目的为研究母质类型和水温耦合作用对红壤崩解的影响。方法以亚热带丘陵区页岩、粉砂岩、泥质瘤状灰岩、泥质灰岩和第四纪红黏土发育的土壤为研究对象,对原状土壤进行室内崩解试验,分析不同水温条件下红壤的崩解特性,并结合土壤孔隙结构和黏土矿物组成,探究母质-水温耦合效应对红壤崩解的影响机制。结果水温是影响红壤崩解的关键环境因素,5~45 ℃条件下,水温升高显著增强红壤崩解性,其中泥质瘤状灰岩和第四纪红黏土发育的土壤崩解率分别增加13.70%、23.20%,主要与孔隙气体压力增大、胶结物溶解 ...
张育铜, 伍铁牛
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