| Citation: | Wang Jing, Xu Yadong, Lin Xiao, Peng Shaoyong, Shi Yuanrun, Zhu Yunhai. Analysis on difference of erosion capacity and river capture prediction in the head of the Xiangjiang tributary constrainted by surface and deep geological information[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 234-240. doi: 10.19509/j.cnki.dzkq.2022.0127
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Based on the comprehensive method of basic surface geological investigation, GIS watershed analysis and deep geophysical analysis, the difference in retrogressive erosion along the Xiangjiang tributary is compared. Two drainage areas in the head of the Xiangjiang tributary, the Chengjiang and Zhujiang Rivers, are selected as subjects with the same source of erosion at Aitang Village. Under comparison with topography, water level elevation, lithology of bedrock strata, tectonic setting and deep geophysical data, the Zhujiang River has greater erosion ability and stronger headward erosion, with easily eroded bedrock and well-developed joints. It is predicted that river capture could occur around Aitang village. The evolution trend may lead to a decrease in water volume of Liyu town in the lower reaches of the Chengjiang River, which will affect urban domestic water and industrial and agricultural production. In addition, the continuous strengthening of retrogressive erosion can cause downcutting erosion of the Cretaceous red layer and the watershed will present a more spectacular Danxia landscape.
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