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Determination of Aquifer Layer Using Geoelectric Resistivity Method in Lappae, Bone Regency, South Sulawesi, Indonesia
Author(s) -
Muhammad Altin Massinai,
Muhammad Fawzy Ismullah Massinai,
Erfan Syamsuddin,
AH Baso,
H Cottang
Publication year - 2021
Publication title -
iop conference series. materials science and engineering
Language(s) - English
Resource type - Journals
eISSN - 1757-899X
pISSN - 1757-8981
DOI - 10.1088/1757-899x/1115/1/012021
Subject(s) - aquifer , geology , bedrock , electrical resistivity and conductivity , layer (electronics) , geotechnical engineering , groundwater , geomorphology , materials science , engineering , electrical engineering , composite material
This research was carried out in Lappae, Bone Regency, an area that was supposedly having difficulty with water sources, remarkably in the dry season. This research aims to determine the water source location and the type of aquifer layer using the Geoelectric resistivity method with the Wenner-Schlumberger configuration. The results showed that the aquifer zone, which was thought to be a sandstone layer, was located at various depths ranging from 25-60 meters with a resistivity value of 25-150 Ωm. Meanwhile, bedrock layers are limestone with a resistivity value of 300 - 1200 Ω m. Based on the type of aquifer layer in the area, namely sandstone and limestone, the aquifer can be classified as a free aquifer because it only has a waterproof layer underneath

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