1) Qiantang River
![点击朗读](/dictall/images/read.gif)
钱塘江
1.
Study on pollutant flux of main sections in Qiantang River based on ADCP;
![点击朗读](/dictall/images/read.gif)
基于ADCP测量的钱塘江主要断面污染物通量研究
2.
Prediction of water quality index in Qiantang River based on BP neural network model;
![点击朗读](/dictall/images/read.gif)
基于BP神经网络的钱塘江水质指标的预测
3.
Water Environmental Simulation of Main Contaminations in the Qiantang River at Low Water Period;
钱塘江枯水期主要污染物水环境模拟
2) Qiantangjiang River
![点击朗读](/dictall/images/read.gif)
钱塘江
1.
On Cofferdam Construction in Strong-tide & Head-wave Area Along Qiantangjiang River;
![点击朗读](/dictall/images/read.gif)
钱塘江强潮顶冲地段围堰的施工
2.
The division of boundary between Qiantangjiang River and Hangzhouwan Bay;
![点击朗读](/dictall/images/read.gif)
钱塘江与杭州湾河海界线的划分
3.
Organic pollution and pollutants' genotoxicity in aquatic environment of Qiantangjiang River
钱塘江水环境有机物污染及遗传毒性检测
4) Billows of QianTang River
![点击朗读](/dictall/images/read.gif)
钱塘江涛
5) Qiantang Estuary
![点击朗读](/dictall/images/read.gif)
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;
![点击朗读](/dictall/images/read.gif)
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
6) the Qiantangjiang River Estuary
![点击朗读](/dictall/images/read.gif)
钱塘江河口
1.
Progress of the study on the groins of the Qiantangjiang River Estuary;
![点击朗读](/dictall/images/read.gif)
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。
补充资料: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。
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