Vertical Electrical Sounding Exploration of Groundwater in Kertajati, Majalengka, West Java, Indonesia

Authors

  • Gumilar Utamas Nugraha Research Center For Geotechnology, Indonesian Institute of Sciences, Indonesia
  • Boy Yoseph CSSSA Faculty of Geological Engineering, Padjadjaran University, Indonesia
  • Andi Agus Nur Faculty of Geological Engineering, Padjadjaran University, Indonesia
  • Pulung Arya Pranantya Research Center For Water Resources, Ministry of Public Works and Housing, Indonesia
  • Lina Handayani Research Center For Water Resources, Ministry of Public Works and Housing, Indonesia
  • Rachmat Fajar Lubis Research Center For Geotechnology, Indonesian Institute of Sciences, Indonesia
  • Hendra Bakti Research Center For Geotechnology, Indonesian Institute of Sciences, Indonesia

DOI:

https://doi.org/10.17014/ijog.8.3.359-369

Keywords:

Remote Sensing, Spatial Data, Gravity Method, Groundwater

Abstract

DOI:10.17014/ijog.8.3.359-369

Continuously increasing population and progressive infrastructural development in the region of Kertajati International Airport, Indonesia, emphasize the need to develop a sustainable water supply network. Airport facilities require sufficient water resources, which can be obtained from surface water and groundwater. Groundwater exploration can provide necessary information for assessing water resources. The purpose of this study is to analyze the configuration of aquifers in the studied area. A Schlumberger array was used to carry out twelve vertical electrical soundings (VES) with AB/2 electrode spacing ranging from 1.5 m to 150 m. IPI2win software was used to qualitatively interpret the VES results and it suggested the presence of three distinct lithological units interpreted as clay, alluvial sand, and a Lower Quaternary formation. In general, resistivity values in the studied area can be divided into five resistivity categories: very low resistivity with values ranging from 1 Ωm to 10 Ωm, low resistivity with values ranging from 10 Ωm to 50 Ωm, medium resistivity with values ranging from 50 Ωm to 100 Ωm, high resistivity with values ranging from 100 Ωm to 200 Ωm, and very high resistivity with values > 200 Ωm. The geo-electric interpretation revealed three geo-electric layers: topsoil (1 - 144 Ω m), sand (1 - 298 Ω m), and clay (1 - 82 Ω m). Aquifers in the studied area are lithologically composed of sand. Clay is the dominant lithology in the studied area, so the presence of aquifers in this area is very limited, and thus the supply of groundwater is also limited. The exploitation of groundwater must be limited and controlled to maintain the sustainability of groundwater in the studied area.

Author Biography

Gumilar Utamas Nugraha, Research Center For Geotechnology, Indonesian Institute of Sciences

 

 

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Published

14-08-2021

How to Cite

Nugraha, G. U., CSSSA, B. Y., Nur, A. A., Pranantya, P. A., Handayani, L., Lubis, R. F., & Bakti, H. (2021). Vertical Electrical Sounding Exploration of Groundwater in Kertajati, Majalengka, West Java, Indonesia. Indonesian Journal on Geoscience, 8(3), 359–369. https://doi.org/10.17014/ijog.8.3.359-369

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