Study on Correlation of Erosion and Deposition Change and Water and Sediment Condition in the Lower Yellow River in Non-flood Season

被引：0

作者：

Lin Xiuzhi ^{[1
,2
]}

Jing Xin'ai ^{[1
,2
]}

Qu Shaojun ^{[1
,2
]}

Liu Chenyu ^{[3
]}

机构：

[1] YRCC, Yellow River Inst Hydraul Res, Zhengzhou 450003, Peoples R China

[2] MWR, Key Lab Yellow River Sediment Res, Zhengzhou 450003, Peoples R China

[3] China Railway Tunnel Grp Co Ltd, Luoyang 471009, Peoples R China

来源：

PROCEEDINGS OF THE 4TH INTERNATIONAL YELLOW RIVER FORUM ON ECOLOGICAL CIVILIZATION AND RIVER ETHICS, VOL V | 2010年

关键词：

non - flood season; condition of water and sediment; change of erosion and deposition; the lower Yellow River;

D O I：

暂无

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

Because of lower sediment concentration flow, the river channel of the lower Yellow River presents an erosion state in non - flood season, but the changes of erosion and deposition are different in different reaches. It is eroded at upstream of Gaocun, basically in equilibrium of erosion and deposition in the reach from Gaocun to Aishan, and deposits at downstream of Aishan. By analyzing the correlations of deposition ratio of different reaches and incoming water and sediment in non - flood season, the change of erosion and deposition in the reaches from Huayuankou to Gaocun and Gaocun to Aishan is not only affected by the incoming water volume, but also by the upstream erosion and deposition as well as sediment concentration renewed. The change of erosion and deposition in the reach from Aishan to Lijin is mainly affected by the upstream erosion/deposition as well as sediment concentration renewed.

引用

页码：165 / +

页数：2

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