Applications of fractal geometry and renormalization group to the Italian seismic activity

被引:18
作者
Carpinteri, A [1 ]
Chiaia, B [1 ]
Invernizzi, S [1 ]
机构
[1] Politecn Torino, Dept Struct Engn & Geotech, I-10129 Turin, Italy
基金
美国国家科学基金会;
关键词
D O I
10.1016/S0960-0779(02)00081-4
中图分类号
O1 [数学];
学科分类号
0701 ; 070101 ;
摘要
In the past two decades, Fractal Geometry developed as a new and powerful mathematical tool able to model a wide class of complex natural systems. Particularly, when joined with renormalization techniques, Fractal Geometry represents the natural and synthetic way to characterize the so-called self-organized processes, emphasizing their universality and the scaling laws arising at the critical points. Nevertheless, the choice of the most relevant seismic parameter is often not trivial, as in the case of Italian seismicity, where magnitude must be replaced by the seismic energy release, in order to obtain unambiguous multiftactal spectra. Moreover, to model the stick-slip phenomenon, it is useful to consider the contact mechanics of self-affine rough faults. A numerical model provides the exact distribution of normal and tangential forces at any rough surface. The Renormalization Group technique represents the theoretical framework able to explain the multifractal distribution of contact micro-forces obtained numerically. As a consequence, the experimentally detected multiftactal release of seismic energy derives directly from the mechanical work of a multiftactal distribution of forces during the slip event. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:917 / 928
页数:12
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