@phdthesis{digilib68185,
           month = {August},
           title = {KOMPARASI METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER DAN DATA BOR UNTUK IDENTIFIKASI AKUIFER BEBAS (UNCONFINED AQUIFER) DI KAWASAN PESISIR SELATAN KABUPATEN BANTUL},
          school = {UIN SUNAN KALIJAGA YOGYAKARTA},
          author = {NIM.: 18106020022 Andre Aldino Kusuma},
            year = {2024},
            note = {Pembimbing: Andi, M.Sc. dan Nugroho Budi Wibowo, S.Si., M. Sc.},
        keywords = {Akuifer bebas, Geolistrik, Konfigurasi Schlumberger, Resistivitas},
             url = {https://digilib.uin-suka.ac.id/id/eprint/68185/},
        abstract = {This research aims to identify unconfined aquifers in the southern coastal area of Bantul Regency, namely Kretek and Sanden Districts. The data used consists of 7 primary data, 8 secondary data and comparing them with 3 logging bor and groundwater table depth data. Data processing uses Progress software for 1D modeling and Rockworks 16 software for 3D modeling. The rock resistivity value ranges from 0.42 to 610.73 ohms. The sand resistivity value ranges from 10.58 to 110.18 ohms. The clay sand resistivity value ranges from 5.43 to 55.57 ohms. The clay soil resistivity value ranges from 0.43 to 28.7 ohms. The gravel sand resistivity value ranges from 204 to 610.73 ?m. The results of the study show that the subsurface lithology model of 1D geoelectric data has similarities with the drill lithology data. The free aquifer layer dominates evenly in each area. The rock layers that make up the free aquifer are sand, clay sand, and gravel sand. While the clay layer is an aquiclude, this layer is spread below and above the aquifer layer.}
}