AMAT1 – MIEEC. Formulário – Transformadas de Laplace f(t). £{f}. Domínio. -. – o s > 0 os. N a los o s > 0 o o avere s > 0 o n! 4 ľ”, n E NO s > 0 o sn+1. T(a + 1). 5. View Notes – formulario-laplace from ENGINEERIN at Universidad del Valle de México. FORMULARIO DE TRANSFORMADAS DE LAPLACE. View Test Prep – FORMULARIO 3 from DIFFERENTI 1 at Autonomous University of the State of Mexico. UNIDAD III. TRANSFORMADA DE LAPLACE Solucin de.

Author: Tygomuro Feshicage
Country: Kenya
Language: English (Spanish)
Genre: Literature
Published (Last): 8 September 2005
Pages: 25
PDF File Size: 18.69 Mb
ePub File Size: 18.1 Mb
ISBN: 863-3-74708-989-4
Downloads: 70080
Price: Free* [*Free Regsitration Required]
Uploader: Mazushicage

Koptyuga, 4, Akademgorodok, Novosibirsk, Russia.

There are considered various aspects of the numerical simulation of seismic waves connected with thin layer reservoirs. As a result we obtain both the horizontal and vertical displacement components, which are important for the analysis of seismic fields in the 3D seismic survey. In order to provide results nearer of the real experiment, in the mathematical formulation of the problem we use the deepened source of the type of the center of expansion. The solution of the problem, constructed in the spectral domain using the temporal Laplace and spatial Fourier-Bessel transforms, is studied in details to prove its applicability to the solution of direct and inverse dynamic seismic problems.

Special attention is done to analysis of the influence of the real part of the Laplace parameter on multi component seismograms corresponded to the horizontal and vertical components of the elastic field. Also, we discuss the computational aspects of the proposed scheme and carry out several analyses of the registered wave fields.


The results obtained demonstrated the potential of the method to help in the process of characterization of thin reservoirs in comparison with other methods: Isto pode estar relacionado a dois fatos. Consideremos um meio composto por n camadas estratificadas: Em virtude disto, as Eqs. Repetindo este procedimento camada por camada, calculamos os valores s ij 0.

Taula Transformadas de Laplace

Agora, utilizando as Eqs. O potencial da onda longitudinal plana incidente pode ser representado da seguinte forma. A seguir, descrevemos as principais modelagens realizadas. As singularidades do espetro observado apresentam mais explicitamente a descontinuidade da estrutura. Na Figura 3 ba escala ampliada do eixo mostra os valores do espectro.


A Figura 4 comprova a similaridade entre a estrutura dosespectros 2D obtidos em diferentes modelos. O desmembramento das transformadas permitiu criar um algoritmo mais efetivo. Este sismograma multicomponente, embora elementar, mostra a possibilidade de identificar os diferentes tipos de componentes das ondas. Na componente horizontal nitidamente revelam-se todos os tipos de ondas.

Isto pode ser justificado pelo uso de um tipo diferente de fonte. Tal procedimento possui vantagens relevantes: University Science Books, Sausalito, California. A method for calculation of stationary elastic oscillations in stratified media.


Numerical Methods in Geophysics. Moscow State University Publ. Flrmulario Waves and Sources. Fundamentals of Seismic Wave Propagation. General method for calculus of electromagnetic field in stratified medium.

Numerical Methods and Programming. Semi-analytical method for the solution of direct dynamical problems in stratified media.

Miscellaneous HP 49/50 Math Applications

A Method for calculation of non-stationary wave fields in non-elastic stratified-inhomogeneous media. The dispersion of surface waves on multilayered media. Bulletin of the Seismological Society of America, Numerical Modeling of Seismic Wave Propagation. New York, Dover Publications. Analytical Techniques in the Theory of Guided Waves.

Basis of mathematical theory of elastic waves propagation. Waves in Stratified Homogeneous Isotropic Media. Fogmulario of elastic waves through a stratified solid. Journal of Applied Physics, Review of elastic and electromagnetic waves propagation in horizontally layered media.

All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License. Services on Demand Journal. Agora, consideremos o sistema auxiliar: Nesse caso caracteriza uma fonte externa. How to cite this article.