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Three-dimensional elastic wave scattering by a layer containing vertical periodic fractures
Seiji Nakagawa1, Kurt T Nihei, Larry R Myer
1Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, USA. snakagawa@lbl.gov
The Journal of the Acoustical Society of America
|June 26, 2003
Summary
This study models elastic wave scattering from periodic fractures using a combined finite element and plane wave numerical method. Results reveal how wave frequency, incidence angle, and fracture properties influence scattering characteristics.
Area of Science:
- Geophysics
- Acoustics
- Materials Science
Background:
- Understanding elastic wave propagation is crucial for characterizing subsurface structures.
- Fractures significantly alter wave propagation, impacting seismic data interpretation.
- Existing models often simplify fracture complexities, limiting accuracy.
Purpose of the Study:
- To numerically simulate and analyze elastic wave scattering from a layer with periodic vertical fractures.
- To investigate the influence of various parameters on scattering patterns.
- To provide a more detailed understanding of wave interactions with fractured media.
Main Methods:
- A numerical technique combining the finite element method (FEM) and plane wave method (PWM).
- Explicit modeling of individual fractures to capture discrete and multiple scattering events.
- Simulation of three-dimensional (3D) elastic wave scattering from a two-dimensional (2D) fractured layer.
Main Results:
- Scattering characteristics are sensitive to wave frequency and angle of incidence.
- Fracture properties, including stiffness, height, and spacing (regular and irregular), demonstrably affect wave scattering.
- The model successfully simulates both direct and multiply scattered wave arrivals.
Conclusions:
- The developed numerical technique accurately captures complex elastic wave scattering phenomena in fractured media.
- Detailed fracture properties play a significant role in modifying wave propagation.
- This research enhances the capability to interpret seismic data in geologically complex, fractured environments.