Navegando por Autor "PEREIRA, Rubenvaldo Monteiro"
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Item Acesso aberto (Open Access) Amplitudes e padrões de polarização de pulsos em meios anisotrópicos(2011-06) PEREIRA, Rubenvaldo Monteiro; PROTÁZIO, João dos Santos; COSTA, Jessé CarvalhoExtracting subsurface lithological information from seismic data has become a great challenge to seismic exploration, as the hypotheses of stratification made by isotropic layers has been insufficient to represent the behavior of elastic field in surveys with great offset between source and receiver, multicomponent geophones, three-dimensional Vertical Seismic Profile (VSP) measures and so forth. Due to this reason, a more realistic model of subsurface is demanded. As a result, the seismic prospecting starts to consider the anisotropic models of subsurface to characterize reservoirs, for example. This paper aims at showing formalism to model the scattering of pulses from incident plane waves in horizontal plain interfaces which separate anisotropic media. This scattering is obtained primarily through the explicit formulation of traction and deformation fields as a function of propagator, polarization and impedance matrices of media. After that, this formalism is used to obtain the reflection and transmission coefficients matrices through a horizontal plain interface to be, subsequently generalized to a scattering through multiple layers. Finally, the amplitude of an analytical pulse is inserted in the incident wave to calculate the scattering of the pulse through stratifications.Item Acesso aberto (Open Access) Estimativa de parâmetros em meios VTI usando aproximações de sobretempo não hiperbólicas(Universidade Federal do Pará, 2015-09-30) PEREIRA, Rubenvaldo Monteiro; CRUZ, João Carlos Ribeiro; http://lattes.cnpq.br/8498743497664023Transversely isotropic (TI) media is a more realistic model for processing seismic data, for example, fractured media with preferred fracture direction, or composite by periodic thin layers. In particular, TI media with vertical symmetry axis (VTI) are widely used as models for P-wave propagation in shales, abundant rock in hydrocarbon reservoirs. However, the P-wave propagation in homogeneous media VTI have as their main characteristics, depend on four parameters of rigidity and also to possess: complicated algebraically phase velocity equation, difficult group velocity equation to explain and moveout equation nonhyperbolic. Therefore, several authors have presented parameterization and obtained approximations to these equations depending on three parameters only. Among these, the moveout approximations have been widely used in inverse methods to estimate lithological parameters in homogeneous media VTI. Such methods have generally been successful in estimated stacking velocity vn and the anellipticity parameter η, since these are the only ones required for generating initial models for the steps of seismic processing in the time domain. One of the most used methods for estimating parameters is the basedsemblance velocity analysis, though, because this method is limited to sections with small offset-depth ratio, adaptations for anisotropic media, considering nonhyperbolic moveout approximatios are required. In this paper, based on anelliptical approximation shifted hyperbola, anelliptical rational approximations are presented for: phase velocity, group velocity and moveout nonhyperbolic in homogeneous VTI horizontally layered media. The validity of these approximations is made by calculating their relative errors by comparing with other known approximations in the literature. To semblance-based velocity analysis is performed to measure the accuracy of the rational moveout approximations to estimate parameters in VTI media. The results demonstrate the great potential of rational approximations in inverse problems. In order to adapt to VTI media, we modify two coherence measurements by semblance which are sensitive to amplitude and phase variations. The accuracy and robustness of the adapted coherence measurements are validated by estimation of in anisotropic parameters in VTI media.