1) sediment coming from land
陆向来沙
2) 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。
3) 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。
4) 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。
5) 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。
6) water and sediment inflow
来水来沙
1.
There are different sources for water flow and sediment in the upper Yellow River with uneven distribution of water and sediment inflows.
黄河上游来水来沙地区分布不均匀，水沙异源。
补充资料：沙陆墟
沙陆墟
江苏无锡人。1934年毕业于上海江南体育专科学校。1934年参加革命工作，历任无锡《人报》记者，《闽北日报》编辑，《南方日报》、《民主报》、《大江南报》及《江东日报》编辑部主任、总编辑、社长，上海大公滑稽剧团、百花滑稽剧团编导及艺委会主任，中国少数民族作家学会理事，无锡市文联艺术指导委员会副主任、文联副主席，无锡市第六、七届政协委员。1938年开始发表作品。1983年加入中国作家协会。
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