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

机译:湖富营养化复苏评估:过滤轨迹方法(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卷积轨迹。在这项研究中,我们开发了滤波轨迹方法(FTM),一种数学模型,建立叶绿素A(CHLA)与营养素滇池湖泊之间的效力关系。 FTM可以在明显随机数据中识别随时间随时间的原因关系,并且过滤轨迹图用于描述个体湖泊生态系统的复杂轨迹的驱动力。我们的分析表明,滇池覆盖水的营养浓度降低到20世纪80年代后期和20世纪90年代初期记录的水平,但CHLA并没有同步下降。生态系统轨迹揭示了复杂过程的UPS和下降,可分为四个阶段:(1)污染阶段(1988-1999):营养投入增加和温度升高发生宏观物质对浮游植物过渡。 ; (2)初始恢复阶段(2000-2006):CHLA对营养负荷减少的响应呈现出表观时间滞后或滞后效应; (3)复发阶段(2007-2011):流域的过量消耗和持续干旱导致CHLA,TP和TN的趋势越来越大; (4)重新修复阶段(2012-2016):水补货项目的实施导致了趋势下降。我们的方法可以大大提高我们对湖泊如何应对环境条件的广泛变化(例如气候变暖)并通过有针对性的营养管理提高水质的理解,从静态到动态管理,从一个湖泊标准到一个湖泊的多标准。

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;

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