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Seismoelectric wave is a wave acquired for underground phenomenons by using the conversion of mechanical energy to electromagnetic energy according to electrokinetic effects mechanism. This wave is just recently discovered and has the ability to create and to complement earth exploration methods. Se...

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Main Author: HANDI PRADANA (NIM 10205055), SABILLY
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/11365
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:11365
spelling id-itb.:113652017-09-27T11:45:14Z#TITLE_ALTERNATIVE# HANDI PRADANA (NIM 10205055), SABILLY Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/11365 Seismoelectric wave is a wave acquired for underground phenomenons by using the conversion of mechanical energy to electromagnetic energy according to electrokinetic effects mechanism. This wave is just recently discovered and has the ability to create and to complement earth exploration methods. Seismoelectric methods measure electric fields in fluid saturated rocks caused by seismic vibration. The sesimoelectric signal's amplitude is miniscule if compared to other signals and the noise that follows. By using sinusoidal methods, seismoelectric signals recorded are then processed to suppress the noise that is unwantedly recorded by subtracting the seismoelectric signal from the field data result from the synthetic noise signal after the frequency and the initial phase of the noise were acquired using Fourier Transformation.<p>This final assignment uses MATLAB Signal Processing Toolbox as the signal processing software. After the seismoelectric signal is free from noise contamination, a correlation between the initial data's amplitude and petrophysics factors like porosity, permeability and density, which are informations of underground conditions, can be acquired. 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 Seismoelectric wave is a wave acquired for underground phenomenons by using the conversion of mechanical energy to electromagnetic energy according to electrokinetic effects mechanism. This wave is just recently discovered and has the ability to create and to complement earth exploration methods. Seismoelectric methods measure electric fields in fluid saturated rocks caused by seismic vibration. The sesimoelectric signal's amplitude is miniscule if compared to other signals and the noise that follows. By using sinusoidal methods, seismoelectric signals recorded are then processed to suppress the noise that is unwantedly recorded by subtracting the seismoelectric signal from the field data result from the synthetic noise signal after the frequency and the initial phase of the noise were acquired using Fourier Transformation.<p>This final assignment uses MATLAB Signal Processing Toolbox as the signal processing software. After the seismoelectric signal is free from noise contamination, a correlation between the initial data's amplitude and petrophysics factors like porosity, permeability and density, which are informations of underground conditions, can be acquired.
format Final Project
author HANDI PRADANA (NIM 10205055), SABILLY
spellingShingle HANDI PRADANA (NIM 10205055), SABILLY
#TITLE_ALTERNATIVE#
author_facet HANDI PRADANA (NIM 10205055), SABILLY
author_sort HANDI PRADANA (NIM 10205055), SABILLY
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/11365
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