Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure

We have proposed a new least-squares method for signal estimation with a complicated and therefore more realistic mathematical model of the multichannel seismic record containing random noise and an arbitrary number of coherent noise wavetrains. It is supposed that the signal and all the coherent no...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Datum:2010
Hauptverfasser: Tyapkin, Yu. K., Silinskaya, E. A.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/117573
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Назва журналу:Geofizicheskiy Zhurnal

Institution

Geofizicheskiy Zhurnal
_version_ 1856543357744971776
author Tyapkin, Yu. K.
Silinskaya, E. A.
author_facet Tyapkin, Yu. K.
Silinskaya, E. A.
author_sort Tyapkin, Yu. K.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T10:57:50Z
description We have proposed a new least-squares method for signal estimation with a complicated and therefore more realistic mathematical model of the multichannel seismic record containing random noise and an arbitrary number of coherent noise wavetrains. It is supposed that the signal and all the coherent noise wavetrains bear individual trace-independent waveforms being mutually uncorrelated in time stationary stochastic processes. The amplitudes and arrival times of these record components vary from trace to trace in an arbitrary manner. Random noise is assumed to be a stationary stochastic process uncorrelated with the signal and all the coherent noise wavetrains and from trace to trace as well. Its spectral (autocorrelation) function is trace independent to within a scale factor, the variance. Under certain conditions, the method may be reduced to two successive stages, namely preliminary subtraction of estimates of all the coherent noise wavetrains and final estimation of the signal from the residual record. On both stages, optimum weighted stacking is used with reference to the variances of random noise and to the amplitudes and arrival times of the corresponding coherent component. A simplified scheme and an advanced scheme for subtracting coherent noise are proposed, which are called the zeroorder and first-order approximations, respectively. The first of them is the generalization of a conventional approach for subtracting coherent noise to the complicated data model adopted in this paper. The second scheme has an obvious advantage over the first scheme, since it allows the distortions that appear when estimating and subsequently subtracting the coherent noise wavetrains to be compensated. A simulation on synthetic data shows the efficiency of the firstorder approximation, and it provides a qualitative and quantitative comparison of those results with the results given by the zero-order approximation.
first_indexed 2025-07-17T11:09:21Z
format Article
id journalsuranua-geofizicheskiy-article-117573
institution Geofizicheskiy Zhurnal
language Russian
last_indexed 2025-07-17T11:09:21Z
publishDate 2010
publisher S. Subbotin Institute of Geophysics of the NAS of Ukraine
record_format ojs
spelling journalsuranua-geofizicheskiy-article-1175732020-10-07T10:57:50Z Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure Tyapkin, Yu. K. Silinskaya, E. A. We have proposed a new least-squares method for signal estimation with a complicated and therefore more realistic mathematical model of the multichannel seismic record containing random noise and an arbitrary number of coherent noise wavetrains. It is supposed that the signal and all the coherent noise wavetrains bear individual trace-independent waveforms being mutually uncorrelated in time stationary stochastic processes. The amplitudes and arrival times of these record components vary from trace to trace in an arbitrary manner. Random noise is assumed to be a stationary stochastic process uncorrelated with the signal and all the coherent noise wavetrains and from trace to trace as well. Its spectral (autocorrelation) function is trace independent to within a scale factor, the variance. Under certain conditions, the method may be reduced to two successive stages, namely preliminary subtraction of estimates of all the coherent noise wavetrains and final estimation of the signal from the residual record. On both stages, optimum weighted stacking is used with reference to the variances of random noise and to the amplitudes and arrival times of the corresponding coherent component. A simplified scheme and an advanced scheme for subtracting coherent noise are proposed, which are called the zeroorder and first-order approximations, respectively. The first of them is the generalization of a conventional approach for subtracting coherent noise to the complicated data model adopted in this paper. The second scheme has an obvious advantage over the first scheme, since it allows the distortions that appear when estimating and subsequently subtracting the coherent noise wavetrains to be compensated. A simulation on synthetic data shows the efficiency of the firstorder approximation, and it provides a qualitative and quantitative comparison of those results with the results given by the zero-order approximation. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010-02-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/117573 10.24028/gzh.0203-3100.v32i1.2010.117573 Geofizicheskiy Zhurnal; Vol. 32 No. 1 (2010); 107-121 Геофизический журнал; Том 32 № 1 (2010); 107-121 Геофізичний журнал; Том 32 № 1 (2010); 107-121 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/117573/111615 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Tyapkin, Yu. K.
Silinskaya, E. A.
Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title_full Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title_fullStr Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title_full_unstemmed Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title_short Approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
title_sort approximations of zero and first orders with an optimized seismic signal estimation complicated by regular and irregular interference of complex structure
url https://journals.uran.ua/geofizicheskiy/article/view/117573
work_keys_str_mv AT tyapkinyuk approximationsofzeroandfirstorderswithanoptimizedseismicsignalestimationcomplicatedbyregularandirregularinterferenceofcomplexstructure
AT silinskayaea approximationsofzeroandfirstorderswithanoptimizedseismicsignalestimationcomplicatedbyregularandirregularinterferenceofcomplexstructure