| dc.description.abstract | Numerical methods for the simulation of wave propagation have extensive applications in exploration
seismology as in velocity estimation and subsurface imaging. Among numerical methods,
the standard finite element method (FEM) presents important advantages such as the ability to
handle meshes to conform to complex geometry, making this technique attractive. However its
main drawback is the longer simulation time it may take compared to other numerical techniques.
Nonetheless, a modified version, the generalized finite element method (GFEM), has the potential
to overcome this limitation. Hence, I have applied the GFEM to simulate the acoustic wave propagation
to test its performance against the standard FEM in models that are relevant to exploration
seismology. The GFEM exploits the partition of unity property of the FEM standard basis functions
by incorporating additional user-defined enrichment functions to improve the efficiency of the
simulation. Specifically, I have incorporated plane waves at different directions to mimic the radial
propagation of transient acoustic waves, with the goal of accelerating the solution convergence.
I have tested this approach using models of interest in exploration seismology, including a low
velocity layer, a karst structure and topography. Results from these specific models show that
the GFEM approach is more efficient than a standard FEM reference solution, with an acceptable
solution accuracy. | en |
