SELF-AFFINE ROUGHENING IN A MODEL EXPERIMENT ON EROSION IN GEOMORPHOLOGY

被引：15

作者：

CZIROK, A ^{[1
]}

SOMFAI, E ^{[1
]}

VICSEK, T ^{[1
]}

机构：

[1] INST TECH PHYS, H-1325 BUDAPEST, HUNGARY

来源：

PHYSICA A-STATISTICAL MECHANICS AND ITS APPLICATIONS | 1994年 / 205卷 / 1-3期

关键词：

D O I：

10.1016/0378-4371(94)90513-4

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

The basic mechanisms producing rough surfaces during geomorphological evolution are studied by carrying out model experiments and analyzing the results in terms of fractal scaling. We have been able to find an experimental evidence for kinetic roughening in our micromodel of mountain ranges. We have observed that during the watering of an initially smooth ridge made of a mixture of granular materials, the surface evolves into a shape analogous to actual mountain profiles with self-affine geometry. For the exponents describing respectively the spatial and the temporal scaling of the surface width, alpha = 0.78 +/- 0.05 and beta almost-equal-to 0.9 have been obtained. Our value for the static exponent alpha is in very good agreement with several earlier results for various mountains and we have calculated the estimate alpha = 0.8 +/- 0.1 for a set of genuine transect profiles taken in the Dolomites, Italy. The results are interpreted in terms of ''landslides'' of widely scattered magnitudes.

引用

页码：355 / 366

页数：12

共 20 条

[11]

Mandelbrot B. B., 1982, FRACTAL GEOMETRY NAT, P1

[12]

MATSUSHITA M, 1989, PHYSICA D, V38, P247

[13] VARIATIONS IN GEOMETRIC MEASURES OF TOPOGRAPHIC SURFACES UNDERLAIN BY FRACTURED GRANITIC PLUTONS [J].