Conditional effects of tides and waves on short‐term marsh sedimentation dynamics

机译：潮汐与波浪对短期沼泽沉降动力学的条件影响

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Abstract > Salt marshes are in danger of degradation due to human impact and climate change. A thorough understanding of mechanisms controlling sedimentation and erosion in salt marshes is essential for their conservation and restoration. To understand short‐term dynamics of sediment availability and deposition around marsh edges, two contrasting marshes, Rattekaai and Sint Annaland, were studied in the Oosterschelde (southwest Netherlands). Suspended sediment concentration (SSC) was measured by siphon samplers along four transects perpendicular to the marsh edge in each marsh, during nine flood tides between March and December 2013. Each transect was comprised of four sampling sites (?10?m and ?1?m on the mudflat and +1?m and +10?m on the marsh plateau, relative to the marsh edge). Sediment deposition was measured along the transects on the marsh, at +1?m and +10?m from the marsh edge, over seven <fi>c</fi> . 14‐day intervals during the same 10‐month period. Two types of sediment traps were used, one measuring gross sediment deposition (TTD – tube trap deposition) and one measuring net sediment deposition (FTD – filter trap deposition). Wave loggers were deployed 10?m away from the marsh edge on the mudflat at each marsh. The results showed that both SSC and sediment deposition varied greatly through space, both between the two marshes and within each marsh along the marsh edge. The SSC and gross sediment deposition were much higher at Rattekaai than at Sint Annaland. SSC was significantly correlated with wind speed during sampling. Sediment deposition rates (TTD and FTD) and retention ratio (FTD/TTD) were significantly correlated with cumulative wave energy during the measurement period. A conceptual model of local sediment dynamics is proposed to explain the sediment dynamics around the marsh edge. This stud </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 =“nl”> <title type =“main”>抽象</ title> >盐沼由于人类的影响和气候变化导致退化的危险。彻底了解控制盐沼的沉降和腐蚀的机制对于他们的保护和恢复至关重要。为了了解泥沙边缘的沉积物可用性和沉积的短期动态，在Oosterschelde（荷兰西南部）研究了两个鲜明的沼泽地，rattekaai和sint Annaland。在2013年3月和12月之间的九个洪水潮汐期间，通过虹吸件沿着垂直于每个沼泽的四个横断面测量悬浮沉积物浓度（SSC）。每个横断面都由四个采样点组成（？10？m和？1？在Mudflat上和+1？m和+10？m在Marsh Plateau上，相对于沼泽边缘）。沉积物沉积沿着沼泽地上的横断面测量，从沼泽边缘处的+1×m和+10·m，超过七个<fi> c </ fi>。在同一10个月期间的14天间隔。使用两种类型的沉积物陷阱，一种测量总沉积物沉积（TTD管疏水阀沉积）和一个测量净沉积物沉积（FTD滤波阱沉积）。波浪记录器在每个沼泽地的Mudflat上的沼泽边缘部署10？M远。结果表明，SSC和沉积物沉积在两个沼泽之间和沿着沼泽边缘的每个沼泽内之间的空间都大大变化。在Rattekaai的SSC和总沉积物沉积比Sint Annaland略高得多。在抽样过程中，SSC与风速显着相关。沉积物沉积速率（TTD和FTD）和保留比（FTD / TTD）在测量期间与累积波能显着相关。提出了局部沉积动力学的概念模型，解释了沼泽边缘周围的沉积动力学。这个镶边 </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10期</span><b style="margin: 0 2px;">|</b><span>共13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=Ma Zhigang&option=202" target="_blank" rel="nofollow">Ma Zhigang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ysebaert Tom&option=202" target="_blank" rel="nofollow">Ysebaert Tom;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wal Daphne&option=202" target="_blank" rel="nofollow">Wal Daphne;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Herman Peter M.J.&option=202" target="_blank" rel="nofollow">Herman Peter M.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>NIOZ Royal Netherlands Institute for Sea Research Department of Estuarine and Delta SystemsUtrecht UniversityYerseke The Netherlands;</p> <p>NIOZ Royal Netherlands Institute for Sea Research Department of Estuarine and Delta SystemsUtrecht UniversityYerseke The Netherlands;</p> <p>NIOZ Royal Netherlands Institute for Sea Research Department of Estuarine and Delta SystemsUtrecht UniversityYerseke The Netherlands;</p> <p>NIOZ Royal Netherlands Institute for Sea Research Department of Estuarine and Delta SystemsUtrecht UniversityYerseke 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=sediment supply&option=203" rel="nofollow">sediment supply;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=deposition&option=203" rel="nofollow">deposition;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=suspended sediment concentration&option=203" rel="nofollow">suspended sediment concentration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=salt marsh&option=203" rel="nofollow">salt marsh;</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> </p> <div class="translation"> 机译：沉积物供应;沉积;悬浮沉积物浓度;盐沼;波; 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