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

被引:3
|
作者
Nugraha, Gumilar Utama [1 ]
Alam, Boy Yoseph Cahya Sunan Sakti Syah [2 ]
Nur, Andi Agus [2 ]
Pranantya, Pulung Arya [3 ]
Handayani, Lina [1 ]
Lubis, Rachmat Fajar [1 ]
Bakti, Hendra [1 ]
机构
[1] Indonesian Inst Sci, Res Ctr Geotechnol, Jakarta, Indonesia
[2] Padjadjaran State Univ, Fac Geol Engn, Sumedang, Indonesia
[3] Minist Publ Works & Housing, Res Ctr Water Resources, Jakarta, Indonesia
来源
INDONESIAN JOURNAL OF GEOSCIENCE | 2021年 / 8卷 / 03期
关键词
vertical electrical sounding; aquifer; groundwater; geo-electric layers; AQUIFER;
D O I
10.17014/ijog.8.3.359-369
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 Omega m to 10 Omega m, low resistivity with values ranging from 10 Omega m to 50 Omega m, medium resistivity with values ranging from 50 Omega m to 100 Omega m, high resistivity with values ranging from 100 Omega m to 200 Omega m, and very high resistivity with values > 200 Omega m. The geo-electric interpretation revealed three geo-electric layers: topsoil (1 -144 Omega m), sand (1 -298 Omega m), and clay (1 -82 Omega 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.
引用
收藏
页码:359 / 369
页数:11
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