DETEKSILAPISAN AIR TANAH DENGAN MENGGUNAKAN METODE GEOLISTRIK KONFIGURASI SCHLUMBERGER DI DESA TAMBUSAI TIMUR ROKAN HULU RIAU
Keywords:
Groundwater, Geoelectrical Method, SchumbergerAbstract
The study has been carried out using Schlumberger configuration geoelectrical method in Tambusai Timur Village. This study aims to detect groundwater as a basis for designing and making boreholes. Data processing is done using software progress. The results showed that the sounding 1 was obtained by groundwater with a type of resistivity value of 35 Ωm at a depth of 12-29 meters. This layer is thought to be associated with the sandy clay layer. Sounding 2 is found at a depth of 5-9 meters, with a type of resistance value of 2 Ωm. Sounding 3 layers of groundwater were found at a depth of 28-45 meters, with a type of resistivity value of 2.24 ,m. This layer is assumed to be associated with sand. Of the three sounding points, sounding 1 and sounding 2 are the most potential layers containing ground water.References
Sharma, P.V. 1997. Environmental and Engineering Geophysics. Cambridge University Press, United Kingdom
Sheriff, R E., 2002, “Encyclopedic Dictionary of Applied Geophysics, 4th edition“, SEG Tulsa, Oklahoma.
Sutarno, D. 1993. Metoda Magnetotellurik, Teori, dan Aplikasinya. J. Kontribusi Fisika. 4: 333-352.
Telford, W.M., L.P. Geldart, R.E. Sheriff, & D.A. Keys 1998. Applied Geophysics.Edisi 1.Cambridge University Press. Cambridge.
Telford, W. M., Geldart, L. P. and Sheriff, R. E., 1990, “Applied Geophysics, Second Edition“, Cambridge University Press, United State of America.
Tipler, P.A. 1996. Fisika untuk Sains dan Teknik.Jilid 2. Edisi Ketiga. Erlangga, Jakarta.
Todd, 1980. Ground Water Hydrokoi. Second Edition, Jhon wiley & Sons. New york
