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The Magmatic Gas Signature of Pacaya Volcano, With Implications for the Volcanic CO ₂2 Flux From Guatemala

机译：Pacaya Volcano的岩浆气体签名，对火山有限公司的影响 _{2 2 来自危地马拉的助焊剂}

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Abstract > Pacaya volcano in Guatemala is one of the most active volcanoes of the Central American Volcanic Arc (CAVA). However, its magmatic gas signature and volatile output have received little attention to date. Here, we present novel volcanic gas information from in‐situ (Multi‐GAS) and remote (UV camera) plume observations in January 2016. We find in‐plume H <sub>2</sub> O/SO <sub>2</sub> and CO <sub>2</sub> /SO <sub>2</sub> ratios of 2‐20 and 0.6‐10.5, and an end‐member magmatic gas signature of 80.5 mol. % H <sub>2</sub> O, 10.4 mol. % CO <sub>2</sub> , and 9.0 mol. % SO <sub>2</sub> . The SO <sub>2</sub> flux is evaluated at 885?±?550 tons/d. This, combined with co‐acquired volcanic plume composition, leads to H <sub>2</sub> O and CO <sub>2</sub> fluxes of 2,230?±?1,390 and 700?±?440, and a total volatile flux of ～3,800 tons/d. We use these results in tandem with previous SO <sub>2</sub> flux budgets for Fuego and Santiaguito to estimate the total volcanic CO <sub>2</sub> flux from Guatemala at ～1,160?±?600 tons/day. This calculation is based upon CO <sub>2</sub> /total S (S <sub>t</sub> ) ratios for Fuego (1.5?±?0.75) and Santiaguito (1.4?±?0.75) inferred from a gas (CO <sub>2</sub> /S <sub>t</sub> ratio) versus trace‐element (Ba/La ratio) CAVA relationship. The H <sub>2</sub> O‐poor and low CO <sub>2</sub> /S <sub>t</sub> ratio (～1.0‐1.5) signature of Pacaya gas suggests dominant mantle‐wedge derivation of the emitted volatiles. This is consistent with 3 He/ 4 He ratios in olivine hosted fluid inclusions (FIs), which range between 8.4 and 9.0 Ra (being Ra the atmospheric 3 He/ 4 He ratio) at the upper limit of MORB range (8?±?1 Ra). These values are the highest ever measured in CAVA and among the highest ever recorded in arc volcanoes worldwide, indicating negligible 4 He contributions from the crust/slab. </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> > 危地马拉的Pacaya火山是中美洲火山弧（Cava）最活跃的火山之一。然而，它的岩浆气体签名和挥发性产量几乎没有关注到日期。在这里，我们在2016年1月出于原位（多天然气）和遥控器（UV摄像机）羽毛观测的新型火山气体信息。我们发现了羽毛 <sub> 2 </ sub> o / SO <sub> 2 </ sub> 和co. <sub> 2 </ sub> /所以 <sub> 2 </ sub> 比例为2-20和0.6-10.5，以及80.5摩尔的端构件岩浆气体特征。％ H <sub> 2 </ sub> o，10.4 mol。％co. <sub> 2 </ sub> 和9.0 mol。％所以 <sub> 2 </ sub> 。所以 <sub> 2 </ sub> 助焊剂在885？±550吨/天中进行评估。这与共同获得的火山羽流组合物联合，导致H. <sub> 2 </ sub> o和co. <sub> 2 </ sub> 助熔剂2,230？±1,390和700？±440，以及〜3,800吨/ d的总挥发性通量。我们使用这些结果与之前的那么 <sub> 2 </ sub> Fuego和Santiaguito的助焊剂预算估计总火山CO <sub> 2 </ sub> 危地马拉的助焊剂在〜1,160？±600吨/天。该计算基于CO <sub> 2 </ sub> /总计（s <sub> t </ sub> fuego的比率（1.5？±0.75）和Santiaguito（1.4？±0.75）从天然气推断（CO <sub> 2 </ sub> / s. <sub> t </ sub> 比率）与微量元素（Ba / La比）Cava关系。 H. <sub> 2 </ sub> o-port和low co <sub> 2 </ sub> / s. <sub> t </ sub> PACAYA GAR的比例（〜1.0-1.5）签名表明发出挥发物的主导地幔楔衍生。这是一致的 3 </ sup> 他/ 4 </ sup> 他在橄榄石托管流体夹杂物（FIS）中的比率，范围在8.4和9.0°之间（是大气 3 </ sup> 他/ 4 </ sup> 他的比率在Morb范围的上限（8？±1 ra）。这些值是CAVA中有史以来最高的测量，并且在全世界的弧火山中录制的最高，表明可以忽略不计 4 </ sup> 他从地壳/平板贡献。 </ 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>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共26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=Battaglia A.&option=202" target="_blank" rel="nofollow">Battaglia A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bitetto M.&option=202" target="_blank" rel="nofollow">Bitetto M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Aiuppa A.&option=202" target="_blank" rel="nofollow">Aiuppa A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rizzo A.L.&option=202" target="_blank" rel="nofollow">Rizzo A.L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chigna G.&option=202" target="_blank" rel="nofollow">Chigna G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Watson I. M.&option=202" target="_blank" rel="nofollow">Watson I. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=DAleo R.&option=202" target="_blank" rel="nofollow">DAleo R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Juárez Cacao F. J.&option=202" target="_blank" rel="nofollow">Juárez Cacao F. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=de Moor M. J.&option=202" target="_blank" rel="nofollow">de Moor M. J.;</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>Dipartimento DiSTeMUniversità di PalermoPalermo Italy;</p> <p>Dipartimento DiSTeMUniversità di PalermoPalermo Italy;</p> <p>Dipartimento DiSTeMUniversità di PalermoPalermo Italy;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaPalermo Italy;</p> <p>INSIVUMEH Ciudad de GuatemalaGuatemala Central America;</p> <p>School of Earth SciencesUniversity of BristolBristol UK;</p> <p>Dipartimento DiSTeMUniversità di PalermoPalermo Italy;</p> <p>INSIVUMEH Ciudad de GuatemalaGuatemala Central America;</p> <p>OVSICORI UNAHeredia Costa Rica Central America;</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=Pacaya&option=203" rel="nofollow">Pacaya;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcanic gases&option=203" rel="nofollow">volcanic gases;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid inclusions&option=203" rel="nofollow">fluid inclusions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CO 2 fluxes&option=203" rel="nofollow">CO 2 