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Evaluation of the origin of nitrate influencing the Klju? groundwater source, Serbia

机译:硝酸盐的来源影响Klju的评估地下水源,塞尔维亚

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This paper describes the use of the dual isotope method involving δ ~(15)N and δ ~(18)O measurements of dissolved nitrates to assess the origin and fate of groundwater nitrate at the Klju? groundwater source, Serbia. A sampling campaign was conducted in September 2007 during flow conditions obtaining groundwater from observation wells and river water fed by a shallow aquifer hosted in alluvial (sandy-gravel) sediments. Nitrate isotope ratios ranged from +5.3 to +16.9‰ and δ ~(18)O _(NO3) values varied from -2.3 to +5.0‰. Two major contamination sources were identified with isotopic compositions characteristic for nitrate derived from nitrification of soil organic nitrogen (+5.3 to +7.8‰ for δ ~(15)N) resulting in nitrate concentrations of 33.6 and 78.8 mg/L and nitrate derived from animal wastes or human sewage, e.g. via septic systems, yielding δ ~(15)N values of +9.9 to +11.9‰ and elevated nitrate concentrations of 31.2-245.8 mg/L. The occurrence of nitrification and denitrification was also revealed based on concentration and isotope data for dissolved nitrate.
机译:本文介绍了使用双同位素方法,包括对溶解的硝酸盐进行δ〜(15)N和δ〜(18)O测量,以评估Klju?地下水硝酸盐的来源和结局。地下水源,塞尔维亚。在流动条件下,于2007年9月进行了一次采样活动,从观测井中获取地下水,并由冲积(砂砾砾石)沉积物中的浅层含水层供给河水。硝酸盐同位素比范围为+5.3至+ 16.9‰,δ〜(18)O _(NO3)值范围为-2.3至+ 5.0‰。确定了两种主要污染源,这些同位素的同位素组成具有土壤有机氮硝化作用所产生的硝酸盐的特征(δ〜(15)N的+5.3至+ 7.8‰),导致硝酸盐浓度分别为33.6和78.8 mg / L,以及动物来源的硝酸盐废物或人类污水,例如通过化粪池系统产生的δ〜(15)N值为+9.9至+ 11.9‰,硝酸盐浓度为31.2-245.8 mg / L。根据溶解的硝酸盐的浓度和同位素数据,还揭示了硝化和反硝化的发生。

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