Offshore aeolian sediment transport across a human‐modified foredune

机译：海上Aeolian沉积物运输在人类修改的常规中

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Abstract >Concepts derived from previous studies of offshore winds on natural dunes are evaluated on a dune maintained for shore protection during three offshore wind events. The potential for offshore winds to form a lee‐side eddy on the backshore or transfer sediment from the dune and berm crest to the water are evaluated, as are differences in wind speed and sediment transport on the dune crest, berm crest and a pedestrian access gap. >The dune is 18–20?m wide near the base and has a crest 4.5?m above backshore elevation. Two sand‐trapping fences facilitate accretion. Data were obtained from wind vanes on the crest and lee of the dune and anemometers and sand traps placed across the dune, on the beach berm crest and in the access gap. Mean wind direction above the dune crest varied from 11 to 3?deg from shore normal. No persistent recirculation eddy occurred on the 12?deg seaward slope. Wind speed on the berm crest was 85–89% of speed at the dune crest, but rates of sediment transport were 2.27 times greater during the strongest winds, indicating that a wide beach overcomes the transport limitation of a dune barrier. Limited transport on the seaward dune ramp indicates that losses to the water are mostly from the backshore, not the dune. The seaward slope gains sand from the landward slope and dune crest. Sand fences causing accretion on the dune ramp during onshore winds lower the seaward slope and reduce the likelihood of detached flows during offshore winds. Transport rates are higher in access gaps than on the dune crest despite lower wind speeds because of flatter slopes and absence of vegetation. Transport rates across dunes and through gaps can be reduced using vegetation and raised walkover structures. 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：lang =“en”> <title type =“main”>抽象</ title> >概念派生从先前的自然沙丘上的海上风研究，在三个海上风赛中保持岸边保护的沙丘上进行评估。评估海上风的潜力，在沙丘和贝尔梅尔斯特将沉淀物上形成李侧涡流，与水中的沉积物沉积物，风速和沉积物运输的差异是沙丘嵴，烧烤和行人进入差距。</ p> > Dune在底部附近18-20？M宽，并且在岸上高度上方有4.5米4.5米。两个砂捕围栏促进了吸收。数据是从风叶片上获得的，在沙丘和风光仪和沙丘上放置在沙滩上的沙子陷阱，在沙滩上，在海滩鲈鱼上以及进入差距。平均风向上方沙丘嵴从岸正常的11到3点变化。在12°坡上没有发生持续的再循环涡流。 Berm Crest上的风速为Dune Crest的85-89％，但最强大的风中，沉积物运输的速率比较大2.27倍，表明广阔的海滩克服了沙丘屏障的运输限制。海上沙丘坡道上的有限运输表明，对水的损失主要来自后岸，而不是沙丘。海坡从陆地坡和沙丘嵴上涨。在陆上风中导致沙丘斜坡上的砂栅造成的砂围落在海上坡度下降，减少海上风中的脱离流动的可能性。尽管风速速度较低，但由于较平坦的斜坡和缺乏植被，但运输率比在沙丘上升速度更高。使用植被和升高的步行结构可以减少沙丘和通过间隙的运输速率。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7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=Nordstrom Karl F.&option=202" target="_blank" rel="nofollow">Nordstrom Karl F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jackson Nancy L.&option=202" target="_blank" rel="nofollow">Jackson Nancy L.;</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>Department of Marine and Coastal SciencesRutgers UniversityNew Brunswick NJ USA;</p> <p>Department of Chemistry and Environmental ScienceNew Jersey Institute of TechnologyNewark NJ 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=aeolian processes&option=203" rel="nofollow">aeolian processes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=beach&option=203" rel="nofollow">beach;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=foredune&option=203" rel="nofollow">foredune;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sand fences&option=203" rel="nofollow">sand fences;</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> </p> <div class="translation"> 机译：Aeolian进程;海滩;致力;沙栅;沉积物运输; 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