土壤结构侵蚀是水侵蚀的初始阶段和前期形式。结构侵蚀是指在微观水流作用下土壤团粒间的联结遭受破坏,土壤侵析而产生的土壤侵蚀过程。土壤淤化的结果导致土块蛰陷,土层密实,干燥后形成地表板结。这一过程并无可见的土壤流失现象,仅为土壤的结构侵蚀,尚属水侵蚀过程的初始阶段。雨滴的溅蚀是引起和加速土壤团粒破坏的主要原因。降雨雨滴具有相当大的动能,它不仅破坏团粘结构,而且使土层密实。溅蚀作用的大小取决于降 Soil erosion is the initial stage of water erosion and early form. Structural erosion refers to the process of soil erosion caused by the destruction of the links between soil aggregates and the soil erosion under the action of micro-flow. As a result of siltation of soil lead to soil block stubborn, dense soil, forming the surface after drying knot. There is no visible phenomenon of soil erosion in this process, which is only the structural erosion of the soil, which is still the initial stage of the water erosion process. Splashing of raindrops is the main reason for causing and accelerating the destruction of soil aggregates. Rainfall has a considerable kinetic energy, it not only destroy the sticky structure, but also make the soil dense. The size of splashing depends on the drop