Coupled FEM/SBFEM investigation on the characteristic analysis of seismic motions of a trapezoidal canyon in a layered half-space
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Publication:1980213
DOI10.1016/J.ENGANABOUND.2021.07.007OpenAlexW3194993787MaRDI QIDQ1980213
Li Yanpeng, Hu Zhiqiang, Li Zhiyuan, Lin Gao
Publication date: 3 September 2021
Published in: Engineering Analysis with Boundary Elements (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.enganabound.2021.07.007
Related Items (2)
The scattering of seismic waves from saturated river valley with water layer: modelled by indirect boundary element method ⋮ A three-dimensional indirect boundary integral equation method for the scattering of seismic waves in a poroelastic layered half-space
Cites Work
- Unnamed Item
- Simulation of the spatially correlated multiple-station earthquake ground motions of the coupled alluvial valley-hill terrain
- Complex variable function method for the scattering of plane waves by an arbitrary hole in a porous medium
- The scaled boundary finite-element method - alias consistent infinitesimal finite-element cell method - for elastodynamics
- High performance of the scaled boundary finite element method applied to the inclined soil field in time domain
- A 2.5D IBEM to investigate the 3D seismic response of 2D topographies in a multi-layered transversely isotropic half-space
- Scattering of plane P- and SV-waves by periodic topography: modeled by a PIBEM
- Two-dimensional FM-IBEM solution to the broadband scattering of elastic waves in a fluid-saturated poroelastic half-space
- Dynamic stress concentration around elliptic cavities in saturated poroelastic soil under harmonic plane waves
- A modified scaled boundary finite element method for three-dimensional dynamic soil-structure interaction in layered soil
- Transmission of Elastic Waves through a Stratified Solid Medium
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