Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data

Jakarta groundwater basin is one of the most developed basins in Indonesia as Jakarta city is located within the basin, with an elevation ranging from 0 to 1000 m above sea level. The study of the basement characteristics of groundwater basins still needs further study in the Jakarta Groundwater Bas...

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Main Authors: Gumilar Utamas Nugraha, Lina Handayani, Rachmat Fajar Lubis, Dadan Dani Wardhana, Karit Lumban Gaol
Format: Article
Language:English
Published: Universitas Gadjah Mada 2020-04-01
Series:Indonesian Journal of Geography
Subjects:
Online Access:https://jurnal.ugm.ac.id/ijg/article/view/46672
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author Gumilar Utamas Nugraha
Lina Handayani
Rachmat Fajar Lubis
Dadan Dani Wardhana
Karit Lumban Gaol
author_facet Gumilar Utamas Nugraha
Lina Handayani
Rachmat Fajar Lubis
Dadan Dani Wardhana
Karit Lumban Gaol
author_sort Gumilar Utamas Nugraha
collection DOAJ
description Jakarta groundwater basin is one of the most developed basins in Indonesia as Jakarta city is located within the basin, with an elevation ranging from 0 to 1000 m above sea level. The study of the basement characteristics of groundwater basins still needs further study in the Jakarta Groundwater Basin. The objective of this study is to examine the basement characteristics of Jakarta Groundwater Basin by satellite gravimetry. Gravity forward models were constructed using Oasis Montaj and 2-D GM-SYS software for two north-south sections, A and B, and west-east section C-D. Regional anomalies in the study area with a value range of 36.7 to 53.2 mGal, while the residual anomaly values in the study area were in the range of -7.0 - 10.0 mGal. There are four rock formations based on forwarding modeling. Holocene Beach Ridge Deposit formation has a density of 2.0 gr/cc. The thickness of this formation is estimated to be around 10-20 meters. Late Pleistocene Alluvial fan has a density of about 2.2 gr/cc. The depth of this layer ranges from 10-50 meters. Early Pleistocene Formation, has a density of 2.35 gr/cc. The thickness of this formation is at a depth of 50-200 meters in the cross-section. The Tertiary Marine Sediment Formation is a basement of the Jakarta Groundwater Basin. This formation has a rock density of 2.45 gr/cc.
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spelling doaj.art-1393167b3d5d42faa8e597744a939fc52022-12-22T00:00:10ZengUniversitas Gadjah MadaIndonesian Journal of Geography0024-95212354-91142020-04-01521425210.22146/ijg.4667226727Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry DataGumilar Utamas Nugraha0Lina Handayani1Rachmat Fajar Lubis2Dadan Dani Wardhana3Karit Lumban Gaol4Research Center For Geotechnology, Indonesian Institute of Sciences , Indonesia.Research Center For Geotechnology, Indonesian Institute of Sciences , Indonesia.Research Center For Geotechnology, Indonesian Institute of Sciences , Indonesia.Research Center For Geotechnology, Indonesian Institute of Sciences , Indonesia.Research Center For Geotechnology, Indonesian Institute of Sciences , Indonesia.Jakarta groundwater basin is one of the most developed basins in Indonesia as Jakarta city is located within the basin, with an elevation ranging from 0 to 1000 m above sea level. The study of the basement characteristics of groundwater basins still needs further study in the Jakarta Groundwater Basin. The objective of this study is to examine the basement characteristics of Jakarta Groundwater Basin by satellite gravimetry. Gravity forward models were constructed using Oasis Montaj and 2-D GM-SYS software for two north-south sections, A and B, and west-east section C-D. Regional anomalies in the study area with a value range of 36.7 to 53.2 mGal, while the residual anomaly values in the study area were in the range of -7.0 - 10.0 mGal. There are four rock formations based on forwarding modeling. Holocene Beach Ridge Deposit formation has a density of 2.0 gr/cc. The thickness of this formation is estimated to be around 10-20 meters. Late Pleistocene Alluvial fan has a density of about 2.2 gr/cc. The depth of this layer ranges from 10-50 meters. Early Pleistocene Formation, has a density of 2.35 gr/cc. The thickness of this formation is at a depth of 50-200 meters in the cross-section. The Tertiary Marine Sediment Formation is a basement of the Jakarta Groundwater Basin. This formation has a rock density of 2.45 gr/cc.https://jurnal.ugm.ac.id/ijg/article/view/46672geophysicshydrogeologygroundwater basinjakartagravimetrygravity satellite dataindonesian journal of geographyindonesiajurnal ugm
spellingShingle Gumilar Utamas Nugraha
Lina Handayani
Rachmat Fajar Lubis
Dadan Dani Wardhana
Karit Lumban Gaol
Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
Indonesian Journal of Geography
geophysics
hydrogeology
groundwater basin
jakarta
gravimetry
gravity satellite data
indonesian journal of geography
indonesia
jurnal ugm
title Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
title_full Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
title_fullStr Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
title_full_unstemmed Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
title_short Basement Characteristics of Jakarta Groundwater Basin Based on Satellite Gravimetry Data
title_sort basement characteristics of jakarta groundwater basin based on satellite gravimetry data
topic geophysics
hydrogeology
groundwater basin
jakarta
gravimetry
gravity satellite data
indonesian journal of geography
indonesia
jurnal ugm
url https://jurnal.ugm.ac.id/ijg/article/view/46672
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AT rachmatfajarlubis basementcharacteristicsofjakartagroundwaterbasinbasedonsatellitegravimetrydata
AT dadandaniwardhana basementcharacteristicsofjakartagroundwaterbasinbasedonsatellitegravimetrydata
AT karitlumbangaol basementcharacteristicsofjakartagroundwaterbasinbasedonsatellitegravimetrydata