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Assessment of lake eutrophication recovery: the filtering trajectory method (FTM) and its application to Dianchi Lake, China

机译:湖泊富营养化恢复评估:过滤轨迹法(FTM)及其在中国滇池的应用

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摘要

Lake ecosystems follow convoluted trajectories impacted by climate change and human stress. In this study, we developed the filtering trajectory method (FTM), a mathematical model, to establish the empirical relationships between chlorophyll a (CHLa) and nutrient concentrations in eutrophic Dianchi Lake, China. FTM can identify cause-effect relationships over time in apparently stochastic data, and a filtering trajectory diagram is used to describe the driving forces of the complex trajectories of individual lake ecosystems. Our analysis showed that the nutrient concentrations of overlying water in Dianchi Lake have decreased to the levels recorded in the late 1980s and early 1990s, but CHLa has not declined synchronously. The ecosystem trajectories revealed the ups and downs of complex processes, which can be divided into four stages: (1) pollution stage (1988-1999): a macrophyte-to-phytoplankton transition occurred with an increase in nutrient inputs and a rise in temperature; (2) initial restoration stage (2000-2006): the response of CHLa to the nutrient load reduction presented an apparent time lag, or hysteresis effect; (3) recurrence stage (2007-2011): excessive water consumption and continuous drought in the watershed resulted in an increasing trend in CHLa, TP and TN; and (4) re-restoration stage (2012-2016): the implementation of a water-replenishment project resulted in a declining trend. Our approach can greatly improve our understanding of how lakes respond to broad changes in environmental conditions (e.g. climate warming) and improve water quality via targeted nutrient management, from static to dynamic management and from One Standard for One Lake to Multiple Standards for One Lake.
机译:湖泊生态系统遵循受气候变化和人类压力影响的曲折轨迹。在这项研究中,我们开发了一种数学模型过滤轨迹法(FTM),以建立中国富营养化滇池中叶绿素a(CHLa)与养分浓度之间的经验关系。 FTM可以识别明显随机数据中随时间变化的因果关系,并使用过滤轨迹图来描述单个湖泊生态系统复杂轨迹的驱动力。我们的分析表明,滇池上覆水的养分浓度已降至1980年代末和1990年代初的水平,但CHLa并没有同步下降。生态系统的轨迹揭示了复杂过程的起伏,可以将其分为四个阶段:(1)污染阶段(1988-1999年):发生了大型植物向浮游植物的过渡,其养分投入增加且温度升高; (2)初始恢复阶段(2000-2006年):CHLa对营养物负荷减少的响应表现出明显的时滞或滞后效应; (3)复发期(2007-2011年):流域过度用水和持续干旱导致CHLa,TP和TN呈上升趋势; (4)恢复阶段(2012-2016年):补水工程的实施导致下降趋势。我们的方法可以极大地增进我们对湖泊如何应对环境条件的广泛变化(例如气候变暖)的了解,并通过有针对性的养分管理从静态到动态管理以及从一个湖泊的一个标准到一个湖泊的多个标准来改善水质。

著录项

  • 来源
    《Environmental Monitoring and Assessment》 |2019年第6期|360.1-360.9|共9页
  • 作者

    Zhao Jian; Fu Guo;

  • 作者单位

    Chinese Res Inst Environm Sci, State Lab Environm Criteria & Risk Assessment, Beijing 100012, Peoples R China;

    Chinese Res Inst Environm Sci, State Lab Environm Criteria & Risk Assessment, Beijing 100012, 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《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Recovery; Eutrophication; Chlorophyll a; Total phosphorus; Dianchi Lake;

    机译:恢复;富营养化;叶绿素a;总磷;滇池;
  • 入库时间 2022-08-18 04:24:19

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