首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO ₂2 Flux Measurements

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Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO ₂2 Flux Measurements

机译：美国黄石国家公园的蒸汽占水热区域中的热量和大规模运输：磁，电磁，电磁，地下温度和漫射CO _{2 2磁通测量的推论}

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Abstract > Vapor‐dominated hydrothermal systems are characterized by localized and elevated heat and gas flux. In these systems, steam and gas ascend from a boiling water reservoir, steam condenses beneath a low‐permeability cap layer, and liquid water descends, driven by gravity (“heat pipe” model). We combine magnetic, electromagnetic, and geoelectrical methods and CO <sub>2</sub> flux and subsurface temperature measurements in the Solfatara Plateau Thermal Area in the Yellowstone Caldera to address several fundamental questions: (1) What are the structural and/or lithological controls on heat and mass transport in vapor‐dominated areas? (2) What is the geometry and size of convecting multiphase thermal plumes? (3) Are thermal plumes associated with subsurface rock alteration and demagnetization? Magnetic and electromagnetic data inversions suggest an asymmetric 50‐ to 100‐m thick basin of glacial deposits with the thickest part adjacent to the margin of a rhyolite flow. The 3‐D electrical conductivity model in the glacial basin reveals a narrow vertical conductor interpreted as a focused multiphase plume, which coincides at the ground surface with the heat and CO <sub>2</sub> flux maxima. The magnetic data suggest that destruction of magnetic minerals due to rock alteration associated with the hydrothermal plume occurs mainly near the ground surface. We propose a model where the buoyant multiphase plume forms in response to decompression, boiling, and phase separation of pressurized thermal groundwater that discharges from the brecciated base of a rhyolite flow into the basin of glacial deposits. Results from multiphase groundwater flow and heat transport numerical simulations corroborate the first‐order characteristics of this model. </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”>摘要</标题> >蒸汽主导的水热系统的特征是局部和升高的热和气体通量。在这些系统中，蒸汽和气体从沸水储存器中升，低渗透盖层下方的蒸汽冷凝，并由重力驱动的液态水下降（“热管”模型）。我们将磁性，电磁和电气方法和CO <sub> 2 </ sub>通量和地下温度测量相结合，在黄石火山油的高原热面积中进行了几个基本问题：（1）结构和/或蒸汽占主导地区热量和大规模运输岩性控制？（2）对流多相热羽毛的几何形状和大小是多少？（3）是与地下岩石改变和退磁相关的热羽毛吗？磁性和电磁数据反转表明，冰川沉积物的不对称50-至100m厚盆地，其厚度与细流石流动裕度相邻。冰川盆地中的3-D电导率模型揭示了作为聚焦的多相羽流解释的窄垂直导体，其在地面与热量和CO <sub> 2 </ sub>通量最大值相一致。磁数据表明，由于与水热羽流相关的岩石改变而导致的磁性矿物质的破坏主要发生在地面附近。我们提出了一种模型，其中潮流式多相羽流响应于加压热地水的减压，沸腾和相分离，其从流纹岩的封闭底部排出到冰川沉积物的盆地中。多相地下水流量和热传输数值模拟的结果证实了该模型的一阶特征。 </ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第1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=Bouligand Claire&option=202" target="_blank" rel="nofollow">Bouligand Claire;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hurwitz Shaul&option=202" target="_blank" rel="nofollow">Hurwitz Shaul;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vandemeulebrouck Jean&option=202" target="_blank" rel="nofollow">Vandemeulebrouck Jean;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Byrdina Svetlana&option=202" target="_blank" rel="nofollow">Byrdina Svetlana;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kass Mason Andrew&option=202" target="_blank" rel="nofollow">Kass Mason Andrew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lewicki Jennifer Lynn&option=202" target="_blank" rel="nofollow">Lewicki Jennifer Lynn;</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>Université Grenoble Alpes Université Savoie Mont Blanc CNRS IRD IFSTTAR ISTerreGrenoble France;</p> <p>U.S. Geological SurveyMenlo Park CA USA;</p> <p>Université Grenoble Alpes Université Savoie Mont Blanc CNRS IRD IFSTTAR ISTerreGrenoble France;</p> <p>Université Grenoble Alpes Université Savoie Mont Blanc CNRS IRD IFSTTAR ISTerreGrenoble France;</p> <p>U.S. Geological SurveyDenver CO USA;</p> <p>U.S. Geological SurveyMenlo Park CA 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=hydrothermal&option=203" rel="nofollow">hydrothermal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geophysical imaging&option=203" rel="nofollow">geophysical imaging;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetic methods&option=203" rel="nofollow">magnetic methods;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geoelectrical methods&option=203" rel="nofollow">geoelectrical methods;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=multiphase flow&option=203" rel="nofollow">multiphase flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yellowstone&option=203" rel="nofollow">Yellowstone;</a> </p> <div class="translation"> 机译：水热;地球物理成像;磁性方法;地电气方法;多相流动;黄石; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:24:16</span> </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591152.html">Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO <sub >2</sub>2 Flux Measurements</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bouligand Claire&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bouligand Claire,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hurwitz Shaul&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hurwitz Shaul,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vandemeulebrouck Jean&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Vandemeulebrouck Jean,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO 22 Flux Measurements

摘要

Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO ₂2 Flux Measurements