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The study on isotopic characteristic of water in Jinxiuchuan river and its environmental significance

机译:金秀川河水同位素特征及其环境意义研究

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A environment isotope study was carried out to reveal the variation of isotope composition in Jinxiuchuan River water in Jinan. The water samples were collected during June and July for 2012 and 2013.The stable isotopes in river water have a wide range from 74.03‰ to -54.8 ‰ for SD, -10.83‰~-7.34‰ for δ~(18)O. The mean isotope values is -64.33‰ for8D, -9.01‰ for δ~(18)O. The d-excess values range from 0.3 7‰ to 16.32%o with an average value of 7.72‰. The regression slope in the regression indicates that the river water is evaporated after recharging.
机译:进行了环境同位素研究,以揭示济南金秀川河水中同位素组成的变异。在2012和2013年6月和7月期间收集了水样。河水中稳定同位素的差距范围为74.03‰至-54.8‰,对于δ〜(18)o的δ〜(18)o。平均同位素值为-64.33‰FOR8D,-9.01°Δ〜(18)o。 D-超值的值范围为0.3 7‰至16.32%o,平均值为7.72‰。回归中的回归斜率表明再充电后河水蒸发。

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