IDENTIFIKASI LAPISAN AKUIFER MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER DI PERUMAHAN ARZA GRIYA MANDIRI JAMBI

Abstract

Water resources are important for the community because water is a basic need for living things, including humans. The increasing human population and rapid infrastructure development have led to a very high demand for clean water. On the other hand, environmental pollution and global warming have caused sources of clean water on the surface to continue to decrease. It is necessary to explore subsurface groundwater to meet the need for clean water. This study aims to determine the distribution and depth of the aquifer layer, which has the potential to store groundwater reserves. The method used in this research is the geoelectrical resistivity method with schlumberger configuration. Data acquisition was carried out at 16 line with a length of each line is 200 m. Data processing is done using Res2Dinv software and Surfer software. From the results of the study, it can be concluded that from the 16 geoelectric line used, the aquifer layer which can be interpreted as containing groundwater is located between 1035'50'' 1036'40'' South Latitude and 103030'50'' 104031'40'' East Longitude towards the south with a depth of 50 100 meters.