Pujomiarto, Dwi Wahyu (2014) Aplikasi metode geolistrik resistivitas konfigurasi Schlumberger untuk mengidentifikasi lapisan akuifer di Desa Slamparejo Kecamatan Jabung Kabupaten Malang / Dwi Wahyu Pujomiarto. Diploma thesis, Universitas Negeri Malang.
Full text not available from this repository.Abstract
Pujomiarto Dwi Wahyu. 2014. Application of Geoelectric Resistivity Method Schlumberger Configuration Using identification Aquifer Layer in the Village District of Jabung Slampangrejo Malang. Thesis Department of Physics Faculty of Mathematics and Natural Science State University of Malang. Advisors (I) Daeng Achmad Suaidi S.Si M.Kom. (II) Sujito S.Pd M.Si. Keywords Geoelectric Schlumberger Configuration Aquifer Resistivity. Village district of Jabung Slampangrejo Malang is a prone area to water shortages. Source of clean water is required to meet the need of local people. Identification of clean water sources by using geoelectrical resistivity method. Geoelectric resistivity method has the advantage to hold a shallow exploration that is not detrimental in its detection. Geoelectric detection was done based on physical properties of rocks against electric current in which each of the different rock types will have different resistivity value. Purpose research is identification aquifer layers for known ground water potential by using schlumberger configuration geoelectric resistivity method sounding type. Identification of aquifer by using schlumberger configuration with 4 tracks Track 1 length of 140 meters the injected current of 20 mA Track 2 length of 160 meters the injected current of 20 mA Track 3 lenght of 150 meters the injected current of 20 60 mA Track 4 length of 210 meters the injected current of 20 120 mA. Based on the result of data processing interpretation of Ip2Win software and geological map show that identificated distribution of aquifer in the village district of Jabung Slamparejo Malang. In track 1 has resistivity value of 18 60 8486 m layer depth of 10 16 meters with types of water in alluvial aquifer. In track 2 has resistivity value of 11.8 16.4 8486 m layer depth of 6.6 13 meters with types of water in alluvial aquifer. In track 4 has resistivity value of 25.1 39.8 8486 m layer depth of 6.5 25 meters with types of water in the alluvial aquifer. The result analysis has been conclusion reseach aquifer layers is not saturated zone it is a not aquifer suppressed. Aquifer layers is not saturated have limit on ground water surface and aquitard of botton laye
| Item Type: | Thesis (Diploma) |
|---|---|
| Subjects: | Q Science > QC Physics |
| Divisions: | Fakultas Matematika dan IPA (FMIPA) > Departemen Fisika (FIS) > S1 Fisika |
| Depositing User: | library UM |
| Date Deposited: | 06 Oct 2014 04:29 |
| Last Modified: | 09 Sep 2014 03:00 |
| URI: | http://repository.um.ac.id/id/eprint/20683 |
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