Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis

The observation of earth seismic activity requires high accuracy and expertise from the observer. The observation that depends on the observer's subjectivity is difficult to be applied on volcanic earthquake activity, since the signal onset is often hardly visible. Polarization analysis was use...

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Main Author: FAISAL DAHLAN (NIM : 12313030), EMIRZA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/21943
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:21943
spelling id-itb.:219432017-10-09T10:31:19ZBody Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis FAISAL DAHLAN (NIM : 12313030), EMIRZA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/21943 The observation of earth seismic activity requires high accuracy and expertise from the observer. The observation that depends on the observer's subjectivity is difficult to be applied on volcanic earthquake activity, since the signal onset is often hardly visible. Polarization analysis was used in this research as a supporting method in the observation of the volcanic earthquake data. The seismogram data of Sinabung Volcano in June - December 2011 was obtained from PVMBG. The polarization analysis was applied on the recorded data of the VT-A earthquake (deep events) with the calculation of Rectilinearity (RL) parameter and the dot product angle parameter of P and S wave polarization. The obtained time window was later used to identify the dominant frequency and the polarity connection between desired signal and unwanted noise. <br /> <br /> <br /> <br /> <br /> Polarization analysis was proven to ease the characterization of the duration between body waves, and the arrival time of Rayleigh wave in every VT-A signal. The recorded VT-A earthquake during data research period was categorized as high frequency (HF) earthquake with 6 – 14 Hz and approximately 0,5 – 3,3 seconds difference between P waves’ and S waves’ onset. The pure P waves’ frequency was dominated by 9 – 14 Hz with approximately 0,05 – 2,7 seconds duration. The pure S and Rayleigh wave were dominated by lower frequency, 5 – 10 Hz for the pure S waves with approximately 0,1 – 1 seconds duration of propagation and 5 – 8 Hz for the Rayleigh waves with approximately 1,2 – 4,7 seconds after the onset of P waves. The existence of noise is significant toward the polarization analysis method. The result of the SNR analysis shows that the ideal SNR for research with polarization analysis is above 12 dB. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description The observation of earth seismic activity requires high accuracy and expertise from the observer. The observation that depends on the observer's subjectivity is difficult to be applied on volcanic earthquake activity, since the signal onset is often hardly visible. Polarization analysis was used in this research as a supporting method in the observation of the volcanic earthquake data. The seismogram data of Sinabung Volcano in June - December 2011 was obtained from PVMBG. The polarization analysis was applied on the recorded data of the VT-A earthquake (deep events) with the calculation of Rectilinearity (RL) parameter and the dot product angle parameter of P and S wave polarization. The obtained time window was later used to identify the dominant frequency and the polarity connection between desired signal and unwanted noise. <br /> <br /> <br /> <br /> <br /> Polarization analysis was proven to ease the characterization of the duration between body waves, and the arrival time of Rayleigh wave in every VT-A signal. The recorded VT-A earthquake during data research period was categorized as high frequency (HF) earthquake with 6 – 14 Hz and approximately 0,5 – 3,3 seconds difference between P waves’ and S waves’ onset. The pure P waves’ frequency was dominated by 9 – 14 Hz with approximately 0,05 – 2,7 seconds duration. The pure S and Rayleigh wave were dominated by lower frequency, 5 – 10 Hz for the pure S waves with approximately 0,1 – 1 seconds duration of propagation and 5 – 8 Hz for the Rayleigh waves with approximately 1,2 – 4,7 seconds after the onset of P waves. The existence of noise is significant toward the polarization analysis method. The result of the SNR analysis shows that the ideal SNR for research with polarization analysis is above 12 dB.
format Final Project
author FAISAL DAHLAN (NIM : 12313030), EMIRZA
spellingShingle FAISAL DAHLAN (NIM : 12313030), EMIRZA
Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
author_facet FAISAL DAHLAN (NIM : 12313030), EMIRZA
author_sort FAISAL DAHLAN (NIM : 12313030), EMIRZA
title Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
title_short Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
title_full Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
title_fullStr Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
title_full_unstemmed Body Waves and Rayleigh Waves Characterization of Sinabung Volcano VT-A Earthquake in June - December 2011 Using Polarization Analysis
title_sort body waves and rayleigh waves characterization of sinabung volcano vt-a earthquake in june - december 2011 using polarization analysis
url https://digilib.itb.ac.id/gdl/view/21943
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