IDENTIFIKASI BATUAN PASIR BERDASARKAN METODE GEOLISTRIK RESISTIVITAS 2D KONFIGURASI WENNER-SCHLUMBERGER DI DESA TALANG BALAI BARU II KECAMATAN TANJUNG RAJA KABUPATEN OGAN ILIR

DERLI, DERLI and Sailah, Siti and Jorena, Jorena (2025) IDENTIFIKASI BATUAN PASIR BERDASARKAN METODE GEOLISTRIK RESISTIVITAS 2D KONFIGURASI WENNER-SCHLUMBERGER DI DESA TALANG BALAI BARU II KECAMATAN TANJUNG RAJA KABUPATEN OGAN ILIR. Undergraduate thesis, Siwijaya University.

[thumbnail of RAMA_45201_08021182126017_cover.jpg] Image
RAMA_45201_08021182126017_cover.jpg - Accepted Version
Available under License Creative Commons Public Domain Dedication.

Download (2MB)
[thumbnail of RAMA_45201_08021182126017.pdf] Text
RAMA_45201_08021182126017.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (1MB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_TURNITIN.pdf] Text
RAMA_45201_08021182126017_TURNITIN.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (2MB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_01_front_ref.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_01_front_ref.pdf - Accepted Version
Available under License Creative Commons Public Domain Dedication.

Download (711kB)
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_02.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_02.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (410kB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_03.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_03.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (292kB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_04.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_04.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (339kB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_05.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_05.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (195kB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_06_ref.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_06_ref.pdf - Bibliography
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (225kB) | Request a copy
[thumbnail of RAMA_45201_08021182126017_0020107001_0010056402_07_lamp.pdf] Text
RAMA_45201_08021182126017_0020107001_0010056402_07_lamp.pdf - Accepted Version
Restricted to Repository staff only
Available under License Creative Commons Public Domain Dedication.

Download (638kB) | Request a copy

Abstract

Sand is one of the mineable mineral resources formed through weathering processes, both mechanical and chemical. Ogan Ilir Regency has the potential for sand mining industry due to the presence of the Ogan River. To evaluate the subsurface potential of sand deposits, a geophysical investigation is required, one of which is the geoelectrical method. The 2D resistivity geoelectrical method with Wenner-Schlumberger electrode configuration involves injecting an electric current into the ground through two current electrodes, while the resulting potential difference is measured using two potential electrodes. From the measurements of current and potential difference at two data acquisition points, variations in subsurface resistivity values were obtained for each layer at the measurement sites. Based on the analysis and interpretation of the resistivity data, the subsurface lithology in the study area consists of three main layers: saturated clay, sandy clay, and sandstone. At the first data acquisition site, the dominant sandstone layer is identified at a depth range of 1.50 to 9.60 meters with resistivity values ranging from >33.6 to 3987 Ωm. At the second site, the sandstone layer is predominantly found at depths between 2.78 and 7.20 meters with resistivity values ranging from >24.9 to 361 Ωm. Keywords : Geoelectrical Method, Wenner-Schlumberger, Sand

Item Type: Thesis (Undergraduate)
Uncontrolled Keywords: Metode Geolistrik, Wenner-Schlumberger, Pasir
Subjects: Q Science > QC Physics > QC801-809 Geophysics. Cosmic physics
Divisions: 08-Faculty of Mathematics and Natural Science > 45201-Physics (S1)
Depositing User: Derli Derli
Date Deposited: 28 Jul 2025 06:34
Last Modified: 28 Jul 2025 06:34
URI: http://repository.unsri.ac.id/id/eprint/181198

Actions (login required)

View Item View Item