Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures

In order to investigate the influence of temperature, confining pressure, and preexisting fissure on creep characteristics of rock mass, multistage creep experiments were performed on shale-like material, with preexisting fissure under different temperatures and confining pressures. The results show...

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Main Authors: Yongyan Wang, Hongwei Wang, Xiao Shi
Format: Article
Language:English
Published: Hindawi Limited 2019-01-01
Series:Advances in Civil Engineering
Online Access:http://dx.doi.org/10.1155/2019/7861305
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spelling doaj-1734d2976ca2444aae583888a9fadfa82020-11-25T02:01:11ZengHindawi LimitedAdvances in Civil Engineering1687-80861687-80942019-01-01201910.1155/2019/78613057861305Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining PressuresYongyan Wang0Hongwei Wang1Xiao Shi2Qingdao University of Science and Technology, Qingdao 266061, ChinaQingdao University of Science and Technology, Qingdao 266061, ChinaQingdao University of Science and Technology, Qingdao 266061, ChinaIn order to investigate the influence of temperature, confining pressure, and preexisting fissure on creep characteristics of rock mass, multistage creep experiments were performed on shale-like material, with preexisting fissure under different temperatures and confining pressures. The results showed that new microcracks generated and propagated with the increase of temperature in both uniaxial and triaxial creep experiments, and the generation and propagation were most pronounced at 60°C and least at 20∼50°C in uniaxial creep experiments. The generation and propagation were restricted by confining pressure. Temperature had less influence on the creep strain rate in triaxial creep experiment, whereas it had a significant influence on the steady-state creep rate in uniaxial creep experiment. The influence of confining pressure on the steady-state creep rate was slight when confining pressure was 1 MPa, whereas it was obvious when confining pressure was 3∼7 MPa. The closure of preexisting fissure promoted the creep strain rate, and the closure was incomplete when confining pressure was below 3 MPa, whereas it was complete when confining pressure at 5 and 7 MPa.http://dx.doi.org/10.1155/2019/7861305
collection DOAJ
language English
format Article
sources DOAJ
author Yongyan Wang
Hongwei Wang
Xiao Shi
spellingShingle Yongyan Wang
Hongwei Wang
Xiao Shi
Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
Advances in Civil Engineering
author_facet Yongyan Wang
Hongwei Wang
Xiao Shi
author_sort Yongyan Wang
title Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
title_short Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
title_full Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
title_fullStr Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
title_full_unstemmed Creep Investigation on Shale-Like Material with Preexisting Fissure under Coupling Temperatures and Confining Pressures
title_sort creep investigation on shale-like material with preexisting fissure under coupling temperatures and confining pressures
publisher Hindawi Limited
series Advances in Civil Engineering
issn 1687-8086
1687-8094
publishDate 2019-01-01
description In order to investigate the influence of temperature, confining pressure, and preexisting fissure on creep characteristics of rock mass, multistage creep experiments were performed on shale-like material, with preexisting fissure under different temperatures and confining pressures. The results showed that new microcracks generated and propagated with the increase of temperature in both uniaxial and triaxial creep experiments, and the generation and propagation were most pronounced at 60°C and least at 20∼50°C in uniaxial creep experiments. The generation and propagation were restricted by confining pressure. Temperature had less influence on the creep strain rate in triaxial creep experiment, whereas it had a significant influence on the steady-state creep rate in uniaxial creep experiment. The influence of confining pressure on the steady-state creep rate was slight when confining pressure was 1 MPa, whereas it was obvious when confining pressure was 3∼7 MPa. The closure of preexisting fissure promoted the creep strain rate, and the closure was incomplete when confining pressure was below 3 MPa, whereas it was complete when confining pressure at 5 and 7 MPa.
url http://dx.doi.org/10.1155/2019/7861305
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AT hongweiwang creepinvestigationonshalelikematerialwithpreexistingfissureundercouplingtemperaturesandconfiningpressures
AT xiaoshi creepinvestigationonshalelikematerialwithpreexistingfissureundercouplingtemperaturesandconfiningpressures
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