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水热运移宏观特性实验系统-深部岩土力学与地下工程国家重点实验室
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</div> <div class="clear"></div> <!--============================头部 结束=============================--> <!--============================主体 开始=============================--> <section class="mbx_nav"> <div class="w1200"> <div class="mianbao"> <span>您所在位置：</span> <a href="../../index.htm">首页</a> >> <a href="../../yqsb1.htm">仪器设备</a> >> <span>正文</span> </div> <big>仪器设备</big> </div> </section> <section class="n_container"> <div class="w1200"> <div class="n_left"> <h1>仪器设备</h1> <div class="con"> <ul> </ul> </div> <div class="gg"> <img src="../../images/gg.jpg" border="0" width="200" height="150"> </div> </div> <div class="n_right"> <div class="n_news_detail"> <article class="n_article"> <script language="javascript" src="../../_dwr/interface/NewsvoteDWR.js"></script><script language="javascript" src="../../_dwr/engine.js"></script><script language="javascript" src="/system/resource/js/news/newscontent.js"></script><script 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220px!important;text-align: center;">重量：</td> <td></td> </tr> <tr> <td style="width: 220px!important;text-align: center;">技术参数：</td> <td></td> </tr> </tbody> </table>--> <div id="vsb_content"><div class="v_news_content"> <p style="text-align: center"><img src="/__local/F/E0/7D/E656B7A4B550275A5D1B2F0C461_0C7E636C_1263B.jpg" width="500" vsbhref="vurl" vurl="/_vsl/FE07DE656B7A4B550275A5D1B2F0C461/0C7E636C/1263B" vheight="" vwidth="500" orisrc="/__local/F/E0/7D/E656B7A4B550275A5D1B2F0C461_0C7E636C_1263B.jpg" class="img_vsb_content"></p> <p><br></p> <p style="text-align:left;font-size: medium;white-space: normal"><strong>仪器名称：水热运移宏观特性实验系统</strong></p> <p style="font-size: medium;white-space: normal"><strong>引进时间：</strong><span lang="EN-US">2020</span>年<span lang="EN-US">11</span>月</p> <p style="font-size: medium;white-space: normal"><strong>技术指标：</strong>实验系统包括：加压注水系统、加热系统、加载系统、数据采集设备、集中控制系统。</p> <p style="font-size: medium;white-space: normal">技术功能优势主要体现在以下六个方面：</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">1</span>）可以测试岩体不同状态（干燥、静态饱水、流动、法向应力等）结构面传热特性；</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">2</span>）可以开展裂隙岩体渗流传热实验；</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">3</span>）自主研制的封水转置，封水效果良好；</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">4</span>）采用对岩样上下表面加热的方法，能够准确得到裂隙进出口水温度、流量等数据；</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">5</span>）实时测量得到大量岩石表面温度数据，能够得到岩石表面的温度场分布情况。</p> <p style="font-size: medium;white-space: normal"><strong>功能及应用：</strong></p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US">1</span>）开展裂隙岩体传热特性实验，获得不同状态裂隙岩体有效热导率，研究温压耦合作用下不同裂隙岩体有效热导率演变规律，分析不同影响因素（干燥、静态饱水、法向应力、岩屑填充等）对裂隙岩体传热特性的影响；</p> <p style="font-size: medium;white-space: normal">（<span lang="EN-US" style="font-family: 仿宋">2</span>）开展裂隙岩体渗流传热实验，获得准确的裂隙进出口水温度、流量等数据及岩石表面的温度场分布情况，分析高温高压作用下不同影响因素（法向应力、裂隙面粗糙度、流量流速、接触情况等）对裂隙岩体渗流传热的影响，揭示固耦合作用下裂隙岩体水热运移机理。</p> <p style="font-size: medium;white-space: normal"><strong>安放地点： </strong>北京海淀清华东路国重实验室<span lang="EN-US">A104</span>室</p> <p style="font-size: medium;white-space: normal"><strong>所属实验室：</strong>深部非线性渗流测试分室（第二分室）</p> <p><br></p> </div></div> <div id="div_vote_id"></div> </div> <!--<p align=right> 上一条：<a href="2255.htm" >恒阻大变形锚杆/索HOPKINSON冲击拉伸实验室</a> 下一条：<a href="2253.htm" >局部流场可视化实验系统</a> </p>--> <!--<p align=right>【<a href="javascript:window.opener=null;window.open('','_self');window.close();">关闭</a>】</p>--> </form> </article> </div> </div> <div class="clear"></div> </div> </section> <!--============================主体 结束=============================--> <!--============================底部 开始=============================--> <footer> <div class="w1200"> <div class="top"> <p>地址：北京市海淀区清华东路16号宝源大厦A2座201室 邮编：100083 <br>Address: Room 201, A2 Baoyuan Building, 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