1)Qiantang Estuary钱塘江河口
1.Impact of water diversion from Xinanjiang Reservoir to north Zhejiang Province on water environment at Qiantang Estuary;浙北引水对钱塘江河口段主要水环境的影响分析
2.Sediment deposition after regulation and reclaiming of Qiantang Estuary;治江缩窄后钱塘江河口泥沙淤积和成因探讨
3.Characteristic of the flood level in the Qiantang Estuary and mobile-bed model for forecast;钱塘江河口洪水特性及动床数值预报模型
英文短句/例句
1.The seawall is utilized for preventing flood and tide at the Qiantang Estuary.钱塘江海塘为钱塘江河口防洪、潮江堤的习称,从土塘到石塘到现代标准海塘,历经两次大的飞跃。
2.Application of numerical model of tidal bore to bridge works in the Qiantang Estuary涌潮数学模型在钱塘江河口桥梁工程中的应用
3.Numerical simulation of effects on storm-induced water level after contraction in Qiantang estuary;钱塘江河口围垦对台风暴潮影响的数值模拟
4.Numerically Simulating the Effect of Reclamation Project on the Tidal Bore in the Qiantang Estuary钱塘江河口围涂工程对涌潮影响的数值研究
5.Numerical method for the storm tide overflow model in Hangzhou bay and Qiantangjiang estuary钱塘江河口杭州湾风暴潮溢流计算方法研究
6.The Effects of Regulation and Reclamation in Qiantang Estuary on Storm Surge at Hangzhou Bay;钱塘江河口区治江围涂对杭州湾风暴潮影响研究
7.The Qiantang estuary model was established,and the formation and propagation process of tidal bore was simulated.制作了钱塘江河口模型,并模拟了涌潮的形成与传播过程.
8.Numerical Simulation for Discontinuous Shallow Water Flow and Its Application to the Analysis of the Tidal Bore at the Qiantang Estuary;浅水间断流动数值模拟及其在钱塘江河口涌潮分析中的应用
9.Application of 2D dynamic water quality model to the upstream Qiantang estuary平面二维动态水质模型在钱塘江河口上段污染控制中的应用
10.Bore pressure on the 2nd passage gate of ship lock of Jinghang Great Canal crossing the Qiantang River京杭运河二通道钱塘江出口船闸闸门涌潮作用力研究
11.The Second Outlet of Beijing-Hangzhou Canal Treatment Based on Moveable Bed Model京杭运河二通道出口钱塘江段治理方案动床模型试验研究
12.Foundation treatment for flood protection works in bore stretch of Qiantang River钱塘江涌潮河段防洪堤工程地基处理
13.We owe the spectacular tidal bore at the mouth of Qiantang River to the special funnel- shaped estuary of the Gulf of Hangzhou.钱塘江潮壮观的成因，主要由钱塘江喇叭形的入海口造成的。
14.Research in Evolvement of Channel and Character of Confined Water of Paleochannel of Qiantangjiang River;钱塘江河道形成及古河道承压水性状研究
15.Study on Salinity Intrusion of Nandujiang Estuary(Lower Reaches of Longtang Dam);南渡江河口（龙塘坝下游）盐水入侵研究
16.Hangzhou's mother river is called Qiantang River, which is also known as Qianjiang River. The Qianjiang CBD is named after this river.杭州的母亲河名为钱塘江，也称钱江。钱江中央商务区就是以钱江命名。
