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Volume 10 Issue 4
Dec.  2022
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Article Contents
Ertekin C, Ulugergerli EU. 2022. Geoelectrical survey over perched aquifers in the northern part of Upper Sakarya River Basin, Türkiye. Journal of Groundwater Science and Engineering, 10(4): 335-352 doi:  10.19637/j.cnki.2305-7068.2022.04.003
Citation: Ertekin C, Ulugergerli EU. 2022. Geoelectrical survey over perched aquifers in the northern part of Upper Sakarya River Basin, Türkiye. Journal of Groundwater Science and Engineering, 10(4): 335-352 doi:  10.19637/j.cnki.2305-7068.2022.04.003

Geoelectrical survey over perched aquifers in the northern part of Upper Sakarya River Basin, Türkiye

doi: 10.19637/j.cnki.2305-7068.2022.04.003
More Information
  • Corresponding author: emin@comu.edu.tr
  • ①TİGEM 2012. Anadolu Tarım İşletmesi Hidrojeolojik ve Jeofizik Etüt Raporu (in Turkish), 73.
  • ②URL1 2019. https://github.com/fatiando (AD 19.11.2019)
  • ③URL2 2019. https://github.com/gimli-org/gimli (AD 19.11.2019)
  • Received Date: 2022-04-06
  • Accepted Date: 2022-09-30
  • Available Online: 2022-12-27
  • Publish Date: 2022-12-31
  • In this study, a groundwater exploration survey was conducted using the DC Resistivity (DCR) method in a hydrogeological setting containing a perched aquifer. DCR data were gathered and an electrical tomography section was recovered using conventional four-electrode instruments with a Schlumberger array and a two-dimensional (2D) inversion scheme. The proposed scheme was tested over a synthetic three-dimensional (3D) subsurface model before deploying it in a field situation. The proposed method indicated that gathering data with simple four-electrode instruments at stations along a line and 2D inversion of datasets at multiple stations can recover depth intervals of the studied aquifer in the hydrogeological setting even if it has a 3D structure. In this study, 2D inversion of parallel profiles formed a pseudo-3D volume of the subsurface resistivity structures and mapped out multiple resistive (>25 ohm·m) bodies at shallow (between 50–100 m) and deep sections (>150 m). In general, the proposed method is convenient to encounter geological units that have limited vertical and spatial extensions in any direction and presents resistivity contrast from groundwater-bearing geologic materials.
  • ①TİGEM 2012. Anadolu Tarım İşletmesi Hidrojeolojik ve Jeofizik Etüt Raporu (in Turkish), 73.
    ②URL1 2019. https://github.com/fatiando (AD 19.11.2019)
    ③URL2 2019. https://github.com/gimli-org/gimli (AD 19.11.2019)
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