CD Skripsi
Zona Pencemaran Air Bawah Tanah Di Sekitar Jalan Budi Daya Kelurahan Tuah Karya Kota Pekanbaru Dengan Menggunakan Metode Geolistrik Konfigurasi Wenner Dan Geokimia
Wenner configuration geoelectricity was used to delineate subsurface structures and establish the depth, distribution, and lithologic characteristics that affect groundwater flow. Geochemistry was a method used to determine the quality of underground water. Based on the results of geoelectric data processing, the subsurface depth reaches 12.4 meters. The lithology of the study area consists of layers of groundwater, clay, dry gravel, limestone, sandstone, basalt, granite, and quartz. The results of geochemical data processing, by measuring water parameters, the pH value is in the range of 4.25 to 6.75 ph, for TDS values ranging from 17 mg/L to 148 mg/L, for conductivity values ranging from 15 µmhos/cm to 55 µmhos/cm and turbidity values are in the range of 0.09 NTU to 2.26 NTU. It can be concluded that from the comparison results of parameter tests and quality standard thresholds that are recommended for consumption by residents if studied based on TDS and Turbidity parameters, while if studied based on pH and Conductivity parameters there are only a few residents' well water that is suitable for consumption. When examined from all the parameters that have been tested, the water that is suitable for consumption is in sample 3B (pH 6.53, TDS 101 mg/L, Conductivity 55 µmhos/cm, and Turbidity 1.41 NTU).
Keywords: Geoelectric, Geochemical, Wenner, Quality, Underground Water.
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