Analisis Aliran Air Bawah Permukaan Dengan Menggunakan Metode Geolistrik

  • Muhammad Ragil Setiawan Institut Teknologi Sumatera
  • Bilal Al Farishi Institut Teknologi Sumatera
  • Lea Kristi Agustin Institut Teknologi Sumatera
Keywords: clean water, geoelctric, aquifer flow

Abstract

Cean water is needed in a human community. The need for clean water can be taken from subsurface water through a pumping process. Efforts to get clean water that has sustainability can be done by knowing the direction of the aquifer flow. The direction of the aquifer flow can be known through subsurface modeling. This study uses the geoelectric method in modeling the subsurface layer to determine the position of the aquifer. Based on the subsurface model, the average depth of an aquifer is between 30-100 meters. The subsurface model shows the type of aquifer depressed with a clay layer as the upper and lower limits of the aquifer. The subsurface water is estimated to have a flow direction from East to West in a confined aquifer.

References

[1] Siringoringo, L. P., Reza R., and Janner N., Hydrogeochemical and Groundwater Assessment for Drinking Purpose at ITERA Campus Area and Its Surrounding, Journal of Geoscience, Engineering, Environment, and Technology, vol. 04 No. 01, p.40-48, 2019.
[2] Setiawan, M.R., Badri, R.M., Singarimbun, A., Kajian Awal Pendugaan Akuifer Air Tanah di Kampus ITERA dengan Metode Geolistrik Konfigurasi Schlumberger, J.Sci. App. Teknol. Sumatera, vol. 2, p. 40-46, 2017.
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Published
2019-11-30
How to Cite
Setiawan, M., Farishi, B., & Agustin, L. (2019). Analisis Aliran Air Bawah Permukaan Dengan Menggunakan Metode Geolistrik. Jurnal Pendidikan Teknologi Kejuruan, 2(4), 111-116. https://doi.org/10.24036/jptk.v2i4.6323
Section
Articles

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