Estimation of cracked soil’s representative elementary volume based on fractal dimension
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Estimation of cracked soil’s representative elementary volume based on fractal dimension
Vol. 34, Issue 10, (2013)
作者机构:
1. 河海大学 岩土力学与堤坝工程教育部重点实验室,南京,210098
2. 河海大学 隧道与城市轨道工程研究所,南京,210098
3. 欧领特钢板桩(中国)有限公司,上海,200122
作者简介:
基金信息:
DOI:
CLC:TU43
Online First:18 October 2013,
Published:2013
稿件说明:
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WANG Yuan, FENG Di, CHEN Shang-xing, et al. Estimation of cracked soil’s representative elementary volume based on fractal dimension[J]. 2013, 34(10).
DOI:
WANG Yuan, FENG Di, CHEN Shang-xing, et al. Estimation of cracked soil’s representative elementary volume based on fractal dimension[J]. 2013, 34(10).DOI:
Estimation of cracked soil’s representative elementary volume based on fractal dimension
Natural soil may be cracked due to wetting–drying cycles
shearing or other effects. Most cracks tend to be connected and form a network. A crack network on a natural soil surface is a random and disordered system. It is hard to describe the distribution characteristics of cracks by the traditional statistical method. Generally
the crack network has fractal dimension. The theory of fractal dimension can be used to describe the distribution characteristics of cracks. Crack images are taken by a digital camera on a soil surface and converted to gray images. A method for determining fractal dimension by photograph is established based on the fractal theory. Then
the fractal dimension of soil cracks can be obtained. According to the physical meaning of representative elementary volume (REV)
a method for estimating the cracked soil’s REV based on the fractal dimension is presented; and some examples are analyzed. The results show that the fractal dimensions are increased with the increasing of crack density
crack aperture and the development of secondary crack. The REV is related to the homogeneity of crack density and crack aperture. It is easy and credible to estimate the cracked soil’s REV by the method mentioned above.