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Contribution of bedrock nitrogen to high nitrate concentrations in stream water

机译:基岩氮对溪流水中高浓度硝酸盐的贡献

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Concentrations of nitrate in stream water throughout the world are reported to be elevated relative to natural background levels. This enrichment is commonly attributed to anthropogenic activities such as atmospheric emissions, livestock feeding, agricultural runoff, timber harvesting practices and domestic/ industrial effluent discharge. Here we show that bedrock containing appreciable concentrations of fixed nitrogen contribute a surprisingly large amount of nitrate to surface waters in certain California watersheds, to an extent that even small areas of these rocks have a profound influence on water quality. As 75% of the rocks now exposed at the Earth's surface are sedimentary in origin, and as these rocks contain about 20% of the global nitrogen inventory, 'geological' nitrogen may be a large and hitherto unappreciated source of nitrate to surface waters. Such a natural nitrate source may be especially significant given that nitrate contamination at very low levels can contribute to surface water eutrophication, may cause infant methaemoglobinaemia ('blue baby' syndrome) and has been implicated in certain cancers. In addition, geological nitrogen may be a source of the 'missing' nitrogen noted in several biogeochemical studies of ecosystem nitrogen budgets.
机译:据报道,全世界溪流水中硝酸盐的浓度相对于自然本底水平要升高。这种浓缩通常归因于人为活动,例如大气排放,牲畜饲养,农业径流,木材采伐方式以及生活/工业废水排放。在这里,我们表明,在某些加利福尼亚流域,基岩中含有相当数量的固定氮,这给地表水中的硝酸盐带来了惊人的数量,甚至这些岩石的很小区域都对水质产生了深远的影响。由于现在暴露在地球表面的岩石中有75%来自沉积物,并且由于这些岩石包含全球总氮存量的20%,因此“地质”氮可能是地表水中迄今尚未发现的大量硝酸盐来源。鉴于非常低的硝酸盐污染水平可能导致地表水富营养化,可能引起婴儿血红蛋白血症(“蓝宝贝”综合症)并且与某些癌症有关,因此这种天然硝酸盐来源可能尤其重要。另外,地质氮可能是生态系统氮预算的几项生物地球化学研究中提到的“缺失”氮的来源。

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