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Phosphorus transport in riverbed sediments and related adsorption and desorption characteristics in the Beiyun River, China

机译:河床沉积物的磷输送及北云江河山沉积物及相关吸附及解吸特性

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摘要

Riverbed sediments are the interface layer in riverine ecosystems connecting the overlying medium of water and the vadose zone. The transport behavior of phosphorus (P), which has been recognized as the primary cause of freshwater eutrophication, in riverbed sediments remains unclear. Understanding the impact of riverbed sediments on P transport is a necessary prerequisite for the development of appropriate strategies to reduce potential groundwater pollution. In this study, riverbed sediments were collected from the upstream, midstream, and downstream sections of the Beiyun River, China, and packed into vertical soil columns to perform leaching experiments to quantify P transport characteristics. In addition, the impact mechanisms were further explored by conducting laboratory batch tests of P adsorption and desorption. The results demonstrated that approximately 80% of P can be adsorbed by riverbed sediments in soil column leaching experiment, and a tailing phenomenon was observed in its desorption. The hydraulic conductivity properties of riverbed sediments were evaluated by the advection-dispersion equation, showing a gradually decreasing adsorption capacity for P from upstream to downstream sections, which was supported by the results obtained from adsorption-desorption thermodynamic and kinetic batch tests. The estimated annual leaching masses of P increased from 60.72 g/(m(2) a) in the upstream section to 132.31 g/(m2 a) in the downstream section. The role of riverbed sediments as a source or sink of P is possibly determined by their coarse sand particles content, and the mean equilibrium P concentration (EPC0). The competitive relationship between P and other forms of nutrients also has an important influence on its source-sink role. These findings suggest that the prevention of the potential P leaching is most needed in the downstream sections of Beiyun River, and corresponding control strategies should be developed to avoid groundwater pollution. (C) 2020 Elsevier Ltd. All rights reserved.
机译:河床沉积物是河流生态系统中的界面层,连接着覆盖的水和散塞区。磷(P)的磷(P)的运输行为被认为是淡水富营养化的主要原因,河床沉积物中尚不清楚。了解河床沉积物对P传输的影响是开发适当战略以减少潜在地下水污染的必要必要条件。在这项研究中,从北云江,中国的上游,中游和下游部分收集河床沉积物,并填充到垂直的土柱中,以进行浸出实验以量化P传输特性。此外,通过进行P吸附和解吸的实验室批量试验进一步探索冲击机制。结果表明,在土柱浸出实验中,大约80%的P可以被河床沉积物吸附,并且在解吸中观察到尾翼现象。通过逆转分散方程评估河床沉积物的液压导电性能,显示从上游逐渐降低的吸附能力,从吸附 - 解吸热力学和动力学批量试验中获得的结果支持。估计的每年浸出量为下游部分上游部分中的60.72g /(2)a)增加到132.31g /(m2a)。河床沉积物作为P的源或水槽的作用可能由其粗砂颗粒含量和平均平衡P浓度(EPC0)决定。 P与其他形式的营养素之间的竞争关系也对其源区的作用具有重要影响。这些研究结果表明,在北云河下游部分中最需要预防潜在的P浸出,以及应制定相应的控制策略来避免地下水污染。 (c)2020 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2020年第3期|115153.1-115153.11|共11页
  • 作者单位

    Cornell Univ Dept Biol & Environm Engn Ithaca NY 14853 USA;

    China Agr Univ Coll Water Conservancy & Civil Engn Beijing 100083 Peoples R China;

    China Agr Univ Coll Water Conservancy & Civil Engn Beijing 100083 Peoples R China;

    China Agr Univ Coll Water Conservancy & Civil Engn Beijing 100083 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Leaching; Column; Advection-dispersion; Phosphorus pollution; CXTFIT;

    机译:浸出;柱;平程分散;磷污染;Cxtfit;

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