fluxes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=3He/4He&option=203" rel="nofollow">3He/4He;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbon isotopes&option=203" rel="nofollow">carbon isotopes;</a> </p> <div class="translation"> 机译：Pacaya;火山气体;流体夹杂物;CO 2助焊剂;3HE / 4HE;碳同位素; </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/0704023360545.html">The Magmatic Gas Signature of Pacaya Volcano, With Implications for the Volcanic CO <sub >2</sub>2 Flux From Guatemala</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Battaglia A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Battaglia A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bitetto M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bitetto M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Aiuppa A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Aiuppa A.,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第3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：Pacaya Volcano的岩浆气体签名，对火山有限公司的影响 <sub> 2 </ sub> 2 来自危地马拉的助焊剂</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_gsa-bulletin_thesis/020414084649.html">Cannonball Bombs, A New Kind of Volcanic Bomb from the Pacaya Volcano, Guatemala</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P. 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O．Melnik</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=A．A．Barmin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,A．A．Barmin</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=R．S．J．Sparks&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,R．S．J．Sparks</a> <span> <a href="/journal-cn-5012/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 世界地震译丛 </a> </span> <span> . 2006</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geological-science-technology_thesis/0201263461131.html">从气体中获得金—火山气体研究新进展对岩浆流体般运金属提供了新认识</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=西蒙.RB&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 西蒙.RB</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张也&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张也</a> <span> <a href="/journal-cn-50289/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质科技动态 </a> </span> <span> . 1993</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201290684937.html">兴蒙造山带中部晚古生代构造格局:来自晚泥盆-早石炭世色日巴彦敖包组碎屑锆石和火山岩岩浆锆石年代学的制约</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王树庆&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王树庆</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡晓佳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,胡晓佳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨泽黎&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨泽黎</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2021</span><span>,第007期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201279713828.html">伊宁地块构造单元划分——来自火山岩浆作用的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李永军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李永军</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=佟丽莉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,佟丽莉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王祚鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王祚鹏</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2020</span><span>,第007期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-65293_thesis/020222935381.html">长白山天池火山岩浆演化及其地质意义:来自熔体包裹体的证据</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=雷敏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 雷敏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴才来&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴才来</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭文峰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郭文峰</a> <span> <a href="/conference-cn-65293/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地质学会2017学术年会 </a> <span> <span> . 2017</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/02031633765.html">部分熔融和浅部岩浆过程对橄榄岩捕掳体掳体水含量的影响：来自安徽天长的实例</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=田真真&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 田真真</a> <span> . 2016</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130489798302.html">A device for rolling and pressing the end of a freely suspended extraction thread of a guatemala velo, against an end of a guatemala roll for tampons. (Machine-translation by Google Translate, not legally binding)</a> <b>[P]</b> . <span> 外国专利：  ES318730A1 </span> <span> . 1966-05-16</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：一种用于将危地马拉绒的自由悬挂的抽出线的末端压在棉塞的危地马拉卷的末端上的装置。（通过Google翻译进行机器翻译，没有法律约束力） </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130404869498.html">New materials using the volcanic ash of active volcanoes</a> <b>[P]</b> . <span> 外国专利：  JP6541191B2 </span> <span> . 2019-07-10</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：使用活性火山灰的新材料 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130405174412.html">NOVEL MATERIAL USING VOLCANIC ASHES OF ACTIVE VOLCANO</a> <b>[P]</b> . <span> 外国专利：  JP2019099947A </span> <span> . 2019-06-24</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：使用活性火山灰的新型材料 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360545','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="" 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The Magmatic Gas Signature of Pacaya Volcano, With Implications for the Volcanic CO 22 Flux From Guatemala

摘要

The Magmatic Gas Signature of Pacaya Volcano, With Implications for the Volcanic CO ₂2 Flux From Guatemala