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摘要:
Slope gradient is one of the critically important factors which drive the erosional response of microtopographic surfaces. This study investigates the effect of slope gradient on the evolution of erosion under accumulative rainfall in laboratory experiments and calculates critical slope values that help evaluate land suitability for farming and similar purposes. Dynamics of accumulative runoff, accumulated sediment and their rates in each erosion stage are studied when the slope gradient varies. The critical slope value for the microtopographic surface was calculated according to the relationship between the sediment yield and slope gradient. The amount of eroded soil downhill in each erosion stage was calculated using DEM data of point cloud. Results show that 1) a steeper slope would increase cumulative runoff;2) cumulative sediment increases rapidly initially and then stabilizes with the increase of slope;3) the critical slope value for the whole erosion is determined as 10°. The findings of the dynamics of interrill erosion and sediment characteristics are useful information for future research of erosion prediction and conservation of soil and water in the Chinese Loess Plateau.
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篇名 Effect of Slope Gradient on Erosion Evolution Process at Microtopographic Tillage Soil Surfaces
来源期刊 地理信息系统(英文) 学科 农学
关键词 Critical SLOPE VALUES CUMULATIVE RUNOFF CUMULATIVE Sediment Interrill EROSION Rate of EROSION
年,卷(期) 2019,(5) 所属期刊栏目
研究方向 页码范围 481-492
页数 12页 分类号 S15
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研究主题发展历程
节点文献
Critical
SLOPE
VALUES
CUMULATIVE
RUNOFF
CUMULATIVE
Sediment
Interrill
EROSION
Rate
of
EROSION
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地理信息系统(英文)
半月刊
2151-1950
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
143
总下载数(次)
0
总被引数(次)
0
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