Recuperação de propriedades acústicas da subsuperfície através da inversão sísmica por mínimos quadrados linear e não linear

In this work, the inverse problem of exploration geophysics is solved through two techniques based on the minimization of the least squares objective function. The nonlinear problem that estimates the acoustic velocity of the medium is solved by seismic full waveform inversion. For this, two multisc...

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Detalles Bibliográficos
Autor: Bautista, Kristian David Torres
Tipo de recurso: tesis de maestría
Estado:Versión publicada
Fecha de publicación:2019
País:Brasil
Institución:Universidade Federal do Rio de Janeiro (UFRJ)
Repositorio:Repositório Institucional da UFRJ
Idioma:portugués
OAI Identifier:oai:pantheon.ufrj.br:11422/14079
Acceso en línea:http://hdl.handle.net/11422/14079
Access Level:acceso abierto
Palabra clave:FWI
LSRTM
Inversão
Geofísica computaciona
CNPQ::ENGENHARIAS::ENGENHARIA CIVIL
Descripción
Sumario:In this work, the inverse problem of exploration geophysics is solved through two techniques based on the minimization of the least squares objective function. The nonlinear problem that estimates the acoustic velocity of the medium is solved by seismic full waveform inversion. For this, two multiscale strategies were considered in order to mitigate the nonlinearity of the problem. In addition, a preconditioner term that approximates the inverse of the Hessian matrix is contemplated to assist in the imaging of the deeper parts of the model and improve the convergence of the optimization algorithm. On the other hand, the linear inverse problem that recovers the true subsurface reflectivity model is solved by the least squares reverse time migration. The numerical examples performed here demonstrate that the inverse operator of the migration problem (implicitly estimated by an iterative solver), has deconvolutive properties, and thus, it can be used to obtain improved seismic sections with better resolution and reflectors with more balanced amplitudes.