Numerical evidence of elliptical polarization in homogeneous fluid‐saturated porous sandstone and the nexus to inhomogeneous plane waves
| Audiencia | Público en general | es_ES |
| Cobertura | México | es_ES |
| Fecha de ingreso | 2026-09-15T00:30:21Z | |
| Fecha de publicación | 2009-01-01 | |
| Resumen | The polarization of body waves in a fluid‐saturated homogeneous porous sandstone is quantified by computing the Green's function; the findings are confirmed with grid modeling. Both results agree that forces in an unbounded homogeneous isotropic porous medium generate harmonic perturbations whose particle motion varies along the wavefront from linear to elliptical; such behavior typically associated to homogeneous and inhomogeneous viscoelastic plane waves in layered media. Following this analogy, it is concluded that the attenuation angle γ is the function of the direction of wave propagation, wave type, and direction of the applied force. With this information, the attenuation angle γ1 of the initial ray segment can be estimated, resolving in a different manner the issue of indeterminacy in the asymptotic ray solution. It is also concluded that the assumption of γ1 = 0 for normally incident viscoelastic plane waves in layered media may be correct, but only for P waves generated by vertical forces; as propagation direction increases, so does the error, the rate depending on Q. The results also show that (1) a P wave resembles a S wave and vice versa for preferred directions and (2) the sense of particle motion is opposite for both waves, prograde and retrograde, respectively, and vice versa, depending on the direction of the applied force. | es_ES |
| Doi | https://doi.org/10.1029/2008jb006141 | es_ES |
| URI | https://riuat.uat.edu.mx/handle/123456789/2309 | |
| Idioma | es | es_ES |
| Editorial | American Geophysical Union (AGU) | es_ES |
| Relación | Journal of Geophysical Research: Solid Earth | es_ES |
| URL relacionado | https://doi.org/10.1029/2008jb006141 | es_ES |
| Derechos | Acceso abierto (Metadatos de producción científica) | es_ES |
| Licencia | http://purl.org/coar/access_right/c_abf2 | es_ES |
| Fuente | Journal of Geophysical Research: Solid Earth | |
| Título | Numerical evidence of elliptical polarization in homogeneous fluid‐saturated porous sandstone and the nexus to inhomogeneous plane waves | es_ES |
| Tipo | Artículo | es_ES |
| Arbitrado | Ha sido Arbitrado | es_ES |
| Autor | Quiroga‐Goode, G. | |
| Autor | Jiménez‐Hernández, S. | |
| Autor | Padilla‐Hernández, R. | |
| Autor | Quiroga‐Goode, G. | es_ES |
| Autor | Jiménez‐Hernández, S. | es_ES |
| Autor | Padilla‐Hernández, R. | es_ES |
| Institución | Universidad Autónoma de Tamaulipas | |
| Institución | Universidad Autónoma de Tamaulipas | es_ES |
| Número | B5 | es_ES |
| URL relacionada | https://doi.org/10.1029/2008jb006141 | |
| Tipo de artículo | Indexado | |
| Tipo de artículo | Indexado | es_ES |
| Volumen | 114 | es_ES |