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Controls on the Deep‐Water Cycle Within Three‐Dimensional Mantle Convection Models

机译：三维地幔对流模型中深水循环的控制

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Abstract >Earth's mantle is known to harbor water in the form of hydrous and nominally anhydrous minerals. How much water the mantle holds and whether it has remained constant through time are open questions. Previous numerical studies of the deep‐water cycle have been limited to box models or 2‐D calculations. Here we present for the first time results from 3‐D mantle convection models. We address the evolution of the mantle's total water content by adapting a well benchmarked mantle convection code to track water, including its feedbacks on dynamics. While Earth's surface is presently covered by one ocean mass of water, our results suggest that the mantle holds approximately two ocean masses of water based on the best estimates from mineral physics. This value varies only weakly for a wide parameter space of additional complex dynamics such as viscosity laws, density controls, and phase change considerations. Our result of a mantle holding two ocean masses conforms with estimates from other branches of Earth science, suggesting that these models could be an excellent tool in understanding the spatial heterogeneity of the water found in the mantle. </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”XML：ID =“GGGE21878-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> >地球的地幔是以含水和名义上无水矿物质的形式含水。地幔持有多少水以及它是否仍然保持不变的时间是开放的问题。以前的深水循环数值研究仅限于盒式型号或二维计算。在这里，我们首次出现来自3-D Mantle对流模型的结果。我们通过调整良好的基准地幔对流代码来跟踪水域来解决地幔总含量的演变，包括其对动态的反馈。虽然地球表面目前被一个海洋大量的水覆盖，但我们的结果表明，地幔基于矿物质的最佳估计，地幔大约有两个海洋气体。该值仅在额外的复杂动态的宽参数空间中缺点，例如粘度法，密度控制和相变注意力。我们持有两个海洋群众的地幔结果符合地球科学的其他分支的估计，这表明这些模型可能是理解地幔中发现的水的空间异质性的优秀工具。</ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2019年第5期</span><b style="margin: 0 2px;">|</b><span>共15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=Price Matthew G.&option=202" target="_blank" rel="nofollow">Price Matthew G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Davies J. H.&option=202" target="_blank" rel="nofollow">Davies J. H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Panton James&option=202" target="_blank" rel="nofollow">Panton James;</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 Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</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=mantle dynamics&option=203" rel="nofollow">mantle dynamics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=deep‐water cycle&option=203" rel="nofollow">deep‐water cycle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle water budget&option=203" rel="nofollow">mantle water budget;</a> </p> <div class="translation"> 机译：地幔动力学;深水循环;地幔水预算; </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/0704023360508.html">Controls on the Deep‐Water Cycle Within Three‐Dimensional Mantle Convection Models</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Price Matthew G.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Price Matthew G.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Davies J. 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