首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Slow Crack Propagation and Slip Correlations
Authors:J Schmittbuhl  A Delaplace  K J Måløy  H Perfettini  J P Vilotte
Institution:Laboratoire de Géologie, UMR 8538, Ecole Normale Supérieure, Paris, France. E-mail: Jean.Schmittbuhl@ens.fr, FR
Laboratoire de Mécanique et Technologie, Ecole Normale Supérieure, Cachan, France., FR
Fysisk Institutt, Universitetet i Oslo, Oslo, Norway., NO
Laboratoire de Géophysique Interne et Tectonophysique, Grenoble, France., FR
Département de Sismologie, UMR 7580, Institut de Physique du Globe, Paris, France., FR
Abstract:— The propagation of an interfacial crack through a weak plane of a transparent Plexiglas block is studied experimentally. The toughness is controlled artificially by a sand blasting procedure, and fluctuates locally in space like uncorrelated random noise. The block is fractured in mode I at low speed (10?7?10?4 m/s). The crack front is observed optically with a microscope and a high resolution digital camera. During the propagation, the front is pinned by micro-regions of high toughness and becomes rough. Roughness of the crack front is analyzed in terms of self-affinity. The in-plane roughness exponent is shown to be 0.63±0.05. Experimental results are compared to a numerical model. The model reproduces the self-affine behavior of the crack front, i.e., long-range correlations of the roughness. Analogies between mode I and mode III are presented in order to discuss implications of the experimental results for creeping faults. Accordingly, correlations of the slip pattern are shown to exist over scales substantially larger than the asperity sizes.
Keywords:
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号