Development law of soil cracks in karst peak-cluster depressions under dry and wet alternations

In an experiment with alternating dry and wet conditions of soil in cultivated land, orchards and forest lands with limestone and dolomite in karst peak depression, combined with digital image processing technology, we investigated the development law of soil surface cracks under alternating dry and...

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Bibliographic Details
Published inYing yong sheng tai xue bao Vol. 34; no. 2; p. 387
Main Authors Luo, Shuyu, Deng, Yusong, Chen, Hongsong, Wang, Jinyue, Liao, Dalan
Format Journal Article
LanguageChinese
Published China 01.02.2023
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Summary:In an experiment with alternating dry and wet conditions of soil in cultivated land, orchards and forest lands with limestone and dolomite in karst peak depression, combined with digital image processing technology, we investigated the development law of soil surface cracks under alternating dry and wet condition. The results showed that with the alternation of wet and dry, the average width of cracks decreased at a fast-slow-slower rate, with an order of limestone > dolomite under the same land use, and orchard > cultivated land > forest soil under the same soil-forming parent rock. In the first four dry and wet alternations, the degrees of soil fragmentation and connectivity were higher in dolomite development than in limestone, with significant differences in fracture development rose diagrams. In the subsequent cycles, soil fragmentation of most samples increased, the difference dominated by parent rock gradually decreased, the crack development rose diagram converged, and the connectivity showed the patt
ISSN:1001-9332
DOI:10.13287/j.1001-9332.202302.018