Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification

The effect of temperature and pressure, which play important roles in the mechanical properties of rocks during deep energy exploitation, has not been sufficiently studied in the previous rock creep models. In order to investigate thermal effect in creep models, a modified Nishihara rheological mode...

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Main Authors: Xingang Wang, Qiangbing Huang, Baoqin Lian, Nina Liu, Jun Zhang
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Materials Science and Engineering
Online Access:http://dx.doi.org/10.1155/2018/4947561
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spelling doaj-65a35e843358441a97b82b314f05e0462020-11-24T20:49:10ZengHindawi LimitedAdvances in Materials Science and Engineering1687-84341687-84422018-01-01201810.1155/2018/49475614947561Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental VerificationXingang Wang0Qiangbing Huang1Baoqin Lian2Nina Liu3Jun Zhang4Key Laboratory of Western China’s Mineral Resource and Geological Engineering of Ministry of Education, School of Geology Engineering and Surveying, Chang’an University, Xi’an 710054, ChinaKey Laboratory of Western China’s Mineral Resource and Geological Engineering of Ministry of Education, School of Geology Engineering and Surveying, Chang’an University, Xi’an 710054, ChinaKey Laboratory of Western China’s Mineral Resource and Geological Engineering of Ministry of Education, School of Geology Engineering and Surveying, Chang’an University, Xi’an 710054, ChinaKey Laboratory of Western China’s Mineral Resource and Geological Engineering of Ministry of Education, School of Geology Engineering and Surveying, Chang’an University, Xi’an 710054, ChinaKey Laboratory of Mine Geological Hazards Mechanism and Control, Shaanxi Institute of Geo-Environment Monitoring, Xi’an 710054, ChinaThe effect of temperature and pressure, which play important roles in the mechanical properties of rocks during deep energy exploitation, has not been sufficiently studied in the previous rock creep models. In order to investigate thermal effect in creep models, a modified Nishihara rheological model, taking into account the coupled effect of thermal damage and stress, was proposed by combining the theoretical formula for thermal damage of rocks with the modified Nishihara model. The improved model introduces a nonlinear viscous dashpot, which can accurately describe the accelerated rheological phase of rocks. To verify the proposed model, a triaxial rheological experiment was conducted on sandstone subjected to thermal damage (600°C). In addition, the stress-strain curves within whole creep process of the rheological experiment were analyzed. Furthermore, the theoretical curves of the modified Nishihara rheological model were compared with the experimental results. Results showed that the theoretical curves relatively agree well with the experimental data, suggesting that the proposed new model is more preferred to describing the rheological curve of sandstone subjected to thermal damage at different rheological stages, in particular, it is capable of depicting the accelerated rheological stage of the sandstone, providing a good ability to describe the creep behavior of rocks under thermal-mechanical coupling.http://dx.doi.org/10.1155/2018/4947561
collection DOAJ
language English
format Article
sources DOAJ
author Xingang Wang
Qiangbing Huang
Baoqin Lian
Nina Liu
Jun Zhang
spellingShingle Xingang Wang
Qiangbing Huang
Baoqin Lian
Nina Liu
Jun Zhang
Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
Advances in Materials Science and Engineering
author_facet Xingang Wang
Qiangbing Huang
Baoqin Lian
Nina Liu
Jun Zhang
author_sort Xingang Wang
title Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
title_short Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
title_full Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
title_fullStr Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
title_full_unstemmed Modified Nishihara Rheological Model considering the Effect of Thermal-Mechanical Coupling and Its Experimental Verification
title_sort modified nishihara rheological model considering the effect of thermal-mechanical coupling and its experimental verification
publisher Hindawi Limited
series Advances in Materials Science and Engineering
issn 1687-8434
1687-8442
publishDate 2018-01-01
description The effect of temperature and pressure, which play important roles in the mechanical properties of rocks during deep energy exploitation, has not been sufficiently studied in the previous rock creep models. In order to investigate thermal effect in creep models, a modified Nishihara rheological model, taking into account the coupled effect of thermal damage and stress, was proposed by combining the theoretical formula for thermal damage of rocks with the modified Nishihara model. The improved model introduces a nonlinear viscous dashpot, which can accurately describe the accelerated rheological phase of rocks. To verify the proposed model, a triaxial rheological experiment was conducted on sandstone subjected to thermal damage (600°C). In addition, the stress-strain curves within whole creep process of the rheological experiment were analyzed. Furthermore, the theoretical curves of the modified Nishihara rheological model were compared with the experimental results. Results showed that the theoretical curves relatively agree well with the experimental data, suggesting that the proposed new model is more preferred to describing the rheological curve of sandstone subjected to thermal damage at different rheological stages, in particular, it is capable of depicting the accelerated rheological stage of the sandstone, providing a good ability to describe the creep behavior of rocks under thermal-mechanical coupling.
url http://dx.doi.org/10.1155/2018/4947561
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