Modeling attenuation and dispersion of acoustic waves in porous media containing immiscible non viscous fluids
This paper reports the results of the propagation of P-waves in porous media, simulated by solving the generalized Biot´s equations in finite differences. In saturated models, it was observed that when a wave advances, the maximum amplitude of the spectrum is shifted to lower frequencies, and that t...
- Autores:
-
Duitama Leal, Alejandro
Almanza, Ovidio
Montes Vides, Luis Alfredo
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2016
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/60483
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/60483
http://bdigital.unal.edu.co/58815/
- Palabra clave:
- 62 Ingeniería y operaciones afines / Engineering
Biot theory
attenuation
viscosity
saturation
porosity
Teoría de Biot
atenuación
viscosidad
saturación
porosidad
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
Summary: | This paper reports the results of the propagation of P-waves in porous media, simulated by solving the generalized Biot´s equations in finite differences. In saturated models, it was observed that when a wave advances, the maximum amplitude of the spectrum is shifted to lower frequencies, and that this maximum amplitude and its frequency are directly related. Besides this, the quality factor decreases with porosity and saturation. Hence, attenuation becomes higher when porosity, saturation, and frequency increase but tends asymptotically towards a constant value. Although phase analysis is generally discarded, it does provide interesting results. It was noted that the wave phase changes linearly with frequency at a rate of change that increases linearly with travel time. This rate increases with saturation but decreases slightly with porosity. This work ignores spherical divergence or scattering and concentrates on intrinsic attenuation caused by friction, particularly between fluids and solid particles. |
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