THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH

The transition mining system from the surface mining into the underground mining method requires,the understanding of longwall coal mine impact such as the presence of upsidence. It occurs at the bottom of valley which is located above the longwall coal mine. Upsidence study in this research is...

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Main Author: D Kusumo, Adriyanto
Format: Dissertations
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/55580
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:55580
spelling id-itb.:555802021-06-18T09:08:35ZTHE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH D Kusumo, Adriyanto Indonesia Dissertations analytical, physical, and synthetical seismic models approach INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/55580 The transition mining system from the surface mining into the underground mining method requires,the understanding of longwall coal mine impact such as the presence of upsidence. It occurs at the bottom of valley which is located above the longwall coal mine. Upsidence study in this research is conducted by understanding the rock properties in South Kalimantan some experiments using analytical model, physical model, and synthetic seismic model. The two main parameters of rock characteristic which are collected in this research are rock strength and rock elasticity. The rock comparison with other locations shows that the modulus elasticity of rock in South Kalimantan shows a high value compared to rocks from Australia. The analytical models are conducted using the plate buckling theory. The experiment result from the analytical model shows the correlation with valley width, critical layer thickness, horizontal stress, and Young’s modulus. The physical models are conducted using base friction method. The experiment result of physical model shows there is a correlation with Hoek and Brown’s equation. The result also shows that the occurrence of upsidence are influenced by: the slope angle is greater than 800, the thickness layer in the valley is less than 3 cm, and the maximum slope height is 10 cm. The synthetic seismic models are conducted using both of crosshole-downhole seimic reflection and seismic tomography. The thin layer, which is one factor to generate upsidence, can be clearly detected using the crosshole-downhole seismic reflection method. 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 transition mining system from the surface mining into the underground mining method requires,the understanding of longwall coal mine impact such as the presence of upsidence. It occurs at the bottom of valley which is located above the longwall coal mine. Upsidence study in this research is conducted by understanding the rock properties in South Kalimantan some experiments using analytical model, physical model, and synthetic seismic model. The two main parameters of rock characteristic which are collected in this research are rock strength and rock elasticity. The rock comparison with other locations shows that the modulus elasticity of rock in South Kalimantan shows a high value compared to rocks from Australia. The analytical models are conducted using the plate buckling theory. The experiment result from the analytical model shows the correlation with valley width, critical layer thickness, horizontal stress, and Young’s modulus. The physical models are conducted using base friction method. The experiment result of physical model shows there is a correlation with Hoek and Brown’s equation. The result also shows that the occurrence of upsidence are influenced by: the slope angle is greater than 800, the thickness layer in the valley is less than 3 cm, and the maximum slope height is 10 cm. The synthetic seismic models are conducted using both of crosshole-downhole seimic reflection and seismic tomography. The thin layer, which is one factor to generate upsidence, can be clearly detected using the crosshole-downhole seismic reflection method.
format Dissertations
author D Kusumo, Adriyanto
spellingShingle D Kusumo, Adriyanto
THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
author_facet D Kusumo, Adriyanto
author_sort D Kusumo, Adriyanto
title THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
title_short THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
title_full THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
title_fullStr THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
title_full_unstemmed THE UPSIDENCE MODELING AT THE BOTTOM OF VALLEY WITH LONGWALL COAL MINE ACTIVTIES UNDERNEATH USING ANALYTICAL, PHYSICAL, AND SYNTHETICAL SEISMIC MODELS APPROACH
title_sort upsidence modeling at the bottom of valley with longwall coal mine activties underneath using analytical, physical, and synthetical seismic models approach
url https://digilib.itb.ac.id/gdl/view/55580
_version_ 1822002113507491840