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Tracing anthropogenic DIC in urban streams based on isotopic and geochemical tracers

机译:基于同位素和地球化学示踪剂追踪城市溪流中的人为DIC

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摘要

To elucidate the type and extent of anthropogenic DIC (dissolved inorganic carbon), carbon isotopic composition of DIC and dissolved ion concentration were determined in three streams (Gap, Yudeung and Daejeon) draining populated Daejeon metropolitan area, South Korea. Seasonal variations in water chemistry and carbon isotopic composition of DIC (delta(13) C-DIC) reflected changing contribution from two main DIC sources, i.e., soil weathering and sewages. DIC input from the soil weathering was characterized by delta C-13(DIC) values ranging from -16.7 to -16.0 % and higher during Jun-Nov. The sewage-derived DIC became dominant during Dec-May with delta(13) C-DIC values ranging from -11.4 to -7.4 %. Si and Cl served as indicators of DIC inputs from soil weathering and sewages, respectively. The higher delta(13) C-DIC values of sewages in the study area indicated that detergents (delta(13) C-DIC of -12.0 to -6.5 %) carried by the urban sewages were the main anthropogenic DIC component. The extent of anthropogenic DIC relative to soil-derived DIC in stream waters increased when the precipitation was low and discharge decreased. The results of this study provide a method to quantify anthropogenic DIC, which can help manage water quality in urban stream waters.
机译:为了阐明人为DIC(溶解的无机碳)的类型和程度,在韩国大田广域市的三个流域(Gap,Yudeung和Daejeon)中,测定了DIC的碳同位素组成和溶解的离子浓度。 DIC的水化学和碳同位素组成的季节性变化(delta(13)C-DIC)反映了来自两个主要DIC来源(即土壤风化和污水)的变化贡献。在6月至11月期间,土壤风化的DIC输入的特征在于C-13(DIC)值介于-16.7%至-16.0%或更高。源自污水的DIC在12月至5月期间占据主导地位,其delta(13)C-DIC值在-11.4%至-7.4%之间。 Si和Cl分别用作土壤风化和污水中DIC投入的指标。研究区域中较高的delta(13)C-DIC值表明,城市污水所携带的去污剂(delta(13)C-DIC为-12.0至-6.5%)是主要的人为DIC成分。当降水量低而排放量减少时,人为源DIC相对于土壤DIC的程度增加。这项研究的结果提供了一种量化人为DIC的方法,该方法可以帮助管理城市溪流水的水质。

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