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Application of nitrogen and boron isotopes for tracing sources of anthropogenic contamination in Monforte-Alter do Chao aquifer system, Portugal

机译:氮和硼同位素在追踪葡萄牙Monforte-Alter do Chao含水层系统中人为污染源中的应用

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摘要

The Monforte-Alter do Chao aquifer system represents one of the main water resources in Alentejo region (SW Portugal), and is located in an area of intensive agriculture and cattle breeding. The groundwater shows varied chemical composition, reflecting fast chemical changes associated with the water-rock interaction, with waters of Ca-HCO_3, Na/Ca-HCO_3, and Na- HCO_3 facies. Some of the waters have strong evidence of nitrogen contamination with nitrate concentrations above 50 mg/l. The implementation of the European Nitrates Directive and the Water Framework Directive has led to the designation of large areas as Nitrate Vulnerable Zones, for being at risk from agricultural nitrate pollution: groundwater containing or that could contain more than 50 mg/l of nitrates. Corrective measures taken to reverse the trend can only be established when the contaminant source is known. In this study, the isotopic compositions of NO_3 (δ~(15)N and δ~(18)O) and B (δ~(11)B) were used to identify the sources of the nitrogen contamination. Despite the occurrence of some evaporation processes, the δ~(15)N and δ~(18)O isotopes allowed to distinguish two groups of waters with different sources of nitrates, fertilizers, and soils or manure and domestic effluents. The analysis of the NO_3 source based on δ~(11)B isotope ratio pointed out contamination by pig farms effluents. However, considering the land occupation and the strong livestock activities in the area, it is possible that the adsorption of ~(11)B isotopes onto clays or the high pH of the groundwater could explain the high δ~(11)B values.
机译:Monforte-Alter do Chao含水层系统代表了阿连特茹地区(葡萄牙西南部)的主要水资源之一,位于集约化农业和养牛场。地下水显示出不同的化学组成,反映出与水-岩石相互作用相关的快速化学变化,以及Ca-HCO_3,Na / Ca-HCO_3和Na-HCO_3相的水。一些水具有明显的氮污染迹象,硝酸盐浓度超过50 mg / l。欧洲《硝酸盐指令》和《水框架指令》的实施已导致将较大的地区指定为硝酸盐脆弱区,因为这些地区容易受到农业硝酸盐污染的威胁:地下水中或硝酸盐含量可能超过50 mg / l。只有在知道污染源的情况下,才能采取纠正趋势的纠正措施。在这项研究中,使用NO_3(δ〜(15)N和δ〜(18)O)和B(δ〜(11)B)的同位素组成来确定氮污染源。尽管发生了一些蒸发过程,但δ〜(15)N和δ〜(18)O同位素仍可以区分具有不同硝酸盐,肥料,土壤或肥料和生活污水的两组水。基于δ〜(11)B同位素比的NO_3源分析指出了养猪场废水的污染。然而,考虑到该地区的土地占用和强大的牲畜活动,〜(11)B同位素在粘土上的吸附或地下水的高pH值可能解释了高δ〜(11)B值。

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  • 来源
    《Sustainable Water Resources Management》 |2019年第1期|249-266|共18页
  • 作者单位

    Departamento de Geologia, Faculdade de Ciencias, Universidade de Lisboa, Ed. C6, Campo Grande, 1749-014 Lisbon, Portugal;

    Departamento de Geologia, Faculdade de Ciencias, Universidade de Lisboa, Ed. C6, Campo Grande, 1749-014 Lisbon, Portugal,Instituto D. Luiz, Faculdade de Ciencias, Universidade de Lisboa, Ed. CI, Campo Grande, 1749-014 Lisbon, Portugal;

    Departamento de Geologia, Faculdade de Ciencias, Universidade de Lisboa, Ed. C6, Campo Grande, 1749-014 Lisbon, Portugal;

    Departamento de Geologia, Faculdade de Ciencias, Universidade de Lisboa, Ed. C6, Campo Grande, 1749-014 Lisbon, Portugal;

    Departamento de Geologia, Faculdade de Ciencias, Universidade de Lisboa, Ed. C6, Campo Grande, 1749-014 Lisbon, Portugal;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Nitrate source; N; O; and B isotopes; Monforte-Alter do Chao aquifer system;

    机译:硝酸盐来源;N;O;和B同位素;Monforte-Alter do Chao含水层系统;

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