| NIM | K1C016047 |
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| Namamhs | USAMAH |
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| Judul Artikel | IDENTIFIKASI SUMBER AIR TANAH MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER DI DESA RANDEGAN KECAMATAN KEBASEN KABUPATEN BANYUMAS |
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| Abstrak (Bhs. Indonesia) | Telah dilakukan survei metode geolistrik resistivitas untuk pemetaan sumber air tanah di Desa Randegan Kecamatan Kebasen Kabupaten Banyumas. Tujuan kegiatan adalah menentukan struktur perlapisan batuan bawah permukaan dan mengidentifikasi akuifer berdasarkan hasil survei geolistrik resistivitas konfigurasi Schlumberger. Untuk mencapai tujuan tersebut telah dilakukan survei geolistrik di tiga lokasi yang dipilih berdasarkan rekomendasi aparat desa. Hasil pengolahan data dan interpretasi diperoleh struktur perlapisan batuan di Desa Randegan berdasarkan nilai resistivitas batuan, terdiri dari tanah penutup (top soil), pasir, dan batuan breksi. Jenis akuifer yang telah teridentifkasi di lokasi sounding RDG-1 pada kedalaman 63,92 m merupakan akuifer tertekan, berupa pasir. Sedangkan di lokasi sounding RDG-2 pada kedalaman 21,18 – 48,14 m berupa pasir, merupakan akuifer tertekan, dan di lokasi sounding RDG-3, juga merupakan akuifer bebas pada kedalaman 11,64 – 24,03 m, jenis batuan serpih (shale). Hasil survei metode geolistrik tersebut didesiminasikan dalam forum pertemuan dan diskusi untuk memberikan informasi mengenai peta sebaran dan kedalaman batuan pembawa air tanah atau akuifer di Desa Randegan. |
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| Abtrak (Bhs. Inggris) | A resistivity geoelectrical survey has been carried out for mapping groundwater sources in Randegan Village, Kebasen District, Banyumas Regency. The objective of this activity is to determine the structure of the subsurface rock layers and identify aquifers based on the results of the Schlumberger configuration resistivity geoelectric survey. To achieve this goal, geoelectrical surveys have been carried out at three locations selected based on recommendations from village officials. The results of data processing and interpretation obtained the rock layer structure in Randegan Village based on the resistivity value of the rock, consisting of top soil, sand and breccia rock. The type of aquifer that has been identified at the RDG-1 sounding location at a depth of 63.92 m is a confined aquifer, in the form of sand. Whereas at the RDG-2 sounding location at a depth of 21.18 - 48.14 m in the form of sand, which is a confined aquifer, and at the RDG-3 sounding location, it is also a free aquifer at a depth of 11.64 - 24.03 m, shale rock type (shales). The survey results of the geoelectric method were disseminated in meeting and discussion forums to provide information regarding the distribution map and depth of groundwater or aquifer-bearing rocks in Randegan Village. |
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| Kata kunci | geolistrik, resistivitas, konfigurasi Schumberger, akuifer, Randegan |
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| Pembimbing 1 | Sugito, S.Si., M.Si |
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| Pembimbing 2 | Hartono, S.Si., M.Si |
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| Pembimbing 3 | - |
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| Tahun | 2023 |
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| Jumlah Halaman | 6 |
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| Tgl. Entri | 2023-08-30 10:56:06.339537 |
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