Capturing pressure- and rate-dependent behaviour of rocks using a new damage-plasticity model

被引:23
作者
Mukherjee, Mousumi [1 ]
Nguyen, Giang D. [1 ]
Mir, Arash [1 ]
Bui, Ha H. [2 ]
Shen, Luming [3 ]
El-Zein, Abbas [3 ]
Maggi, Federico [3 ]
机构
[1] Univ Adelaide, Sch Civil Environm & Min Engn, Adelaide, SA, Australia
[2] Monash Univ, Dept Civil Engn, Clayton, Vic, Australia
[3] Univ Sydney, Sch Civil Engn, Sydney, NSW, Australia
基金
澳大利亚研究理事会;
关键词
Constitutive models; Rocks; Geomaterials; Pressure-dependent; Rate-dependent; Strain rate; Damage; Plasticity; Brittle; Ductile; BRITTLE-DUCTILE TRANSITION; TRIAXIAL COMPRESSION TESTS; STRAIN-RATE; UNIAXIAL COMPRESSION; LOADING RATE; POROUS ROCK; GRANITE; STRENGTH; FAILURE; FRICTION;
D O I
10.1016/j.ijimpeng.2017.01.006
中图分类号
TH [机械、仪表工业];
学科分类号
0802 ;
摘要
Rock response to confining pressure and strain rate can change dramatically from very brittle to ductile. Capturing this transition is crucial for a correct prediction of rock mass failure due to blasting, explosion or drilling in mining. In this work, a new constitutive model that accounts for the effects of both confining pressure and strain rate on the nominal strength and post peak behaviour is proposed for dry intact rocks and other similar geological materials. The key features of the proposed constitutive model are the employment of a single loading function that evolves from initial yielding to ultimate failure during damaging and the rate-dependent enhancement so that the strain rate effects can be faithfully described at different confining pressures. The model can adequately capture both the brittle and ductile responses as well as the brittle-ductile transition as a result of both strain rate and confining pressure. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:208 / 218
页数:11
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