中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Effects of rill morphology characteristics on particle size selectivity using indoor simulation experiments with two types of soil from the Loess Plateau

文献类型:期刊论文

作者Sun, Liying2; Dai, Qingyuan2
刊名JOURNAL OF SOILS AND SEDIMENTS
出版日期2024-09-09
卷号N/A
关键词Rill erosion Rill morphology Particle selectivity Indoor rainfall experiment Particle size distribution
DOI10.1007/s11368-024-03895-7
产权排序1
文献子类Article ; Early Access
英文摘要Purpose The relations between rill morphology indicators and particle size selectivity by rainfall events were investigated, providing a new perspective on the mechanism of rill morphology indicators impacting on rill erosion processes. Materials and methods Indoor rainfall experiments were carried out with three-dimensional (3D) laser scanning technique for better monitoring the rill morphological indicators, using two types of soil collected from the north part and the south part of the Loess Plateau, respectively. Results and discussions The higher degree of headward erosion is occurred on loamy clay (LC) soil from the south part of the Loess Plateau with the higher total length (6.65 m) due to the higher clay content. Higher degree of side erosion is demonstrated on sandy loam (SL) soil from the north part of the Loess Plateau with the higher mean rill width (0.09 +/- 0.00 m) due to the higher sand content. The ratios of rill width to depth do not show significant differences on two types of soil with the average value greater than 1, indicating the relatively higher degree of side erosion than downward erosion on both soils. Silt fraction is selected with much higher efficiency than other fractions in two types of soil due to the dominant silt fractions in the primary soil. Rill width (W) is the most sensitive indicator to the particle size selectivity, as both the contents of clay, silt and fine particles and the enrichment ratio of silt show significantly (P < 0.05) positive correlations with W. While, the enrichment ratio of sand fraction shows significantly (P < 0.05) negative correlations with rill maximum depth and degree of contour line departure. Conclusions The differences of rill morphology indicators on two types of soil slope mainly depend on soil texture and the development processes of rills.
WOS关键词EROSION PROCESSES ; INTERRILL EROSION ; SLOPE GRADIENT ; RAINFALL INTENSITY ; WATER EROSION ; FLOW ; TRANSPORT ; ENRICHMENT ; IMPACTS ; CHINA
WOS研究方向Environmental Sciences & Ecology ; Agriculture
WOS记录号WOS:001309286500001
源URL[http://ir.igsnrr.ac.cn/handle/311030/207903]  
专题陆地水循环及地表过程院重点实验室_外文论文
通讯作者Sun, Liying
作者单位1.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Sun, Liying,Dai, Qingyuan. Effects of rill morphology characteristics on particle size selectivity using indoor simulation experiments with two types of soil from the Loess Plateau[J]. JOURNAL OF SOILS AND SEDIMENTS,2024,N/A.
APA Sun, Liying,&Dai, Qingyuan.(2024).Effects of rill morphology characteristics on particle size selectivity using indoor simulation experiments with two types of soil from the Loess Plateau.JOURNAL OF SOILS AND SEDIMENTS,N/A.
MLA Sun, Liying,et al."Effects of rill morphology characteristics on particle size selectivity using indoor simulation experiments with two types of soil from the Loess Plateau".JOURNAL OF SOILS AND SEDIMENTS N/A(2024).

入库方式: OAI收割

来源:地理科学与资源研究所

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