Fractal Analysis of Permeability of Unsaturated Fractured Rocks

被引:2
|
作者
Jiang, Guoping [1 ]
Shi, Wei [2 ]
Huang, Lili [2 ]
机构
[1] Guangzhou Univ, Earthquake Engn Res Test Ctr, Guangzhou 510405, Guangdong, Peoples R China
[2] Ningbo Polytech, Ningbo 315800, Zhejiang, Peoples R China
来源
关键词
POROUS-MEDIA; HEAT-TRANSFER; MODEL; GEOMETRY;
D O I
10.1155/2013/490320
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A physical conceptual model for water retention in fractured rocks is derived while taking into account the effect of pore size distribution and tortuosity of capillaries. The formula of calculating relative hydraulic conductivity of fractured rock is given based on fractal theory. It is an issue to choose an appropriate capillary pressure-saturation curve in the research of unsaturated fractured mass. The geometric pattern of the fracture bulk is described based on the fractal distribution of tortuosity. The resulting water content expression is then used to estimate the unsaturated hydraulic conductivity of the fractured medium based on the well-known model of Burdine. It is found that for large enough ranges of fracture apertures the new constitutive model converges to the empirical Brooks-Corey model.
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页数:5
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