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Combining multi-physical measurements to quantify bedload transport and morphodynamics interactions in an Alpine braiding river reach

机译:结合多物理场测量来量化高山辫状河河段的基床输运和形态动力学相互作用

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摘要

Understanding the interactions between bedload transport and morpholdynamics in braided streams has important applications in river management and restoration. Direct field measurements addressing this question are however scarce as they are often challenging to perform. Here, we report an extensive two-month field campaign in an Alpine braided reach (La Severaisse river, French Alps) that experienced predictable daily peak discharge (48 events observed) generating significant bedload transport and morphological changes during the melting season. We monitored these processes using a wide range of direct and indirect techniques (bedload sampling, continuous seismic measurements, pebbles tracking, topographic surveys, remote sensing using ground control cameras and drone flights). Doing so, surrogate measurements allowed to extend temporally discrete manual bedload sampling, and to extend spatially local riverbed cross section measurements. These measurements provide unique complementary constraints on the targeted physics, at various spatial and temporal scales which enabled us to draw robust conclusions. Data showed a progressive decrease in bedload transport for a given flow rate along the two months period. Simultaneously, river morphology in the braided sections changed from an incised to a more distributed configuration which led to a decrease of local maxima in dimensionless shear stresses in the braided reach for similar flow conditions. This control of bedload transport by maximum local shear stresses was in line with tracked pebble surveys indicating that coarse bedload particles were mostly transported in the main active channel. At the reach scale, this transport was found to be more efficient in laterally confined sections than in braided ones which has important implications in terms of bedload estimation in alternative confined and braided (unconfined) rivers. Finally, this study highlight the interest to combine a large variety of traditional and innovative measurements techniques to better understand complex sediment transport processes in the field. (C) 2019 Elsevier B.V. All rights reserved.
机译:理解辫状河床质输运与形态动力学之间的相互作用在河流管理和恢复中具有重要的应用。然而,解决直接问题的直接现场测量很困难,因为执行起来通常很困难。在这里,我们报告了一个高山辫状河段(法国阿尔卑斯山的拉塞韦莱斯河)进行了为期两个月的野外活动,该活动经历了可预见的每日高峰排放(观测到48个事件),在融化季节产生了明显的床荷运输和形态变化。我们使用广泛的直接和间接技术(床载采样,连续地震测量,卵石跟踪,地形勘测,使用地面控制相机的遥感和无人机飞行)来监视这些过程。这样做,替代测量可以扩展时间上离散的手动基床采样,并扩展空间上局部的河床横截面测量。这些测量结果在各种时空尺度上对目标物理学提供了独特的补充约束,使我们能够得出可靠的结论。数据显示,在给定的流速下,两个月内的床载运输量逐渐减少。同时,编织段中的河流形态从切变变为分布更广,这导致相似流量条件下编织段中无因次剪应力的局部最大值减小。通过最大局部剪切应力控制床荷运输与跟踪的卵石调查一致,表明粗床荷颗粒大部分在主要活动通道中运输。在河段范围内,发现这种输送方式在横向密闭段中比在辫状段中更有效,这对替代密闭和辫状(非密闭)河流的河床负荷估算具有重要意义。最后,这项研究突出了将多种传统和创新的测量技术相结合以更好地了解野外复杂泥沙输送过程的兴趣。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Geomorphology 》 |2020年第15期| 106877.1-106877.17| 共17页
  • 作者

  • 作者单位

    Univ Grenoble Alpes ETNA Irstea Grenoble France;

    Univ Grenoble Alpes IGE Grenoble INP CNRS IRD Grenoble France;

    Univ Grenoble Alpes ETNA Irstea Grenoble France|Univ Grenoble Alpes IGE Grenoble INP CNRS IRD Grenoble France;

    Univ Lyon UMR CNRS EVS 5600 Lyon France;

    Univ Grenoble Alpes GIPSA Lab Grenoble INP CNRS Grenoble France;

    Univ Lumiere Lyon 2 UMR 5600 CNRS Environm Ville Soc Bron France;

    EDF DTG Grenoble France;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Multi-physical measurements; Braided river; Bedload transport; Morphodynamic;

    机译:多物理量测量;辫状河载重运输;形态动力学;

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