Three‐Dimensional Sediment Dynamics in Well‐Mixed Estuaries: Importance of the Internally Generated Overtide, Spatial Settling Lag, and Gravitational Circulation

Wei Xiaoyan; Kumar Mohit; Schuttelaars Henk M.

摘要

Abstract > To investigate the dominant sediment transport and trapping mechanisms, a semi‐analytical three‐dimensional model is developed resolving the dynamic effects of salt intrusion on sediment in well‐mixed estuaries in morphodynamic equilibrium. As a study case, a schematized estuary with a converging width and a channel‐shoal structure representative for the Delaware estuary is considered. When neglecting Coriolis effects, sediment downstream of the estuarine turbidity maximum (ETM) is imported into the estuary through the deeper channel and exported over the shoals. Within the ETM region, sediment is transported seaward through the deeper channel and transported landward over the shoals. The largest contribution to the cross‐sectionally integrated seaward residual sediment transport is attributed to the advection of tidally averaged sediment concentrations by river‐induced flow and tidal return flow. This contribution is mainly balanced by the residual landward sediment transport due to temporal correlations between the suspended sediment concentrations and velocities at the M <sub>2</sub> tidal frequency. The M <sub>2</sub> sediment concentration mainly results from spatial settling lag effects and asymmetric bed shear stresses due to interactions of M <sub>2</sub> bottom velocities and the internally generated M <sub>4</sub> tidal velocities, as well as the salinity‐induced residual currents. Residual advection of tidally averaged sediment concentrations also plays an important role in the landward sediment transport. Including Coriolis effects hardly changes the cross‐sectionally integrated sediment balance, but results in a landward (seaward) sediment transport on the right (left) side of the estuary looking seaward, consistent with obser </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 Type =“main”> <标题类型=“main”>抽象</ title> >调查主导沉积物运输和捕获机制，开发了一种分析盐的动态效果的半分析三维模型形态学性均衡良混河中沉积物的侵入。作为一项研究案例，考虑了具有融合宽度的示意性河口和特拉华河口的沟渠结构代表。当忽略科里奥利效应时，通过更深的通道进口到河口浊度下游（ETM）的沉积物进口到河口中并出口浅滩。在ETM地区内，沉积物通过更深的通道向海上运输，并在浅滩上运输着陆。对横截面综合的海鲜沉积物传输的最大贡献归因于河流诱导的流动和潮热率的平均沉积物浓度的平均。由于悬浮沉积物浓度和 2 </ sub>潮汐频率的速度之间的时间相关性，这种贡献主要受到残留的陆地沉积物运输。 m </ i> <sub> 2 </ sub>沉积物浓度主要由空间沉降滞后效应和由于 m </ i> <sub的相互作用而产生的不对称床剪切应力产生>底部速度和内部产生的 m </ i> <sub> 4 </ sub>潮流，以及盐度诱导的残余电流。剩余平均平均沉积物浓度也在陆地沉积物运输中起着重要作用。包括科里奥利效应几乎没有改变横向综合沉积物平衡，但导致陆地（左侧）沉积物运输在河口的右侧（左侧）侧面，与观察者一致 </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-34643/'>《Journal of Geophysical Research, C. Oceans: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共29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=Wei Xiaoyan&option=202" target="_blank" rel="nofollow">Wei Xiaoyan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kumar Mohit&option=202" target="_blank" rel="nofollow">Kumar Mohit;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schuttelaars Henk M.&option=202" target="_blank" rel="nofollow">Schuttelaars Henk M.;</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>Applied MathematicsDelft University of TechnologyDelft the Netherlands;</p> <p>Applied MathematicsDelft University of TechnologyDelft the Netherlands;</p> <p>Applied MathematicsDelft University of TechnologyDelft the Netherlands;</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=estuarine turbidity maximum (ETM)&option=203" rel="nofollow">estuarine turbidity maximum (ETM);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=salt intrusion&option=203" rel="nofollow">salt intrusion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment transport&option=203" rel="nofollow">sediment transport;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=well‐mixed&option=203" rel="nofollow">well‐mixed;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=gravitational circulation&option=203" rel="nofollow">gravitational circulation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lateral processes&option=203" rel="nofollow">lateral processes;</a> </p> <div class="translation"> 机译：河卤素浊度最大（ETM）;盐侵入;沉积物运输;良好的混合;引力循环;侧向过程; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025579535.html">Three‐Dimensional Sediment Dynamics in Well‐Mixed Estuaries: Importance of the Internally Generated Overtide, Spatial Settling Lag, and Gravitational Circulation</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Xiaoyan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wei Xiaoyan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kumar Mohit&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kumar Mohit,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schuttelaars Henk M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Schuttelaars Henk M. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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different view points of spatial three-dimensional space over time</a> <b>[P]</b> . <span> 外国专利：  FR2963470A1 </span> <span> . 2012-02-03</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：用于编辑视听的方法，例如电视节目涉及随着时间的推移自动生成空间二维的流，该流对应于空间三维空间随时间的不同视点 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704025579535','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div 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