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Decaying Lava Extrusion Rate at El Reventador Volcano, Ecuador, Measured Using High‐Resolution Satellite Radar

机译:厄瓜多尔EL Reventador Volcano腐烂的熔岩挤出率,采用高分辨率卫星雷达测量

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Abstract > Lava extrusion at erupting volcanoes causes rapid changes in topography and morphology on the order of tens or even hundreds of meters. Satellite radar provides a method for measuring changes in topographic height over a given time period to an accuracy of meters, either by measuring the width of radar shadow cast by steep sided features, or by measuring the difference in radar phase between two sensors separated in space. We measure height changes, and hence estimate extruded lava volume flux, at El Reventador, Ecuador, between 2011 and 2016, using data from the RADARSAT‐2 and TanDEM‐X satellite missions. We find that 39 new lava flows were extruded between 9 February 2012 and 24 August 2016, with a cumulative volume of 44.8M?m 3 dense rock equivalent and a gradually decreasing eruption rate. The average dense rock rate of lava extrusion during this time is 0.31?±?0.02?m 3 ?s ?1 , which is similar to the long‐term average from 1972 to 2016. Apart from a volumetrically small dyke opening event between 9 March and 10 June 2012, lava extrusion at El Reventador is not accompanied by any significant magmatic ground deformation. We use a simple physics‐based model to estimate that the volume of the magma reservoir under El Reventador is greater than 3?km 3 . Our lava extrusion data can be equally well fit by models representing a closed reservoir depressurising during the eruption with no magma recharge, or an open reservoir with a time‐constant magma recharge rate of up to 0.35?±?0.01?m 3 ?s ?1 . </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 =“JGRB52462-ABS-ABS-ABS-ABS-ABS-ABS-0001”> <标题类型=“MAIN”>摘录</标题> <P>熔岩挤出在爆发火山时会导致快速变化在数十甚至数百米的地形和形态上。卫星雷达提供了一种用于通过测量通过陡峭的侧面特征的雷达阴影的宽度或通过测量空间中分开的两个传感器之间的雷达相位之间的雷达相位宽度来测量仪表的准确性的地形高度变化的方法。我们测量高度变化,因此,在2011年和2016年间,El Reventador,El Reventador估计挤出熔岩体积助熔剂,2011年至2016年间,使用来自Radarsat-2和Tandem-X卫星任务的数据。我们发现,2012年2月9日和2016年8月24日挤压了39个新的熔岩流量,累计体积为44.8MΩ米 3 </ sup>致密的岩石当量和逐渐降低的喷发率。此时熔岩挤出的平均密集岩速率为0.31?±0.02?m 3 </ sup>Δs?1 </ sup>,类似于1972年的长期平均值到2016年。除了2012年3月9日至6月10日之间的大量小型堤坝开放活动之外,EL Reventador的熔岩挤出不伴随着任何显着​​的岩浆地面变形。我们使用简单的基于物理的模型来估计EL RevEndor下的Magma水库的体积大于3?Km 3 </ sup>。我们的熔岩挤出数据可以同样适合于代表在没有岩浆补给的喷发过程中闭合储存器减压的模型适合,或者具有时间常数岩浆充电率最高0.35Ω的开放储存器±0.01?m 3 </ sup>?s ?1 </ sup>。 </ 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>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共23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=Arnold D. W. D.&option=202" target="_blank" rel="nofollow">Arnold D. W. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Biggs J.&option=202" target="_blank" rel="nofollow">Biggs J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Anderson K.&option=202" target="_blank" rel="nofollow">Anderson K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vallejo Vargas S.&option=202" target="_blank" rel="nofollow">Vallejo Vargas S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wadge G.&option=202" target="_blank" rel="nofollow">Wadge G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ebmeier S. K.&option=202" target="_blank" rel="nofollow">Ebmeier S. K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Naranjo M. F.&option=202" target="_blank" rel="nofollow">Naranjo M. F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mothes P.&option=202" target="_blank" rel="nofollow">Mothes P.;</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>COMET School of Earth SciencesUniversity of BristolBristol UK;</p> <p>COMET School of Earth SciencesUniversity of BristolBristol UK;</p> <p>U.S. Geological Survey California Volcano ObservatoryMenlo Park CA USA;</p> <p>Instituto GeofísicoEscuela Politécnica NacionalQuito Ecuador;</p> <p>COMET Department of MeteorologyUniversity of ReadingReading UK;</p> <p>COMET School of Earth SciencesUniversity of BristolBristol UK;</p> <p>Instituto GeofísicoEscuela Politécnica NacionalQuito Ecuador;</p> <p>Instituto GeofísicoEscuela Politécnica NacionalQuito Ecuador;</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=InSAR&option=203" rel="nofollow">InSAR;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lava flows&option=203" rel="nofollow">lava flows;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eruption rate&option=203" rel="nofollow">eruption rate;</a> </p> <div class="translation"> 机译:insar;熔岩流动;喷发率; </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/0704025591675.html">Decaying Lava Extrusion Rate at El Reventador Volcano, Ecuador, Measured Using High‐Resolution Satellite Radar</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arnold D. 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break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译:利用多个测得的衰减间隔的衰减率来测量薄的固体电介质体积电阻率的方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130410360314.html">How the system, to generate satellite, a synthetic aperture radar (sar) image in the satellite or aerial platform equipped with the system to generate a plurality of sar images on satellite or aerial platform</a> <b>[P]</b> . <span> 外国专利: <!-- 日本专利: --> JP6066934B2 </span> <span> . 2017-01-25</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:该系统如何产生卫星,在装有该系统的卫星或空中平台上的合成孔径雷达(SAR)图像如何在卫星或空中平台上产生多个SAR图像 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130434150816.html">High resolution, synthetic aperture, side-looking radar system e.g., for satellites, has n-different spatial spectral regions for 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