IDENTIFIKASI LAPISAN BAWAH PERMUKAAN MENGGUNAKAN METODE GEOLISTRIK DI SEKITAR REMBESAN LUMPUR DI DESA BAKUSTULAMA, KECAMATAN TASIFETO BARAT, KABUPATEN BELU
Abstract
The study has been conducted to identify subsurface layers using the Wenner-Schlumberger geoelectric method. This research aims to understand the rock layering and hydrogeology at the research site. The research was conducted with a field survey on four 480-meter-long tracks in Bakustulama Village. Rock resistivity data was measured using a resistivity meter and analyzed using Res2DinV software to produce a 2D cross-sectional model. This method utilizes rock resistivity to determine the nature and layering of rocks in the subsurface, focusing on potentially water-saturated zones and fractures. The results show that the subsurface layer in Bakustulama Village consists of sandstone in the upper layer (0-20 meters) with medium resistivity (100-700 Ωm), followed by a highly water-saturated clay layer with low resistivity (0-100 Ωm), and a limestone layer with high resistivity (700-1000).
The subsoil in the Bakustulama Area is diversely arranged, with sandstone layers at the surface to a depth of about 20 meters that suspected to have high porosity and are easily drained by water. Underneath, water-saturated clay layers are dominant and difficult for fluids to pass through.
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References
[2] Jusfarida dan Aleik, A. A. (2020). Aktivitas Tektonik Sebagai Pemicu Munculnya Mud Volcano Buhjel Tase Madura. Prosiding, Seminar Teknologi Kebumian dan Kelautan (SEMITAN II), Vol. 2, No. 1.
[3] Jonathan, S. H., Desi, Y., Ario, B. W. dan Suliantara. (2016). Rembesan Migas Di Daerah Timor Barat. Lembaran Publikasi Minyak Dan Gas Bumi, Vol. 50, No. 3, 1-8.).
[4] Dian, C., Rumi, A. dan Ni Made, C. P. (2018). Penerapan Metode Geolistrik Konfigurasi Wenner-Schlumberg Untuk Analisis Rembesan Pada Maindam Waduk Greneng, Kabupaten Blora. Jurnal Teknik Pengairan, Vol. 9, No. 2, 114-124
[5] Yuristina, A. P., Supriyadi., Khumaedi. (2015). Pendugaan Persebaran Air Bawah Permukaan Metode Geolistrik Konfigurasi Wenner-Schlumberger Di Desa Tanggungarjo, Kabupaten Grobingan. Unnesa Physsics Jurnal (UPJ). Vol. 4, No. 1.
[6] Sakka. (2002). Metoda Geolistrik Resistivitas. Fakultas Matematika dan Ilmu Pengetahuan Alam. Makasar: UNHAS.
[7] Iman, C. P., Heri, P. dan Nana, R., Juanda. (2011). Aplikasi Metoda Geolistrk Konfigurasi Wenner-Schlumberger Pada Survey Gerakan Tanah di Bajawa, NTT. Bulletin Vulkanologi dan Bencana Geologi, Vol. 6, No. 2, 1-10.
[8] Wahyudi A., Azrul A., Muhardi. (2021). Penggunaan Metode Geolistrik Resistivitas Untuk Identifikasi Lapisan Bawah Permukaan Daerah Gunung Tujuh, Kabupaten Kayong Utara. Jurnal Fisika Unand (JFU).Vol. 10, No. 1, 62-69.
[9] Sianturi H.L., Adi Susilo., Juliany N. M., Redi K. Pingak. (2023). Analysis of Landslide Using Resistivity Method in the Avalanche Area of Tolnaku, Kupang Regency, East Nusa Tenggara, Indonesia. International Journal of Safety and Security Engineering. Vol. 13, No. 5, 925-931
[10] Loke, M. H. (1999). Electrical imaging surveys for environmental and engineering studies, A practical guide to 2-D and 3-D surveys. Geophysical Prospecting
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Jl. Adisucipto, Penfui-Kupang, Lasiana, Klp. Lima, Kota Kupang, Nusa Tenggara Timur., Indonesia
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