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	Comparative study on rain splash erosion of representative soils in china
	Cheng Qinjuan1,2; Cai Qiangguo1; Ma Wenjun3
刊名	Chinese geographical science
	2008-06-01
卷号	18期号:2页码:155-161
关键词	Rain splash erosion Black soil Loess soil Red soil Purple soil Soil crust
ISSN号	1002-0063
DOI	10.1007/s11769-008-0155-9
通讯作者	Cai qiangguo(caiqg@igsnrr.ac.cn)
英文摘要	As the first event of soil erosion, rain splash erosion supplies materials for subsequent transportation and entrainment. the loess plateau, the southern hilly region and the northeast china are subject to serious soil and water loss; however, the characteristics of rain splash erosion in those regions are still unclear. the objectives of the study are to analyze the characteristics of splash erosion on loess soil, red soil, purple soil and black soil, and to discuss the relationship between splash erosion and soil properties. soil samples spatially distributed in the abovementioned regions were collected and underwent simulated rainfalls at a high intensity of 1.2mm/min, lasting for 5, 10, 15, and 20min, respectively. rain splash and soil crust development were analyzed. it shows that black soil sample from heilongjiang province corresponds to the minimum splash erosion amount because it has high aggregate content, aggregate stability and organic matter content. loess soil sample from inner mongolia corresponds to the maximum splash erosion amount because it has high content of sand particles. loess soil sample from shanxi province has relatively lower splash erosion amount because it has high silt particle content and low aggregate stability easily to be disrupted under rainfalls with high intensity. although aggregate contents of red soil and purple soil samples from hubei and guangdong provinces are high, the stability is weak and prone to be disrupted, so the splash erosion amount is medium. splash rate which fluctuates over time is observed because soil crust development follows a cycling processes of formation and disruption. in addition, there are two locations of soil crust development, one appears at the surface, and the other occurs at the subsurface.
WOS关键词	INFILTRATION ; MINERALOGY ; DETACHMENT ; RUNOFF
WOS研究方向	Environmental Sciences & Ecology
WOS类目	Environmental Sciences
语种	英语
出版者	SPRINGER
WOS记录号	WOS:000256419600007
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2390168
专题	中国科学院大学
通讯作者	Cai Qiangguo
作者单位	1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 2.Grad Univ, Chinese Acad Sci, Beijing 100049, Peoples R China 3.China Agr Univ, Coll Resources & Environm, Beijing 100094, Peoples R China
推荐引用方式 GB/T 7714	Cheng Qinjuan,Cai Qiangguo,Ma Wenjun. Comparative study on rain splash erosion of representative soils in china[J]. Chinese geographical science,2008,18(2):155-161.
APA	Cheng Qinjuan,Cai Qiangguo,&Ma Wenjun.(2008).Comparative study on rain splash erosion of representative soils in china.Chinese geographical science,18(2),155-161.
MLA	Cheng Qinjuan,et al."Comparative study on rain splash erosion of representative soils in china".Chinese geographical science 18.2(2008):155-161.

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