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	The Spatio-temporal Invariability of Sediment Concentration and the Flow-Sediment Relationship for Hilly Areas of the Chinese Loess Plateau
	Mingguo ZHENG[1]; Fen QIN[2]; Jishang YANG[3]; Qiangguo CAI[4]
	2014
会议名称	The 6th International Symposium on Larger Asian River(第六届亚洲大河国际学术会议)
会议日期	2014-05-09
关键词	Scale Hyperconcentrated flow Sediment yield Soil erosion Model
页码	163-163
URL标识	查看原文
内容类型	会议论文
URI标识	http://www.corc.org.cn/handle/1471x/5230068
专题	河南大学
作者单位	1.[1]Key Laboratory of Water Cycle and Related Land Surface Processes,Institute of Geographic Sciences & 2.Natural Resources Research,Chinese Academic of Sciences,Beijing 100101,China[2]College of Environment and Planning,Henan University,Kaifeng 475001,China[3]Yellow River Institute of Hydraulic Research,YRCC,Zhengzhou 450003,China[4]Key Laboratory of Water Cycle and Related Land Surface Processes,Institute of Geographic Sciences & 3.Natural Resources Research,Chinese Academic of Sciences,Beijing 100101,China
推荐引用方式 GB/T 7714	Mingguo ZHENG[1],Fen QIN[2],Jishang YANG[3],et al. The Spatio-temporal Invariability of Sediment Concentration and the Flow-Sediment Relationship for Hilly Areas of the Chinese Loess Plateau[C]. 见:The 6th International Symposium on Larger Asian River(第六届亚洲大河国际学术会议). 2014-05-09.

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