2015Advanced materials researchOpen access

The Study on Isotopic Characteristic of Water in Jinxiuchuan River and its Environmental Significance

Yong Sen Wang, Zhenghe Xu

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Abstract

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 δD, -10.83‰~-7.34‰ forδ18O. The mean isotope values is-64.33‰ forδD, -9.01‰ forδ18O. The d-excess values range from 0.37‰ to 16.32‰ with an average value of 7.72‰. The regression slope in the regression indicates that the river water is evaporated after recharging.

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What this paper is about

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 δD, -10.83‰~-7.34‰ forδ18O. The mean isotope values is-64.33‰ forδD, -9.01‰ forδ18O. The d-excess values range from 0.37‰ to 16.32‰ with an average value of 7.72‰. The regression slope in the regression indicates that the river water is evaporated after recharging.

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Available abstract

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 δD, -10.83‰~-7.34‰ forδ18O. The mean isotope values is-64.33‰ forδD, -9.01‰ forδ18O. The d-excess values range from 0.37‰ to 16.32‰ with an average value of 7.72‰. The regression slope in the regression indicates that the river water is evaporated after recharging.

Key concepts: Isotope, Environmental science, Stable isotope ratio, Range (aeronautics), Hydrology (agriculture), Environmental chemistry, Geology, Chemistry

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