Surface morphology of soil cracks in Yuanmou Dry-hot Valley Region, Southwest China |
| |
Authors: | Donghong Xiong Yi Long Dongchun Yan Xiaoning Lu Zhonghua Ji Haidong Fang |
| |
Institution: | 1. Key Laboratory of Mountain Hazards and Surface Process, CAS, Chengdu, 610041, Sichuan, China 2. Institute of Mountain Hazards and Environment, CAS, Chengdu, 610041, Sichuan, China 3. Department of Environmental Engineering, Chengdu University of Information Technology, Chengdu, 610225, Sichuan, China 4. Institute for Tropical Eco-Agricultural Sciences, Yunnan Academy of Agriculture Sciences, Yuanmou, 651300, Yunnan, China
|
| |
Abstract: | Surface morphology of soil cracks is one of the important factors influencing the water evaporation rate in cracked soil in
Yuanmou Dry-hot Valley Region, Southwest China. Quantitative study of the complicated surface morphology of soil cracks is
a prerequisite for further studies of soil-cracking mechanisms. The present paper establishes a quantitative indicator system
by application of concepts and methods originating from Fractal Geometry and Network Analysis. These indicators can effectively
express the complicated features of soil-crack network structure. Furthermore, a series of values related to soil-crack morphology
was obtained by image processing on field photos of soil-crack quads, and gradation criteria for the degree of development
of soil cracks were determined. Finally, the changes in values of the morphological indicators under different degrees of
development were analyzed in detail. Our results indicate that (1) the degree of development of soil cracks can be divided
into five grades, i.e., feeble development, slight development, medium development, intensive development and extremely intensive
development; (2) the values of the indicators change predictably with increasing degree of development of soil cracks. The
area density (Dc) increases, and both the area-weighted mean ratio of crack area to perimeter (AWMARP), which reflects the
intensity of cracking, and the index r, which is related to the connectivity of a soil crack, grow uniformly (albeit with different forms). AWMRAP increases at
a geometric rate while r shows logarithmmic growth, indicating a gradual increase in the connectivity of a soil crack. Nevertheless, the area-weighted
mean of soil-crack fractal dimension (AWMFRAC) shows a decreasing trend, indicating a gradual decline in the complexity of
cracks as area density increases. |
| |
Keywords: | Soil crack Surface morphology Quantitative indicator Degree of development Southwest China |
本文献已被 维普 SpringerLink 等数据库收录! |
|