Seismic responses of P wave incident stratified unsaturated soil site under thermal effects
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Publication:6576381
DOI10.1007/S00707-024-03964-5zbMATH Open1548.74439MaRDI QIDQ6576381
Publication date: 22 July 2024
Published in: Acta Mechanica (Search for Journal in Brave)
analytical solutiontransfer matrix methodnumerical solutionHelmholtz vector decomposition principlewave amplitude coefficient conversion matrix
Bulk waves in solid mechanics (74J10) Thermal effects in solid mechanics (74F05) Soil and rock mechanics (74L10) Seismology (including tsunami modeling), earthquakes (86A15)
Cites Work
- Title not available (Why is that?)
- A continuum theory of porous media saturated by multiple immiscible fluids. I: Linear poroelasticity
- Thermoelasticity
- Reflection and transmission of elastic waves at an elastic/porous solid saturated by two immiscible fluids
- A generalized dynamical theory of thermoelasticity
- High-frequency homogenization for periodic media
- Rayleigh–Bloch waves along elastic diffraction gratings
- Bloch waves in periodic multi-layered acoustic waveguides
- Transmission of Elastic Waves through a Stratified Solid Medium
- Nonstationary Rayleigh waves on the thermally-insulated surfaces of some thermoelastic bodies of revolution
- Dynamic response of imperfect interfaces on the reflection and transmission of the waves in context of generalised thermo-elasticity
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