作者: E. Bouchaud , S. Navéos
DOI: 10.1051/JP1:1995150
关键词: Geometry 、 Trie 、 Physics 、 Quasistatic process 、 Crack velocity 、 Fracture (geology) 、 Crossover
摘要: Four fracture profiles corresponding to four diOEere1~t crack velocities are studied on trie same sample and show existence of a crossover lengthscale ( decreasmg with the velocity. For lengthscales larger thon (, previously reported roughl~ess index ct 0.84 is recovered. At smaller than profile lits quasi-static (QS) hypothesis, 1-e-, measured roughness close (~s CI 0.45. It now clearly established that surfaces can be considered as self-affine objects. After pioneering work Mandelbrot et ai. (l), many experiments using various experi-