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The Role of Particle Size, Ballast, Temperature, and Oxygen in the Sinking Flux to the Deep Sea

机译：粒径，镇流器，温度和氧气在深海的沉没通量中的作用

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Abstract > The “transfer efficiency” of organic particles from the surface to depth is a critical determinant of ocean carbon sequestration. Recently, direct observations and geochemical analyses have revealed a systematic geographical pattern of transfer efficiency, which is highest in high latitude regions and lowest in the subtropical gyres. We evaluate the possible causes of this pattern using a mechanistic model of sinking particle dynamics. The model represents the size distribution of particles, the effects of mineral ballast, seawater temperature (which influences both particle settling velocity and microbial metabolic rates), and O <sub>2</sub> . Parameters are optimized within reasonable ranges to best match the observational constraints. Our model shows that no single factor can explain the observed pattern of transfer efficiency, but the biological effect of temperature on remineralization rate and particle size effects together can reproduce most of the regional variability with both factors contributing to low transfer efficiency in the subtropical gyres and high transfer efficiency in high latitudes. Particle density from mineral ballast has a similar directional effect to temperature and size but plays a substantially smaller role in our optimum solution, due to the opposing patterns of silicate and calcium carbonate ballasting. Oxygen effects modestly improved model fit by depressing remineralization rates and thus increasing transfer efficiency in the Eastern Tropical Pacific. Our model implies that climate‐driven changes to upper ocean temperature and associated changes in surface plankton size distribution would reduce the carbon sequestration efficiency in a warmer ocean. </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> >从表面到深度的有机颗粒的“转移效率”是海洋的关键决定因素碳汇。最近，直接观察和地球化学分析揭示了转移效率的系统地理模式，其在高纬度地区最高，并且在亚热带的旋转中最低。我们使用沉没粒子动力学的机械模型评估这种模式的可能原因。该模型代表粒子的尺寸分布，矿物镇流器的影响，海水温度（影响颗粒沉降速度和微生物代谢率）和O <SUB> 2 </ sub>。参数在合理的范围内优化，以最佳匹配观察约束。我们的模型表明，没有单一因素可以解释观察到的转移效率模式，但是温度对倒耳率和粒度效应的生物学效应可以再现大部分区域变异性，这两种因素有助于亚热带旋转效率的低转移效率和高纬度的高转移效率。来自矿物镇流器的粒子密度与温度和尺寸相似的方向效果，但由于硅酸盐的相反模式和碳酸钙压载，因此在我们的最佳溶液中起着显着较小的作用。氧气效应通过按下再矿化速率，从而提高东热带太平洋的转移效率，氧气效应适度改善的模型适合。我们的模型意味着气候驱动的上海温度和表面浮游音尺寸分布的相关变化会降低较温暖的海洋中的碳封存效率。 </ 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-23728/'>《Global Biogeochemical Cycles》</a> <b style="margin: 0 2px;">|</b><span>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共19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=Cram Jacob A.&option=202" target="_blank" rel="nofollow">Cram Jacob A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Weber Thomas&option=202" target="_blank" rel="nofollow">Weber Thomas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leung Shirley W.&option=202" target="_blank" rel="nofollow">Leung Shirley W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McDonnell Andrew M. P.&option=202" target="_blank" rel="nofollow">McDonnell Andrew M. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liang Jun‐Hong&option=202" target="_blank" rel="nofollow">Liang Jun‐Hong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deutsch Curtis&option=202" target="_blank" rel="nofollow">Deutsch Curtis;</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>School of OceanographyUniversity of WashingtonSeattle WA USA;</p> <p>School of OceanographyUniversity of WashingtonSeattle WA USA;</p> <p>School of OceanographyUniversity of WashingtonSeattle WA USA;</p> <p>College of Fisheries and Ocean SciencesUniversity of Alaska FairbanksFairbanks AK USA;</p> <p>Department of Oceanography and Coastal Sciences College of the Coast and EnvironmentLouisiana State UniversityBaton Rouge LA USA;</p> <p>School of OceanographyUniversity of WashingtonSeattle WA 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/165.html" title="地质学">地质学;</a><a href="https://www.zhangqiaokeyan.com/clc/5109.html" title="生物地球化学、气体地球化学">生物地球化学、气体地球化学;</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=biological pump&option=203" rel="nofollow">biological pump;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=remineralization&option=203" rel="nofollow">remineralization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ballast&option=203" rel="nofollow">ballast;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=export flux&option=203" rel="nofollow">export flux;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=marine snow&option=203" rel="nofollow">marine snow;</a> </p> <div class="translation"> 机译：生物泵;再矿化;镇流器;出口助焊剂;海洋雪; </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/0704023423644.html">The Role of Particle Size, Ballast, Temperature, and Oxygen in the Sinking Flux to the Deep Sea</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cram Jacob A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Cram Jacob A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Weber Thomas&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Weber Thomas,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leung Shirley W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Leung Shirley W.,</a> <a href="/journal-foreign-23728/" target="_blank" rel="nofollow" class="tuijian_authcolor">Global Biogeochemical Cycles .</a> <span>2018</span><span>,第5期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：粒径，镇流器，温度和氧气在深海的沉没通量中的作用</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_proceedings-national-academy-sciences-united-states-america_thesis/020416971036.html">Role of macroscopic particles in deep-sea oxygen consumption</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexander B. 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