Impact of Seabed Resuspension on Oxygen and Nitrogen Dynamics in the Northern Gulf of Mexico: A Numerical Modeling Study

Moriarty Julia M.; Harris Courtney K.; Friedrichs Marjorie A. M.; Fennel Katja; Xu Kehui

摘要

Abstract >Resuspension affects water quality in coastal environments by entraining seabed organic matter into the water column, which can increase remineralization, alter seabed fluxes, decrease water clarity, and affect oxygen and nutrient dynamics. Nearly all numerical models of water column biogeochemistry, however, simplify seabed and bottom boundary layer processes and neglect resuspension. Here we implemented HydroBioSed, a coupled hydrodynamic‐sediment transport‐biogeochemical model to examine the role of resuspension in regulating oxygen and nitrogen dynamics on timescales of a day to a month. The model was implemented for the northern Gulf of Mexico, where the extent of summertime hypoxia is sensitive to seabed and bottom boundary layer processes. Results indicated that particulate organic matter remineralization in the bottom water column increased by an order of magnitude during resuspension events. This increased sediment oxygen consumption and ammonium production, which were defined as the sum of seabed fluxes of oxygen and ammonium, plus oxygen consumption and ammonium production in the water column due to resuspended organic matter. The increases in remineralization impacted biogeochemical dynamics to a greater extent than resuspension‐induced seabed fluxes and oxidation of reduced chemical species. The effect of resuspension on bottom water biogeochemistry increased with particulate organic matter availability, which was modulated by sediment transport patterns. Overall, when averaged over the shelf and on timescales of a month in the numerical model, cycles of erosion and deposition accounted for about two thirds of sediment oxygen consumption and almost all of the sediment ammonium production. </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 Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >通过将海底有机物质夹入水柱中，将海底有机物质纳入水柱中的水质影响。增加再矿化，改变海床通量，降低水清晰度，并影响氧气和营养动态。然而，几乎所有数值模型的水柱生物地球化学，简化海床和底部边界层过程并忽略了重悬浮。在这里，我们实施了含氢，一种偶联的流体动力学 - 沉积物传输 - 生物地球织化学模型，以检查重悬浮在调节氧气和氮动力学对每天时间到一个月的时间的作用。该模型是为墨西哥北部的北湾实施的模型，夏季缺氧程度对海底和底部边界层工艺敏感。结果表明，底部水塔中的颗粒状有机物质再矿化在重悬浮事件期间增加了数量级。这种增加的沉积物氧气消耗和铵产量，其被定义为氧气和铵的海底助焊剂和由于重组有机物质而在水柱中加上氧气消耗和铵生产。再矿化的增加会影响生物地球化学动力学，而不是重新悬浮诱导的海底助熔剂和减少化学物质的氧化。重悬浮对底部水生物地球化学的影响随粒状有机物质可用性而增加，其被沉积物传输模式调节。总体而言，当在架子上平均并且在数值模型中的一个月的时间尺寸时，侵蚀和沉积周期占沉积物氧消耗的约三分之二，几乎所有沉积物铵生产。</ p> </摘要> </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10期</span><b style="margin: 0 2px;">|</b> <span>共27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=Moriarty Julia M.&option=202" target="_blank" rel="nofollow">Moriarty Julia M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harris Courtney K.&option=202" target="_blank" rel="nofollow">Harris Courtney K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Friedrichs Marjorie A. M.&option=202" target="_blank" rel="nofollow">Friedrichs Marjorie A. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fennel Katja&option=202" target="_blank" rel="nofollow">Fennel Katja;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Kehui&option=202" target="_blank" rel="nofollow">Xu Kehui;</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>Virginia Institute of Marine ScienceCollege of William and Mary Gloucester PointGloucester VA USA;</p> <p>Virginia Institute of Marine ScienceCollege of William and Mary Gloucester PointGloucester VA USA;</p> <p>Virginia Institute of Marine ScienceCollege of William and Mary Gloucester PointGloucester VA USA;</p> <p>Department of OceanographyDalhousie UniversityHalifax Nova Scotia Canada;</p> <p>Department of Oceanography and Coastal SciencesLouisiana State UniversityBaton Rouge LA 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=Regional Ocean Modeling System (ROMS)&option=203" rel="nofollow">Regional Ocean Modeling System (ROMS);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=northern Gulf of Mexico continental shelf hypoxia&option=203" rel="nofollow">northern Gulf of Mexico continental shelf hypoxia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment transport and resuspension&option=203" rel="nofollow">sediment transport and resuspension;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=particulate organic carbon (POC)&option=203" rel="nofollow">particulate organic carbon (POC);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=nitrogen&option=203" rel="nofollow">nitrogen;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oxygen&option=203" rel="nofollow">oxygen;</a> </p> <div class="translation"> 机译：区域海洋建模系统（ROM）;墨西哥大陆架北湾缺氧;沉积物运输和重新悬浮;颗粒有机碳（POC）;氮气;氧气; </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/0704025578977.html">Impact of Seabed Resuspension on Oxygen and Nitrogen Dynamics in the Northern Gulf of Mexico: A Numerical Modeling Study</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moriarty Julia M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Moriarty Julia M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harris Courtney K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Harris Courtney K.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Friedrichs Marjorie A. 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