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| 3D CREEP CONSTITUTIVE EQUATION OF MODIFIED NISHIHARA MODEL AND ITS PARAMETERS IDENTIFICATION |
| QI Yajing1,JIANG Qinghui1,2,WANG Zhijian3,ZHOU Chuangbing1,2 |
| (1. State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan,Hubei 430072,China;2. School of Civil and Architectural Engineering,Wuhan University,Wuhan,Hubei 430072,China;3. Key Laboratory of Geological Hazards on Three Gorges Reservoir Area,Ministry of Education,China Three Gorges University,Yichang,Hubei 443002,China) |
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Abstract The classical Nishihara model is composed of the Hooke body,viscoelastic body and viscoplastic body,which can hardly describe the rheological feature of nonlinear accelerating creep of rocks. By connecting a nonlinear viscous dashpot with a strain trigger and the classical Nishihara model in series,a modified Nishihara model is obtained and a 3D creep constitutive equation for rocks under constant stress is deduced. Through fitting with a rheological curve from experiments on red sandstones from Wanzhou in the Three Gorges reservoir area,parameters of the modified Nishihara model are derived. Comparison between the actual experimental data and the fitting curve of the modified Nishihara model shows that not only an adequate reflection of primary and steady creep stages,but also a well depiction of accelerating creep stage can be obtained. Accelerating creep is a key stage for landslides forecast. So success of the modified Nishihara model in representing this stage contributes greatly to landslide forecasting.
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Received: 22 April 2011
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