Identifikasi Air Tanah di Daerah Pesisir Pantai Kolbano
DOI:
https://doi.org/10.25077/jfu.10.2.262-266.2021Abstract
Telah dilakukan penelitian identifikasi air tanah di wilayah pesisir Kolbano yang bertujuan untuk mengetahui dan menentukan kedalaman air tanah di lokasi penelitian. Metode yang digunakan adalah metode geolistrik dengan konfigurasi Schlumberger. Data yang diperoleh di lokasi penelitian diolah menggunakan software Res2dinv untuk mendapatkan nilai resistivitas batuan di lapangan. Hasil inversi menunjukkan nilai resistivitas batuan terukur pada 3 lintasan yaitu 17,1-27,626 Ωm. Berdasarkan nilai resistivitas yang diperoleh, diasumsikan terdapat 3 jenis lapisan batuan di lapangan, yaitu lempung dengan resistivitas (10-100) Ωm dan aluvium dengan resistivitas (101–800 Ωm) dan batugamping (101–27.626 Ωm). Potensi batuan sebagai batuan akuifer adalah alluvium. Air tanah yang tersimpan di batuan aluvium terletak pada kedalaman (12-20 m).
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Research on groundwater identification in the coastal area of Kolbano has been carried out, which aims to determine and determine the depth of groundwater at the research location. The method used is the geoelectric method with a Schlumberger configuration. The data obtained at the research location were processed using res2dinv software to obtain the rock resistivity value in the field. The inversion results show the measured rock resistivity value on 3 measurement line, namely 17.1-27.626 Ωm Based on the resistivity value obtained, it is assumed that there are 3 types of rock layers in the field, consisting of clay with resistivity (10-100 Ωm) and alluvium with resistivity (101-800 Ωm) and limestone (101-27.626Ωm). Rocks Potential as aquifer rocks is alluvium. Groundwater stored in alluvium rocks lies at a depth (12-20 m).
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