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一种新的岩石流变模型
引用本文:邓荣贵,周德培,张倬元,付小敏. 一种新的岩石流变模型[J]. 岩石力学与工程学报, 2001, 20(6): 780-784
作者姓名:邓荣贵  周德培  张倬元  付小敏
作者单位:1. 西南交通大学岩土工程系,
2. 成都理工学院土木工程系,
基金项目:国家自然科学基金资助项目(49202040).
摘    要:根据岩石加速蠕变阶段的力学特性,提出了一种非牛顿流体粘滞阻尼元件,将该阻尼元件与描述岩石减速蠕变和等速蠕变特性的传统模型结合,构成了新的综合流变力学模型,并应用于描述某大型水电工程坝区断层岩蠕变特性,效果良好。

关 键 词:岩石流变模型 断层 岩石 减速蠕变 等速蠕变特性
文章编号:1000-6915(2001)06-0780-05
收稿时间:2000-01-11
修稿时间:2000-01-11

A NEW RHEOLOGICAL MODEL FOR ROCKS
DengRonggui,ZhouDepei,ZhangZhuoyuan,FuXiaomin. A NEW RHEOLOGICAL MODEL FOR ROCKS[J]. Chinese Journal of Rock Mechanics and Engineering, 2001, 20(6): 780-784
Authors:DengRonggui  ZhouDepei  ZhangZhuoyuan  FuXiaomin
Abstract:Rheological deformation is a basic mechanical property of rock. All rocks have acceleration creep property. Conventional rheologic models can't study accelerated creep property but deceleration creep and equal velocity creep properties of rock. A new rheological multiple model is put forward to study accelerated creep of rock, based on rheological properties of rock. The new rheological multiple model can contain the properties of many conventional rheological models. The good results are obtained when it is applied to analyze creep testing data of fault rock from the dam site of a large hydro-power station on Yalong River of China.
Keywords:rheological model of rock   creep properties of fault rock   creep
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