1) The South bronch of the Gan River
赣江南支
2) mainbranch of the Gan River
赣江主支
3) Gan River
赣江
1.
Microcystins pollution in Gan River and Poyang Lake during spring and summer;
赣江及鄱阳湖春夏两季微囊藻毒素的污染研究
2.
Bird Diversity of Gan River in Ji an,Anhui Province;
安徽赣江吉安段鸟类多样性研究
3.
Gan River Lower Reaches Stream Transition and Influence to Environment;
赣江下游河道变迁及对环境的影响赣中
4) Ganjiang River
赣江
1.
Studies on the distribution of perpendicularity pollution of Cu element of sediments in Wucheng section of Ganjiang River;
赣江吴城段底质Cu元素垂直污染分布研究
2.
Dynamic Analysis of Couping Relation Retween Suspended Load and Soil and Water Loss of Ganjiang River in Jiangxi Province;
赣江河流悬移质泥沙与水土流失的耦合关系动态分析
3.
2-D sediment mathematical model for Ganjiang River waterway project;
赣江航道整治工程泥沙数学模型
5) Ganjiang
赣江
1.
Studies on the Model of Spatial Structure in Ganjiang Basin;
赣江流域空间结构模式研究
2.
Based on the hydrology sample data of the long-term rainfall, runoff and sand of the represertive station in Ganjiang Basin, the effect of the sand changing law by mankind activity was studied.
以赣江流域代表性站长系列降水、径流、泥沙等水文样本资料,研究人类活动对泥沙变化规律的影响,得到赣江流域泥沙变化规律及其发展态势,为水土保持、防洪、航运、灌溉、流域规划、河道治理、水利工程安全运行、河流泥沙站网的合理布设等国民经济建设提供科学依据。
3.
The flood forecast system of Ganjiang watershed can give the automatic flood forecst of 27 main forecast stations of Ganjiang watershed.
赣江流域洪水预报系统实现了赣江流域27个主要预报站点的自动化洪水预报,有效地减少了预报查算时间,增长了洪水预报的预见期,提高了预报精度,在实际应用中发挥了作用。
6) South Jiangxi
赣南
1.
The Pneumatothermal Fluid Leaching Metallogenic Mechanism of Felsic Cryptoexplosive Breccia─Examplined by No.6722 Uranium Deposit in south Jiangxi;
论长英质隐爆角砾岩的气热流体溶浸成矿机制──以赣南6722铀矿床为例
2.
Protection of Plant Resources and Diversity in South Jiangxi;
赣南植物资源与植物多样性保护
3.
The Discovery of Late Jurassic Shoshonitic Rocks in South Jiangxi;
赣南晚侏罗世橄榄玄粗岩系列的发现
补充资料:赣江
赣江 中国长江中游主要支流之一,江西省最大河流。东源贡水为正源,出武夷山黄竹岭,由绵水和湘水汇合而成。西源章水出大庾岭。章、贡两水在赣州市汇合后始称赣江。曲折北流,经吉安市、樟树市、丰城市到南昌市,分四条支流注入鄱阳湖。全长991千米,其中干流长751千米,流域面积8.35万平方千米。赣州以上为上游,山地纵横,支流众多,主要有湘水、濂江、梅江、平江、桃江、上犹江等,分别汇入章水和贡水。赣州至新干为中游,由于河流切割遂犹山地,多峡谷和险滩急流;万安以下,河流进入吉泰盆地,河面渐宽,水势和缓,东西两岸有孤江、遂川江、蜀水、禾水、泷水等较大支流汇入,水量大增;吉水到新干段,切穿武功山余脉,形成一较长的峡谷带。新干以下为下游,山势渐退,江面逐渐开阔,水流平缓。有袁水和绵河汇入。流域气候温和,雨量充足,年均降水量1400~1800毫米。多年平均年径流量687亿立方米。水能蕴藏量360万千瓦。干流上可常年通行100~300吨的轮驳船队和客船。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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