Can crack front waves explain the roughness of cracks?

被引:93
作者
Bouchaud, E
Bouchaud, JP [1 ]
Fisher, DS
Ramanathan, S
Rice, JR
机构
[1] Ctr Etud Saclay, Serv Phys Etat Condense, F-91191 Gif Sur Yvette, France
[2] Ctr Etud Saclay, Serv Phys & Chim Surfaces & Interfaces, F-91191 Gif Sur Yvette, France
[3] Harvard Univ, Dept Phys, Lyman Lab, Cambridge, MA 02138 USA
[4] Harvard Univ, Div Engn & Appl Sci, Cambridge, MA 02138 USA
[5] Bell Labs, Lucent Technol, Murray Hill, NJ 07974 USA
[6] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
基金
美国国家科学基金会;
关键词
dynamic fracture; surface roughness; crack branching and bifurcation; fractography;
D O I
10.1016/S0022-5096(01)00137-5
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We review recent theoretical progress on the dynamics of brittle crack fronts and its relationship to the roughness of fracture surfaces. We discuss the possibility that the small scale roughness of cracks, which is characterized by a roughness exponent similar or equal to0.5, could be caused by the generation, during local instabilities by depinning, of diffusively broadened corrugation waves, which have recently been observed to propagate elastically along moving crack fronts. We find that the theory agrees plausibly with the orders of magnitude observed. Various consequences and limitations, as well as alternative explanations, are discussed. We argue that another mechanism, possibly related to damage cavity coalescence, is needed to account for the observed large scale roughness of cracks that is characterized by a roughness exponent similar or equal to0.8. (C) 2002 Published by Elsevier Science Ltd.
引用
收藏
页码:1703 / 1725
页数:23
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