The influence of neap–spring tidal variation and wave energy on sediment flux in salt marsh tidal creeks

机译：NeAp-Spring潮汐变化和波能对盐沼溪小溪沉积物通量的影响

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Abstract > Sediment flux in marsh tidal creeks is commonly used to gauge sediment supply to marshes. We conducted a field investigation of temporal variability in sediment flux in tidal creeks in the accreting tidal marsh at China Camp State Park adjacent to northern San Francisco Bay. Suspended‐sediment concentration (SSC), velocity and depth were measured near the mouths of two tidal creeks during three 6‐ to 10‐week deployments: two in winter and one in summer. Currents, wave properties and SSC were measured in the adjacent shallows. All deployments spanned the largest spring tides of the season. Results show that tidally averaged suspended‐sediment flux (SSF) in the tidal creeks varied from slightly landward to strongly bayward with increasing tidal energy. SSF was negative (bayward) for tidal cycles with maximum water surface elevation above the marsh plain. Export during the largest spring tides dominated the cumulative SSF for each deployment. During ebb tides following the highest tides, velocities exceeded 1?m?s ?1 in the narrow tidal creeks, resulting in negative tidally averaged water flux, and mobilizing sediment from the creek banks or bed. Storm surge also produced negative SSF. Tidally averaged SSF was positive in wavy conditions with moderate tides. Spring tide sediment export at the creek mouth was about twice that at a station 130?m further up the tidal creek. The negative tidally averaged water flux near the creek mouth during spring tides indicates that in the lower marsh some of the water flooding directly across the bay–marsh interface drains through the tidal creeks, and suggests that this interface may be a pathway for sediment supply to the lower marsh as well. Copyright ? 2018 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：lang =“en”xml：id =“esp4401-abs-0001”> <标题类型=“main” >抽象</ title> >沼泽潮汐溪流的沉积物通常用于衡量沼泽的沉积物。在旧金山北部南部南部州立园区的潮汐沼泽中潮汐溪水中的沉积物通量的沉积物通量的沉积物通量的临时变异研究。在三个6至10周的部署期间，在两个潮汐小溪的嘴附近测量悬浮沉积物浓度（SSC），速度和深度：冬季两人和夏季一个。在相邻的浅中测量电流，波形和SSC。所有部署都跨越了本赛季最大的春季潮流。结果表明，随着潮汐能量，潮汐小溪中的平均悬浮沉积物通量（SSF）因略微落地而变化而异。 SSF是阴性（贝沃德），用于潮汐循环，沼泽平原上方的最大水面高度。在最大的春季潮汐期间导出主导每个部署的累积SSF。在最高潮汐之后的EBB潮汐期间，速度超过1？M？S <SUP> 1// / SUP>在狭窄的潮汐小溪中，导致阴性平均水通量，从溪岸或床上调动沉积物。风暴浪涌也产生了负面的SSF。平均平均SSF在具有中等潮汐的波浪状况中是正的。溪口的春潮沉积物出口大约是在130的两倍的两倍？米进一步达到潮汐溪。春季潮汐期间溪口附近的负整平均水通量表明，在较低的沼泽中，一些水洪水直接穿过湾沼泽界面穿过潮汐小溪，并表明该界面可能是沉积物供应的途径较低的沼泽也是如此。版权？ 2018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11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=Lacy Jessica R.&option=202" target="_blank" rel="nofollow">Lacy Jessica R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferner Matthew C.&option=202" target="_blank" rel="nofollow">Ferner Matthew C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Callaway John C.&option=202" target="_blank" rel="nofollow">Callaway John C.;</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>US Geological SurveyPacific Coastal and Marine Science CenterSanta Cruz 95060 CA USA;</p> <p>San Francisco Bay National Estuarine Research ReserveSan Francisco State UniversityTiburon 94920 CA USA;</p> <p>Department of Environmental ScienceUniversity of San FranciscoSan Francisco 94117 CA USA;</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 flux to marshes&option=203" rel="nofollow">sediment flux to marshes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=neap‐spring tidal variability&option=203" rel="nofollow">neap‐spring tidal variability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=salt marsh tidal creeks&option=203" rel="nofollow">salt marsh tidal creeks;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=suspended‐sediment flux&option=203" rel="nofollow">suspended‐sediment flux;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=estuarine sediment transport&option=203" rel="nofollow">estuarine sediment transport;</a> </p> <div class="translation"> 机译：泥沙泥浆泥浆;Neap-Spring潮汐变异性;盐沼潮汐小溪;悬浮沉积物助焊剂;河口沉积物运输; 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