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首页> 外文期刊>Central european geology >NITRATE AND SULFATE ISOTOPES IN THE GROUNDWATER OF THE SANDY HALTERN FORMATION (GERMANY) TO INVESTIGATE NITRATE REDUCTION PROCESSES
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NITRATE AND SULFATE ISOTOPES IN THE GROUNDWATER OF THE SANDY HALTERN FORMATION (GERMANY) TO INVESTIGATE NITRATE REDUCTION PROCESSES

机译:沙质盐岩地层(德国)地下水中的硝酸盐和硫酸盐同位素,用于研究硝酸盐还原过程

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摘要

With a thickness of up to 300 m, the sandy aquifer of the Haltern Formation is one of the most important drinking water resources in north-west Germany (NRW). Six water works extract around 53 Mio. m~3 a year of groundwater and deliver drinking water to around 4 Mio. costumers. Five of these catchment areas were investigated in this study. Due to the intensive agricultural land use a strong nitrate input into the shallow groundwater occurs and leads to significantly increasing nitrate concentrations in the shallow groundwater.
机译:Haltern组的含砂含水层厚度最大为300 m,是德国西北部(NRW)最重要的饮用水资源之一。六处水厂提取了约53兆欧的水。每年m〜3的地下水,并将饮用水输送到4 Mio左右。顾客。在这项研究中对其中五个集水区进行了调查。由于耕地的密集使用,硝酸盐大量输入到浅层地下水中,并导致浅层地下水中硝酸盐浓度显着增加。

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