MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION

<p align="justify">CSAMT is an electromagnetic method with an artificial source capable of generating data with a more stable signal than the magnetoteluric method. CSAMT data acquisition that is relatively fast and characteristics of the data that have good lateral resolution are no...

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Main Author: IHSAN REZQA NIM: 12314070, MUHAMMAD
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/29236
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:29236
spelling id-itb.:292362018-09-27T11:17:13ZMODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION IHSAN REZQA NIM: 12314070, MUHAMMAD Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/29236 <p align="justify">CSAMT is an electromagnetic method with an artificial source capable of generating data with a more stable signal than the magnetoteluric method. CSAMT data acquisition that is relatively fast and characteristics of the data that have good lateral resolution are not supported by an easy and simple modeling process.Therefore, a simple inversion method is needed so that it can model CSAMT data quickly and efficiently. Zohdy-Oldenburg direct inversion is a method that can overcome these problems for magnetotelluric data. Therefore this inversion method will be applied to model the 1-D CSAMT data. In this research, we will use synthetic data formed from variations of resistivity model and also CSAMT data from North Sulawesi geothermal field. Then we use two types of thickness model that is effective depth model and constantly increased thickness model. In the constantly increased thickness model, the first thickness and the corresponding increment are determined using grid search. The thickness model data are then combined with pseudo resistivity data to form the subsurface model. The resistivity value is then updated until the Error value reaches a minimum. Based on the inversion process,Zohdy-Oldenburg inversion method is able to produce calculation data that is fit with observation data. Subsurface models based on effective depth is able to produce better results than the constantly thickening model due to the effective depth better describes the subsurface conditions of CSAMT data. However, there is a discrepancy between the inversion result model and the actual model due to the presence of near-field data that does not represent the actual subsurface conditions.<p align="justify"> 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 <p align="justify">CSAMT is an electromagnetic method with an artificial source capable of generating data with a more stable signal than the magnetoteluric method. CSAMT data acquisition that is relatively fast and characteristics of the data that have good lateral resolution are not supported by an easy and simple modeling process.Therefore, a simple inversion method is needed so that it can model CSAMT data quickly and efficiently. Zohdy-Oldenburg direct inversion is a method that can overcome these problems for magnetotelluric data. Therefore this inversion method will be applied to model the 1-D CSAMT data. In this research, we will use synthetic data formed from variations of resistivity model and also CSAMT data from North Sulawesi geothermal field. Then we use two types of thickness model that is effective depth model and constantly increased thickness model. In the constantly increased thickness model, the first thickness and the corresponding increment are determined using grid search. The thickness model data are then combined with pseudo resistivity data to form the subsurface model. The resistivity value is then updated until the Error value reaches a minimum. Based on the inversion process,Zohdy-Oldenburg inversion method is able to produce calculation data that is fit with observation data. Subsurface models based on effective depth is able to produce better results than the constantly thickening model due to the effective depth better describes the subsurface conditions of CSAMT data. However, there is a discrepancy between the inversion result model and the actual model due to the presence of near-field data that does not represent the actual subsurface conditions.<p align="justify">
format Final Project
author IHSAN REZQA NIM: 12314070, MUHAMMAD
spellingShingle IHSAN REZQA NIM: 12314070, MUHAMMAD
MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
author_facet IHSAN REZQA NIM: 12314070, MUHAMMAD
author_sort IHSAN REZQA NIM: 12314070, MUHAMMAD
title MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
title_short MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
title_full MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
title_fullStr MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
title_full_unstemmed MODELING OF 1-DIMENSION CONTROLLED SOURCE AUDIO-FREQUENCY MAGNETOTELLURICS (CSAMT) DATA USING ZOHDY-OLDENBURG DIRECT INVERSION
title_sort modeling of 1-dimension controlled source audio-frequency magnetotellurics (csamt) data using zohdy-oldenburg direct inversion
url https://digilib.itb.ac.id/gdl/view/29236
_version_ 1822922854882082816