The discrete Kalman filtering approach for seismic signals deconvolution
- Departement of Physics Intitut Teknologi Bandung, Jl. Ganesha 10 Bandung (Indonesia)
Seismic signals are a convolution of reflectivity and seismic wavelet. One of the most important stages in seismic data processing is deconvolution process; the process of deconvolution is inverse filters based on Wiener filter theory. This theory is limited by certain modelling assumptions, which may not always valid. The discrete form of the Kalman filter is then used to generate an estimate of the reflectivity function. The main advantage of Kalman filtering is capability of technique to handling continually time varying models and has high resolution capabilities. In this work, we use discrete Kalman filter that it was combined with primitive deconvolution. Filtering process works on reflectivity function, hence the work flow of filtering is started with primitive deconvolution using inverse of wavelet. The seismic signals then are obtained by convoluting of filtered reflectivity function with energy waveform which is referred to as the seismic wavelet. The higher frequency of wavelet gives smaller wave length, the graphs of these results are presented.
- OSTI ID:
- 22068979
- Journal Information:
- AIP Conference Proceedings, Vol. 1454, Issue 1; Conference: ICPAP 2011: International conference on physics and its applications, Bandung (Indonesia), 10-11 Nov 2011; Other Information: (c) 2012 American Institute of Physics; Country of input: International Atomic Energy Agency (IAEA); ISSN 0094-243X
- Country of Publication:
- United States
- Language:
- English
Similar Records
Digital seismic inverse methods
Deconvolution of noisy transient signals: a Kalman filtering application