#TITLE_ALTERNATIVE#

This study discusses about ultrasonic tomography method in isotropic and anisotropic crystals media. Media in the form of rock slice (synthetics case). The rock has a base mass is clay, in which minerals are plagioclase, orthoclase, and olivine, and the presence of voids. Anisotropy represented by m...

Full description

Saved in:
Bibliographic Details
Main Author: MUTIA SARI (NIM: 22310304), VANI
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/20594
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:20594
spelling id-itb.:205942017-10-09T10:24:09Z#TITLE_ALTERNATIVE# MUTIA SARI (NIM: 22310304), VANI Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20594 This study discusses about ultrasonic tomography method in isotropic and anisotropic crystals media. Media in the form of rock slice (synthetics case). The rock has a base mass is clay, in which minerals are plagioclase, orthoclase, and olivine, and the presence of voids. Anisotropy represented by maximum velocity, minimum velocity, and minerals orientation. Rocks with different mineral reconstructed using tomography reconstruction algorithms, Back Projection Technique (BPT), Simultaneous Iterative Reconstruction Technique (SIRT), and Modified Iterative Reconstruction Technique Simultaneous (MSIRT) to obtain images of internal velocity distribution (tomogram). The research was done to accelerate the determination of the composition of rocks, without damaging the rock. <br /> <br /> <br /> <br /> <br /> Initially, software calibration performed using the directly initial slowness from the velocity model to SIRT and MSIRT algorithm. Then, the initial slowness varied using the average velocity, BPT velocity, and seismic velocity anisotropy. As for the BPT algorithm, slowness variation is not done earlier because the algorithm uses the average slowness of each raypath. <br /> <br /> <br /> <br /> <br /> Reconstruction results of this study provide information that tomography reconstruction algorithm able to detect the presence of other minerals in the rock. The best result was shown by MSIRT algorithm with the initial slowness from seismic velocity anisotropy, which can reconstruct the position and shape of the mineral right. It can be seen visually and from the resulting reconstruction error. 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 This study discusses about ultrasonic tomography method in isotropic and anisotropic crystals media. Media in the form of rock slice (synthetics case). The rock has a base mass is clay, in which minerals are plagioclase, orthoclase, and olivine, and the presence of voids. Anisotropy represented by maximum velocity, minimum velocity, and minerals orientation. Rocks with different mineral reconstructed using tomography reconstruction algorithms, Back Projection Technique (BPT), Simultaneous Iterative Reconstruction Technique (SIRT), and Modified Iterative Reconstruction Technique Simultaneous (MSIRT) to obtain images of internal velocity distribution (tomogram). The research was done to accelerate the determination of the composition of rocks, without damaging the rock. <br /> <br /> <br /> <br /> <br /> Initially, software calibration performed using the directly initial slowness from the velocity model to SIRT and MSIRT algorithm. Then, the initial slowness varied using the average velocity, BPT velocity, and seismic velocity anisotropy. As for the BPT algorithm, slowness variation is not done earlier because the algorithm uses the average slowness of each raypath. <br /> <br /> <br /> <br /> <br /> Reconstruction results of this study provide information that tomography reconstruction algorithm able to detect the presence of other minerals in the rock. The best result was shown by MSIRT algorithm with the initial slowness from seismic velocity anisotropy, which can reconstruct the position and shape of the mineral right. It can be seen visually and from the resulting reconstruction error.
format Theses
author MUTIA SARI (NIM: 22310304), VANI
spellingShingle MUTIA SARI (NIM: 22310304), VANI
#TITLE_ALTERNATIVE#
author_facet MUTIA SARI (NIM: 22310304), VANI
author_sort MUTIA SARI (NIM: 22310304), VANI
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/20594
_version_ 1821120205657473024