Variability in Benthic Exchange Rate, Depth, and Residence Time Beneath a Shallow Coastal Estuary

机译：浅沿海地区下面的底栖汇率，深度和停留时间的变异性

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Abstract > Hydrodynamically driven benthic exchange of water between the water column and shallow seabed aquifer is a significant and dynamic component of coastal and estuarine fluid budgets. Associated exchange of solutes promotes ecologically important chemical reactions, so quantifying benthic exchange rates, depths, and residence times constrains coastal chemical cycling estimates. We present the first combined field, numerical, and analytical modeling investigation of wave‐induced exchange. Temporal variability of exchange was calculated with data collected by instruments deployed in a shallow estuary for 11 days. Differential pressure sensors recorded pressure gradients across the seabed, and up‐ and down‐looking ADCPs recorded currents and pressures to determine wave parameters, surface‐water currents, and water depth. Wave‐induced exchange was calculated (1) directly from differential pressure measurements, and indirectly with an analytical model based on wave parameters from (2) ADCP and (3) wind data. Wave‐induced exchange from pressure measurements and ADCP‐measured wave parameters matched well, but both exceeded wind‐based values. Exchange induced by tidal pumping and current‐bed form interaction—the other primary drivers in shallow coastal waters were calculated from tidal stage variation and ADCP‐measured currents. Exchange from waves (mean?=?20.0 cm/d; range?=?1.75–92.3 cm/d) greatly exceeded exchange due to tides (mean?=?3.7 cm/d) and current‐bed form interaction (mean?=?6.5 × 10 ?2 cm/d). Groundwater flow models showed aquifer properties affect wave‐driven benthic exchange: residence time and depth increased and exchange rates decreased with increasing hydraulic diffusivity (ratio of aquifer permeability to compressibility). This new understanding of benthic exchange will help managers assess its control over chemical fluxes to mar </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</标题> >水柱与浅海底含水层之间的水交换是沿海和河口流体预算的重要而动态的成分。相关的溶质交流促进了生态上重要的化学反应，因此量化了底栖汇率，深度和居留时期限制了沿海化学循环估计。我们介绍了波浪诱导交换的第一个组合领域，数值和分析模拟调查。通过在浅水河口中部署的仪器收集的数据来计算交换的时间变化。差压传感器通过海底录制压力梯度，上下和下眼的ADCPS记录的电流和压力，以确定波浪参数，表面水流和水深。将波浪诱导的交换直接从差压测量计算（1），并与来自（2）ADCP和（3）风数据的波参数间接的分析模型间接。波浪引起的压力测量和ADCP测量波参数匹配良好，但两者都超过了基于风的值。由潮汐泵浦和电流床形式互动的交换 - 从潮汐阶段变化和ADCP测量电流计算浅沿海水域中的其他初级驱动器。从波开始（平均值？= 20.0cm / d;范围？= 1.75-92.3cm / d）由于潮汐（平均值？= 3.7cm / d）和电流床形式相互作用而大大超过交换（平均值？= ？6.5×10 ？2 </ sup> cm / d）。地下水流动模型显示出含水层性能影响波浪驱动的底栖交换：随着液压扩散率的增加（含水层渗透率与压缩性的渗透率的比率比较）增加，汇率增加和汇率下降。这种新的对底层交换的了解将帮助管理人员评估其对3月的化学势量的控制 </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3期</span><b style="margin: 0 2px;">|</b><span>共17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=Russoniello Christopher J.&option=202" target="_blank" rel="nofollow">Russoniello Christopher J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heiss James W.&option=202" target="_blank" rel="nofollow">Heiss James W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Michael Holly A.&option=202" target="_blank" rel="nofollow">Michael Holly A.;</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 Geological SciencesUniversity of DelawareNewark DE USA;</p> <p>Department of Geological SciencesUniversity of DelawareNewark DE USA;</p> <p>Department of Geological SciencesUniversity of DelawareNewark DE 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=benthic exchange&option=203" rel="nofollow">benthic exchange;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hypokymatic flow&option=203" rel="nofollow">hypokymatic flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=coastal groundwater&option=203" rel="nofollow">coastal groundwater;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine groundwater discharge&option=203" rel="nofollow">submarine groundwater discharge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=waves&option=203" rel="nofollow">waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tides and currents&option=203" rel="nofollow">tides and currents;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Delaware Inland Bays&option=203" rel="nofollow">Delaware Inland Bays;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=USA&option=203" rel="nofollow">USA;</a> </p> <div class="translation"> 机译：底层交换;低代理流动;沿海地下水;潜艇地下水放电;波浪;潮汐和电流;特拉华内陆海湾;美国; </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 >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/0704025579406.html">Variability in Benthic Exchange Rate, Depth, and Residence Time Beneath a Shallow Coastal Estuary</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Russoniello Christopher J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Russoniello Christopher J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heiss James W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Heiss James W.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Michael Holly A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Michael Holly A. </a> <a href="/journal-foreign-34643/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research, C. 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