Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China

Two important features of the high slopes at Gushui Hydropower Station are layered accumulations (rock-soil aggregate) and multilevel toppling failures of plate rock masses; the Gendakan slope is selected for case study in this paper. Geological processes of the layered accumulation of rock and soil...

Full description

Bibliographic Details
Main Authors: Jia-wen Zhou, Chong Shi, Fu-gang Xu
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2013/540636
id doaj-74b690052944491aaf3363128eee0989
record_format Article
spelling doaj-74b690052944491aaf3363128eee09892020-11-24T21:28:38ZengHindawi LimitedThe Scientific World Journal1537-744X2013-01-01201310.1155/2013/540636540636Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest ChinaJia-wen Zhou0Chong Shi1Fu-gang Xu2State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu, Sichuan 610065, ChinaResearch Institute of Geotechnical Engineering, Hohai University, Nanjing, Jiangsu 210098, ChinaState Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu, Sichuan 610065, ChinaTwo important features of the high slopes at Gushui Hydropower Station are layered accumulations (rock-soil aggregate) and multilevel toppling failures of plate rock masses; the Gendakan slope is selected for case study in this paper. Geological processes of the layered accumulation of rock and soil particles are carried out by the movement of water flow; the main reasons for the toppling failure of plate rock masses are the increasing weight of the upper rock-soil aggregate and mountain erosion by river water. Indoor triaxial compression test results show that, the cohesion and friction angle of the rock-soil aggregate decreased with the increasing water content; the cohesion and the friction angle for natural rock-soil aggregate are 57.7 kPa and 31.3° and 26.1 kPa and 29.1° for saturated rock-soil aggregate, respectively. The deformation and failure mechanism of the rock-soil aggregate slope is a progressive process, and local landslides will occur step by step. Three-dimensional limit equilibrium analysis results show that the minimum safety factor of Gendakan slope is 0.953 when the rock-soil aggregate is saturated, and small scale of landslide will happen at the lower slope.http://dx.doi.org/10.1155/2013/540636
collection DOAJ
language English
format Article
sources DOAJ
author Jia-wen Zhou
Chong Shi
Fu-gang Xu
spellingShingle Jia-wen Zhou
Chong Shi
Fu-gang Xu
Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
The Scientific World Journal
author_facet Jia-wen Zhou
Chong Shi
Fu-gang Xu
author_sort Jia-wen Zhou
title Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
title_short Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
title_full Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
title_fullStr Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
title_full_unstemmed Geotechnical Characteristics and Stability Analysis of Rock-Soil Aggregate Slope at the Gushui Hydropower Station, Southwest China
title_sort geotechnical characteristics and stability analysis of rock-soil aggregate slope at the gushui hydropower station, southwest china
publisher Hindawi Limited
series The Scientific World Journal
issn 1537-744X
publishDate 2013-01-01
description Two important features of the high slopes at Gushui Hydropower Station are layered accumulations (rock-soil aggregate) and multilevel toppling failures of plate rock masses; the Gendakan slope is selected for case study in this paper. Geological processes of the layered accumulation of rock and soil particles are carried out by the movement of water flow; the main reasons for the toppling failure of plate rock masses are the increasing weight of the upper rock-soil aggregate and mountain erosion by river water. Indoor triaxial compression test results show that, the cohesion and friction angle of the rock-soil aggregate decreased with the increasing water content; the cohesion and the friction angle for natural rock-soil aggregate are 57.7 kPa and 31.3° and 26.1 kPa and 29.1° for saturated rock-soil aggregate, respectively. The deformation and failure mechanism of the rock-soil aggregate slope is a progressive process, and local landslides will occur step by step. Three-dimensional limit equilibrium analysis results show that the minimum safety factor of Gendakan slope is 0.953 when the rock-soil aggregate is saturated, and small scale of landslide will happen at the lower slope.
url http://dx.doi.org/10.1155/2013/540636
work_keys_str_mv AT jiawenzhou geotechnicalcharacteristicsandstabilityanalysisofrocksoilaggregateslopeatthegushuihydropowerstationsouthwestchina
AT chongshi geotechnicalcharacteristicsandstabilityanalysisofrocksoilaggregateslopeatthegushuihydropowerstationsouthwestchina
AT fugangxu geotechnicalcharacteristicsandstabilityanalysisofrocksoilaggregateslopeatthegushuihydropowerstationsouthwestchina
_version_ 1725969344372932608