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1)  Receive the tide and wash the silt
纳潮冲淤
2)  Rising and fall of tide
洪冲潮淤
3)  scouring and desilting
冲淤减淤
4)  scour and silting
冲淤
1.
Based on the one dimensional sediment mathematical model,sediment scour and silting in the lower Yellow River after Xiaolangdi reservoir operation are researched;therein the change law of scour and silting in the river reach of Aishan to Lijin is analyzed emphatically.
运用一维泥沙数学模型 ,对小浪底水库运行后黄河下游河道泥沙冲淤进行模拟研究 ,其中着重分析艾山~利津河段的冲淤变化规律 作者认为小浪底水库可使黄河下游总体上保持 2 0年不淤 ,5 0年内相对减淤率为 5 1 6% ;艾山~利津河段也有减淤效果 ,但相对减淤率仅为全下游平均值的 5 7% ,河床抬升速度仍然较
2.
The study results of the reactive effect of the Yellow River delta changes on its estuarine course and the delta development model are introduced, the emphasis is placed on the factors affecting the Yellow River delta formation and the evolution process of scour and silting, and it is confirmed that the numerical computational method, remote sensing and GIS .
重点评述了黄河三角洲的形成影响因素和冲淤演变过程,肯定了数值计算方法和遥感与GIS技术已经成为定量计算与半定量分析黄河三角洲冲淤演变的重要研究手段。
5)  scouring and silting
冲淤
1.
Then,the scouring and silting characteristics of debris flow and their af- fecting factors including debris flow scale and local channel.
通过实际测量,分析了泥石流在沟道内冲淤特征以及影响泥石流冲淤特征的因素,如泥石流活动规模和局部沟道条件等。
2.
The changes of scouring and silting of the Yellow River Delta is complicated and speedy, and it clearly lies on the changes of the coastline.
黄河三角洲地区冲淤演变复杂快速,最明显的表现是该地区海岸线的淤进蚀退。
6)  erosion and deposition
冲淤
1.
Effect of the implementation of the first-stage project of the deepwater channel regulation in the Yangtze River Estuary on the erosion and deposition in the South Passage;
长江口深水航道治理一期工程实施对南槽冲淤演变的影响
2.
Analysis on erosion and deposition evolution of the lower Yellow River;
黄河下游河道冲淤演变的分析
3.
From the law of the digging load in Fengqiwo river,it is concluded that the critical discharge of gravel bed-load in Neijiang river is 200m~3/s;the digging action in this river section has no direct effect on the relationship of flow depth and discharge;the erosion and deposition of river bed at Wotie section are mainly in.
本文分析了凤栖窝河段淘淤的规律性,得出:内江河段卵石的临界起动流量为200m3/s;凤栖窝淘淤对该河段的水位流量关系没有直接的影响;卧铁断面平均河床高程的冲淤变化主要受内江流量和河段内卵石运动的影响,淘淤的持续效应不长;内江流量大于400m3/s或涨水过程中以冲刷为主,而在流量小于400m3/s或降水过程中则以淤积为主;外江闸和飞沙堰闸的运行是凤栖窝长期不淘淤的前提条件。
补充资料:迎潮送潮辞·送潮
【诗文】:
潮西来兮又东下,日染中流兮红洒洒。汀葭苍兮屿蓼枯,
风骚牢兮愁烟孤。大几望兮微将晦翳,睨瀛溶兮敛然而退。
爱长波兮数数,一幅巾兮无缨可濯。帆生尘兮楫有衣,
怅潮之还兮吾犹未归。



【注释】:



【出处】:
全唐诗:卷621-22
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