期刊文献+
共找到2篇文章
< 1 >
每页显示 20 50 100
基于热-水-力数值模拟的饱和正常固结黏土热压缩现象
1
作者 张锋 熊勇林 《同济大学学报(自然科学版)》 EI CAS CSCD 北大核心 2023年第1期1-7,F0002,共8页
既有饱和正常固结土体加热试验研究表明,温度升高时,土体的体积变化表现为体积收缩,这与热胀冷缩基本通识相违背。针对这一问题,通过热-水-力(THM)完全耦合有限元程序对饱和正常固结黏土的加热试验进行了数值模拟。结果表明,由于黏土的... 既有饱和正常固结土体加热试验研究表明,温度升高时,土体的体积变化表现为体积收缩,这与热胀冷缩基本通识相违背。针对这一问题,通过热-水-力(THM)完全耦合有限元程序对饱和正常固结黏土的加热试验进行了数值模拟。结果表明,由于黏土的热传导系数及渗透系数都比较低,在升温过程中,试样内部会形成温度差,进而产生超孔隙水压,随着超孔隙水压的消散,最终使土体表现为热压缩现象。当增大土体的渗透系数时,土体内部不产生超孔隙水压,这时土体表现为热膨胀。因此,饱和正常固结土体升温引起的热压缩现象并非土体基本力学特性,而是一个边界值问题。 展开更多
关键词 试验 热-水-力数值分析 正常固结黏土 弹黏塑性本构模型
在线阅读 下载PDF
Coupled thermo-hydro-mechanical-migratory model for dual-porosity medium and numerical analysis 被引量:6
2
作者 张玉军 杨朝帅 《Journal of Central South University》 SCIE EI CAS 2011年第4期1256-1262,共7页
A coupled thermo-hydro-mechanical-migratory model of dual-porosity medium for saturated-unsaturated ubiquitous-joint rockmass was established,in which the stress field and the temperature field were single,but the see... A coupled thermo-hydro-mechanical-migratory model of dual-porosity medium for saturated-unsaturated ubiquitous-joint rockmass was established,in which the stress field and the temperature field were single,but the seepage field and the concentration field were double,and the influences of sets,spaces,angles,continuity ratios,stiffnesses of fractures on the constitutive relationship of the medium were considered.Also,the relative two-dimensional program of finite element method was developed.Taking a hypothetical nuclear waste repository as a calculation example,the case in which the rockmass was unsaturated dual-porosity medium and radioactive nuclide leak was simulated numerically,and the temperatures,negative pore pressures,saturations,flow velocities,nuclide concentrations and principal stresses in the rockmass were investigated.The results show that the negative pore pressures and nuclide concentrations in the porosity and fracture present different changes and distributions.Even though the saturation degree in porosity is only about 1/10 that in fracture,the flow velocity of underground water in fracture is about three times that in porosity because the permeability coefficient of fracture is almost four orders higher than that of porosity.The value of nuclide concentration in fracture is close to that in porosity. 展开更多
关键词 ubiquitous-joint rockmass dual-porosity medium thermo-hydro-mechanical-migratory coupling model numericalanalysis
在线阅读 下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部