首页> 外文期刊>Science in China. Series E >Strontium isotopic geochemistry of the changjiang estua- rine waters: Implications for water-sediment interaction
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Strontium isotopic geochemistry of the changjiang estua- rine waters: Implications for water-sediment interaction

机译:长江口水域锶同位素地球化学:水-沉积物相互作用的意义

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The Sr concentrations 87_sr/86_sr ratios have been measured for the Chjangjiang es- tuarine waters with a main purpose to understand physical and chemical processes at the estuary. The result shows that the Changjiang River water has higher Sr concentration (150 ng/g) and Lower 87_sr/86_sr ratio (0.7105) when compared with the average values (0.7119 for 87_sr86_sr and 78ppb for Sr, respectively) of large world rivers. In the mixing process, no simple mixing of two End-members has been found according to the variations of Sr concentration and isotope ratios.
机译:已对长江江水的Sr浓度87_sr / 86_sr比进行了测量,其主要目的是了解河口的物理和化学过程。结果表明,与世界大型河流的平均值(分别为87_sr86_sr和0.7ppb的平均值)相比,长江水的Sr浓度较高(150 ng / g),而87_sr / 86_sr比率较低(0.7105)。在混合过程中,没有发现根据Sr浓度和同位素比率的变化简单地混合两个末端成员。

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