三峡水库消落带泥沙和土壤的可蚀性空间分布及差异
Abstract
目的为探究三峡水库消落带沉积泥沙与原地土壤间的可蚀性空间分布及差异。方法以三峡水库土质消落带为研究对象,分别采集沉积泥沙和原地土壤样品,测试颗粒组成和总有机碳含量,计算颗粒组成的体积维数(Dv)、结构稳定性指数(SSI)和可蚀性因子(K),分析可蚀性的空间分异及类别间的差异。结果1)三峡水库消落带沉积泥沙的SSI和K的平均值分别为26.26%和0.046 65(t·hm2·h)/(MJ·mm·hm2),均显著高于原地土壤的15.06%和0.045 90(t·hm2·h)/(MJ·mm·hm2)(p
Fields of Study & Subjects
Soil erosion and sediment transport
Hydrology and Sediment Transport Processes
Environmental and Agricultural Sciences
Publication details
- Journal / source
- DOAJ (DOAJ: Directory of Open Access Journals)
- Publication date
- 1 February 2026
- Language
- ZH