采矿与安全工程学报 ›› 2013, Vol. 30 ›› Issue (1): 68-73.

• 论文 • 上一篇    下一篇

渗流作用下裂隙岩体冻结温度场分布规律研究

  

  1. 中国矿业大学深部岩土力学与地下工程国家重点实验室,力学与建筑工程学院,江苏  徐州  221008
  • 收稿日期:2011-12-04 出版日期:2013-01-15 发布日期:2013-01-17
  • 作者简介:高娟(1988-),女,甘肃省静宁县人,研究生,从事渗流地层人工冻结方面的研究。 E-mail:gaojuan2611261@126.com Tel:18952239504
  • 基金资助:

    国家重点基础研究发展计划(973)项目(2010CB226800);
    国家自然科学基金重点项目(50834004);
    中国博士后科学基金面上项目(2011M500968)

Research on distribution law of frozen temperature field of fractured rock mass with groundwater seepage

  • Received:2011-12-04 Online:2013-01-15 Published:2013-01-17

摘要: 建立了渗流作用下裂隙岩体双孔冻结的数值计算模型,采用COMSOL Multiphysics有限元分析软件,实现了裂隙岩体冻结过程中耦合及相变问题的模拟,分析了裂隙存在对岩体冻结温度场及渗流场的影响,研究了不同渗流速度下对应的冻结温度场的分布规律。结果表明:裂隙的存在会减薄上游冻结壁厚度,等温线在冻结壁外圈形成“心形”分布;渗流速度对冻结壁的发育及其交圈时间影响较大,渗流速度愈大,冻结壁发育愈慢,交圈时间愈长。在本文条件下,当渗流速度小于7 m/d时,流速与交圈时间基本呈线性关系;当渗流速度超过7 m/d时,交圈时间呈现急剧增长,达到10 m/d时,交圈时间趋于无限大,即交不上圈。

关键词: 冻结温度场, 渗流, 裂隙岩体, 冻结壁, 交圈时间

Abstract: A numerical calculation model of fractured rock mass artificial seepage freezing with two holes was set up,and the problem of coupling and phase change during the freezing process were simulated by using the COMSOL Multiphysics finite-element analysis software.The influence of the fracture on the distribution of freezing temperature field and seepage field was analyzed.The distribution law of freezing temperature field corresponding to the different flow velocities was researched.The results show that the existence of fracture reduces the thickness of the frozen wall in the upstream,and the isotherms outside the frozen wall show“heart-shaped”distribution.The seepage velocity has a great influence on both the frozen wall development and the closure time.If the seepage velocity is increasing,the development of freezing wall will become slower and the closure time will become longer accordingly.In this paper,when the seepage velocity is less than 7 m/d,the closure time shows a linear relationship with the seepage velocity basically.But when the seepage velocity is more than 7 m/d,the closure time mount up sharply,the closure time tends to be infinite once the velocity exceeds 10 m/d,namely reach the unable closure stage.

Key words: freezing temperature field;seepage;the fractured rock mass;freezing wall;closure time