Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic

The moment of P-wave arrival can provide us with many information about the nature of a seismic event. Without adequate knowledge regarding the onset moment, many properties of the events related to location, polarization of P-wave, and so forth are impossible to receive. In order to save time requi...

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Main Authors: Jakub Sokolowski, Jakub Obuchowski, Radoslaw Zimroz, Agnieszka Wylomanska, Eugeniusz Koziarz
Format: Article
Language:English
Published: Wiley 2016-01-01
Series:Shock and Vibration
Online Access:http://dx.doi.org/10.1155/2016/4051701
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author Jakub Sokolowski
Jakub Obuchowski
Radoslaw Zimroz
Agnieszka Wylomanska
Eugeniusz Koziarz
author_facet Jakub Sokolowski
Jakub Obuchowski
Radoslaw Zimroz
Agnieszka Wylomanska
Eugeniusz Koziarz
author_sort Jakub Sokolowski
collection DOAJ
description The moment of P-wave arrival can provide us with many information about the nature of a seismic event. Without adequate knowledge regarding the onset moment, many properties of the events related to location, polarization of P-wave, and so forth are impossible to receive. In order to save time required to indicate P-wave arrival moment manually, one can benefit from automatic picking algorithms. In this paper two algorithms based on a method finding a regime switch point are applied to seismic event data in order to find P-wave arrival time. The algorithms are based on signals transformed via a basic transform rather than on raw recordings. They involve partitioning the transformed signal into two separate series and fitting logarithm function to the first subset (which corresponds to pure noise and therefore it is considered stationary), exponent or power function to the second subset (which corresponds to nonstationary seismic event), and finding the point at which these functions best fit the statistic in terms of sum of squared errors. Effectiveness of the algorithms is tested on seismic data acquired from O/ZG “Rudna” underground copper ore mine with moments of P-wave arrival initially picked by broadly known STA/LTA algorithm and then corrected by seismic station specialists. The results of proposed algorithms are compared to those obtained using STA/LTA.
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institution Kabale University
issn 1070-9622
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language English
publishDate 2016-01-01
publisher Wiley
record_format Article
series Shock and Vibration
spelling doaj-art-1b2655264f6c442eb2b81508e7b1dcb32025-02-03T01:02:12ZengWileyShock and Vibration1070-96221875-92032016-01-01201610.1155/2016/40517014051701Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment CharacteristicJakub Sokolowski0Jakub Obuchowski1Radoslaw Zimroz2Agnieszka Wylomanska3Eugeniusz Koziarz4KGHM CUPRUM Ltd., CBR, Sikorskiego 2-8, 53-659 Wrocław, PolandKGHM CUPRUM Ltd., CBR, Sikorskiego 2-8, 53-659 Wrocław, PolandKGHM CUPRUM Ltd., CBR, Sikorskiego 2-8, 53-659 Wrocław, PolandFaculty of Pure and Applied Mathematics, Hugo Steinhaus Center, Wroclaw University of Science and Technology, Janiszewskiego 14a, 50-370 Wrocław, PolandKGHM Polska Miedź S.A. O/ZG “Rudna”, Henryka Dąbrowskiego 50, 59-100 Polkowice, PolandThe moment of P-wave arrival can provide us with many information about the nature of a seismic event. Without adequate knowledge regarding the onset moment, many properties of the events related to location, polarization of P-wave, and so forth are impossible to receive. In order to save time required to indicate P-wave arrival moment manually, one can benefit from automatic picking algorithms. In this paper two algorithms based on a method finding a regime switch point are applied to seismic event data in order to find P-wave arrival time. The algorithms are based on signals transformed via a basic transform rather than on raw recordings. They involve partitioning the transformed signal into two separate series and fitting logarithm function to the first subset (which corresponds to pure noise and therefore it is considered stationary), exponent or power function to the second subset (which corresponds to nonstationary seismic event), and finding the point at which these functions best fit the statistic in terms of sum of squared errors. Effectiveness of the algorithms is tested on seismic data acquired from O/ZG “Rudna” underground copper ore mine with moments of P-wave arrival initially picked by broadly known STA/LTA algorithm and then corrected by seismic station specialists. The results of proposed algorithms are compared to those obtained using STA/LTA.http://dx.doi.org/10.1155/2016/4051701
spellingShingle Jakub Sokolowski
Jakub Obuchowski
Radoslaw Zimroz
Agnieszka Wylomanska
Eugeniusz Koziarz
Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
Shock and Vibration
title Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
title_full Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
title_fullStr Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
title_full_unstemmed Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
title_short Algorithm Indicating Moment of P-Wave Arrival Based on Second-Moment Characteristic
title_sort algorithm indicating moment of p wave arrival based on second moment characteristic
url http://dx.doi.org/10.1155/2016/4051701
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AT radoslawzimroz algorithmindicatingmomentofpwavearrivalbasedonsecondmomentcharacteristic
AT agnieszkawylomanska algorithmindicatingmomentofpwavearrivalbasedonsecondmomentcharacteristic
AT eugeniuszkoziarz algorithmindicatingmomentofpwavearrivalbasedonsecondmomentcharacteristic