Two new conceptual models for the formation and degradation of baymouth spits by longshore drift and fluvial discharge (Iguape, SE Brazil)

Alcántara‐Carrió Javier; Dinkel Thaya M.; Portz Luana; Mahiques Michel M.

摘要

Abstract >This study describes the formation of two successive baymouth spits systems on the south‐eastern Brazilian coast and the degradation of the first system. The study area includes the Jureia Beach spit, the deflected Ribeira de Iguape River mouth, the central Iguape sandy headland, the Icapara Inlet of the Mar Pequeno Lagoon and the northern end of the Comprida Island barrier spit. The wave and river flow patterns were combined with the coastline evolution and the alongshore migration rates deduced from satellite images. Initially, both spits showed convergent alongshore migration rates equal to or less than 83?m/yr. However, the extreme river flow due to high rainfall during a very strong El Ni?o event in 1983 eroded the inland side of the Jureia Beach spit, which finally retreated due to wave erosion. In 1989, a sand bank emerged in the river mouth, which attached to the central headland forming a recurved northeastward spit. In 1994, the high fluvial discharge associated with another very strong El Ni?o event caused the landward migration of the new spit and emersion of a second sand bank. This second sand bank merged with the Jureia Beach spit in 1997 at an alongshore migration rate of 1795.6?m/yr. Wave erosion of the central headland continued and the attached spit disappeared in 2000. In 2009, the headland erosion merged the river mouth and the Icapara Inlet, which resulted in flanking baymouth spits in a configuration that remains today. Therefore, two models for the formation of baymouth spits have been documented for wave‐dominated microtidal coasts in humid tropical regions with intense fluvial discharge. The convergent longshore migration of the spits is controlled by both the bidirectional longshore drift and the fluvial discharge, the latter eroding the fronting spit, supplying sediments and acting as a hydraulic blocka </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：lang =“en”> <title type =“main”>抽象</ title> >本研究描述了两种连续的巴西海岸海岸的两个连续八南吐痰系统以及第一系统的退化。该研究区包括库里亚海滩吐痰，偏转的Ribeira de Iguape河口，中央Iguape Sandy Beakland，Mar Pequeno泻湖的Icapara入口和CompriDa Island Barrier Spit的北端。波浪和河流流动模式与卫星图像推导的海岸线演变和沿海迁移率相结合。最初，两种吐痰显示到沿岸迁移率等于或小于83Ωm/ yr。然而，1983年在一个非常强大的EL NI期间降雨量的极端河流侵蚀了库里亚海滩吐的内陆方面，这终于由于波浪侵蚀而撤退。 1989年，一家在河口中出现的沙岸，附着在中央岬角形成了一个重新的东北吐痰。 1994年，与另一个非常强大的EL NI的高河流放电导致了新吐痰和第二次沙岸的落地迁移。第二次沙岸银行与1997年的Jureia Beach Spit合并，沿岸迁移率为1795.6？M / YR。中央岬角的波浪侵蚀继续，附带的唾液于2000年消失。2009年，爆头侵蚀合并了河口和icapara入口，导致侧翼的八卦茅斯以今天的配置。因此，已经记录了两种用于形成Baymouth Spits的模型，用于潮湿的热带地区的波浪主导的微观沿海，具有强烈的液体放电。吐痰的融合龙岸迁移由双向龙头漂移和河流放电来控制，后者侵蚀前部吐，供应沉积物和用作液压块 </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3期</span><b style="margin: 0 2px;">|</b><span>共15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=Alcántara‐Carrió Javier&option=202" target="_blank" rel="nofollow">Alcántara‐Carrió Javier;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dinkel Thaya M.&option=202" target="_blank" rel="nofollow">Dinkel Thaya M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Portz Luana&option=202" target="_blank" rel="nofollow">Portz Luana;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mahiques Michel M.&option=202" target="_blank" rel="nofollow">Mahiques Michel 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>Instituto OceanográficoUniversidade de S?o PauloS?o Paulo Brazil;</p> <p>Facultad de CienciasUniversidad de AlicanteSan Vicente del Raspeig Alicante 03690 Spain;</p> <p>Department Ingeniaría Civil y AmbientalUniversidad de la Costa. BarranquillaAtlántico Colombia;</p> <p>Instituto OceanográficoUniversidade de S?o PauloS?o Paulo Brazil;</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=sand barrier&option=203" rel="nofollow">sand barrier;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=inlet&option=203" rel="nofollow">inlet;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=river mouth&option=203" rel="nofollow">river mouth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wave&option=203" rel="nofollow">wave;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=El Ni?o&option=203" rel="nofollow">El Ni?o;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydraulic blockage&option=203" rel="nofollow">hydraulic blockage;</a> </p> <div class="translation"> 机译：沙屏;入口;河口;波;el ni？o;液压堵塞; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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 >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023139218.html">Two new conceptual models for the formation and degradation of baymouth spits by longshore drift and fluvial discharge (Iguape, SE Brazil)</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alcántara‐Carrió Javier&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alcántara‐Carrió Javier,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dinkel Thaya M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dinkel Thaya M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Portz Luana&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Portz Luana,</a> <a href="/journal-foreign-22319/" target="_blank" rel="nofollow" class="tuijian_authcolor">Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group .</a> <span>2018</span><span>,第3期</span> </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：龙岸漂移和河流排放（Iguape，Se Brazil）的两种新的概念模型</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204121744838.html">A diachronic view of the net longshore sediment drift during the Late Holocene at the Jequitinhonha River delta, Brazil, using numerical modeling</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abilio C.s.p. 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break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：信息概念模型（SSKM）管理系统以及使用这种管理系统搜索信息的方法 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130464933172.html">Apparatus for analysis of natural language, natural language process analysis, process analysis expressoes of natural language; process of consultation with a relational database.The use of a conceptual model in a system of natural language in computer analysis of resident, the process of creating a conceptual model and the process of creation of meta knowledge</a> <b>[P]</b> . <span> 外国专利：  BR9001025A </span> <span> . 1991-02-26</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：自然语言分析设备，自然语言过程分析，自然语言过程分析表达;关系数据库的咨询过程。在居民计算机分析中自然语言系统中概念模型的使用，概念模型的创建过程和元知识的创建过程 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" 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