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A combined field sampling-modeling approach for computing sediment transport during flash floods in a gravel-bed stream

机译:一种组合场采样建模方法,用于计算砾石床流中山洪暴发期间的泥沙输送

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摘要

[1] Field sampling in unwadeable and flashy flood events encounters the problem that lateral variability of flow hydraulics and sediment transport cannot be captured adequately, and there is also an accuracy problem because parameters change while being measured. Moreover, event based gravel-sand mixed transport data in rapidly changing conditions are largely missing, in particular for gravel-bed rivers in small catchments. In this study, field measurements of bed load, suspended load, flow velocities, water depths, and cross-section geometry were collected during flood events at a monitoring station near the mouth of the Versilia River, Italy. Since the observed hydrographs are characterized by short durations, to the order of a few hours, an analysis of the lateral and temporal flow variability was carried out to enable the design of a sampling strategy and to minimize the errors created by the time variations of discharge associated with unsteady flow conditions. The measurements were interpreted using a 1-D hydro-morphodynamic numerical model simulating the dynamics of flow and sediment discharges during a flood event for a given return period. The flow and sediment rating curves were then developed through an integrated approach combining different methodologies: field measurements, laboratory analyses, and mathematical modeling. The developed approach allows one to capture the main physical mechanisms associated to the transport of sand-gravel mixtures, such as selective transport, and the hysteretic behavior of sediment transport produced by rapid and intense flood events.
机译:[1]在无法进退的暴雨事件中进行现场采样会遇到一个问题,即无法充分捕获流动水力和泥沙输送的横向变化,并且由于测量时参数会发生变化,因此还存在精度问题。此外,在快速变化的条件下,尤其是在小流域的砾石河道中,缺少基于事件的砾石-砂混合运输数据。在这项研究中,在意大利Versilia河口附近的监测站发生洪水事件期间,收集了床荷载,悬浮荷载,流速,水深和横截面几何形状的现场测量结果。由于观测到的水文图的特征是持续时间短至数小时左右,因此对侧向和时间流量变化进行了分析,以设计采样策略并使排放时间随时间变化而产生的误差最小化。与不稳定的流动条件有关。使用一维水力-形态动力学数值模型解释了测量结果,该模型模拟了给定返回期洪水事件期间的水流和泥沙排放动力学。然后通过综合方法将流量和沉积物的额定曲线结合不同的方法:田间测量,实验室分析和数学建模。所开发的方法使人们能够捕获与砂砾混合料的运输相关的主要物理机制,例如选择性运输以及快速和强烈洪水事件产生的沉积物运输的滞后行为。

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  • 来源
    《Water resources research》 |2013年第10期|6642-6655|共14页
  • 作者单位

    CERAFRI-Center of Research and Advanced Education for Hydrogeological Risk Prevention, via Ⅺ Febbraio 2, IT-55040 Retignano di Stazzema (LU), Italy;

    Department of Civil and Environmental Engineering, University of Florence, Firenze, Italy;

    Department of Civil and Environmental Engineering, University of Florence, Firenze, Italy;

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  • 正文语种 eng
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