Research output: Contribution to journal › Article › peer-review
High-resolution seismic data deconvolution by A0 algorithm. / Krasnov, Fedor; Butorin, Alexander.
In: Geosciences (Switzerland), Vol. 8, No. 12, 497, 12.2018.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - High-resolution seismic data deconvolution by A0 algorithm
AU - Krasnov, Fedor
AU - Butorin, Alexander
N1 - Publisher Copyright: © 2018 by the authors. Licensee MDPI, Basel, Switzerland.
PY - 2018/12
Y1 - 2018/12
N2 - Sparse spikes deconvolution is one of the oldest inverse problems, which is a stylized version of recovery in seismic imaging. The goal of sparse spike deconvolution is to recover an approximation of a given noisy measurement T = W ∗ r + W0. Since the convolution destroys many low and high frequencies, this requires some prior information to regularize the inverse problem. In this paper, the authors continue to study the problem of searching for positions and amplitudes of the reflection coefficients of the medium (SP&ARCM). In previous research, the authors proposed a practical algorithm for solving the inverse problem of obtaining geological information from the seismic trace, which was named A0. In the current paper, the authors improved the method of the A0 algorithm and applied it to the real (non-synthetic) data. Firstly, the authors considered the matrix approach and Differential Evolution approach to the SP&ARCM problem and showed that their efficiency is limited in the case. Secondly, the authors showed that the course to improve the A0 lays in the direction of optimization with sequential regularization. The authors presented calculations for the accuracy of the A0 for that case and experimental results of the convergence. The authors also considered different initialization parameters of the optimization process from the point of the acceleration of the convergence. Finally, the authors carried out successful approbation of the algorithm A0 on synthetic and real data. Further practical development of the algorithm A0 will be aimed at increasing the robustness of its operation, as well as in application in more complex models of real seismic data. The practical value of the research is to increase the resolving power of the wave field by reducing the contribution of interference, which gives new information for seismic-geological modeling.
AB - Sparse spikes deconvolution is one of the oldest inverse problems, which is a stylized version of recovery in seismic imaging. The goal of sparse spike deconvolution is to recover an approximation of a given noisy measurement T = W ∗ r + W0. Since the convolution destroys many low and high frequencies, this requires some prior information to regularize the inverse problem. In this paper, the authors continue to study the problem of searching for positions and amplitudes of the reflection coefficients of the medium (SP&ARCM). In previous research, the authors proposed a practical algorithm for solving the inverse problem of obtaining geological information from the seismic trace, which was named A0. In the current paper, the authors improved the method of the A0 algorithm and applied it to the real (non-synthetic) data. Firstly, the authors considered the matrix approach and Differential Evolution approach to the SP&ARCM problem and showed that their efficiency is limited in the case. Secondly, the authors showed that the course to improve the A0 lays in the direction of optimization with sequential regularization. The authors presented calculations for the accuracy of the A0 for that case and experimental results of the convergence. The authors also considered different initialization parameters of the optimization process from the point of the acceleration of the convergence. Finally, the authors carried out successful approbation of the algorithm A0 on synthetic and real data. Further practical development of the algorithm A0 will be aimed at increasing the robustness of its operation, as well as in application in more complex models of real seismic data. The practical value of the research is to increase the resolving power of the wave field by reducing the contribution of interference, which gives new information for seismic-geological modeling.
KW - Differential evolution
KW - Discrete loss function
KW - Geological medium factors
KW - Limiting accuracy
KW - The Ricker wavelet
UR - http://www.scopus.com/inward/record.url?scp=85067920967&partnerID=8YFLogxK
U2 - 10.3390/geosciences8120497
DO - 10.3390/geosciences8120497
M3 - Article
AN - SCOPUS:85067920967
VL - 8
JO - Geosciences (Switzerland)
JF - Geosciences (Switzerland)
SN - 2076-3263
IS - 12
M1 - 497
ER -
ID: 88695570