Jordi Mahardika Puntu, Cholisina Anik Perwita, Sukir Maryanto
Department of Physics, Faculty of Mathematic and Natural Science,
Brawijaya University, Jalan Veteran Malang, 65145, Indonesia
MLA 8 Puntu, Jordi Mahardika, et al. "3D MODELLING FOR DETERMINATION OF GROUNDWATER DRILLING LOCATION USING GEOELECTRIC RESISTIVITY METHOD DIPOLE-DIPOLE CONFIGURATION." IJETSI, vol. 3, no. 6, Dec. 2018, pp. 258-263, ijetsi.org/more2018.php?id=18. Accessed Dec. 2018.
APA Puntu, J., Perwita, C., & Maryanto, S. (2018, December). 3D MODELLING FOR DETERMINATION OF GROUNDWATER DRILLING LOCATION USING GEOELECTRIC RESISTIVITY METHOD DIPOLE-DIPOLE CONFIGURATION. IJETSI, 3(6), 258-263. Retrieved from ijetsi.org/more2018.php?id=18
Chicago Puntu, Jordi Mahardika, Cholisina Anik Perwita, and Sukir Maryanto. "3D MODELLING FOR DETERMINATION OF GROUNDWATER DRILLING LOCATION USING GEOELECTRIC RESISTIVITY METHOD DIPOLE-DIPOLE CONFIGURATION." IJETSI 3, no. 6 (December 2018), 258-263. Accessed December, 2018. ijetsi.org/more2018.php?id=18.
References [1]. AGI, 2016. American Geosciences
Institutes. [Online] Available at:
http://www.k5geosource.org/1conten
t/1sc/water/ [Accessed on March,
2016].
[2]. Irjan, 2012. Pemetaan potensi air
tanah (Aquifer) berdasarkan
interpretasi resistivitas Wenner
Sounding. Fakultas Sains dan
Teknologi UIN Malang, Volume I,
pp. 1-12.
[3]. Kurniawan, D., 2008. Meeting the
needs of clean water for people in
Housing Pucanggading. Semarang:
Diponegoro University.
[4]. Muslim, 2009. The basic concept of
fluid physics. Bandung: University of
Education Indonesia.
[5]. Todd, 1980. Groundwater
Hydrology, 2nd edition. Toronto:
John Wiley.
[6]. Trimper, P., 2014. Groundwater.
[Online] Available at:
http://www.env.gov.nl.ca/env/waterr
es/cycle/groundwater/ [Accessed on
April 2016].
[7]. Yudistira, A., 2012. Study of the
potential direction of groundwater
for domestic needs in the Sleman
district. Yogyakarta: Gadjah Mada
University.
Abstract: We attempt to determine groundwater drilling location at Villa Tlogomas Residential,
Lowokwaru Subdistrict, Malang City East Java where the new unit will be built, using the
geoelectric resistivity method, dipole-dipole configuration. Measurements were taken at five
lines. Line 1, 2 and 3 with a long stretch 100 meters. Line 4 and line 5 with a long stretch 60
meters. Line 4 and 5 intersect line 1 until 3 on the north and south. The distance between the
electrodes as far as 5 meters for each line. Based on 2D modeling and 3D modeling, it can be
found lithology in the research areas consist of soil or wet clays, tuff, saturated gravel, and
breccias. The groundwater distribution in the saturated gravel which located at a depth about 6,7
meters to 11,8 meters below the subsurface. From the modeling results, the point of groundwater
drilling is recommended at a depth 9-11 meters in 4 drilling points which is in the point where
the line intersects each other.
The International Journal of Engineering Technology and Scientific Innovation Inviting Papers/Articles for Upcoming Issue Volume: 09, Issue: 05 "September-October 2024".
Submit your Paper through Online Submission System. Authors also can Send Paper to submit@ijetsi.org ....... Impact Factor for IJETSI is 2.512