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Contaminant exchange rates in estuaries - New formulae accounting for advection and dispersion

机译:河口中的污染物汇率-计算对流和扩散的新公式

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摘要

The transport timescales of water in an estuary are important measurements for monitoring pollution threats to the estuarine ecosystem. In this study we re-evaluated the application of simple analytical solutions to estimate these timescales and found that the Land Ocean Interaction Costal Zone model (LOI-CZ) uses similar equation as from the fresh water fraction model, and thus often resulting in shortened transport timescales. Therefore, the LOICZ model is neither based upon the well-known Knudsen relation nor Fischer formulation. Three transport timescales, namely water renewal, residence time and exposure time were calculated using analytical solutions for a range of estuaries worldwide. The analytical results were compared with available estimates of residence times from numerical models. The theoretical for-rrjulation from the LOICZ, the fresh water fraction model, and a newly proposed modified LOICZ model were used to calculate water renewal. Residence times and exposure times were calculated using the Constituent-oriented Age and Residence time Theory (CART). The modified LOICZ model was found to be the most comparable to residence times from numerical models, with r~2 ~ 0.7. In addition to the proposed modified LOICZ model (which uses Fischer formulation), we have developed an advection-disper-sion timescale diagram. This graphic conceptual model provides a visual representation of the relative contribution of advective and dispersive processes to water renewal for different estuaries. Estuaries can be categorized as either dominated by dispersion, dominated by advection, or having dispersion and advection of similar magnitude.
机译:河口水的运输时间尺度是监测河口生态系统污染威胁的重要指标。在这项研究中,我们重新评估了简单分析方法在估算这些时间尺度方面的应用,发现陆地海洋相互作用沿海带模型(LOI-CZ)使用的公式与淡水分数模型相似,因此通常会缩短运输时间时间尺度。因此,LOICZ模型既不是基于众所周知的Knudsen关系,也不是基于Fischer公式。使用分析方法针对全球范围内的一系列河口计算了三个运输时间表,即换水,停留时间和暴露时间。将分析结果与数值模型可得到的停留时间估计值进行了比较。 LOICZ的理论计算,淡水分数模型和新提出的改良LOICZ模型用于计算水的更新。停留时间和暴露时间使用面向成分的年龄和停留时间理论(CART)计算。从数值模型发现改进的LOICZ模型与停留时间最可比,r〜2〜0.7。除了提出的改进的LOICZ模型(使用菲舍尔公式)之外,我们还开发了对流-弥散-时间尺度图。该图形概念模型直观地表示了平流和分散过程对不同河口换水的相对贡献。河口可以分为以散布为主,以平流为主,或散布和平流具有相似的大小。

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  • 来源
    《Progress in Oceanography》 |2014年第1期|139-153|共15页
  • 作者单位

    School of Engineering and Physical Sciences, James Cook University, Townsvitle, QLD 4811, Australia,Oceanografic Institute of University of Sao Paulo, Sao Paulo, SP CEP: 05508120, Brazil,School of Physical, Environmental and Mathematical Sciences, University of New South Wales at Australian Defence Force Academy (UNSW-ADFA), ACT 2600, Australia;

    School of Engineering and Physical Sciences, James Cook University, Townsvitle, QLD 4811, Australia;

    Universite catholique de Louvain (UCL), Institute of Mechanics, Materials and Civil Engineering (IMMC), 4 Avenue Georges Lemaxtre, Bte L4.05.02, B-1348 Louvain-la-Neuve, Belgium,Universite catholique de Louvain (UCL), Earth and Life Institute (ELI), Georges Lemaxtre Centre for Earth and Climate Research (TECLIM), 3 Place Louis Pasteur, Bte L4.03.08, B-1348 Louvain-la-Neuve, Belgium;

    National Oceanography Centre, Joseph Proudman Building, 6 Brownlow Street, Liverpool L3 5DA, UK;

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