Bedload Transport and Its Implication on Bed Morphology at a River Confluence

IF 0.9 4区 环境科学与生态学 Q4 WATER RESOURCES
Nabina Khanam, Sushant Kumar Biswal
{"title":"Bedload Transport and Its Implication on Bed Morphology at a River Confluence","authors":"Nabina Khanam, Sushant Kumar Biswal","doi":"10.1134/s0097807823601310","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>River confluences are the key elements within fluvial systems, where three-dimensional flow fields and sedimentation patterns can have a substantial effect on the hydraulics, bed morphology of stream courses, and environments. The present study is configured to realize the alterations in bedload transportation and in bedform at confluence channel in relation to particular hydrological occurrences. It is anticipated that the patterns of the flow attributes following the confluence to be different from those in the conditions reported in other publication. Therefore, this article concisely reports the various flow aspects, examines the corresponding river bed patterns, and provides a brief description of the different flow properties. On the basis of field findings in response to fluctuation in the flow of contributory tributaries, the recorded morphological and sedimentological changes are explained. To accomplish this, bedload transport, bed surveys, and particle size distribution measurements were carried out at the study site during different hydrological seasons at intervals of two months from January 2018 to March 2019. The three major goals of this work were to comprehend the symmetry between two confluence channels, estimate bedload transport, and investigate the consequences of net fluvial behavior on bedform dynamics. The short-term impacts of stream flow irregularity on channel morphology and particle structures were discovered by repeated transect studies and bed material sampling at a small asymmetrical river junction. Results show that the confluence involves the shifting in the scour region, frequent erosion and deposition of sediments, and bar development at the downstream confluence as flow rate fluctuates following the hydrological changeability in the confluence channels. The average bedload at the confluence appears to be irregular in favor of the tributary, since two-thirds of the total bedload was carried across the shallow zone of the cross-section. A high speed digital camera was used to detect sand ripples, and video technique was utilized to obtain statistics on the presence of ripple geometries. Asymmetric two-dimensional ripples were observed in relatively calm weather conditions and in moderate winds. It was discovered that ripples generated by the two-dimensional flow were supplanted by flatbed circumstances and the normal two-dimensional wash-out ripples after the medium wind periods, demonstrating that the presence of a combined flow increases the induced bed shear stress.</p>","PeriodicalId":49368,"journal":{"name":"Water Resources","volume":"10 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2024-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Water Resources","FirstCategoryId":"93","ListUrlMain":"https://doi.org/10.1134/s0097807823601310","RegionNum":4,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"WATER RESOURCES","Score":null,"Total":0}
引用次数: 0

Abstract

River confluences are the key elements within fluvial systems, where three-dimensional flow fields and sedimentation patterns can have a substantial effect on the hydraulics, bed morphology of stream courses, and environments. The present study is configured to realize the alterations in bedload transportation and in bedform at confluence channel in relation to particular hydrological occurrences. It is anticipated that the patterns of the flow attributes following the confluence to be different from those in the conditions reported in other publication. Therefore, this article concisely reports the various flow aspects, examines the corresponding river bed patterns, and provides a brief description of the different flow properties. On the basis of field findings in response to fluctuation in the flow of contributory tributaries, the recorded morphological and sedimentological changes are explained. To accomplish this, bedload transport, bed surveys, and particle size distribution measurements were carried out at the study site during different hydrological seasons at intervals of two months from January 2018 to March 2019. The three major goals of this work were to comprehend the symmetry between two confluence channels, estimate bedload transport, and investigate the consequences of net fluvial behavior on bedform dynamics. The short-term impacts of stream flow irregularity on channel morphology and particle structures were discovered by repeated transect studies and bed material sampling at a small asymmetrical river junction. Results show that the confluence involves the shifting in the scour region, frequent erosion and deposition of sediments, and bar development at the downstream confluence as flow rate fluctuates following the hydrological changeability in the confluence channels. The average bedload at the confluence appears to be irregular in favor of the tributary, since two-thirds of the total bedload was carried across the shallow zone of the cross-section. A high speed digital camera was used to detect sand ripples, and video technique was utilized to obtain statistics on the presence of ripple geometries. Asymmetric two-dimensional ripples were observed in relatively calm weather conditions and in moderate winds. It was discovered that ripples generated by the two-dimensional flow were supplanted by flatbed circumstances and the normal two-dimensional wash-out ripples after the medium wind periods, demonstrating that the presence of a combined flow increases the induced bed shear stress.

Abstract Image

河流汇合处的床面负荷迁移及其对河床形态的影响
摘要 河流汇流处是河流系统中的关键要素,其三维流场和沉积模式可对水力学、河道床面形态和环境产生重大影响。本研究的目的是了解与特定水文现象相关的汇流河道床面负荷运输和床面形态的变化。预计汇流后的水流属性模式与其他出版物中报道的情况有所不同。因此,本文简明扼要地报告了各方面的水流情况,研究了相应的河床形态,并简要介绍了不同的水流属性。根据对支流流量波动的实地调查结果,解释了所记录的形态和沉积学变化。为此,在 2018 年 1 月至 2019 年 3 月的不同水文季节,每隔两个月在研究地点进行了床面负荷迁移、床面调查和粒径分布测量。这项工作的三大目标是理解两条汇流河道之间的对称性、估算床面负荷迁移量以及研究净河道行为对床面动力学的影响。通过在一个小型非对称河流交汇处反复进行横断面研究和床面物质取样,发现了水流不规则性对河道形态和颗粒结构的短期影响。结果表明,随着汇流河道水文变化率的波动,汇流河道的冲刷区发生移动,沉积物频繁侵蚀和沉积,下游汇流处出现了条形发育。由于三分之二的总床面负荷被带过断面的浅水区,因此汇合处的平均床面负荷似乎对支流有利。我们使用高速数码相机检测沙质波纹,并利用视频技术获得波纹几何形状的统计数据。在相对平静的天气条件和中等风力下观察到了不对称的二维波纹。结果发现,二维流产生的波纹在中风期后被平板情况和正常的二维冲刷波纹所取代,这表明联合流的存在增加了诱导的床面剪应力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Water Resources
Water Resources 环境科学-水资源
CiteScore
1.60
自引率
20.00%
发文量
86
审稿时长
6-12 weeks
期刊介绍: Water Resources is a journal that publishes articles on the assessment of water resources, integrated water resource use, water quality, and environmental protection. The journal covers many areas of research, including prediction of variations in continental water resources and regime; hydrophysical, hydrodynamic, hydrochemical and hydrobiological processes, environmental aspects of water quality and protection; economic, social, and legal aspects of water-resource development; and experimental methods of studies.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信