一维粘弹性非饱和多孔介质瞬态响应的解析解

IF 3.6 2区 工程技术 Q2 ENGINEERING, GEOLOGICAL
Yun Zhao, Ya-bo Shi, Zhang-long Chen, Jing Hu, Ping Xu, Zhen-dong Shan
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引用次数: 0

摘要

拉普拉斯变换方法广泛应用于粘弹性动力学问题的求解。然而,这种方法的数值反演过程存在不稳定性,特别是对于长时间响应问题。此外,通过拉普拉斯变换方法得到的解通常是半解析的。针对非饱和粘弹性多孔介质的一维瞬态响应问题,提出了基于有限傅里叶变换方法的解析解。首先,利用问题的对称性,将典型应力-位移边界问题的解转化为应力-应力边界问题的解。其次,通过有限傅里叶正弦和余弦变换,将原二阶粘弹性偏微分控制方程在频域上转化为一阶常微分方程组进行求解,并利用状态空间方法在频域上给出解析解。最后,利用有限傅里叶反变换方法在时域上给出了原问题的级数解析解。通过与拉普拉斯解方法和已有弹性解结果的比较,验证了所提方法的准确性。数值算例分析表明,阻尼系数对波速有显著影响。随着阻尼系数的增大,波相一般呈减小趋势。随着饱和度的增加,波的速度增大,波的速度减小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Analytical Solution for the Transient Response of a One-Dimensional Viscoelastic Unsaturated Porous Medium

Analytical Solution for the Transient Response of a One-Dimensional Viscoelastic Unsaturated Porous Medium

The Laplace transform method is widely used for solving viscoelastic dynamic problems. However, the numerical inversion process of this method suffers from instability, especially for long-duration response issues. Moreover, the solutions obtained via the Laplace transform method are often semi-analytical. In this study, addressing the one-dimensional transient response problem of unsaturated viscoelastic porous media, an analytical solution is proposed based on the finite Fourier transform method. First, leveraging the symmetry of the problem, the solution of a typical stress-displacement boundary problem is transformed into the solution of a stress-stress boundary problem. Second, by applying finite Fourier sine and cosine transforms, the original second-order viscoelastic partial differential governing equations are transformed into a system of first-order ordinary differential equations in the frequency domain for solution, and the analytical solution in the frequency domain is provided using the state-space method. Finally, the finite Fourier inverse transform method is used to present the analytical solution in series form for the original problem in the time domain. The accuracy of the proposed method is validated through comparison with the Laplace solution method and existing elastic solution results. The analysis of numerical examples shows that the damping coefficient η $\eta $ has a significant influence on the P 3 ${P}_3$ wave velocity. As the damping coefficient η $\eta $ increases, the wave phase generally tends to decrease. With the increase in saturation S w ${S}_w$ , the velocities of P 1 ${P}_1$ and P 2 ${P}_2$ waves increase, while the velocity of the P 3 ${P}_3$ wave decreases.

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来源期刊
CiteScore
6.40
自引率
12.50%
发文量
160
审稿时长
9 months
期刊介绍: The journal welcomes manuscripts that substantially contribute to the understanding of the complex mechanical behaviour of geomaterials (soils, rocks, concrete, ice, snow, and powders), through innovative experimental techniques, and/or through the development of novel numerical or hybrid experimental/numerical modelling concepts in geomechanics. Topics of interest include instabilities and localization, interface and surface phenomena, fracture and failure, multi-physics and other time-dependent phenomena, micromechanics and multi-scale methods, and inverse analysis and stochastic methods. Papers related to energy and environmental issues are particularly welcome. The illustration of the proposed methods and techniques to engineering problems is encouraged. However, manuscripts dealing with applications of existing methods, or proposing incremental improvements to existing methods – in particular marginal extensions of existing analytical solutions or numerical methods – will not be considered for review.
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