CD Skripsi
Analisa Potensi Air Bawah Tanah Dengan Menggunakan Metode Geolistrik Aturan Werner Dan Geokimia Di Keluarahan Rejosari Tenayan Raya Pekanbaru
The interpretation of groundwater in Rejosari Village, Tenayan Raya, Pekanbaru
City has been carried out using geochemical and geoelectrical methods using Wenner rules.
This study aims to identify aquifer layers, to determine flow patterns, and groundwater
quality. Measurements were carried out on two tracks with a length of 68 meters and 100
meters respectively. Based on the results of data processing, it is known that the groundwater
aquifer layer is at a depth of 5-15 meters below the surface with a resistivity value of 9,42 –
160,40 m. The pattern of groundwater flow in the study area tends to spread and is located at
a certain depth. In track one, the aquifer layer is on the upper surface, while for track 2 the
distribution is to a depth of 18 meters. The lithology of the subsurface layer in this study area
is a layer of peat with a resistivity value of 138,9 – 170,8 m, gravel with a resistivity value of
117,4 – 160,4 and sandstone with a resistivity value of 117,4-170,8 m. The average
groundwater quality testing is obtained in terms of some parameters such as pH, turbidity
and COD with a value of 7,3, 0,53 NTU, and (8-23) mg/L, respectively. Overall, the
results of the water quality test in the research area are suitable for consumption because it is
too alkaline, but it is still safe and suitable for other needs.
Keywords: Geoelectric, Subsoil, Rock Resistivity, Wenner, Water Quality
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