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Characterization and source identification of nitrogen in a riverine system of monsoon-climate region, China

机译:季风气候区河流系统中氮的特征与来源识别

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摘要

There are inaeasing concerns in nitrogen (N) pollution worldwide, especially in aquatic ecosystems, and thus quantifying its sources in waterways is critical for pollution prevention and control. In this study, we investigated the spatio-temporal variabilities of inorganic N conœntratíon (i.e., NO~-_3, NH~+_4 ) and total dissolved N (TDN) and identified their sources in waters and suspended matters using an isotopical approach in the Jinshui River, a river with a length of 87 km in the monsoon-climate region of China. The spatio-temporal inorganic N concentrations differed significantly along the longitudinal gradient in the river network. The NO~-_3, NH~-_4 and TDN concentrations ranged from 0.02 to 1.12 mg 1~(-1), 0.03 to 4.28 mg 1~(-1), and 033 to 2.78 mg 1~(-1), respectively. The ~(15)N tracing studies demonstrated that N in suspended organic matter was in the form of suspended particulate nitrogen (SPN) and was primarily from atmospheric deposition and agricultural fertilizer. In contrast, N in stream waters was mainly in the form of nitrate and was from atmospheric deposition, fertilizers, soil, and sewage. Meanwhile, both δ~(15)N-SPN and δ~(15)N-NO~-_3 peaked in the rainy season (ίe.,July) because of higher terrigenous sourœs via rain mnofF, demonstrating the dominant diffusive N sources in the catchment Thus, our results could provide critical information on N pollution control and sustainable watershed management of the riverine ecosystem in monsoon-climate region.
机译:全世界,特别是在水生生态系统中,对氮(N)污染的关注日益增加,因此,量化水道中的氮源对于污染的预防和控制至关重要。在这项研究中,我们调查了无机N含量(即NO〜-_3,NH〜+ _4)和总溶解氮(TDN)的时空变化,并利用同位素方法在水体中确定了它们的来源。金水河,是中国季风气候区长87公里的河流。沿河网的纵向梯度,无机氮的时空差异很大。 NO〜-_3,NH〜-_4和TDN浓度分别为0.02至1.12 mg 1〜(-1),0.03至4.28 mg 1〜(-1)和033至2.78 mg 1〜(-1)。 。 〜(15)N示踪研究表明,悬浮有机物中的N呈悬浮颗粒氮(SPN)形式,主要来自大气沉积物和农业肥料。相反,溪流水中的氮主要以硝酸盐的形式存在,来自大气沉积,肥料,土壤和污水。同时,δ〜(15)N-SPN和δ〜(15)N-NO〜-__ 3在雨季(7月,ete)均达到峰值,这是由于雨mnofF带来了更高的陆源变质,这说明了该地区的主要扩散N源。流域因此,我们的结果可以为季风气候区河流生态系统的氮污染控制和可持续流域管理提供重要信息。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第15期|608-615|共8页
  • 作者单位

    Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy ofSdences, Wuhan 430074, PR China ,The University of Chinese Academy of Saences, Beijing 10049, PR China;

    Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sdences, Chongqing 400714, PR China;

    Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy ofSdences, Wuhan 430074, PR China ,The University of Chinese Academy of Saences, Beijing 10049, PR China;

    Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy ofSdences, Wuhan 430074, PR China ,The University of Chinese Academy of Saences, Beijing 10049, PR China;

    Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy ofSdences, Wuhan 430074, PR China;

    Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, The Chinese Academy ofSdences, Wuhan 430074, PR China;

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

    Jinshui River; Nitrogen pollution; Isotopic enrichments; Water quality; Headwaters;

    机译:金水河氮污染;同位素富集;水质;上游源头;

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