Multifractal for structural planes in rock mass of dam site area of Yujianhe Reservoir, Guiyang
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Multifractal for structural planes in rock mass of dam site area of Yujianhe Reservoir, Guiyang
Vol. 27, Issue 7期 刊出日, (2006)
作者机构:
中国地质大学 工程学院,武汉 430074,2.中国地质大学 计算机学院,武汉,430074
作者简介:
基金信息:
DOI:
CLC:TU452
Online First:19 November 2013,
Published:2006
稿件说明:
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WANG Hong-xing, WANG Guan, TANG Hui-ming, et al. Multifractal for structural planes in rock mass of dam site area of Yujianhe Reservoir, Guiyang[J]. 2006, 27(7期 刊出日).
DOI:
WANG Hong-xing, WANG Guan, TANG Hui-ming, et al. Multifractal for structural planes in rock mass of dam site area of Yujianhe Reservoir, Guiyang[J]. 2006, 27(7期 刊出日).DOI:
Multifractal for structural planes in rock mass of dam site area of Yujianhe Reservoir, Guiyang
The multifractal of the structural planes in rock mass of dam site area of the Yujianhe Reservoir in Guiyang
the capital Guizhou Province
is studied. The results of measurement and statistics of the structural planes in rock mass are applied to study multifractal. At first
multifractal for structural planes is studied using selected area in Area A. Different unit measure in different unit is selected to divide the studied area into squared unit mesh. And then
suitable different real number values are chosen
scale index is gotten using linear fitting method; their relation is obtained. Multifractal dimension
singular index and multifractal spectrum values are obtained using related formulae. Finally
multifractal dimension values
singular index and multifractal spectra values in other areas are obtained using the same method and contrasted. Its results show that the maximum values and average values of multifractal dimensions
singular indexes and multifractal spectra values are in Area A greatest in all selected areas. It shows that the structural planes in rock mass of Area A are complex and inhomogeneous; its engineering property and quality of rock mass are poorer. And the order of arrangement in good and poor quality is given according to the results of multifractal.