A soil erosion model including interrill erosion and rill erosion was developed for hillslope. The rainfall and slope characteristics affecting soil erosion on hillslopes was analyzed by simulation. The results show that the slope length and gradient, rainfall intensity and process have varying influence on runoff and soil erosion. The unit discharge of runoff and erosion rate increases with increases in the rainfall intensity and the slope length. The same precipitation but with different rainfall processes may cause different runoff and erosion results. The effect of the slope gradient on runoff and soil erosion can be both positive and negative. There exists a critical slope gradient for runoff and soil erosion
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
Runoff generation and soil loss from slopes have been studied for decades, but the relationships amo...
Abstract In order to discuss the effect of rainfall patterns and land use types on soil erosion, the...
The variation of soil erosion across scales remains a controversial issue. A theoretical framework, ...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
To date interrill erosion processes are not fully understood under different rainfall and soil condi...
The prediction and estimate of soil erosion is fundamental important for understanding the effect of...
The degree and length of the slope are two essential features of topography in relation to runoff an...
Characteristics of soil erosion change along a long slope in the gentle hilly areas in black soil re...
Rill formation is the predominant erosion process in slope land in the Loess Plateau, China. This st...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
Runoff generation and soil loss from slopes have been studied for decades, but the relationships amo...
Abstract In order to discuss the effect of rainfall patterns and land use types on soil erosion, the...
The variation of soil erosion across scales remains a controversial issue. A theoretical framework, ...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
International audienceThe influence of slope gradient on erosion rate differs for rill and interrill...
To date interrill erosion processes are not fully understood under different rainfall and soil condi...
The prediction and estimate of soil erosion is fundamental important for understanding the effect of...
The degree and length of the slope are two essential features of topography in relation to runoff an...
Characteristics of soil erosion change along a long slope in the gentle hilly areas in black soil re...
Rill formation is the predominant erosion process in slope land in the Loess Plateau, China. This st...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...
International audienceNumerical simulation experiments of water erosion at the local scale (20 × 5 m...