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Tracing freshwater nitrate sources in pre-alpine groundwater catchments using environmental tracers

机译:使用环境示踪剂追踪高山前地下水流域中的淡水硝酸盐源

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Groundwater is one of the main resources for drinking water. Its quality is still threatened by the widespread contaminant nitrate (NOT). In order to manage groundwater resources in a sustainable manner, we need to find options of lowering nitrate input. Particularly, a comprehensive knowledge of nitrate sources is required in areas which are important current and future drinking water reservoirs such as pre-alpine aquifers covered with permanent grassland. The objective of the present study was to identify major sources of nitrate in groundwater with low mean nitrate concentrations (8 +/- 2 mg/L). To achieve the objective, we used environmental tracer approaches in four pre-alpine groundwater catchments. The stable isotope composition and tritium content of water were used to study the hydrogeology and transit times. Furthermore, nitrate stable isotope methods were applied to trace nitrogen from its sources to groundwater. The results of the nitrate isotope analysis showed that groundwater nitrate was derived from nitrification of a variety of ammonium sources such as atmospheric deposition, mineral and organic fertilizers and soil organic matter. A direct influence of mineral fertilizer, atmospheric deposition and sewage was excluded. Since temporal variation in stable isotopes of nitrate were detected only in surface water and locally at one groundwater monitoring well, aquifers appeared to be well mixed and influenced by a continuous nitrate input mainly from soil derived nitrogen. Hydrogeological analysis supported that the investigated aquifers were less vulnerable to rapid impacts due to long average transit times, ranging from 5 to 21 years. Our study revealed the importance of combining environmental tracer approaches and a comprehensive sampling campaign (local sources of nitrate, soil water, river water, and groundwater) to identify the nitrate sources in groundwater and its vulnerability. In future, the achieved results will help develop targeted strategies for a sustainable groundwater management focusing more on soil nitrogen storage. (C) 2015 Elsevier B.V. All rights reserved.
机译:地下水是饮用水的主要资源之一。其质量仍然受到普遍存在的硝酸盐(NOT)的威胁。为了以可持续的方式管理地下水资源,我们需要找到降低硝酸盐输入量的选择。特别是,在当前和将来重要的饮用水水库,例如覆盖有永久草地的高山前蓄水层等地区,需要全面了解硝酸盐来源。本研究的目的是确定平均硝酸盐浓度较低(8 +/- 2 mg / L)的地下水中硝酸盐的主要来源。为了实现这一目标,我们在四个高山前地下水流域使用了环境示踪剂方法。使用稳定的同位素组成和水中的ium含量来研究水文地质学和穿越时间。此外,采用硝酸盐稳定同位素法从源头到地下水中追踪氮。硝酸盐同位素分析的结果表明,地下水硝酸盐源自多种铵源的硝化作用,例如大气沉积,矿物和有机肥料以及土壤有机质。排除了矿物肥料,大气沉积物和污水的直接影响。由于仅在地表水和一处地下水监测井中局部检测到硝酸盐稳定同位素的时间变化,因此含水层似乎混合得很好,并受到主要来自土壤氮的连续硝酸盐输入的影响。水文地质分析表明,由于较长的平均渡越时间(从5到21年),被调查含水层较不易受到快速影响。我们的研究表明了结合环境示踪剂方法和全面采样活动(硝酸盐,土壤水,河水和地下水的本地来源)以识别地下水中硝酸盐来源及其脆弱性的重要性。将来,取得的成果将有助于制定有针对性的可持续地下水管理战略,重点更多地放在土壤氮存储上。 (C)2015 Elsevier B.V.保留所有权利。

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