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首页> 外文期刊>The Science of the Total Environment >Evaluation of geochemical processes and nitrate pollution sources at the Ljubljansko polje aquifer (Slovenia): A stable isotope perspective
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Evaluation of geochemical processes and nitrate pollution sources at the Ljubljansko polje aquifer (Slovenia): A stable isotope perspective

机译:卢布尔雅那polje含水层(斯洛文尼亚)的地球化学过程和硝酸盐污染源评估:稳定的同位素视角

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摘要

The Ljubljansko polje aquifer, which is the main supply of drinking water for the local population in Ljubljana, Slovenia is highly vulnerable to anthropogenic pollution. In this study, the geochemistry ofmajor constituents including nitrate concentrations and the dual isotopes of nitrate were used to ascertain the spatial distribution of processes and nitrate sources in the groundwater from seven wells at three different water supplies: Klece, Hrastje and Jarski prod. The groundwater is of the Ca2+-Mg2+-HCO3- type approaching equilibrium with respect to dolomite and are moderately supersaturated with calcite. The groundwater nitrate concentrations ranged from 5.32 to 50.1 mg L-1 and are well above the threshold value for anthropogenic activity (3 mg L-1). The delta N-15(NO3) values ranged from 1.4 to 9.7 parts per thousand, while delta O-18(NO3) values were from 6.3 to 34.6 parts per thousand. Based on isotope mixing model three sources of nitrate were identified: atmospheric deposition, fertilizers and soil nitrogen. At Klece 8, Klece 12 and Jarski prod 3 the low delta N-15(NO3) and high delta O-18(NO3) values result from pristine nitrate sources, while in Hrastje 3 and Klece 11 equal amounts of nitrate derived from soils with mixed fertilization and sewage. The data also indicate that the main sources of high nitrate concentrations in groundwater are from fertilizers and sewage-manure (comprising up to 64%). Such levels occurred in the Hrastje and Klece 11 wells where precipitation is the main source of groundwater. Nitrate derived from atmospheric deposition accounted for approximately 10% of the nitrate in the groundwater. The message from this study is that to reduce the nitrogen load and improve water quality will involve containment and the careful management of sources from urban and agriculture inputs such as sewage-manure and fertilizers. (c) 2018 The Authors. Published by Elsevier B.V.
机译:Ljubljansko polje含水层是斯洛文尼亚卢布尔雅那当地居民的主要饮用水来源,极易受到人为污染的影响。在这项研究中,主要成分的地球化学特征包括硝酸盐浓度和硝酸盐的双重同位素被用于确定来自三个不同供水源的七个井的地下水的过程和硝酸盐来源的空间分布:Klece,Hrastje和Jarski产品。地下水为Ca2 + -Mg2 + -HCO3-型,相对于白云石已趋于平衡,并且已被方解石适度过饱和。地下水中硝酸盐的浓度范围为5.32至50.1 mg L-1,远高于人为活动阈值(3 mg L-1)。 δN-15(NO3)值范围为千分之1.4至9.7,而δO-18(NO3)值则为千分之6.3至34.6。根据同位素混合模型,确定了硝酸盐的三种来源:大气沉积,肥料和土壤氮。在Klece 8,Klece 12和Jarski prod 3中,低硝酸盐N-15(NO3)和高δO-18(NO3)值来自原始硝酸盐源,而在Hrastje 3和Klece 11中,等量硝酸盐来自土壤混合施肥和污水。数据还表明,地下水中硝酸盐含量高的主要来源是化肥和污水肥料(占64%)。这种水平发生在Hrastje和Klece 11井中,那里的降水是地下水的主要来源。来自大气沉积的硝酸盐约占地下水硝酸盐的10%。这项研究传达的信息是,减少氮负荷和改善水质将涉及围堵和对城市和农业投入源(如污水,肥料和化肥)的来源进行精心管理。 (c)2018作者。由Elsevier B.V.发布

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