A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock

To investigate the brittle creep failure process of rock material, the time-dependent properties of brittle rocks under the impact of homogeneity are analyzed by the numerical simulation method, RFPA-Creep (2D). Deformation is more palpable for more homogeneous rock material under the uniaxial creep...

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Autores principales: Hao-Zhe Chen, Zhu-Shan Shao, Dong-Dong Jin, Zhe Zhang, Dong-Bo Zhou
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Lenguaje:EN
Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:7d0db000013c48aab56d4bedfc729c012021-11-25T18:13:51ZA Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock10.3390/ma142268181996-1944https://doaj.org/article/7d0db000013c48aab56d4bedfc729c012021-11-01T00:00:00Zhttps://www.mdpi.com/1996-1944/14/22/6818https://doaj.org/toc/1996-1944To investigate the brittle creep failure process of rock material, the time-dependent properties of brittle rocks under the impact of homogeneity are analyzed by the numerical simulation method, RFPA-Creep (2D). Deformation is more palpable for more homogeneous rock material under the uniaxial creep loading condition. At a low stress level, diffusion creep may occur and transition to dislocation creep with increasing applied stress. The law for increasing creep strain with the homogeneity index under a constant confined condition is similar to the uniaxial case, and dislocation creep tends to happen with increasing confining pressure for the same homogeneity index. The dilatancy index reaches its maximum at a high stress level when rock approaches failure, and the evolution of the dilatancy index with the homogeneity index under the same confining pressure is similar to the uniaxial case and is more marked than that under the unconfined condition. Both uniaxial and triaxial creep failure originate from the ductile damage accumulation inside rock. The dominant shear-type failure is exhibited by uniaxial creep and the conventional compression case presents the splitting-based failure mode. Under confining pressure, the creep failure pattern is prone to shear, which is more notable for the rock with higher homogeneity.Hao-Zhe ChenZhu-Shan ShaoDong-Dong JinZhe ZhangDong-Bo ZhouMDPI AGarticlecreephomogeneitystress levelsteady creep ratedilatancyfailure patternTechnologyTElectrical engineering. Electronics. Nuclear engineeringTK1-9971Engineering (General). Civil engineering (General)TA1-2040MicroscopyQH201-278.5Descriptive and experimental mechanicsQC120-168.85ENMaterials, Vol 14, Iss 6818, p 6818 (2021)
institution DOAJ
collection DOAJ
language EN
topic creep
homogeneity
stress level
steady creep rate
dilatancy
failure pattern
Technology
T
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
Engineering (General). Civil engineering (General)
TA1-2040
Microscopy
QH201-278.5
Descriptive and experimental mechanics
QC120-168.85
spellingShingle creep
homogeneity
stress level
steady creep rate
dilatancy
failure pattern
Technology
T
Electrical engineering. Electronics. Nuclear engineering
TK1-9971
Engineering (General). Civil engineering (General)
TA1-2040
Microscopy
QH201-278.5
Descriptive and experimental mechanics
QC120-168.85
Hao-Zhe Chen
Zhu-Shan Shao
Dong-Dong Jin
Zhe Zhang
Dong-Bo Zhou
A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
description To investigate the brittle creep failure process of rock material, the time-dependent properties of brittle rocks under the impact of homogeneity are analyzed by the numerical simulation method, RFPA-Creep (2D). Deformation is more palpable for more homogeneous rock material under the uniaxial creep loading condition. At a low stress level, diffusion creep may occur and transition to dislocation creep with increasing applied stress. The law for increasing creep strain with the homogeneity index under a constant confined condition is similar to the uniaxial case, and dislocation creep tends to happen with increasing confining pressure for the same homogeneity index. The dilatancy index reaches its maximum at a high stress level when rock approaches failure, and the evolution of the dilatancy index with the homogeneity index under the same confining pressure is similar to the uniaxial case and is more marked than that under the unconfined condition. Both uniaxial and triaxial creep failure originate from the ductile damage accumulation inside rock. The dominant shear-type failure is exhibited by uniaxial creep and the conventional compression case presents the splitting-based failure mode. Under confining pressure, the creep failure pattern is prone to shear, which is more notable for the rock with higher homogeneity.
format article
author Hao-Zhe Chen
Zhu-Shan Shao
Dong-Dong Jin
Zhe Zhang
Dong-Bo Zhou
author_facet Hao-Zhe Chen
Zhu-Shan Shao
Dong-Dong Jin
Zhe Zhang
Dong-Bo Zhou
author_sort Hao-Zhe Chen
title A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
title_short A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
title_full A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
title_fullStr A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
title_full_unstemmed A Numerical Investigation into the Effect of Homogeneity on the Time-Dependent Behavior of Brittle Rock
title_sort numerical investigation into the effect of homogeneity on the time-dependent behavior of brittle rock
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/7d0db000013c48aab56d4bedfc729c01
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