摘要
通过对桃汛试验前后两个时段对比分析,认为桃汛试验没有增加万家寨库区淤积;库区淤积形态有所调整,淤积三角洲向坝前推进,库尾段平均河底高程没有抬升。
Through the analysis of the data before and after the spring flood experiment,the results indicated that spring flood experiment did not increase deposition in the reservoir,but changed the deposition patterns,pushed the delta downstream,without resulting in the rising of the river bed within the backwater zone.
出处
《泥沙研究》
CSCD
北大核心
2011年第6期22-26,共5页
Journal of Sediment Research
基金
国家重点基础研究发展计划资助(2011CB403303)
中央级公益性科研院所科研业务费专项(HKY-JBYW-2010-09)
关键词
桃汛试验
冲淤
万家寨水库
潼关高程
spring flood experiment
erosion and deposition
Yellow River
Wanjiazhai Reservoir
Tongguan elevation
