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首页> 外文期刊>Journal of hydro-environment research >Hydrodynamic modeling and characterizing of Lagrangian flows in the West Scott Creek wetlands system, South Carolina
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Hydrodynamic modeling and characterizing of Lagrangian flows in the West Scott Creek wetlands system, South Carolina

机译:南卡罗来纳州西斯科特克里克湿地系统中拉格朗日流的水动力模型和特征

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With increased recognition of the value of tidal wetlands and their defining hydrology, the need for better understanding of tidal flow and mixing characteristics is vital to any wetland restoration and enhancement projects and studies. A numerical modeling study was carried out to study the mixing and transport processes in the tide dominated West Scott Creek Estuary, South Carolina. The West Scott Creek estuary is a system of meandering tidal creeks and salt marsh between Edisto Island and the Edisto Beach barrier island. A coupled, depth-integrated hydrodynamic and particle transport model was developed. The model was calibrated and verified against a set of field-measured hydrodynamic data and the model-predicted water elevations, velocities and discharges were in good agreement with the field measurements. The hydrodynamically calibrated model was coupled with a particle tracking module to quantify the residence time distribution and associated transport mechanisms in a spatially varying situation. Computed residence time distribution, under tidal forcing, indicates a strong spatial variation and a non-monotonic distribution along the thalweg of the creek. The model computed a residence time of 4.92 days at the head of the creek. Numerical analysis of the Lagrangian flow field indicated varying mixing regions (strong and weak) within the wetland and the result is anticipated to provide useful information to assess the impact of coastal development in and around the West Scott Creek estuary including the restoration of tidal hydrology.
机译:随着人们对潮汐湿地价值及其确定的水文学的认识得到提高,对潮汐流和混合特性的更好了解对于任何湿地恢复和改善项目和研究都至关重要。进行了数值模拟研究,以研究南卡罗来纳州西斯科特克里克河口占主导的潮汐的混合和输运过程。西斯科特克里克河口是由埃迪斯托岛和埃迪斯托海滩屏障岛之间蜿蜒的潮汐小溪和盐沼组成的系统。建立了深度耦合的流体动力学和颗粒传输的耦合模型。根据一组现场测量的水动力数据对模型进行了校准和验证,模型预测的水位,速度和流量与现场测量结果非常吻合。流体动力学校准的模型与粒子跟踪模块耦合,以量化在空间变化情况下的停留时间分布和相关的传输机制。在潮汐强迫作用下,计算出的停留时间分布表明沿小河沿岸有很强的空间变化和非单调分布。该模型计算出在小溪顶部的停留时间为4.92天。拉格朗日流场的数值分析表明,湿地内混合区域(强和弱)变化,并且预期结果将提供有用的信息,以评估西斯科特克里克河口及其周围沿海发展的影响,包括潮汐水文学的恢复。

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