Effect of seasonal freeze-thaw on soil anti-scouribility and its related physical property in hilly Loess Plateau

Seasonal freeze-thaw plays a significant role in soil properties as well as the management of soil and water resources in northern latitudes. Soil erodibility primarily relies on soil anti-scouribility (AS) in the concentrated flow erosion zones of the Loess Plateau. An understanding of the characteristics of freeze-thaw soil is essential for erosion essence in the seasonal freeze-thaw area. The primary goal of this study was to evaluate the differences in soil AS and its related freeze-thaw-induced soil physical properties, as well as root density before and after a cycle of freeze-thaw.