Deconvolução Com O Modelo De Goupillaud

The aim of this paper is the study of the supression of the source time effect from seismic traces. The<br>simulations of the experiment uses the Goupillaud model for seismic wave propagation and, in this case, a<br>further apilcation would be the supression of the reverberation component to improve the higher frequency<br>response of the filter. This problem is mathematically described as a stochastic process, non stationary, time<br>invariant, time domain processed and frequency domain analysed. This subject is called compression of the<br>seismic pulse, and it is accomplished here successefully by the method of Kalman.