Abstract:Abstract-In this paper we propose two multichannel blind deconvolution algorithms for the restoration of two-dimensional (2D) seismic data. Both algorithms are based on a 2D reflectivity prior model, and use iterative multichannel deconvolution procedures which deconvolve the seismic data, while taking into account the spatial dependency between neighboring traces. The first algorithm employs in each step a modified maximum posterior mode (MPM) algorithm which estimates a reflectivity column from the correspon… Show more
“…In a seismic survey, the convolution of the source wavelet with a subsurface reflectivity series is recorded as a seismic trace. In a multichannel scenario [8], [11]- [13], the seismic traces are typically modeled as convolutions of the same waveform with multiple reflectivity models. Early work on seismic blind deconvolution depended on two major assumptions: the impulse response of the earth is a white sequence and the source wavelet is minimum phase.…”
In this work, an efficient numerical scheme is presented for seismic blind deconvolution in a multichannel scenario. The proposed method iterate with two steps: first, wavelet estimation across all channels and second, refinement of the reflectivity estimate simultaneously in all channels using sparse deconvolution. The reflectivity update step is formulated as a basis pursuit denoising problem and a sparse solution is obtained with the spectral projected-gradient algorithm -faithfulness to the recorded traces is constrained by the measured noise level. Wavelet re-estimation has a closed form solution when performed in the frequency domain by finding the minimum energy wavelet common to all channels. Nothing is assumed known about the wavelet apart from its time duration. In tests with both synthetic and real data, the method yields sparse reflectivity series and stable wavelet estimates results compared to existing methods with significantly less computational effort.
“…In a seismic survey, the convolution of the source wavelet with a subsurface reflectivity series is recorded as a seismic trace. In a multichannel scenario [8], [11]- [13], the seismic traces are typically modeled as convolutions of the same waveform with multiple reflectivity models. Early work on seismic blind deconvolution depended on two major assumptions: the impulse response of the earth is a white sequence and the source wavelet is minimum phase.…”
In this work, an efficient numerical scheme is presented for seismic blind deconvolution in a multichannel scenario. The proposed method iterate with two steps: first, wavelet estimation across all channels and second, refinement of the reflectivity estimate simultaneously in all channels using sparse deconvolution. The reflectivity update step is formulated as a basis pursuit denoising problem and a sparse solution is obtained with the spectral projected-gradient algorithm -faithfulness to the recorded traces is constrained by the measured noise level. Wavelet re-estimation has a closed form solution when performed in the frequency domain by finding the minimum energy wavelet common to all channels. Nothing is assumed known about the wavelet apart from its time duration. In tests with both synthetic and real data, the method yields sparse reflectivity series and stable wavelet estimates results compared to existing methods with significantly less computational effort.
“…In order to quantify and compare the performances of the multichannel and single-channel algorithms, we used the four loss functions suggested in Kaaresen (1998), and three new ones defined in Ram et al (2010). The means and standard deviations of the loss functions calculated for the estimates obtained by single-channel and multichannel deconvolution are shown in percents in Table 1.…”
Section: Synthetic Datamentioning
confidence: 99%
“…In this paper, which summarizes some of the results in Ram et al (2010), we introduce a multichannel blind deconvolution algorithm. The algorithm is based on the MBG I reflectivity model and iteratively deconvolves the seismic data, while taking into account the spatial dependency between neighboring traces.…”
In this paper we introduce a multichannel blind deconvolution algorithm for the restoration of two-dimensional (2D) seismic data. This algorithm is based on a 2D reflectivity prior model, which takes into account the spatial dependency between neighboring traces. Each reflectivity column is estimated from the corresponding observed trace using the estimate of the preceding reflectivity column and a modified maximum posterior mode (MPM) algorithm. The MPM algorithm employs a Gibbs sampler to simulate realizations of seismic reflectivities. We apply the algorithm to synthetic and real data, and demonstrate improved results compared to those obtained by a single-channel deconvolution method.
“…Multichannel seismic deconvolution methods promote horizontal continuity of the seismic reflectivity by considering more than one trace in each channel estimation (Idier and Goussard, 1993;Mendel et al, 1981;Kormylo and Mendel, 1982;Kaaresen and Taxt, 1998;Heimer et al, 2007;Cohen, 2009, 2008;Ram et al, 2010;Gholami and Sacchi, 2013;Mirel and Cohen, 2017;.…”
We introduce a multichannel method to recover 3D reflectivity from 3D seismic data. The algorithm is formulated so that it promotes sparsity of the solution and also fits the earth Qmodel of attenuation and dispersion propagation effects of reflected waves. In addition, the algorithm also takes into consideration spatial correlation between neighboring traces. These features, together with low computational cost, make the proposed method a good solution for the emerging need to process large volumes of 3D seismic data. The robustness of the proposed technique compared to single-channel recovery is demonstrated by synthetic and real data examples.
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