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Reflection of a plane wave from a two-layered seafloor with non-parallel interface between the layers
Panagiotis I Papadakis1, George S Piperakis1, Michael A Kalogerakis2
1Institute of Applied and Computational Mathematics, Foundation for Research and Technology Hellas, Nikolaou Plastira 100, Vassilika Vouton, GR 700 13 Heraklion, Crete, Greece.
This study introduces the Coherent Reflection Coefficient (CRC) for seafloor acoustics, accounting for slanted layers. Even small inclinations significantly alter reflection coefficients, impacting geophysical inversions.
Area of Science:
- Geophysics
- Acoustics
- Oceanography
Background:
- Seafloor acoustic reflection is crucial for geophysical surveys.
- Existing models often assume parallel layers, limiting accuracy for complex geology.
- The reflection coefficient quantifies acoustic energy returning from the seafloor.
Purpose of the Study:
- To extend the reflection coefficient concept to seafloors with non-parallel layers.
- To introduce and formulate the Coherent Reflection Coefficient (CRC).
- To develop a numerical tool for CRC calculations and analyze its impact on geophysical inversions.
Main Methods:
- Mathematical derivation of the Coherent Reflection Coefficient (CRC).
- Numerical implementation and code development for CRC calculations.
- Comparison of results for slanted versus parallel seafloor layers.
Main Results:
- The CRC formulation extends acoustic reflection analysis to non-parallel seafloor interfaces.
- Numerical simulations show substantial differences in reflection coefficients for slanted layers, even at small inclinations.
- A user-friendly toolbox facilitates CRC computation for realistic seafloor models.
Conclusions:
- Non-parallel seafloor layers significantly affect acoustic reflection coefficients.
- The CRC provides a more accurate model for complex seafloor geometries.
- This work enhances geophysical inversion schemes for improved seafloor parameter estimation.
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