Repo Dosen ULM

Identifikasi Lapisan Akuifer Tertekan Dengan Metode Geolistrik di Desa Lok Rawa Kecamatan Mandastana Kabupaten Barito Kuala Kalimantan Selatan

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dc.contributor.author Anwar, Samsul
dc.contributor.author Wahyono, Sri Cahyo
dc.contributor.author Fahruddin
dc.date.accessioned 2022-04-26T03:31:47Z
dc.date.available 2022-04-26T03:31:47Z
dc.date.issued 2020-07-01
dc.identifier.issn 2303-016X
dc.identifier.issn 2549-1156
dc.identifier.uri https://repo-dosen.ulm.ac.id//handle/123456789/23905
dc.description.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. en_US
dc.language.iso en en_US
dc.publisher 'Jurusan Fisika Fakultas MIPA, Universitas Lampung en_US
dc.subject geoelectric, Schlumberger configuration, aquifer. en_US
dc.title Identifikasi Lapisan Akuifer Tertekan Dengan Metode Geolistrik di Desa Lok Rawa Kecamatan Mandastana Kabupaten Barito Kuala Kalimantan Selatan en_US
dc.type Article en_US


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