, China University of Geosciences, Wuhan 430074, ChinaEngineering Faculty, China University of Geosciences, Wuhan 430074, ChinaRainfall and reservoir level fluctuation are two of the main factors contributing to reservoir landslides. However, in China’s Three Gorges Reservoir Area, when the reservoir water level fluctuates significantly, it comes at a time of abundant rainfall, which makes it difficult to distinguish which factor dominates the deformation of the landslide. This study focuses on how rainfall and reservoir water level decline affect the seepage and displacement field of Baijiabao landslide spatially and temporally during drawdown of reservoir water level in the Three Gorges Reservoir Area, thus exploring its movement mechanism. The monitoring data of the landslide in the past 10 years were analyzed, and the correlation between rainfall, reservoir water level decline, and landslide displacement was clarified. By the numerical simulation method, the deformation evolution mechanism of this landslide during drawdown of reservoir water level was revealed, respectively, under three conditions, namely, rainfall, reservoir water level decline, and coupling of the above two conditions. The results showed that the deformation of the Baijiabao landslide was the coupling effect of rainfall and reservoir water level decline, while the latter effect is more pronounced.http://dx.doi.org/10.1155/2017/3724867
spellingShingle Nenghao Zhao
Bin Hu
Qinglin Yi
Wenmin Yao
Chong Ma
The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
Geofluids
title The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
title_full The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
title_fullStr The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
title_full_unstemmed The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
title_short The Coupling Effect of Rainfall and Reservoir Water Level Decline on the Baijiabao Landslide in the Three Gorges Reservoir Area, China
title_sort coupling effect of rainfall and reservoir water level decline on the baijiabao landslide in the three gorges reservoir area china
url http://dx.doi.org/10.1155/2017/3724867
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