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Ground-roll extraction using the Karhunen-Loeve transform in the time-frequency domain. / Serdyukov, Aleksander S.

в: Geophysics, Том 87, № 2, 01.03.2022, стр. A19-A24.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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Serdyukov AS. Ground-roll extraction using the Karhunen-Loeve transform in the time-frequency domain. Geophysics. 2022 март 1;87(2):A19-A24. doi: 10.1190/geo2021-0453.1

Author

BibTeX

@article{31c4d74638564b9a8f048bb60fd6b9e4,
title = "Ground-roll extraction using the Karhunen-Loeve transform in the time-frequency domain",
abstract = "Ground-roll suppression is critical for seismic reflection data processing. Many standard methods, i.e., f-k fan filtering, fail when spatially aliased surface wave interference is present in the data. Spatial aliasing is a common problem; receiver spacing is often not dense enough to extract wavenumbers of low-velocity surface waves. It has long been known that the Karhunen-Loeve (KL) transform can be used to suppress aliased ground roll. However, the ground roll should be flattened before suppression, which is challenging due to the dispersion of surface wave velocities. I propose to solve this problem via the time-frequency domain. I apply the S-transform, which was previously shown to perform well in the multichannel analysis of surface waves. A simple complex-valued constant phase shift is a suitable model of surface wave propagation in common-frequency S-transform gathers. Therefore, it is easy to flatten the corresponding S-transform narrow-band frequency surface wave packet and extract it from the data by principal component analysis of the corresponding complex-valued data-covariance matrix. As the result, our S-transform KL (SKL) method filters the aliased ground roll without damaging the reflection amplitudes. The advantages of SKL filtering have been confirmed by synthetic- and field-data processing.",
keywords = "common shot, KL transform, reduced-rank filtering, signal processing, surface wave",
author = "Serdyukov, {Aleksander S.}",
note = "Funding Information: The research was supported by the Russian Science Foundation (project no. 20-77-10023). I would like to thank the editor-in-chief, J. Etgen, the associate and assistant editors of this paper, A. Kaslilar and J. Blanch, and three anonymous reviewers for their comments and corrections that improved the manuscript. Publisher Copyright: {\textcopyright} 2022 Society of Exploration Geophysicists.",
year = "2022",
month = mar,
day = "1",
doi = "10.1190/geo2021-0453.1",
language = "English",
volume = "87",
pages = "A19--A24",
journal = "Geophysics",
issn = "0016-8033",
publisher = "SOC EXPLORATION GEOPHYSICISTS",
number = "2",

}

RIS

TY - JOUR

T1 - Ground-roll extraction using the Karhunen-Loeve transform in the time-frequency domain

AU - Serdyukov, Aleksander S.

N1 - Funding Information: The research was supported by the Russian Science Foundation (project no. 20-77-10023). I would like to thank the editor-in-chief, J. Etgen, the associate and assistant editors of this paper, A. Kaslilar and J. Blanch, and three anonymous reviewers for their comments and corrections that improved the manuscript. Publisher Copyright: © 2022 Society of Exploration Geophysicists.

PY - 2022/3/1

Y1 - 2022/3/1

N2 - Ground-roll suppression is critical for seismic reflection data processing. Many standard methods, i.e., f-k fan filtering, fail when spatially aliased surface wave interference is present in the data. Spatial aliasing is a common problem; receiver spacing is often not dense enough to extract wavenumbers of low-velocity surface waves. It has long been known that the Karhunen-Loeve (KL) transform can be used to suppress aliased ground roll. However, the ground roll should be flattened before suppression, which is challenging due to the dispersion of surface wave velocities. I propose to solve this problem via the time-frequency domain. I apply the S-transform, which was previously shown to perform well in the multichannel analysis of surface waves. A simple complex-valued constant phase shift is a suitable model of surface wave propagation in common-frequency S-transform gathers. Therefore, it is easy to flatten the corresponding S-transform narrow-band frequency surface wave packet and extract it from the data by principal component analysis of the corresponding complex-valued data-covariance matrix. As the result, our S-transform KL (SKL) method filters the aliased ground roll without damaging the reflection amplitudes. The advantages of SKL filtering have been confirmed by synthetic- and field-data processing.

AB - Ground-roll suppression is critical for seismic reflection data processing. Many standard methods, i.e., f-k fan filtering, fail when spatially aliased surface wave interference is present in the data. Spatial aliasing is a common problem; receiver spacing is often not dense enough to extract wavenumbers of low-velocity surface waves. It has long been known that the Karhunen-Loeve (KL) transform can be used to suppress aliased ground roll. However, the ground roll should be flattened before suppression, which is challenging due to the dispersion of surface wave velocities. I propose to solve this problem via the time-frequency domain. I apply the S-transform, which was previously shown to perform well in the multichannel analysis of surface waves. A simple complex-valued constant phase shift is a suitable model of surface wave propagation in common-frequency S-transform gathers. Therefore, it is easy to flatten the corresponding S-transform narrow-band frequency surface wave packet and extract it from the data by principal component analysis of the corresponding complex-valued data-covariance matrix. As the result, our S-transform KL (SKL) method filters the aliased ground roll without damaging the reflection amplitudes. The advantages of SKL filtering have been confirmed by synthetic- and field-data processing.

KW - common shot

KW - KL transform

KW - reduced-rank filtering

KW - signal processing

KW - surface wave

UR - http://www.scopus.com/inward/record.url?scp=85123958214&partnerID=8YFLogxK

U2 - 10.1190/geo2021-0453.1

DO - 10.1190/geo2021-0453.1

M3 - Article

AN - SCOPUS:85123958214

VL - 87

SP - A19-A24

JO - Geophysics

JF - Geophysics

SN - 0016-8033

IS - 2

ER -

ID: 35428194