CD Skripsi
Identifikasi Kualitas Dan Potensi Air Bawah Tanah Di Kelurahan Padang Terubuk Kota Pekanbaru Menggunakan Metode Geolistrik Konfigurasi Wenner Dan Geokimia
The Wenner configuration geoelectric method is used to obtain a picture of subsurface structures and determine the depth, distribution, and lithological properties that affect the movement of underground water. Meanwhile, geochemical analysis is carried out to evaluate the quality of underground water in terms of physical and chemical parameters such as pH, electrical conductivity, TDS, and turbidity. The data obtained from the research location was then processed using Microsof excel software to obtain pseudo-resistivity values, while to see cross-sectional results Res2Din software was used. The results of interpretation on the track with a length of 100 meters have a depth of up to 12.4 meters below the surface, groundwater sources are found at depths of 6.28 to 12.4 meters with resistivity values of 10-52.9 Ωm with lithological arrangements of sand, clay, groundwater, silt. Geochemical analysis The results of water suitable for consumption are in sample B with values (pH 6.66, TDS 125 mg / L, conductivity 212 μS / cm and turbidity 3.34 NTU), sample I with values (pH 6.52, TDS 54 mg / L, conductivity 172 μS / cm and turbidity 0.02 NTU), sample K with values (pH 7.88, TDS 102 mg / L, conductivity 240 μS / cm and turbidity 0.27 NTU) and sample M with values (pH 7.47, TDS 51 mg/L, conductivity 92 μS/cm and turbidity 0.05 NTU).
Keywords: Underground water, Geoelectric Method, Wenner Configuration, Geochemistry
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