RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY

According to the data from PT Perusahaan Listrik Negara (Persero), the contribution of renewable energy to power plants can also be quite significant, already reaching 13.42% until May 2019. Indonesia is located in the circle of fire, which increases energy with geothermal energy resources. With...

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Main Author: Muhammad Rashad, Rifki
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/47227
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:47227
spelling id-itb.:472272020-03-17T07:25:46ZRADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY Muhammad Rashad, Rifki Indonesia Final Project geothermal, Patuha, radon, geological structure, potential zone. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/47227 According to the data from PT Perusahaan Listrik Negara (Persero), the contribution of renewable energy to power plants can also be quite significant, already reaching 13.42% until May 2019. Indonesia is located in the circle of fire, which increases energy with geothermal energy resources. With this potential resources, Indonesia can improve it’s geothermal energy development. One of the first steps in enhancing the geothermal utilization in Indonesia is exploration activity. A preliminary exploration method for determining zones that have geothermal potential from the surface is by analyzing the concentration of radon gas in ground gas. In this study, delineation of the geothermal potential zone in the Patuha geothermal field was carried out by measuring the composition of radon from soil gas that has been taken out from 1,5 meter depth shallow wells. The radon measurement of 18 wells were conducted from April to August 2019. Measured radon gas concentrations are ranging from 190 Bq/m3 to 27,400 Bq/m3. Radon gas concentration with the highest values are at PPL05, PPL06, PPL07 and PA02. Radon gas concentration values are then correlated with lithology and geological structure. Radon gas concentration values have stong correlaton with geological structures i.e. faults. Whereas for lithology parameters, there is no correlation. Radon gas concentration values are used for delineation of geothermal potential zones. Based on this study, it can be concluded that there are two geothermal potential zones, namely at S-N directed zone in PPL07-PPL06 and at NW-SE directed zone in PPL05-PA02. 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 According to the data from PT Perusahaan Listrik Negara (Persero), the contribution of renewable energy to power plants can also be quite significant, already reaching 13.42% until May 2019. Indonesia is located in the circle of fire, which increases energy with geothermal energy resources. With this potential resources, Indonesia can improve it’s geothermal energy development. One of the first steps in enhancing the geothermal utilization in Indonesia is exploration activity. A preliminary exploration method for determining zones that have geothermal potential from the surface is by analyzing the concentration of radon gas in ground gas. In this study, delineation of the geothermal potential zone in the Patuha geothermal field was carried out by measuring the composition of radon from soil gas that has been taken out from 1,5 meter depth shallow wells. The radon measurement of 18 wells were conducted from April to August 2019. Measured radon gas concentrations are ranging from 190 Bq/m3 to 27,400 Bq/m3. Radon gas concentration with the highest values are at PPL05, PPL06, PPL07 and PA02. Radon gas concentration values are then correlated with lithology and geological structure. Radon gas concentration values have stong correlaton with geological structures i.e. faults. Whereas for lithology parameters, there is no correlation. Radon gas concentration values are used for delineation of geothermal potential zones. Based on this study, it can be concluded that there are two geothermal potential zones, namely at S-N directed zone in PPL07-PPL06 and at NW-SE directed zone in PPL05-PA02.
format Final Project
author Muhammad Rashad, Rifki
spellingShingle Muhammad Rashad, Rifki
RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
author_facet Muhammad Rashad, Rifki
author_sort Muhammad Rashad, Rifki
title RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
title_short RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
title_full RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
title_fullStr RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
title_full_unstemmed RADON GAS CONCENTRATION ANALYSIS FOR GEOTHERMAL POTENTIAL ZONE DELINEATION IN PATUHA GEOTHERMAL FIELD, CIWIDEY, BANDUNG REGENCY
title_sort radon gas concentration analysis for geothermal potential zone delineation in patuha geothermal field, ciwidey, bandung regency
url https://digilib.itb.ac.id/gdl/view/47227
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