Studi Geolistrik 2 Dimensi Untuk Eksplorasi Air Tanah di Kawasan Bukit Gambir, Johor, Malaysia
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Institusion
Universitas Islam Riau
Author
Fikri, M.zeki Al
Subject
QE Geology
Datestamp
2022-03-09 10:22:51
Abstract :
Geographically the research area is located in Bukit Gambir, Johor, Malaysia, with coordinates 2 ° 12 '50, 4''U / 102 ° 39 '27.36' 'T, Resistivity data collection is carried out from survey line one (GS1) to line survey two (GS2), The problem of water difficulties that occur in research conducted Research that aims to study the distribution of resistivity values, geological conditions, groundwater resistivity values, and groundwater levels in the study area. The 2 Dimensional Electrical Resistivity Imaging Survey (ERI) was carried out using ABEM Terrameter SAS 400 and ABEM Selector ES10-64 by adjusting the electrode-dipole poles, the resulting data were then processed using Res2DInv software and interpreted based on Telford, 1990. 46 resistivity meeting , 9 - 23165 ?m. The resistivity value of 46.9 - 430 ?m is interpreted as claystone, and the resistivity value of 1043 - 23165 ?m is interpreted as sandstone. the presence of aquifers can be obtained at a depth of 20 m - 130 m based on the resistivity values in GS1 and GS2.
Geographically the research area is located in Bukit Gambir, Johor, Malaysia, with coordinates 2 ° 12 '50, 4''U / 102 ° 39 '27.36' 'T, Resistivity data collection is carried out from survey line one (GS1) to line survey two (GS2), The problem of water difficulties that occur in research conducted Research that aims to study the distribution of resistivity values, geological conditions, groundwater resistivity values, and groundwater levels in the study area. The 2 Dimensional Electrical Resistivity Imaging Survey (ERI) was carried out using ABEM Terrameter SAS 400 and ABEM Selector ES10-64 by adjusting the electrode-dipole poles, the resulting data were then processed using Res2DInv software and interpreted based on Telford, 1990. 46 resistivity meeting , 9 - 23165 ?m. The resistivity value of 46.9 - 430 ?m is interpreted as claystone, and the resistivity value of 1043 - 23165 ?m is interpreted as sandstone. the presence of aquifers can be obtained at a depth of 20 m - 130 m based on the resistivity values in GS1 and GS2.
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