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Modelling the impact of runoff generation on agricultural and urban phosphorus loading of the subtropical Poyang Lake (China)

机译:径流生成对亚热带鄱阳湖农业和城市磷负荷的影响建模(中国)

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摘要

Water quality degradation and eutrophication in surface water bodies caused by excessive phosphorus loads from agriculture and urbanisation are widespread problems. Although phosphorus (P) is often the limiting factor of aquatic ecosystems, only few studies have characterised the primary factors that influence P export in subtropical monsoon catchments. This study aims to assess the temporal and spatial variations in P fluxes, and to investigate the factors controlling P export in a subtropical catchment. Runoff and P export in the Le An River catchment, which flow to Poyang Lake (China) were evaluated using the HYPE model. Sensitivity analysis and calibration of hydrological and P transport parameters were undertaken using PEST. Results show that: (a) HYPE reproduced sufficiently well (NSE ≥ 0.73, PBIAS ≤ 14.5) the stream flow dynamics for widely varying climatic conditions and across six sub-catchments of contrasting physiographic characteristics; (b) HYPE captured intra-annual patterns of total P (TP) loads, although with overestimation of annual TP loads by 8.5-47.0 across two monitoring sites; (c) TP loads had the ranges between 0.24 and 0.88 kg/ha/yr and 4.31-4.69 kg/ha/ yr from forest-dominant upstream areas and the downstream plains region, respectively, with the latter being more urbanised and having higher percentage of agriculture; (d) Soil erosion from surface runoff and adsorption/ desorption of soil P are the main factors controlled P export from the catchment; (e) most P export occurred during March-August when rainfall-runoff is highest and agricultural practices are most active; (f) stream TP concentrations were greatly affected by point source inputs, especially during low-flow conditions in downstream plains region. This study indicates that measures to reduce TP export to receiving water bodies in subtropical monsoon areas, like Poyang Lake, should focus on managing diffuse sources from soil erosion and surface runoff etc., whereas improvem
机译:农业和城市化导致的地表水体水质退化和富营养化是普遍存在的问题。尽管磷(P)通常是水生生态系统的限制因素,但只有少数研究描述了影响亚热带季风集水区磷输出的主要因素。本研究旨在评估副热带集水区磷通量的时空变化,并研究控制磷输出的因素。采用HYPE模型评价流向鄱阳湖(中国)的乐安河流域径流和磷输出量。使用PES对水文和磷输运参数进行了敏感性分析和校准。结果表明:(a) HYPE再现得足够好(NSE ≥ 0.73, |PBIAS|≤ 14.5%),在气候条件变化很大的情况下,以及六个具有不同地貌特征的子集水区的河流流动动态;(b) HYPE捕获了总磷(TP)负荷的年内模式,尽管在两个监测点中高估了8.5-47.0%的年TP负荷;(c) TP负荷范围为0.24-0.88公斤/公顷/年和4.31-4公斤/公顷/年。69公斤/公顷/年,分别来自以森林为主的上游地区和下游平原地区,后者城市化程度更高,农业比例更高;(d) 地表径流造成的土壤侵蚀和土壤磷的吸附/解吸是控制流域磷输出的主要因素;(e)大多数磷出口发生在3-8月,此时降雨径流量最高,农业实践最活跃;(f)河流TP浓度受点源输入影响很大,特别是在下游平原地区的低流量条件下。本研究表明,减少TP向鄱阳湖等亚热带季风区接收水体的出口的措施应侧重于管理土壤侵蚀和地表径流等扩散源,同时改善

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  • 来源
    《Journal of Hydrology》 |2020年第3期|125490-1-125490-13|共13页
  • 作者单位

    Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 East Beijing Road, 210008 Nanjing,China;

    College of Science and Engineering, and National Centre for Groundwater Research and Training, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia;

    Department of Geography and Environmental Studies, Ryerson University, Toronto, 350 Victoria Street, Ontario, CanadaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, A-1 Fuxing Road,Haidian District, 100038 Beijing, ChinaState Key Laboratory of Hydrology and Water Resources and Hydraulic Engineering Science, Nanjing Hydraulic Research Institute, 223 Guangzhou Road, 210029 Nanjing, ChinaJiangxi Province Hydrology Bureau, 1499 Jiangnan Street, Xihu District, 330008 Nanchang, ChinaDepartment of Aquatic Ecosystem Analysis and Management, Helmholtz Centre for Environmental Research-UFZ, 39114 Magdeburg, Germany;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 英语
  • 中图分类 水文科学(水界物理学);
  • 关键词

    Phosphorus export; Rainfall-runoff; Sensitivity analysis; HYPE; Catchment model; Nutrient loads;

    机译:磷出口;降雨-径流;敏感度分析;炒作;集水区模型;养分负荷;
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