Estimation of bed material transport in gravel-bed streams using the virtual velocity approach: Insights from the North-Western Himalayas, India

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-06-23 DOI:10.1002/esp.5910
Anshul Yadav, Sumit Sen, Luca Mao, Marwan A. Hassan
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Abstract

This study focuses on evaluating the sediment mobility and transport patterns in two Himalayan rivers (Aglar and Paligad Rivers) during monsoon and non-monsoon flows. The virtual velocity approach involving the measurements of the bed proportional mobility (Y), active layer depth (ds), displacement length and virtual velocity of mobilized grains was employed. Both local (0.5 m subsections) and wetted cross-sectional average parameters were used. While using local parameters the total annual bed material transport was estimated to be 67 100 (±20 400 t) and 18 400 t (±6000 t) in the Aglar and Paligad Rivers, respectively. Of this, nearly 60% of transport occurred during the monsoon and the overall contribution of partial transport (PT) remained low (<6%). However, based on cross-section average parameters, total transport was estimated to be 42 300 (±15 800 t) and 12 200 t (±4700 t), in Aglar and Paligad, respectively, with nearly 79% and 68% occurring during the monsoon. Moreover, the contribution of PT increased to nearly 18% and 29% for the Aglar and Paligad Rivers, respectively. Additionally, the dependence of PT on Y and full transport on ds results in an abrupt shift in transport rates at the transition from partial to full transport, causing discontinuity in transport curves. Therefore, a unified function was proposed to represent the extent of transport for both partial and full transport, yielding continuous transport curves. These findings are particularly relevant for efficient river management as the region houses several hydropower plants and is highly vulnerable to climate change.

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利用虚拟速度法估算砾石溪流的床面物质迁移:印度西北喜马拉雅山脉的启示
本研究的重点是评估喜马拉雅山脉两条河流(阿格拉尔河和帕利加德河)在季风和非季风水流期间的泥沙流动和迁移模式。研究采用了虚拟速度法,包括测量河床比例移动量(Y)、活动层深度(ds)、位移长度和移动颗粒的虚拟速度。采用了局部参数(0.5 米分段)和湿润断面平均参数。使用局部参数时,估计阿格拉河和帕利加德河的年河床物质迁移总量分别为 67 100 吨(±20 400 吨)和 18 400 吨(±6000 吨)。其中,近 60% 的迁移发生在季风期间,部分迁移(PT)的总体贡献率仍然很低(<6%)。然而,根据横截面平均参数,估计阿格拉河和帕利加德河的总漂移量分别为 42 300 吨(±15 800 吨)和 12 200 吨(±4700 吨),其中近 79% 和 68% 发生在季风期间。此外,PT 对阿格拉尔河和帕利加德河的贡献率分别增至近 18% 和 29%。此外,PT 对 Y 的依赖性和完全输运对 ds 的依赖性导致输运率在从部分输运向完全输运过渡时突然转变,造成输运曲线的不连续性。因此,我们提出了一个统一的函数来表示部分输运和全输运的输运范围,从而得到连续的输运曲线。由于该地区拥有多个水电站,并且极易受到气候变化的影响,因此这些发现对于有效管理河流尤其重要。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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