饱和砂层渗流冻结水热耦合模型与试验验证
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  • 英文篇名:Mathematical Model and Test Verification of Seepage Freezing in Saturated Sand Layer
  • 作者:程桦 ; 林键 ; 王彬 ; 荣传新
  • 英文作者:CHENG Hua;LIN Jian;WANG Bin;RONG Chuan-xin;School of Civil Engineering and Architecture,Anhui University of Science and Technology;
  • 关键词:饱和砂层 ; 渗流冻结 ; 水热耦合 ; 多孔介质 ; 模型试验 ; 数值计算
  • 英文关键词:saturated sand layer;;seepage freezing;;coupled water and heat transfer;;porous media;;model test;;numerical calculation
  • 中文刊名:KXJS
  • 英文刊名:Science Technology and Engineering
  • 机构:安徽理工大学土木建筑学院;
  • 出版日期:2018-04-28
  • 出版单位:科学技术与工程
  • 年:2018
  • 期:v.18;No.445
  • 基金:国家自然科学基金(51374010,51474004,51778004)资助
  • 语种:中文;
  • 页:KXJS201812006
  • 页数:7
  • CN:12
  • ISSN:11-4688/T
  • 分类号:43-49
摘要
为研究渗流作用下饱和砂层冻结规律,根据冻结过程中土体水分迁移及热量变化、热力学和渗流力学的基本理论,并考虑冻结过程中绝对孔隙率的降低对渗流的影响,基于Harlan水热耦合模型,建立了饱和砂层含相变全参数渗流冻结耦合数学模型,并应用COMSOL有限元软件与MATLAB编程,实现了耦合数学模型的数值求解。设计了相似模型试验验证了该模型及方法的合理性。研究结果表明:数值模拟结果与试验结果较为吻合,数学模型与求解方法合理、有效,为今后渗流地层冻结的拓展研究提供可靠数学与试验基础。
        In order to deal with the freezing law of saturated sand layer in seepage process,according to the basic theory of soil moisture transfer and heat change,thermodynamics and seepage mechanics in freezing process,the decrease of absolute porosity in freezing process is also considered,based on the coupled model of Harlan,a mathematical model of full frozen coupling with phase change in saturated sand layer is established. The numerical solution of the coupling mathematical model is realized by using COMSOL finite element software and MATLAB programming,and the similarity model test is designed to verify the rationality of the model and method. The results show that the numerical simulation results are in good agreement with the experimental results,and the mathematical model and the solution method are reasonable and effective. It provides a reliable mathematical and experimental basis for the further study of seepage formation freezing.
引文
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