Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions

The instability process of bedding rock slope with weak interlayer may be induced under rainfall infiltration conditions. Due to this, we conducted a research of model test for the instability process, based on the similarity theory. With use of the recent 50 years’ rainfall data of Changsha, China,...

Full description

Bibliographic Details
Main Authors: Zhongming He, Baolin Wang
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2018/8201031
id doaj-c2a5001660d64ef4971099c0b6395308
record_format Article
spelling doaj-c2a5001660d64ef4971099c0b63953082020-11-24T21:27:36ZengHindawi LimitedAdvances in Civil Engineering1687-80861687-80942018-01-01201810.1155/2018/82010318201031Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall ConditionsZhongming He0Baolin Wang1Key Laboratory of Special Environment Road Engineering of Hunan Province, Changsha University of Science and Technology, Changsha 410114, ChinaSchool of Traffic and Transportation Engineering, Changsha University of Science and Technology, Changsha 410114, ChinaThe instability process of bedding rock slope with weak interlayer may be induced under rainfall infiltration conditions. Due to this, we conducted a research of model test for the instability process, based on the similarity theory. With use of the recent 50 years’ rainfall data of Changsha, China, we analyzed the seepage characteristics, mechanical characteristics, and deformation laws of the slope under the conditions of long-time heavy rain and short-time rainstorm, respectively. The test results show that the original seepage characteristics of the slope were changed by the existence of weak interlayer, presented the “double seepage” effect, resulted in the seepage characteristics of rock and soil in the shallow layer and weak interlayer of the slope showed a sickle “Γ” distribution, and the adjacent rock layer presented a curve-type “S” distribution. With the increase of rainfall duration, the weak interlayer gradually became muddy and softened, and then the plastic flow zone was formed locally. The stress concentration phenomenon was gradually generated in the weak interlayer due to the influence of the gravitational field of the upper rock mass. The large infiltration of rainwater led to the phenomenon of plastic flow extrusion of the slope at the weak interlayer extrusion. With the further penetration of the tensile cracks in the upper part of the weak interlayer, the slope had a large settlement displacement and gradually formed sliding shear deformation along the weak structural plane. Under the condition of equal rainfall amount, the condition of long-time heavy rain has a greater influence on the stability of the bedding rock slope with weak interlayer than that of short-time rainstorm. The failure form of slope could be divided into four stages: prechange stage, interlayer extrusion stage, slip-pull-fracture stage and plastic flow-shear failure stage.http://dx.doi.org/10.1155/2018/8201031
collection DOAJ
language English
format Article
sources DOAJ
author Zhongming He
Baolin Wang
spellingShingle Zhongming He
Baolin Wang
Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
Advances in Civil Engineering
author_facet Zhongming He
Baolin Wang
author_sort Zhongming He
title Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
title_short Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
title_full Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
title_fullStr Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
title_full_unstemmed Instability Process Model Test for Bedding Rock Slope with Weak Interlayer under Different Rainfall Conditions
title_sort instability process model test for bedding rock slope with weak interlayer under different rainfall conditions
publisher Hindawi Limited
series Advances in Civil Engineering
issn 1687-8086
1687-8094
publishDate 2018-01-01
description The instability process of bedding rock slope with weak interlayer may be induced under rainfall infiltration conditions. Due to this, we conducted a research of model test for the instability process, based on the similarity theory. With use of the recent 50 years’ rainfall data of Changsha, China, we analyzed the seepage characteristics, mechanical characteristics, and deformation laws of the slope under the conditions of long-time heavy rain and short-time rainstorm, respectively. The test results show that the original seepage characteristics of the slope were changed by the existence of weak interlayer, presented the “double seepage” effect, resulted in the seepage characteristics of rock and soil in the shallow layer and weak interlayer of the slope showed a sickle “Γ” distribution, and the adjacent rock layer presented a curve-type “S” distribution. With the increase of rainfall duration, the weak interlayer gradually became muddy and softened, and then the plastic flow zone was formed locally. The stress concentration phenomenon was gradually generated in the weak interlayer due to the influence of the gravitational field of the upper rock mass. The large infiltration of rainwater led to the phenomenon of plastic flow extrusion of the slope at the weak interlayer extrusion. With the further penetration of the tensile cracks in the upper part of the weak interlayer, the slope had a large settlement displacement and gradually formed sliding shear deformation along the weak structural plane. Under the condition of equal rainfall amount, the condition of long-time heavy rain has a greater influence on the stability of the bedding rock slope with weak interlayer than that of short-time rainstorm. The failure form of slope could be divided into four stages: prechange stage, interlayer extrusion stage, slip-pull-fracture stage and plastic flow-shear failure stage.
url http://dx.doi.org/10.1155/2018/8201031
work_keys_str_mv AT zhongminghe instabilityprocessmodeltestforbeddingrockslopewithweakinterlayerunderdifferentrainfallconditions
AT baolinwang instabilityprocessmodeltestforbeddingrockslopewithweakinterlayerunderdifferentrainfallconditions
_version_ 1725974654412128256