17.Simulation of flow pattern in the approach channel of the closed-type harbor on huge tidal reach in the Qiantang river钱塘江强潮河段建设“闭合式港”引航道流态模拟
18.The Large Bridge at the world famous strong tide river part-The site scene during construction period of the2 nd Qiantangjiang River Bridge.世界著名强涌潮河段的首座大桥——钱塘江第二大桥在施工期的场景。
相关短句/例句
Qiantang River estuary钱塘江河口
1.Remote sensing investigation on vegetati on index based on MODIS data in Qiantang River estuary;基于MODIS数据的钱塘江河口段植被指数遥感调查
2.Economic benefit evaluation of development of shoals in Qiantang River estuary钱塘江河口滩涂开发经济效益评估
3.Duo to special geographical site and configuration, the magnitude of typhoon surge in Qiantang river estuary is violent.钱塘江河口杭州湾由于独特的海湾地理位置和形态 ,引起台风暴潮强烈增水。
3)Qiantangjiang Estuary钱塘江河口
1.Evolvement and regulation of Xisan furrow in south bank of Qiantangjiang Estuary;钱塘江河口南岸西三潮沟形成演变及其治理
2.Experimental study of profiled-block stability in Qiantangjiang estuary;钱塘江河口异型块体抗冲稳定特性试验研究
3.Numerical method for the storm tide overflow model in Hangzhou bay and Qiantangjiang estuary钱塘江河口杭州湾风暴潮溢流计算方法研究
4)the Qiantangjiang River Estuary钱塘江河口
1.Progress of the study on the groins of the Qiantangjiang River Estuary;钱塘江河口护塘丁坝的研究进展
2.According to the datum gathered from the Qiantangjiang River Estuary about preventing flood,preventing tide,irrigation,navigation,water supply,journey etc.根据收集到的有关钱塘江河口防洪、御潮、灌溉、航运、供水、旅游等方面的资料,分析、计算了该河口防洪御潮资源和水资源、滩涂、岸线及涌潮资源等的储存量。
5)Qiantang estuary钱塘江河口段
1.Analysis on tidal-driven dilution and transportation of contaminants in Qiantang estuary;钱塘江河口段潮动力对污染物稀释扩散作用探讨
6)Qiantang River seawalls钱塘江海塘
延伸阅读
钱塘江钱塘江中国浙江省最大河流。旧称浙江。有两源：正源发源于安徽省休宁县西南六股尖，自西向东南，入浙江省后至建德市梅城与来自西南的兰江相汇后，向东北流至澉浦附近，注入杭州湾，全长605千米。流域面积4.88万平方千米。钱塘江自河源至河口，各段分别有不同名称。河源段名冯村河，自鹤城至流口称大源河，流口至屯溪名率水，屯溪至浦口称青溪，浦口至梅城称新安江，淳安以上又称徽江，亦称歙港，梅城至桐庐称桐江，桐庐至萧山闻家堰称富春江，闻家堰至杭州闸口段，河道曲折，形如反写“之”字，称之江，闸口以下流经钱塘县(今杭州)的一段始名钱塘江。现以最后一段名称泛指整条河流。南源开化江发源于浙、皖、赣交界的莲花尖(后又改为安徽省休宁县的青芝棣尖)，其上、中、下游各段也随地而异称，上游衢州以上称常山江；中游衢州到兰溪称衢江，又名信安江，衢江自西北向东南流，至南溪后北折，因沿兰阴山东麓流出，古时两岸多兰花，故名兰江，又称兰溪，北流至梅城汇入主流。钱塘江地处亚热带季风气候区，雨量充沛，年降水量1600～2000毫米。水系发达，较大的支流除兰江以外，还有乌溪江、金华江(婺江)、壶源溪、浦阳江和曹娥江等。干支流的中、上游，大多穿行在地面起伏较大的山地、丘陵之中，河床比降大，险滩、跌水多，属山区性河流。梅城以下至芦茨埠，是著名的七里泷峡谷。出七里泷后，河面开阔，水流缓慢，水量大增，多年平均径流量431.4亿立方米，径流的多年变化较小。水力资源丰富，理论蕴藏量达262.8万千瓦，可供开发利用的有205万千瓦，已建成新安江、富春江、黄坛口等水电站。干流自梅城以上通轮至建德市白沙。梅城以下，百吨级船只终年可在杭州到兰溪之间的江道上行驶。钱塘江杭州段
