Abstract:
Research on the analysis of underground water in Rimbo Panjang Village using Sclumberger
Geoelectric and Hydrogeochemical methods. Geoelectric is a method used to determine the
nature of electric currents in the earth by detecting on the surface of the earth. Identification of
the aquifer layer was carried out on 2 lines with a length of 100 meters. Based on the results of
the analysis using progress software, the first path produces a resistivity value of 101.78 Ωm -
837.45 Ωm and the second path 118.02 Ωm - 863.84 Ωm. Groundwater samples at the study site
were tested for pH, TDS and coli bacteria. The results showed that all water samples has acidic
levels with an average pH of 5.5 so that rust often occurred on water pipes and caused smel
water, whereas TDS results was not exceed the quality standard and coli bacteria exceeded the
quality standard so the water was not suitable for consumption.
