Eksplorasi Air Tanah di Jakarta

The purpose of the geoelectricity resistivity survey in DKI Jakarta, i.e. in Taman Duta Cimanggis Resident and the Ministry of Environment Office is to find out the distribution of penetration zone beneath the surface. The geoelectricity method is intended to find out the depth and spread formation of the lower layer surface of the acquired resistivity value based prediction. Based on that resistivity distribution, geological subsurface conditions can then be interpreted. Hydrogeological condition in the research site was included to the aquifer system with wide range of groundwater spreads. Rocks which are expected to be aquifer in both site are sandy clay and sand. From the geoelectricity estimation observation results, the aquifer layer can be found out, i.e. in Taman Duta CImanggis Resident was in depth of 20-60 m below the ground surface with the lithological form of sand. While in the Ministry of Environment Office By Pass were in depth of 10-20 m (aquifer I layer with the lithological form of sandy clay) and 30-35 (aquifer II layer with the lithological form of sand)