Perbandingan Hasil Deteksi Air Tanah Dengan Metode Geolistrik Konfigurasi Schlumberger, Wenner, Wenner-Schlumberger, Dipole-Dipole Dan Pole-Pole

  • Ashady Adhe Universitas Pembangunan Nasional “Veteran” Yogyakarta
  • Waterman SB Universitas Pembangunan Nasional Veteran Yogyakarta
  • Nurkhamim Universitas Pembangunan Nasional Veteran Yogyakarta

Abstract

Water is an essential resource for human being and the needs significantly increases from time to time. The highly demand of water may cause water scarcity. Based on that condition, groundwater exploration is urgently needed, where at least the location and depth of the groundwater can be identified through an accurate method. Geoelectric, on the other hand, is a geophysics method that is commonly used for identifying geology structures, including for groundwater exploration or identification. The objectivity of this research was to compare the geoelectric configuration accuracy, which Schlumberger, Wenner, Wenner-Schlumberger, Dipole-dipole, and Pole-pole were discussed. As a result, configuration of Wenner amd Wenner-Schlumberger showed the best results based on the vertical resolutiuon, the CST, and the sounding parameters.

References

[1] As’ari, Seni H J T. Metode geolistrik konfigurasi dipole-dipole untuk identifikasi daerah patahan manado di kecamatan singkil kota manado, MIPA UNSRAT Online. 2016; 2: 99-102.
[2] Kurniawan, Basra., Akmam., dan Sudiar, Nofi Yendri. Estimasi Kedalaman Batuan Dasar Di Desa Kampung Manggis Kecamatan Padang Panjang Barat Menggunakan Metode Inversi Robust 2D Data Geolistrik Tahanan Jenis Konfigurasi Wenner. Pillar of Physics. 2014; 1: 49-56.
[3] Andrias S W. Aplikasi metode geolistrik resistivitas konfigurasi wenner untuk menentukan struktur tahan di halaman belakang SCC ITS Surabaya, fisika Indonesia. 2016; 55
[4] Muntaha, Jakaria A.L, Febrian D S. Identifikasi Struktur Tanah Bawah Permukaan Tempat Pemrosesan Akhir (TPA) Manggar dengan Menggunakan Metode Geolistrik Konfigurasi Schlumberger. Aplikasi Teknik Sipil. 2019; 17 No.1
[5] Prastowo, R., Helmi, H., Trianda, O., & Umam, R. Identification of Slip Surfaces Using the Geoelectric Imaging Method in the Kalirejo Area, Kokap District, Yogyakarta, Indonesia. JIPF (Jurnal Ilmu Pendidikan Fisika), 6(3), 234-242. 2021
[6] Prastowo, R., Helmi, H., Trianda, O., & Umam, R. Identification of Andesite Resource Potential In Kalirejo Area, Kokap Sub-District, Kulon Progo Using Resistivity Method. In Forum Geografi, 35 (1). 2021
[7] Wilson, E.M,Hidrologi Teknik. Institut Teknologi Bandung, Bandung. 1993
[8] Sutandi, M.C,Air Tanah. Universitas Kristen Maranatha, Bandung,
[9] Telford, W.M., Geldart, L.P., dan Sheriff, R.E, Applied Geophysics, 2nd edition, Cambridge University Press, Cambridge. 1990
[10] Wahyono C. S, W.Utama, N Priyantari, “Penentuan Bidang Gelincir Pada Daerah Rawan Longsor Dengan Menggunakan Metode Geolistrik 2-D Di Desa Lumbang Rejo, Prigen, Pasuruhan. Program Pasca sarjana Fisika. FMIPA ITS. Surabaya, 2013
Published
2022-11-11
How to Cite
Ashady Adhe, Waterman SB and Nurkhamim (2022) “Perbandingan Hasil Deteksi Air Tanah Dengan Metode Geolistrik Konfigurasi Schlumberger, Wenner, Wenner-Schlumberger, Dipole-Dipole Dan Pole-Pole”, ReTII, pp. 132-139. Available at: //journal.itny.ac.id/index.php/ReTII/article/view/3542 (Accessed: 22June2024).