Slowness surface calculation for different media using the symbolic mathematics language maple®
Starting from the equation in different media, we obtain the different type of waves that can exists in such media. The evaluation of the eigenvalues and eigenvectors let us construct the slowness surfaces. In general complex calculations case have to be made. In this work, routines were implemented...
- Autores:
-
Piedrahita, Carlos
Piedrahita, Carlos
Salinas, Trino
Altamar, Hernando
Pachano, Karen
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2004
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/34065
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/34065
http://bdigital.unal.edu.co/24145/
- Palabra clave:
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
| Summary: | Starting from the equation in different media, we obtain the different type of waves that can exists in such media. The evaluation of the eigenvalues and eigenvectors let us construct the slowness surfaces. In general complex calculations case have to be made. In this work, routines were implemented in the symbolic language MAPLE® and the slowness surfaces were plotted. This work is relevant for the modelling of equivalent media that simulates natural fractured reservoirs, like those common in the Colombian foothills. It is important to understand the seismic response of this reservoirs for exploration of this areas. |
|---|