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Attenuates periodic/ringing events
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Cepstrum(reverse order of Spec) Deconvolution is a wavelet-removal technique that works by transforming seismic data into the cepstrum where source periodicities (multiples, bubble pulses, reverberations) appear as isolated peaks. By applying a lifter (reverse order of fil) filter in the quefrency domain, these periodic components are removed, producing a cleaner, more reflectivity-like trace.
What is Cepstrum Deconvolution?
Cepstrum deconvolution is a method for removing the source wavelet from seismic data by converting the signal into the cepstrum domain — a special domain where reverberations, multiples, and periodic wavelet signatures appear as distinct peaks and can be isolated and removed.
It is especially good at:
•Removing short-period multiples
•Removing source bubble effects in marine data
•Removing ghosts
•Flattening reverberations
•Extracting the minimum-phase wavelet
Why Use Cepstrum Deconvolution?
Traditional deconvolution (spiking/predictive) struggles when:
•Wavelet is mixed-phase
•Reverberations are embedded inside the wavelet
•Multiples have regular periodicity
•Data have strong source bubble oscillations
Cepstrum deconvolution excels because:
•Convolution becomes addition in the cepstrum
•Periodic wavelet features show up as distinct spikes
•These can be suppressed using windows or filters
How Cepstrum Deconvolution Works?
A seismic trace is: x(t) = w(t) * r(t)
Step 1 — Fourier Transform: X(f) = W(f) . R(f)
Step 2 — Take Log Spectrum: ln X(f) = ln W(f) + ln R(f)
This is the key: Convolution becomes addition.
| Step 3 — Inverse FFT of log spectrum → Cepstrum |
C(Ƭ) = F-1 {ln X(f)}
•Ƭ is called "quefrency"
•Peaks at particular t correspond to periodicities (multiples, bubble oscillations)
Step 4 — Apply a “lifter” (cepstral filter)
•Suppress long-period or short-period components
•Remove wavelet periodicity
•Keep reflectivity terms
Step 5 - Transform back
Ẍ(f) = exp {FFT(Cfiltered)}
Inverse FFT gives the cepstrum-deconvolved trace.

What Cepstrum Deconvolution Removes?
Short-path multiples - Bubble pulse or peg-leg multiples appear as repeating periodic events that are strong in cepstrum.
Ghost effects - Source/receiver ghost period appears as a cepstrum peak.
Source wavelet periodicity - Any oscillatory wavelet component (Vibroseis sweep edges, bubble oscillation).
Reverberations / ringing - Room acoustics / poor weathering layers.
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If value is too small - we may be attenuating the primaries, if the value is too big , we may not attenuating the multiples. Optimum values are recommended. For marine bubbles, anything between 20-40ms is a good starting point.
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Cepstrum deconvolution separates convolution into addition by taking log of the spectrum and inverse transforming it (the “cepstrum”). This allows us to detect and remove periodic wavelet components.
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YouTube video lesson, click here to open [VIDEO IN PROCESS...]
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Yilmaz. O., 1987, Seismic data processing: Society of Exploration Geophysicist
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