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利用稳定同位素追踪中国北方过度开采地下水区域硝酸盐的污染来源和转化。

Tracing nitrate pollution sources and transformations in the over-exploited groundwater region of north China using stable isotopes.

机构信息

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China.

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China.

出版信息

J Contam Hydrol. 2018 Nov;218:1-9. doi: 10.1016/j.jconhyd.2018.06.001. Epub 2018 Jun 15.

Abstract

Nitrate contamination in groundwater has become an environmental problem of widespread concern. In this study, we used environmental isotopes (δN-NO and δO-NO) and an isotope mixing model (SIAR) to identify the main sources of nitrate pollution, and factors controlling nitrate pollution, and to quantify the relative contributions of potential NO sources in an over-exploited groundwater region, north China. The results showed that human activities had dramatically increased the mean concentration of groundwater NO reaching 124.4 mg/L. In Hutuo River pluvial fan region, groundwater nitrate came from many kinds of pollution sources and the predominant sources were sewage and/or manure. Nitrification might be one of the most important nitrogen transformation processes and groundwater intensely exploited was a major inducing factor for the NO pollution. The highest contribution of groundwater NO was sewage and/or manure which the percent in the Hutuo River valley plain unit, upper pluvial fans of Hutuo River and central pluvial fans of Hutuo River was 54.9%, 55.0% and 61.8%, respectively, followed by soil N, NH in fertilizer and rain, NO fertilizer, and NO in precipitation. We suggested that the local government must strengthen the sewage treatment for the collection of domestic sewage, and must prohibit over-exploitation of groundwater in order to prevent NO contamination of in groundwater.

摘要

地下水硝酸盐污染已成为一个广泛关注的环境问题。本研究采用环境同位素(δN-NO 和 δO-NO)和同位素混合模型(SIAR),识别硝酸盐污染的主要来源和控制因素,并定量评估华北地区一个过度开采地下水区域中潜在硝酸盐源的相对贡献。结果表明,人类活动显著增加了地下水硝酸盐的平均浓度,达到 124.4mg/L。在滏阳河冲积扇地区,地下水硝酸盐来自多种污染源,主要污染源是污水和/或粪肥。硝化作用可能是最重要的氮转化过程之一,而地下水的过度开采是硝酸盐污染的主要诱发因素。地下水硝酸盐的最大贡献来自污水和/或粪肥,在滏阳河河谷平原单元、滏阳河上游冲积扇和滏阳河中冲积扇的贡献率分别为 54.9%、55.0%和 61.8%,其次是土壤氮、肥料中的氨和雨水中的氮、肥料中的硝酸盐和降水中的硝酸盐。我们建议当地政府必须加强污水处理,收集生活污水,同时必须禁止过度开采地下水,以防止地下水硝酸盐污染。

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