1) Yerqiang River
叶尔羌河
1.
Numerical modeling of Flow-sediment movement in the Middle Course of Xinjiang Yerqiang River;
新疆叶尔羌河中游河段水沙运动的数值模拟
2.
A method for the frequency analysis of flash flood——Take an example of Yerqiang river;
一种突发性洪水频率分析计算方法——以叶尔羌河为例
3.
Study on Dynamic Variation of Water-salt in Salinized Irrigation Area of Xinjiang Yerqiang River
新疆叶尔羌河盐碱化灌区水盐动态规律研究
2) Yeerqiang River
叶尔羌河
1.
Taking the Yeerqiang River Valley, Xinjiang as an example, types, degrees, characteristics, and causes of soil salinization were analyzed in relation to groundwater table in this district.
以新疆叶尔羌河流域为例,分析了该地区土壤盐渍化的类型、程度、特征、成因以及与地下水埋深的关系。
3) Yarkant River
叶尔羌河
1.
Foundation Treatment Experimental Study of Canal Head Sluice in Xinjiang Yarkant River Basin
新疆叶尔羌河流域中游渠首水闸基础处理试验研究
2.
Classification and Species Diversity of Plantation Communities of the Commonweal Forestry in Lower Reaches of Yarkant River
叶尔羌河下游公益林植物群落分类及其物种多样性特征
4) the headwater region of the Yarkant River
叶尔羌河源流区
5) the middle reaches of the Yeerqiang River
叶尔羌河中游
1.
The aiticle introduces the geographical environment and hydrogeologic conditions of the headwork in the middle reaches of the Yeerqiang River,analyses the problems of seepage existing in the diversion dyke,makes a specific comparison of the design plans for the seepage prevention of the diversion dyke,and also elaborates the proper choice of the measures of handling the prevention of seepage.
介绍了叶尔羌河中游渠首的地理情况和水文地质条件,分析了导流堤存在的渗流问题,对防渗设计方案进行了具体比较,并论述了防渗处理措施的合理选择。
6) Yarkant River Basin
叶尔羌河流域
1.
Analysis on the landscape processing changes of Yarkant River Basin in recent 40 years
40年来叶尔羌河流域景观变化过程分析
补充资料:叶尔羌河
叶尔羌河 塔里木河正源。位于中国新疆维吾尔自治区塔里木盆地西南部,是塔里木盆地西部最大的河流。源出喀喇昆仑山北麓,上源有大面积的冰川分布。干流在莎车西南的喀群出山口后,进入平原流经塔克拉玛干沙漠的边缘,在上游水库附近与阿克苏河汇合后始称塔里木河。从主源拉斯开木河源头至伊里克苏沟口为上游,长244千米 ,两岸山势陡峻,平均比降6.57‰,有克勒青河注入。由伊里克苏沟口至喀群为中游,长252千米,平均比降4.7‰~5.96‰,两岸高山夹峙,河道曲折,有支流塔什库尔干河汇入。喀群以下为下游,地势由山丘消逝为平原,两岸渠系密布,坡降平缓,淤积严重,水流蜿蜒曲折。全长1078千米,流域面积9.37万平方千米。流域内有地表水资源74.6亿立方米。喀群站最大年径流量为88.1亿立方米,最小年径流量为44.7亿立方米。径流年际变化相对稳定,反映了河水靠降水及冰川融水补给的特点。 |
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