ISSN 1000-3665 CN 11-2202/P

    考虑温度影响的改进西原流变模型及一维固结解

    Improved Nishihara rheological model coupling temperature and one-dimensional consolidation solution

    • 摘要: 随着我国热能源开发,热力管道工程大规模应用,由此带来的岩土体应力、变形、渗流和温度耦合作用问题已经成为岩土工程领域的研究热点。在长期荷载作用下,岩土体的变形和强度随时间而变化,尤其是软土,具有明显的流变特征。传统的各流变模型并未考虑升温方式和温度对其各参数的影响。为了能更好地反映流变固结特性,考虑软黏土的黏弹塑性,在西原模型基础上,引入温度膨胀系数,建立了热力耦合作用下的改进西原模型,给出了其应力-应变关系,并利用Laplace变换和逆变换求解了一维热固结方程,得到了其解析解。计算结果表明:固结压力一定时,温度升高加快土体固结;温度一定时,土体中孔压随固结压力增大而减小;改进西原模型的弹性模量越大,孔压消散速率越大,土体固结越快;土颗粒受温度影响而产生的热膨胀对于孔压消散的作用非常小;黏滞系数越小,孔压消散更快,土体固结越快;试验结果与考虑土体的黏弹塑性的热力耦合改进西原模型计算结果吻合,改进西原模型可以较好地描述土体的热力耦合特性。

       

      Abstract: With the development of thermal energy and thermal power pipeline engineering and the large-scale application of ground-source heat pump technology in China, the problems of stress, deformation, seepage, and temperature coupling of rock and soil have become research hotspots in geotechnical engineering. Under a long-term loading, the deformation and strength of rock and soil bodies (especially the soft soil) change with time and are of obvious rheological characteristics. The traditional rheological models do not consider the effects of temperature and temperature rise mode on their parameters. In order to better reflect the rheological consolidation characteristics, the viscoelastic-plasticity of the soft clay is considered, the improved Nishihara model under thermo-mechanical coupling is established based on the Nishihara model by introducing the temperature expansion coefficient, and the stress-strain relationship is given. The analytical solutions are obtained for one-dimensional heat consolidation equation by using the Laplace transform and the inverse transform. The results show that when the consolidation pressure is constant, the temperature rise will accelerate the consolidation of the soil. When the temperature is constant, the pore pressure in the soil decreases with the increasing consolidation pressure. When the elastic modulus of the improved Nishihara model is increased, the speed of pore pressure dissipation and the consolidation of the saturated soil are accelerated. The thermal expansion caused by temperature of the soil particles has a very small effect on the dissipation of the pore pressure. The smaller the viscous coefficient, the faster the pore pressure dissipates and the faster the soil is consolidated. The experimental results are in good agreement with the thermal coupling of the viscoelastic-plasticity of the soil. The improved Nishihara model can better describe the thermal coupling characteristics of the soil.

       

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