1) sediment coming from the sea
海向来沙
1.
The paper analyzes and calculates the sediment coming from the sea by utilizing the observed hydrological and tidal data of the Yellow River estuary.
利用黄河口实测水文及潮汐资料分析计算了海向来沙情况。
2) sediment coming from land
陆向来沙
3) coastal transverse ridge
海岸横向沙脊
1.
On the typical coastal transverse ridge at Changli Gold Coast in Hebei Province,which is one of the most typical coastal Aeolian distribution regions in China and famous for the tall and typical coastal transverse ridges.
观测结果表明,海岸横向沙脊表面的风沙流结构特征基本表现为0~40 cm高程内气流搬运的沙尘物质浓度或质量随高度递减并符合指数分布,20~60 cm高程内符合幂函数分布,40~60 cm高程内输沙量与高度之间则为多项式函数关系。
4) incoming sediment
来沙
1.
The downstream sedimentation index induced by incoming sediment from the middle reaches of the Yellow River,the area rich in sediment and coarse sand,and the source area dominated by coarse sand are analyzed by using profile method.
利用输沙量平衡法分析了黄河中游6站来水来沙对库区及下游的淤积作用,利用断面法分析了黄河中游、多沙粗沙区和粗泥沙集中来源区来沙对下游的淤积指标。
5) runoff and sediment load
来水来沙
1.
Response of the bank-full discharge to runoff and sediment load in the Lower Weihe River;
渭河下游平滩流量变化对来水来沙的响应
2.
Based on two phases(1987?2002)vector data about wetland in lower Yellow River basin and runoff and sediment load data,we reconstructed the former landscape structure and elucidated the changes in landscape patterns during the last 20 years,and discussed the feedback to the runoff and sediment load.
利用黄河下游利津、泺口和花园口1950-2005年水沙数据、1987年和2002年两期下游滩地、河流和坑塘湿地数据,运用景观生态学基本理论,分析黄河下游湿地景观格局的演变,讨论湿地时空变化对来水来沙的反馈效应。
6) water & sediment load
来水来沙
1.
This article studies the characteristics of the water & sediment load from 1960 to 1997 and the longitudinal & transversal bed profile from 1977 to 2002 by employing statistic analysis.
近年来,黄河下游来水来沙出现一些新的特点,水沙的变化必然影响下游河床纵剖面和横断面的调整变化。
补充资料：向来
①副词。一向；从来：向来如此｜向来心直口快｜向来不吸烟。②原来：失向来之烟霞。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条