摘要
冻融力学研究正温、负温环境交替变化对材料的物理力学性质的影响。由于软岩为强度低、孔隙度大、胶结程度差、含有大量膨胀性粘土矿物的松散、软弱岩层。因此,软岩的水-热-力耦合不是一个简单的过程。初步提出了软岩的水-热迁移机理,进而提出了软岩水-热-力耦合的基本数学模型。最后用ANSYS软件模拟了隧道围岩温度场与应力场,得到了隧道围岩冻胀力的分布趋势。
Freezing-thawing environment affects the stability of soft rocks in cold region.Because soft rocks have low strength and high porosity and contain large amount of expansive clay minerals,the freezing-thawing process of soft rock is complicated.Based on physical properties of soft rock and water-rock interaction and theories on continuum medium,heat conduction and mass transfer,basic equations of freezing-thawing process are established.The equations consider water movement,heat conduct,phase change of water and relevant latent heat.The FEM software,ANSYS,is employed to simulate the temperature distribution of soft rock tunnel and temperature-stress field.Simulation results agree with the practice.Liquid-thermal-stress coupling models are set up,in which soft rocks is taken as 3D elasticity body and the damage of soft rocks is considered.The distribution of frost-heaving force is determined by analytical method,and the damage parameters and elastic moduli of soft rocks in different stages are determined by using the equation of rheological damage.
出处
《岩石力学与工程学报》
EI
CAS
CSCD
北大核心
2004年第z1期4373-4377,共5页
Chinese Journal of Rock Mechanics and Engineering
基金
国家自然科学基金(40372119)
教育部优秀青年教师基金(2091)
陕西省自然科学基金(2003D05)资助项目。
关键词
岩石力学
软岩
水-热-力耦合
冻融损伤
rock mechanics,soft rock,liquid-heat-stress coupling,freezing-thawing damage