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Contribution of point sources and non-point sources to nutrient and carbon loads and their influence on the trophic status of the Ganga River at Varanasi, India

机译:点源和非点源对养分和碳负荷的贡献及其对印度瓦拉纳西恒河营养状况的影响

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摘要

To determine the possible contributions of point and non-point sources to carbon and nutrient loading in the Ganga River, we analyzed N, P, and organic carbon (OC) in the atmospheric deposits, surface runoff, and in the river along a 37-km stretch from 2013 to 2015. We also assessed the trophic status of the river as influenced by such sources of nutrient input. Although the river N, P, and productivity showed a declining trend with increasing discharge, runoff DOC and dissolved reactive phosphorus (DRP) increased by 88.05 and 122.7% between the Adpr and Rjht sites, indicating contributions from atmospheric deposition (AD) coupled with land use where agriculture appeared to be the major contributor. Point source input led to increased river concentrations of NO3-, NH4+, DRP, and DOC by 10.5, 115.9, 115.2, and 67.3%, respectively. Increases in N, P, and productivity along the gradient were significantly negatively correlated with river discharge (p < 0.001), while river DOC and dissolved silica showed positive relationships. The results revealed large differences in point and non-point sources of carbon and nutrient input into the Ganga River, although these variations were strongly influenced by the seasonality in surface runoff and river discharge. Despite these variations, N and P concentrations were sufficient to enhance phytoplankton growth along the study stretch. Allochthonous input together with enhanced autotrophy would accelerate heterotrophic growth, degrading the river more rapidly in the near future. This study suggests the need for large-scale inter-regional time series data on the point and non-point source partitioning and associated food web dynamics of this major river system.
机译:为了确定点源和非点源对恒河中碳和养分含量的可能贡献,我们分析了大气沉积物,地表径流和沿37-径流河中的氮,磷和有机碳(OC)。从2013年到2015年,这条河的延伸距离为1公里。我们还评估了河流的营养状况,受营养输入来源的影响。尽管河流N,P和生产力随着排放量的增加而呈下降趋势,但Adpr和Rjht站点之间的径流DOC和溶解性反应性磷(DRP)分别增加了88.05和122.7%,表明大气沉降(AD)加上土地的贡献在农业似乎是主要贡献者的地方使用。点源输入导致河流中NO3-,NH4 +,DRP和DOC的浓度分别增加了10.5%,115.9、115.2和67.3%。氮,磷和生产力沿梯度的增加与河流流量呈显着负相关(p <0.001),而河流DOC和溶解的二氧化硅呈正相关。结果表明,进入恒河的碳源和养分的点源和面源差异很大,尽管这些变化受地表径流和河流流量的季节性影响很大。尽管存在这些差异,但氮和磷的浓度仍足以促进浮游植物在整个研究过程中的生长。异源输入和增强的自养能力将加速异养生长,在不久的将来会更快地降解河流。这项研究表明,需要有关该主要河流系统的点和非点源分区以及相关食物网动态的大规模区域间时间序列数据。

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2017年第9期|475.1-475.19|共19页
  • 作者

    Yadav Amita; Pandey Jitendra;

  • 作者单位

    Banaras Hindu Univ, Ganga River Ecol Res Lab, Environm Sci Div, Ctr Adv Study Bot,Inst Sci, Varanasi 221005, Uttar Pradesh, India;

    Banaras Hindu Univ, Ganga River Ecol Res Lab, Environm Sci Div, Ctr Adv Study Bot,Inst Sci, Varanasi 221005, Uttar Pradesh, India;

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

    Atmospheric deposition; DOC; Ganga River; Surface runoff; Point source; Trophic status;

    机译:大气沉降DOC甘加河地表径流点源营养状态;
  • 入库时间 2022-08-17 13:25:55

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