GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA

The government has made a roadmap to increase geothermal capacity to 9.3 GW by 2035. To reach this target, exploration and exploitation of geothermal areas in Indonesia must be increased. The Arjuno-Welirang geothermal area in East Java Province is one area that has not been exploited, even thoug...

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Main Author: Ires Bujana, Malta
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/61955
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:61955
spelling id-itb.:619552021-09-28T20:13:27ZGEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA Ires Bujana, Malta Indonesia Final Project gravity, Moving Average, Quadratic Polynomial, Arjuno-Welirang, heat source, upflow, outflow, geothermal INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/61955 The government has made a roadmap to increase geothermal capacity to 9.3 GW by 2035. To reach this target, exploration and exploitation of geothermal areas in Indonesia must be increased. The Arjuno-Welirang geothermal area in East Java Province is one area that has not been exploited, even though it has potential resources of up to 180 MW. Potential geothermal sources are estimated to be in the Welirang Volcano area, where there are geothermal manifestations in the form of solfatara-fumarola. The purpose of this study is to analyze and determine the conceptual model of the geothermal system in the Arjuno-Welirang geothermal area using the gravity method. Gravity data was obtained from the gravity data acquisition by The Arjuno-Welirang Integrated Geophysical Survey Team in 2010 which can be accessed at the library of the Center for Coal and Geothermal Mineral Resources (PSDMBP). Gravity data processing will produce a Complete Bouguer Anomaly Map with a value range of -5 mGal to 70 mGal. Then, the regional and residual anomalies are separated using the Moving Average and Quadratic Polynomial methods, where the window width is determined by performing a 1- dimensional spectral analysis. The low anomaly is seen in the southern area, which is an area of interest where possible geothermal locations are located. 2.5D modeling shows that low anomaly values can be indicated as magma with a density contrast of -0.3 gr/cc, which may act as a heat source. The outflow zone is likely to be in the hot spring manifestation area. 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 government has made a roadmap to increase geothermal capacity to 9.3 GW by 2035. To reach this target, exploration and exploitation of geothermal areas in Indonesia must be increased. The Arjuno-Welirang geothermal area in East Java Province is one area that has not been exploited, even though it has potential resources of up to 180 MW. Potential geothermal sources are estimated to be in the Welirang Volcano area, where there are geothermal manifestations in the form of solfatara-fumarola. The purpose of this study is to analyze and determine the conceptual model of the geothermal system in the Arjuno-Welirang geothermal area using the gravity method. Gravity data was obtained from the gravity data acquisition by The Arjuno-Welirang Integrated Geophysical Survey Team in 2010 which can be accessed at the library of the Center for Coal and Geothermal Mineral Resources (PSDMBP). Gravity data processing will produce a Complete Bouguer Anomaly Map with a value range of -5 mGal to 70 mGal. Then, the regional and residual anomalies are separated using the Moving Average and Quadratic Polynomial methods, where the window width is determined by performing a 1- dimensional spectral analysis. The low anomaly is seen in the southern area, which is an area of interest where possible geothermal locations are located. 2.5D modeling shows that low anomaly values can be indicated as magma with a density contrast of -0.3 gr/cc, which may act as a heat source. The outflow zone is likely to be in the hot spring manifestation area.
format Final Project
author Ires Bujana, Malta
spellingShingle Ires Bujana, Malta
GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
author_facet Ires Bujana, Malta
author_sort Ires Bujana, Malta
title GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
title_short GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
title_full GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
title_fullStr GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
title_full_unstemmed GEOTHERMAL SYSTEM MODELLING BASED ON GRAVITY DATA OF ARJUNO-WELIRANG GEOTHERMAL FIELD, EAST JAVA, INDONESIA
title_sort geothermal system modelling based on gravity data of arjuno-welirang geothermal field, east java, indonesia
url https://digilib.itb.ac.id/gdl/view/61955
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