Scale invariance and stratification: The unified multifractal model of hydraulic conductivity

被引：4
|
作者：
Tchiguirinskaia, I [1 ]
机构：
[1] Clemson Univ, Dept Environm Sci & Engn, Anderson, SC 29625 USA
来源：
FRACTALS-COMPLEX GEOMETRY PATTERNS AND SCALING IN NATURE AND SOCIETY | 2002年 / 10卷 / 03期
关键词：
hydraulic conductivity; heterogeneity; stratification; scaling; multifractals;
D O I：
10.1142/S0218348X02001373
中图分类号：
O1 [数学];
学科分类号：
0701 ; 070101 ;
摘要：
A fairly large body of observational evidence shows that the hydraulic conductivity is an extremely heterogeneous physical phenomenon that exhibits wide variability over a broad range of horizontal and vertical scales. Stochastic multifractals that result from continuous dynamic cascades are suggested as an appropriate model to capture the scale-invariance and stratification of the Columbus site hydraulic conductivity. Then, observed interrelations between estimates of multifractal parameters, those characterize vertical and horizontal scaling regimes, are interpreted by the unified multifractal model.
引用
收藏
页码：329 / 334
页数：6
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