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	The spatio-temporal invariability of sediment concentration and the flow-sediment relationship for hilly areas of the Chinese Loess Plateau
	Zheng, Mingguo[1]; Qin, Fen[2]; Yang, Jishang[3]; Cai, Qiangguo[4]
刊名	CATENA
	2013
卷号	109页码:164-176
关键词	Scale Hyperconcentrated flow Sediment yield Soil erosion Model
ISSN号	0341-8162
DOI	http://dx.doi.org/10.1016/j.catena.2013.03.017
URL标识	查看原文
收录类别	SCI(E)
WOS记录号	WOS:000321729400017
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/5245230
专题	河南大学
作者单位	1.[1]Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China. 2.[2]Henan Univ, Coll Environm & Planning, Kaifeng 475001, Peoples R China. 3.[3]YRCC, Yellow River Inst Hydraul Res, Zhengzhou 450003, Peoples R China. 4.[4]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	Zheng, Mingguo[1],Qin, Fen[2],Yang, Jishang[3],et al. The spatio-temporal invariability of sediment concentration and the flow-sediment relationship for hilly areas of the Chinese Loess Plateau[J]. CATENA,2013,109:164-176.
APA	Zheng, Mingguo[1],Qin, Fen[2],Yang, Jishang[3],&Cai, Qiangguo[4].(2013).The spatio-temporal invariability of sediment concentration and the flow-sediment relationship for hilly areas of the Chinese Loess Plateau.CATENA,109,164-176.
MLA	Zheng, Mingguo[1],et al."The spatio-temporal invariability of sediment concentration and the flow-sediment relationship for hilly areas of the Chinese Loess Plateau".CATENA 109(2013):164-176.

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