The origin of volatiles in the        <fc >E</fc>E        arth's mantle

Hier‐Majumder Saswata; Hirschmann Marc M.

摘要

Abstract > The Earth's deep interior contains significant reservoirs of volatiles such as H, C, and N. Due to the incompatible nature of these volatile species, it has been difficult to reconcile their storage in the residual mantle immediately following crystallization of the terrestrial magma ocean (MO). As the magma ocean freezes, it is commonly assumed that very small amounts of melt are retained in the residual mantle, limiting the trapped volatile concentration in the primordial mantle. In this article, we show that inefficient melt drainage out of the freezing front can retain large amounts of volatiles hosted in the trapped melt in the residual mantle while creating a thick early atmosphere. Using a two‐phase flow model, we demonstrate that compaction within the moving freezing front is inefficient over time scales characteristic of magma ocean solidification. We employ a scaling relation between the trapped melt fraction, the rate of compaction, and the rate of freezing in our magma ocean evolution model. For cosmochemically plausible fractions of volatiles delivered during the later stages of accretion, our calculations suggest that up to 77% of total H <sub>2</sub> O and 12% of CO <sub>2</sub> could have been trapped in the mantle during magma ocean crystallization. The assumption of a constant trapped melt fraction underestimates the mass of volatiles in the residual mantle by more than an order of magnitude. </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”> <标题类型=“main”>抽象</ title> > 地球的深层内部含有挥发物的重要储存器，如H，C和N.由于这些挥发性物种的性质不相容，在地面岩浆岩浆海洋结晶后，难以将它们的储存在尸体岩浆的结晶之后（MO ）。随着岩浆海洋冻结，通常认为非常少量的熔体保留在残余地幔中，限制了原始地幔中的被困的挥发性浓度。在本文中，我们表明，冻结前的熔体排水效率低下可以在残留地幔中托管在残留罩中托管的大量挥发物，同时产生厚厚的早期气氛。使用两相流模型，我们证明了移动冻结前的压实在岩浆海洋凝固的时间尺度上效率低下。我们采用了陷阱熔体分数，压实速率与我们岩浆海洋演化模型中的冻结速率之间的缩放关系。对于在炎症的后期阶段递增的挥发物的挥发物的挥发性的挥发物的溶性部分，我们的计算表明，占H总量的77％ <sub> 2 </ sub> o和12％的co <sub> 2 </ sub> 在岩浆海洋结晶期间可能被困在地幔中。恒定被捕获的熔体馏分的假设低估了残余地幔中的挥发物的质量超过了数量级。 </ 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>2017年第8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=Hier‐Majumder Saswata&option=202" target="_blank" rel="nofollow">Hier‐Majumder Saswata;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hirschmann Marc M.&option=202" target="_blank" rel="nofollow">Hirschmann Marc M.;</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 Earth SciencesRoyal Holloway University of LondonEgham UK;</p> <p>Department of Earth SciencesUniversity of MinnesotaMinneapolis Minnesota 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=magma ocean&option=203" rel="nofollow">magma ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=early Earth&option=203" rel="nofollow">early Earth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volatile&option=203" rel="nofollow">volatile;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle&option=203" rel="nofollow">mantle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=primitive atmosphere&option=203" rel="nofollow">primitive atmosphere;</a> </p> <div class="translation"> 机译：岩浆海洋;早期地球;挥发性;地幔;原始气氛; 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The origin of volatiles in the EE arth's mantle

摘要