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Identifikasi Air Tanah Dangkal Menggunakan Metode Geolistrik Konfigurasi Wenner Dan Hidrogeokimia Di Jalan Matoa Rayasidomulyo Barat Kecamatan Tampan
Water is the main requirement for living things. Broadly speaking, water is divided into surface water and subsurface water. This study uses the Wenner Configuration Geoelectric method to identify shallow groundwater on Jalan Matoa Raya Sidomulyo Barat with coordinates N 0˚26'30,19214 '' and E 101˚24'20,3602 ''. This research was taken by the Wenner Configuration Geoelectric method because this method can determine surface groundwater with 2 trajectories used with a path length of 100 meters and a space between the electrodes of 4 meters on each path. The results showed that from the two different routes on Jalan Matoa Raya the resistivity value of 360Ωm-719Ωm was a layer of sand and gravel. Resistivity 826Ωm-1711Ωm is a layer of sand and sandstone. Resistivity 1898Ωm-4839Ωm is a layer of dry gravel and clay or marl. The overall resistivity value ranges from 360Ωm - 4839Ωm at line 1 in this path there is no groundwater found. In line 2 the resistivity value varies from 243Ωm to 7769Ωm. Resistivity 243Ωm-770Ωm is the layer of groundwater and gravel. Resistivity 834Ωm-2083Ωm is a layer of sand and clay or marl. The resistivity of 2862Ωm-7769Ωm is a layer of dry sandstone and gravel, on this track there is groundwater. The water quality test based on pH parameters shows that the water is acidic (pH
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