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- W3145655204 abstract "Turpan 盆位于西北的中国的干旱地区，典型关上的内陆盆被高山包围。它是之一最在世界上的干旱区域并且作为结果，在这个区域的地下水为国内、农业的使用是很重要的。在现在的学习，主要元素(K+ ， Na+ ， Ca2+ ， Mg2+ ， HCO3， SO4 2 和 Cl ) 和在地下水的环境同位素(18O， 2H 和 T ) 的关系被分析在 Turpan 盆以内调查地区性的 hydrochemistry 的进化。hydrochemistry 结果与高全部的溶解固体(TDS ) 表明那地下水集中被钠氯化物(Na-Cl ) 和钠硫酸盐(Na-SO4 ) 类型统治流水，而那与低 TDS 集中(典型地从近的山区) 被钙酸式碳酸盐(Ca-HCO3 ) 统治类型水。在 Turpan 盆以内的地下水 hydrochemistry 的进化是钙碳酸盐降水，蒸发集中，阳离子交换和 evaporites 的溶解的结果(即岩盐，芒硝和石膏) 。而且，与灌溉实践联系的 evaporite 溶解在地下水 salinization 起一个关键作用，特别在盆的中央部分。环境同位素表明地下水被降水在山区和灌溉回来流动的快垂直渗入再装。在南部的亚盆，浅地下水和深地下水在大约 40 m 的深度被分开，与以 hydrochemical 和同位素的特征的实质的差别。结果在西北的中国为与在 Turpan 盆和另外的区域的持续的水资源利用有关的决策是有用的。" @default.
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- W3145655204 date "2014-01-01" @default.
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- W3145655204 title "Groundwater hydrochemistry and isotope geochemistry in the Turpan Basin, northwestern China" @default.
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