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带相变瞬态温度场问题的扩展有限元解析
引用本文:何敏,李宁,高焕焕,刘乃飞.带相变瞬态温度场问题的扩展有限元解析[J].冰川冻土,2016,38(4):1044-1051.
作者姓名:何敏  李宁  高焕焕  刘乃飞
作者单位:1. 西安理工大学 岩土工程研究所, 陕西 西安 710048;2. 西北勘测设计研究院有限公司, 陕西 西安 710065
基金项目:国家自然科学基金项目(11572246;5117913);西安理工大学博士学位论文创新基金项目(207-002J1306)
摘    要:带相变瞬态传热问题是寒区工程多场耦合问题求解的关键.在剖析常规有限元法在求解带相变瞬态温度场问题的不足的基础上,结合冻土冻融温度变化的特点,提出采用扩展有限元法求解冻土工程带相变瞬态传热问题的新方法,以四边形单元为例推导了冻土工程温度场的求解格式,详细剖析了瞬态传热过程中移动界面水平集函数的构造、单元刚度矩阵的形成及高斯积分的求解.据此编写了相应的扩展有限元程序,通过经典Stefan问题全面验证了程序的正确性与合理性.

关 键 词:水热力耦合  相变  瞬态温度场  扩展有限元  
收稿时间:2016-05-28
修稿时间:2016-07-11

Extended finite element method analysis for the transient temperature field with phase change
HE Min,LI Ning,GAO Huanhuan,LIU Naifei.Extended finite element method analysis for the transient temperature field with phase change[J].Journal of Glaciology and Geocryology,2016,38(4):1044-1051.
Authors:HE Min  LI Ning  GAO Huanhuan  LIU Naifei
Institution:1. Institute of Geotechnical Engineering, Xi'an University of Technology, Xi'an 710048, China;2. Xibei Engineering Corporation Limited of the Power Construction Corporation of China, Xi'an 710065, China
Abstract:Transient heat transfer with phase change is the key to the solving of the multi-field coupling problems in cold regions.The freezing process of frozen soil can be divided into four stages based on the measured freez-ing curves in Changchun.Analyzing the shortage of the traditional finite element method in solving the phase change problem and the characteristic of frozen soil′s freezing process,the extended finite element method (XFEM)was proposed for solving the transient heat transfer problem with phase change for permafrost engineer-ing.The XFEM interpolating function and solving format of temperature field with phase change was derived that taking quadrilateral element as an example.Based on the study of the constructing and solving of the level set function,building of the stiffness matrix and subdividing of the elements,a XFEM program for the transient heat transfer problem with phase change was proposed in this paper which has been verified by classical Stefan prob-lem.
Keywords:THM coupling  ice-water phase change  transient temperature field  extended finite element method
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