Soil erosion by water is a result of detachment of particles or small aggregates from the soil
surface followed by transport of the detached material. One of the elements that affects …

Tillage-induced microtopography may affect hydrological and erosion processes.
Nevertheless, how the tillage practices affect hydrological-sediment connectivity at the plot …

Seepage is the prominent hydrological process on tilled hillslopes covered by purple soil,
which can easily exacerbate slope instability and soil loss. Laboratory simulated …

Tillage practices change microtopography and hydrological process, which significantly
affects soil erosion. The objective of this study is understanding storm-driven …

Soil erosion is a multi-scale geographical interface process with high spatiotemporal
variability. This study aimed to assess runoff and sediment dynamics under different …

The tilled slopes in the loess region are characterized by artificial management practices
that result in variations in microtopography, which serve as both the site of water erosion and …

Soil surface microtopography plays a significant role in rill erosion. In addition, upslope
inflow has a large effect on downslope soil erosion processes. Experiments including four …

Soil development and erosion are important and opposing processes in the evolution of
high-mountainous landscapes, though their dynamics are not fully understood. We …

Surface roughness and slope gradient are two important factors influencing soil erosion. The
objective of this study was to investigate the interaction of surface roughness and slope …

Soil surface roughness (SSR) modifies interactions and feedback processes between
terrestrial and atmospheric systems driven by both the abiotic and biotic components of …