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Analytical study of the reflection and transmission coefficient of the submarine interface

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Wybrane pełne teksty z tego czasopisma
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Języki publikacji
EN
Abstrakty
EN
The analytical study of the reflection and transmission coefficient of the seafloor interface is essential for the characterization of the ocean bottom in marine seismic exploration. Based on the boundary conditions of the seafloor interface, the analytical expression of the reflection and transmission coefficient at the submarine interface is derived in this study by using the steady-state wave solution of the elastic wave in a homogeneous, isotropic medium. With this analytical expression, the characteristics of the reflection and transmission coefficient at the submarine interface are analysed and discussed using critical angles. The results show that the change in the reflection and transmission coefficient with the incidence angle presents a ‘‘segmented’’ characteristic, in which the critical angle is the dividing point. The amplitude value and phase angle of the coefficient at the submarine interface change dramatically at the critical angle, which is related to the P- and S-wave velocities in the seabed layer. Compared with the stiff seabed, the soft seabed has a larger P-wave critical angle and an absence of the converted S-wave critical angle, owing to the low P- and S-wave velocities in the solid seabed layer. By analysing and discussing the special changes that occur in the coefficient values at the critical angle, the reflection and transmission characteristics of the different incident angles are obtained. Synthetic models of both stiff and soft seafloors are provided in this study to verify the analytical results. Finally, we compared our synthetic results with real data from the Gulf of Mexico, which enabled the validation of our conclusions.
Czasopismo
Rocznik
Strony
449--460
Opis fizyczny
Bibliogr. 40 poz.
Twórcy
autor
  • State Key Laboratory of Earthquake Dynamics, Institute of Geology, Earthquake Administration China, Beijing, China
  • Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 10029, China
autor
  • State Key Laboratory of Earthquake Dynamics, Institute of Geology, Earthquake Administration China, Beijing, China
autor
  • State Key Laboratory of Earthquake Dynamics, Institute of Geology, Earthquake Administration China, Beijing, China
Bibliografia
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  • 19. Long JJ, Li GZ, Zou DP (2014) Theoretical relations of longitudinal wave velocity and physical- mechanical properties for seafloor sediments and comparison. Acta Oceanol Sin (in Chinese) 36(7):111–117
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  • 33. Skopintseva L, Ayzenberg M, Landrø M (2011) Long-offset AVO inversion of PP reflections from plane interfaces using effective reflection coefficients. Geophysics 76(6):889–893
  • 34. Sun PY, Lu XL, Li YP (2008) Elastic parameter AVO approximations and their applications. In: 78th Annual International Meeting, SEG, Expanded Abstracts, pp 523–527
  • 35. Xu Y, Bancroft JC (1997) Joint AVO analysis of PP and PS seismic data. Crewes Research Report, pp 1–44
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-f0418524-d7c2-4dd3-a114-339e5625763a
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