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- W4383219983 abstract "Porous media are widely used in many fields. In particular, a building’s subgrade is a typical porous medium and is constantly subjected to static and dynamic thermal and normal loads, which may degrade structural performance. To permit understanding and improvement of the subgrade load bearing performance, this paper presents the analysis of a three-dimensional (3D) half-space elastic subgrade coupling of multi-fields using normal mode analysis (NMA) under Ezzat’s fractional order generalized theory of thermoelasticity. The influence of fraction order parameter, load frequency, and permeability coefficient on the thermo-hydro-mechanical dynamic (THMD) coupling response of fluid-saturated poro-elastic subgrade is analyzed with a two load including thermal impact and normal load all applied to the surface of the subgrade. The distributions of the dimensionless vertical displacement, temperature, stress, excess pore water pressure, and strain in the porous structure are analyzed and discussed in detail. The results of this paper show that the load frequency plays an important role on all dimensionless physical variables, the fraction order parameter only has a significant effect on the physical variables of the upper surface subjected to thermal impact, and the permeability coefficient mainly affects the stress, strain, and excess pore water pressure. The developed computational method can improve the decoupling speed without any transformation, and eliminates the limitation of numerical inverse transformation; the method has wide potential application in many engineering fields." @default.
- W4383219983 created "2023-07-06" @default.
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- W4383219983 date "2023-01-01" @default.
- W4383219983 modified "2023-09-27" @default.
- W4383219983 title "Three-Dimensional Thermo-Hydro-Mechanical Dynamic Analysis of a Half-Space Under Fractional Order Theory of Thermoelasticity" @default.
- W4383219983 doi "https://doi.org/10.1615/jpormedia.2023046653" @default.
- W4383219983 hasPublicationYear "2023" @default.
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