Land use and its adjustment may greatly affect soil detachment process by overland flow via
altering soil properties, root systems, and tillage operations, but few studies were performed …

The loess region of China is one of the most heavily eroded areas in the world. Soil
detachment capacity by rill flow (D c) is a key parameter for quantifying intensity of rill …

Land use has a significant effect on soil properties, and therefore on soil erodibility. In many
cases, land use controls soil erosion to a greater extent than does climate change or other …

Rill erosion is one of the most important types of soil erosion that has caused the destruction
of many lands in recent decades, and its management has become an essential issue in …

Permanent gullies are often initiated from rill erosion, followed by the formation of abrupt,
deep and wide gullies when topsoil and subsoil are carried away by fast-flowing surface …

Rill erosion is particularly intense after deforestation on hillslopes with steep and long
profiles. Since the rill detachment capacity (“D c”) shows a noticeable variability resulting …

The factors influencing soil erosion may vary with scale. It remains unclear whether the
spatial variation in soil erosion resistance is controlled by regional variables (eg …

Rill erosion plays an important role in the amount of soil detachment and the transport
sediment load on hillslope. Quantification of the soil erosion requires a more precise …

Although several scientists have recently studied overland flow detachment, the
methodology of measurement has not yet been properly discussed. This study compares …

Vegetation restoration significantly affected root traits during farmland abandonment,
thereby considerably altering the soil detachment process. However, few studies have …