首页> 外文期刊>RSC Advances >Combing N-15 and O-18 to identify the distribution and the potential sources of nitrate in human-impacted watersheds, Shandong, China
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Combing N-15 and O-18 to identify the distribution and the potential sources of nitrate in human-impacted watersheds, Shandong, China

机译:梳理N-15和O-18,以确定人类受影响的流域硝酸盐的分布和潜在来源,中国

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摘要

Identifying the anthropogenic and natural sources of nitrate emissions contributing to surface water continues to be an enormous challenge. It is necessary to control the water quality in the watershed impacted by human disturbance. In this study, water chemical parameters including nitrate (NO3-) concentrations, N-15-NO3-, O-18-NO3-, and O-18-H2O were analyzed to investigate the contamination and sources of NO3- in two watershed rivers (Jinyun, JYN and Jinyang, JYA), Jinan, Shandong, China. Results indicated NO3- concentrations in the JYN were significantly higher than those in the JYA (P 0.05), probably because of high N input of the extensive farmlands or orchards in the drainage basin. N-15-NO3- and O-18-NO3-, associated with Cl-, indicated that nitrate-nitrogen (NO3--N) was not derived from atmospheric deposition but came principally from manure/sewage and soil organic matter in these two watersheds. The microbial nitrification took place in the nitrate of manure/sewage and soil nitrate. The combination of NO3- concentration and nitrogen and oxygen isotope suggested that NO3- had undergone microbial denitrification after entering the rivers. Furthermore, NO3- concentrations had significant temporal and spatial variation highlighting differential sources and fates. These results expand our understanding of mechanisms driving NO3- retention and transport and provide strategies in managing NO3- contamination in different land use watersheds around the world.
机译:确定有助于地表水的硝酸盐排放的人为和自然来源仍然是一个巨大的挑战。有必要控制受人类扰动影响的流域的水质。在该研究中,分析了包括硝酸盐(NO 3)浓度,N-15-NO3-,O-18-NO 3-和O-18-H2O的水化学参数,研究了两个流域河流中NO3-的污染和来源(金云,Jinn和Jinyang,Jya),山东济南,中国。结果表明,JYN中的NO 3浓度明显高于JYA(P <0.05)的浓度,可能是因为在排水盆中的广泛的农田或果园的高度输入。与CL-相关的N-15-NO 3和O-18-NO3-表明硝酸氮(NO3 - N)不是来自大气沉积,而是主要来自这两个中的粪肥/污水和土壤有机物。流域。微生物硝化发生在粪肥/污水和土壤硝酸盐的硝酸盐中。 NO 3浓度和氮和氧同位素的组合表明,在进入河流后,NO3-没有经过微生物反硝化。此外,NO3浓度具有显着的时间和空间变化,突出差分来源和命名。这些结果扩大了我们对驾驶No3保留和运输机制的理解,并在世界各地的不同土地使用流域管理No3污染方面提供策略。

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  • 来源
    《RSC Advances》 |2018年第41期|共7页
  • 作者单位

    Univ Jinan Sch Water Conservancy &

    Environm Jinan 250022 Shandong Peoples R China;

    Univ Jinan Sch Water Conservancy &

    Environm Jinan 250022 Shandong Peoples R China;

    Univ Jinan Sch Water Conservancy &

    Environm Jinan 250022 Shandong Peoples R China;

    Univ Jinan Sch Water Conservancy &

    Environm Jinan 250022 Shandong Peoples R China;

    Univ Western Australia Sch Plant Biol Crawley WA 6009 Australia;

    Univ Jinan Sch Water Conservancy &

    Environm Jinan 250022 Shandong Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 化学;
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