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首页> 外文期刊>Geochemistry, geophysics, geosystems >Fluid Flux in Fractured Rock of the Alpine Fault Hanging‐Wall Determined from Temperature Logs in the DFDP‐2B Borehole, New Zealand
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Fluid Flux in Fractured Rock of the Alpine Fault Hanging‐Wall Determined from Temperature Logs in the DFDP‐2B Borehole, New Zealand

机译：在高山故障悬挂壁的裂缝岩石中的液体通量从DFDP-2B钻孔，新西兰的温度测量确定

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Abstract > Sixteen temperature logs were acquired during breaks in drilling of the 893m‐deep DFDP‐2B borehole, which is in the Alpine Fault hanging‐wall. The logs record various states of temperature recovery after thermal disturbances induced by mud circulation. The long‐wavelength temperature signal in each log was estimated using a sixth‐order polynomial, and residual (reduced) temperature logs were analyzed by fitting discrete template wavelets defined by depth, amplitude, and width parameters. Almost two hundred wavelets are correlated between multiple logs. Anomalies generally have amplitudes 1°C, and downhole widths 20m. The largest amplitudes are found in the first day after mud circulation stops, but many anomalies persist with similar amplitude for up to 15 days. Our models show that thermal and hydraulic diffusive processes are dominant during the first few days of re‐equilibration after mud circulation stops, and fluid advection of heat in the surrounding rock produces temperature anomalies that may persist for several weeks. Models indicate that the fluid flux normal to the borehole within fractured zones is of order 10 ?7 to 10 ?6 m s ?1 , which is 2–3 orders of magnitude higher than the regional flux. Our approach could be applied more widely to boreholes, as it uses the thermal re‐equilibration phase to derive useful information about the surrounding rock mass and its fluid flow regime. </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”>抽象</ title> > 在893m-Deep DFDP-2B钻孔的钻孔中获得了十六个温度日志，这是在Alpine Fault悬挂墙中的钻孔。原木在泥浆循环引起的热干扰后记录各种温度恢复状态。使用第六阶多项式估计每个日志中的长波长温度信号，并且通过拟合由深度，幅度和宽度参数定义的离散模板小波来分析残差（减小）温度日志。几乎两百个小波在多个日志之间相关。异常通常具有振幅＆ 1℃，井下宽度且井下宽度。最大的幅度在泥浆循环停止后的第一天发现，但许多异常持续存在相似的振幅，最多15天。我们的模型表明，在泥浆循环停止后的重新平衡的前几天热量和液压扩散过程在泥浆循​​环停止后的前几天是显着的，而流体在周围岩石中的热量会产生可能持续数周的温度异常。模型表明骨折区域内的钻孔正常的流体通量是订单10 ？7 </ sup> 到10. ？6 </ sup> 多发性硬化症 ？1 </ sup> ，比区域助焊剂高2-3个数量级。我们的方法可以更广泛地应用于钻孔，因为它使用热再平衡阶段来导出关于周围岩体和流体流动状态的有用信息。 </ 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8期</span><b style="margin: 0 2px;">|</b><span>共16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=Janku‐Capova Lucie&option=202" target="_blank" rel="nofollow">Janku‐Capova Lucie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sutherland Rupert&option=202" target="_blank" rel="nofollow">Sutherland Rupert;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Townend John&option=202" target="_blank" rel="nofollow">Townend John;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doan Mai‐Linh&option=202" target="_blank" rel="nofollow">Doan Mai‐Linh;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Massiot Cécile&option=202" target="_blank" rel="nofollow">Massiot Cécile;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Coussens Jamie&option=202" target="_blank" rel="nofollow">Coussens Jamie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Célérier Bernard&option=202" target="_blank" rel="nofollow">Célérier Bernard;</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 Geography Environment and Earth SciencesVictoria University of WellingtonPO Box 600 Wellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonPO Box 600 Wellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonPO Box 600 Wellington New Zealand;</p> <p>Univ. Grenoble Alpes Univ. Savoie Mont Blanc CNRS IRD IFSTTAR ISTerre 38000 Grenoble France;</p> <p>GNS ScienceLower Hutt Wellington New Zealand;</p> <p>Ocean and Earth ScienceNational Oceanography Centre Southampton University of Southampton European WaySouthampton SO14 3ZH United Kingdom;</p> <p>Géosciences MontpellierUniversité de Montpellier CNRSMontpellier France;</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=permeability&option=203" rel="nofollow">permeability;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=groundwater&option=203" rel="nofollow">groundwater;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrogeology&option=203" rel="nofollow">hydrogeology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geothermal&option=203" rel="nofollow">geothermal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=aquifer&option=203" rel="nofollow">aquifer;</a> </p> <div class="translation"> 机译：渗透率;地下水;水文地质;地热;含水层; </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/0704023360438.html">Fluid Flux in Fractured Rock of the Alpine Fault Hanging‐Wall Determined from Temperature Logs in the DFDP‐2B Borehole, New Zealand</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Janku‐Capova Lucie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Janku‐Capova Lucie,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sutherland Rupert&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sutherland Rupert,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Townend John&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Townend John,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第8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：在高山故障悬挂壁的裂缝岩石中的液体通量从DFDP-2B钻孔，新西兰的温度测量确定</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704014465002.html">Large-displacement, hydrothermal frictional properties of DFDP-1 fault rocks, Alpine Fault, New Zealand: Implications for deep rupture propagation</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niemeijer A. 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href="/patent-detail/06130424295951.html">Bit less drilling system for drilling deep holes in e.g. tunnel for mounting power cable, has casing designed as lattice and made of plastic with low temperature, metal and ceramics, and device manipulating rock and borehole wall</a> <b>[P]</b> . <span> 外国专利： <!-- 德国专利： --> DE102010004609A1 </span> <span> . 2011-08-25</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：用于钻深孔的无位钻孔系统，例如用于安装电力电缆的隧道，具有设计成格子的外壳，该外壳由耐高温的塑料，金属和陶瓷制成，并具有操纵岩石和井壁的装置 </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" 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