Shear fracture (Mode II) of brittle rock

被引:235
|
作者
Rao, QH [1 ]
Sun, ZQ
Stephansson, O
Li, CL
Stillborg, B
机构
[1] Cent S Univ, Coll Resource Environm & Civil Engn, Changsha 410083, Peoples R China
[2] Royal Inst Technol, S-10044 Stockholm, Sweden
[3] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany
[4] Lulea Univ Technol, Div Rock Mech, S-97187 Lulea, Sweden
关键词
shear fracture; fracture criterion; fracture toughness; scale effect; finite element method; rock;
D O I
10.1016/S1365-1609(03)00003-0
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Mode II fracture initiation and propagation plays an important role under certain loading conditions in rock fracture mechanics. Under pure tensile, pure shear, tension- and compression-shear loading, the maximum Mode I stress intensity factor, K-Iax, always larger than the maximum Mode II stress intensity factor, K-IImax. For brittle materials. Mode I fracture toughness. K-IC, is usually smaller than Mode II fracture toughness, K-IIC. Therefore, K-Imax reaches K-IC before K-IImax reaches K-IIC, which inevitably leads to Mode I fracture. Due to inexistence of Mode II fracture under pure shear, tension- and compression-shear loading, classical mixed mode fracture criteria can only predict Mode I fracture but not Mode II fracture. A new mixed mode fracture criterion has been established for predicting Mode I or Mode II fracture of brittle materials. It is based on the examination of Mode I and Mode II stress intensity factors on the arbitrary plane theta, K-I(theta) and K-II(theta), varying with 0(-180degrees less than or equal to 0 less than or equal to + 180degrees), no matter what kind of loading condition is applied. Mode I fracture occurs when (K-IImax/K-Imax) < 1 or 1 < (K-IImax/K-Imax) < (K-IIC/K-IC) and K-Imax = K-IC at theta(IC). Mode II fracture occurs when (K-IImax/K-Imax) > (K-IIC/K-IC) and K-IImax = K-IIC at theta(IIC). The validity of the new criterion is demonstrated by experimental results of shear-box testing. Shear-box test of cubic specimen is a potential method for determining Mode II fracture toughness K-IIC of rock since it can create a favorable condition for Mode II fracutre, i.e, K-IImax is always 2-3 times larger than K-Imax and reaches K-IIC before K-Imax reaches K-IC. The size effect on K-IIC for single- and double-notched specimens has been studied for different specimen thickness B, dimensionless notch length a/W (or 2a/W) and notch inclination angle x. The test results show that K-IIC decreases as B increases and becomes a constant when B is equal to or larger than W for both the single- and double-notched specimens. When a/W (or 2a/W) increases, K-IIC decreases and approaches a limit. The x has a minor effect on K-IIC when x is within 65-75degrees. Specimen dimensions for obtaining a reliable and reproducible value of K-IIC under shear-box testing are presented. Numerical results demonstrate that under the shear-box loading condition, tensile stress around the notch tip can be effectively restrained by the compressive loading. At peak load, the maximum normal stress is smaller than the tensile strenght of rock, while the maximum shear stress is larger than the shear strenght in the presence of compressive stress, which results in shear failure. (C) 2003 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:355 / 375
页数:21
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