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All Journal Jurnal Teori dan Aplikasi Fisika
Samsul Anwar
Program Studi Fisika, Universitas Lambung Mangkurat
Materials Science & Nanotechnology Physics

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Identifikasi Lapisan Akuifer Tertekan Dengan Metode Geolistrik di Desa Lok Rawa Kecamatan Mandastana Kabupaten Barito Kuala Kalimantan Selatan Samsul Anwar; Sri Cahyo Wahyono; Fahruddin Fahruddin
Jurnal Teori dan Aplikasi Fisika Vol 8, No 2 (2020): Jurnal Teori dan Aplikasi Fisika
Publisher : Universitas Lampung

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23960/jtaf.v8i2.2447

Abstract

One way to be able to identify rocks below the surface, depth, including groundwater aquifer layers is to do geophysical measurements using the schlumberger geoelectric method. This study aims to determine thickness and depth of aquifers in Lok Rawa Village, Mandastana District, Barito Kuala Regency. The results of the schlumberger configuration geoelectric study showed rock layers in Lok Rawa Village at the measurement points GL1, GL2 and GL3 consisting of weathered, sand, and fine clay (silt) layers. Lapiasan aquifers in Lok Rawa Village at the measurement points GL1, GL2 and GL3 consisting of free aquifer layers are estimated to occur at a depth of  3─5 m with a resistivity value of  7─15 Ωm. Depressed aquifer layer is estimated to be at a depth  of 25─75 m and  ≥ 110 m with resistivity values of  7─15 Ωm. Of the 2 types of aquifer layers, the most confined aquifer layer has the potential to contain ground water.  
Co-Authors Fahruddin Fahruddin Sri Cahyo Wahyono