马天辉

个人信息Personal Information

副研究员

博士生导师

硕士生导师

性别:男

毕业院校:东北大学

学位:博士

所在单位:土木工程系

学科:岩土工程

办公地点:土木4#楼330

联系方式:QQ: 19928600 wechat: tianhuima

电子邮箱:tianhuima@dlut.edu.cn

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出版著作和论文

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Numerical test investigation on unloading rockburst processes

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论文类型:期刊论文

发表时间:2011-05-01

发表刊物:Yanshilixue Yu Gongcheng Xuebao/Chinese Journal of Rock Mechanics and Engineering

收录刊物:EI、PKU、ISTIC、Scopus

卷号:30

期号:SUPPL. 1

页面范围:3120-3128

ISSN号:10006915

摘要:In order to explore the mechanism of rockburst induced by unloading, the process of instability failure under unloading is exhibited by rock failure process analysis software (RFPA2D). Taking the example of basic mechanical parameters of the granite, firstly, the two-dimensional numerical test of uniaxial loading failure for the square numerical specimen is simulated; and then, for the same specimen, the surrounding rock unloading test under the condition of bidirectional load is simulated. The numerical test results show that: (1) There is a large differences on the rock failure mechanisms and failure modes between the uniaxial loading test and unloading instability test. (2) The progressive microcracks propagation is dominant in failure process of uniaxial loading test; and the microcracks concentrate on the local fracture plane. Before the main fractures induced, Acoustic emission (AE) phenomenon which is the omen of many microruptures appears; and it is the typical rockburst mode of instability induced by the progressive failure. (3) The brittle characteristic during the rock unloading failure in the biaxial test under confining pressure is more evident. The unloading failure is mainly released by sudden, high energy density. At the same time, it shows intense dilatation failure characteristics along the unloading direction; and the failure mode is large-area shear fracture combined with local tension fracture. On the contrary to the uniaxial loading, there is nearly no omen of any microfracture before the main fracture; and it is the typical failure mode of transient rockburst.