Transport of suspended sediments under the influence of bank macro‐roughness

机译：银行宏观粗糙度影响下悬浮沉积物的运输

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Abstract >River restoration works often include measures to promote morphological diversity and enhance habitat suitability. One of these measures is the creation of macro‐roughness elements, such as lateral cavities and embayments, in the banks of channelized rivers. However, in flows that are heavily charged with fine sediments in suspension, such as glacier‐fed streams and very low‐gradient reaches of large catchment rivers, these lateral cavities may trap these sediments. Consequently, the morphological changes may be affected, and the functionality of the restoration interventions may be compromised. Herein, we analyse the influence of these macro‐roughness elements on the transport of fine sediments in the main channel. Laboratory tests with uniform flow charged with sediments in a channel with banks equipped with large‐scale rectangular roughness elements were carried out. The laboratory experiments covered a wide range of rectangular cavity geometrical configurations and shallowness ratios. The influence of key parameters such as flow shallowness, geometric ratios of the cavities and initial sediment concentration was tested. Surface particle image velocimetry, sediment samples and temporal turbidity records were collected during the experiments. The amount of sediments captured by the cavities, the temporal evolution of the concentration of sediments in suspension and the flow hydrodynamics are cross‐analysed and discussed. It is shown that the trapping efficiency of the macro‐roughness elements is a clear function of the channel geometry and the shallowness of the flow. Copyright ? 2017 John Wiley & Sons, Ltd. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“esp4243-abs-0001”> <标题类型=“main”>抽象</ title> < P>河流修复工作往往包括促进形态多样性的措施，提高栖息地适用性。其中一个措施是在通道化河流的河岸中创建宏观粗糙度元素，例如横向腔和扶手。然而，在悬浮液中大量收取细沉积物的流动中，例如冰川喂料的溪流和大型集水河的非常低梯度达到，这些横向腔可能会捕获这些沉积物。因此，形态学变化可能受到影响，并且可能会损害恢复干预的功能。在此，我们分析了这些宏观粗糙度元素对主频道细菌的运输的影响。进行了具有均匀流量的实验室测试，在配备有大规模矩形粗糙度元件的堤岸中充电的沉积物。实验室实验涵盖了广泛的矩形腔几何配置和浅不良比率。测试诸如流量浅，空腔几何比的关键参数的影响和初始沉积物浓度。在实验期间收集表面粒子图像速度，沉积物样品和时间浊度记录。腔捕获的沉积物量，悬浮液中沉积物浓度的时间演变和流动流体动力学的交叉分析和讨论。结果表明，宏观粗糙度元素的捕获效率是通道几何形状和流量的浅作函数。版权？ 2017年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2018年第1期</span><b style="margin: 0 2px;">|</b><span>共14页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Juez Carmelo&option=202" target="_blank" rel="nofollow">Juez Carmelo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bühlmann Iria&option=202" target="_blank" rel="nofollow">Bühlmann Iria;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Maechler Gaetan&option=202" target="_blank" rel="nofollow">Maechler Gaetan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schleiss Anton J.&option=202" target="_blank" rel="nofollow">Schleiss Anton J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Franca Mário J.&option=202" target="_blank" rel="nofollow">Franca Mário J.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>école Polytechnique Fédérale de Lausanne (EPFL)Laboratoire de Constructions Hydrauliques (LCH)Lausanne Switzerland;</p> <p>école Polytechnique Fédérale de Lausanne (EPFL)Laboratoire de Constructions Hydrauliques (LCH)Lausanne Switzerland;</p> <p>école Polytechnique Fédérale de Lausanne (EPFL)Laboratoire de Constructions Hydrauliques (LCH)Lausanne Switzerland;</p> <p>école Polytechnique Fédérale de Lausanne (EPFL)Laboratoire de Constructions Hydrauliques (LCH)Lausanne Switzerland;</p> <p>école Polytechnique Fédérale de Lausanne (EPFL)Laboratoire de Constructions Hydrauliques (LCH)Lausanne Switzerland;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bank macro‐roughness&option=203" rel="nofollow">bank macro‐roughness;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=river embayments&option=203" rel="nofollow">river embayments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lateral cavities&option=203" rel="nofollow">lateral cavities;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fine sediments&option=203" rel="nofollow">fine sediments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment transport in suspension&option=203" rel="nofollow">sediment transport in suspension;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrodynamics&option=203" rel="nofollow">hydrodynamics;</a> </p> <div class="translation"> 机译：银行宏观粗糙度;河流倒膜;侧腔;细沉积物;悬浮沉积物;流体动力学; 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