中国三条大河流域地表水的氯和硫同位素地球化学特征研究

大河流域 地表水 氯同位素 硫同位素 氧同位素
郎赟超 2014-01 项目
There is a little previous literature on isotope geochemistry study of chlorine cycle in freshwater regions by far. We propose to carry out a study on the chlorine and sulfur isotope geochemistry of surface waters from three large rivers in China. We will quantify isotopic composition variations of chlorine, sulfur and oxygen of dissolved sulfate in surface water of major river basins with different climate, geological and geographical backgrounds. The characteristics of the isotopic variations will be used to identify the sources of the related elements and compounds, to elucidate the factors controlling Cl and S cycling within river basins in different climatic zones, and to distinguish the natural versus anthropogenic sources. The expected results will provide new supporting scientific data on, and insights to, aquatic geochemistry of river basins. The study will advance the frontier of environmental chlorine isotope geochemistry.
目前对淡水流域Cl循环的同位素地球化学研究仍然很少。本研究以我国大陆处于不同气候带、地质背景和人为活动影响下的三条大河(长江、黄河和松花江)流域内的地表水为研究对象,分析河水中的的氯以及硫酸盐的硫和氧地球化学特征,结合水化学和水体中氧同位素等手段,确定流域中氯和硫区域分布格局,来探讨不同流域水循环过程中影响氯和硫元素循环的关键因素,辨识流域内氯和硫的自然来源和人为输入的贡献。研究成果能为流域的物质地球化学循环研究提供新的科学数据,并将对氯同位素地表地球化学理论的完善具有重要贡献。