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Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu

Received: 27 July 2019     Accepted: 24 August 2019     Published: 16 September 2019
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Abstract

Background: The condition of the land in Kawatuna Sub-district is dry, with vegetation overgrown only with shrubs. Dry land condition makes people difficult to get clean water sources for their daily needs. Purpose: This research aims to find out the existence of an aquifer and the depth of the aquifer in Kawatuna Sub-district. Method: The method used in this research is Vertical Electrikal Soundin (VES) with Sclumberger Configuration. The measurement is conducted on 10 measuring points. Data is processed using IP2WIN. Result: The result shown by the program is in the form of distribution of resistivity(ρ), thickness (h), and depth (d) of each subsurface layer. Aquifer layer is shown by the resistivity value of 32.15Ωm-48.03 Ωm and formation factor value of 2-5. This layer consists of sands, pebbles, and sandstones. The upper limit of this later is in the depth of 50.05-72.75m, while the lower limit is undetectable. Conclusion: Aquifer layer is distributed to the east and to the west. It can be seen from the depth of aquifer in the west which tends to be shallower than that in the east. Commonly, this layer is located below the impermeable clay layer.

Published in American Journal of Water Science and Engineering (Volume 5, Issue 3)
DOI 10.11648/j.ajwse.20190503.11
Page(s) 105-110
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2019. Published by Science Publishing Group

Keywords

Aquifer, Geo-Electric Resistivity, Sclumberge Configuration, Vertical Electrical Sounding (VES)

References
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Cite This Article
  • APA Style

    Muhammad Rusydi, Mohammad Dahlan Tahir Musa, Badaruddin, Yandry Albert Momor, Sandra Sandra, et al. (2019). Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu. American Journal of Water Science and Engineering, 5(3), 105-110. https://doi.org/10.11648/j.ajwse.20190503.11

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    ACS Style

    Muhammad Rusydi; Mohammad Dahlan Tahir Musa; Badaruddin; Yandry Albert Momor; Sandra Sandra, et al. Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu. Am. J. Water Sci. Eng. 2019, 5(3), 105-110. doi: 10.11648/j.ajwse.20190503.11

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    AMA Style

    Muhammad Rusydi, Mohammad Dahlan Tahir Musa, Badaruddin, Yandry Albert Momor, Sandra Sandra, et al. Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu. Am J Water Sci Eng. 2019;5(3):105-110. doi: 10.11648/j.ajwse.20190503.11

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  • @article{10.11648/j.ajwse.20190503.11,
      author = {Muhammad Rusydi and Mohammad Dahlan Tahir Musa and Badaruddin and Yandry Albert Momor and Sandra Sandra and Mauludin Kurniawan and Sitti Rugaya and Rustan Efendi and Rahmawati and Syaiful Hendra and Hajra Rasmita Ngemba},
      title = {Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu},
      journal = {American Journal of Water Science and Engineering},
      volume = {5},
      number = {3},
      pages = {105-110},
      doi = {10.11648/j.ajwse.20190503.11},
      url = {https://doi.org/10.11648/j.ajwse.20190503.11},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajwse.20190503.11},
      abstract = {Background: The condition of the land in Kawatuna Sub-district is dry, with vegetation overgrown only with shrubs. Dry land condition makes people difficult to get clean water sources for their daily needs. Purpose: This research aims to find out the existence of an aquifer and the depth of the aquifer in Kawatuna Sub-district. Method: The method used in this research is Vertical Electrikal Soundin (VES) with Sclumberger Configuration. The measurement is conducted on 10 measuring points. Data is processed using IP2WIN. Result: The result shown by the program is in the form of distribution of resistivity(ρ), thickness (h), and depth (d) of each subsurface layer. Aquifer layer is shown by the resistivity value of 32.15Ωm-48.03 Ωm and formation factor value of 2-5. This layer consists of sands, pebbles, and sandstones. The upper limit of this later is in the depth of 50.05-72.75m, while the lower limit is undetectable. Conclusion: Aquifer layer is distributed to the east and to the west. It can be seen from the depth of aquifer in the west which tends to be shallower than that in the east. Commonly, this layer is located below the impermeable clay layer.},
     year = {2019}
    }
    

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  • TY  - JOUR
    T1  - Mapping of the Distribution of Aquifier in KawatunaSub-district, Mantikulore District, Palu
    AU  - Muhammad Rusydi
    AU  - Mohammad Dahlan Tahir Musa
    AU  - Badaruddin
    AU  - Yandry Albert Momor
    AU  - Sandra Sandra
    AU  - Mauludin Kurniawan
    AU  - Sitti Rugaya
    AU  - Rustan Efendi
    AU  - Rahmawati
    AU  - Syaiful Hendra
    AU  - Hajra Rasmita Ngemba
    Y1  - 2019/09/16
    PY  - 2019
    N1  - https://doi.org/10.11648/j.ajwse.20190503.11
    DO  - 10.11648/j.ajwse.20190503.11
    T2  - American Journal of Water Science and Engineering
    JF  - American Journal of Water Science and Engineering
    JO  - American Journal of Water Science and Engineering
    SP  - 105
    EP  - 110
    PB  - Science Publishing Group
    SN  - 2575-1875
    UR  - https://doi.org/10.11648/j.ajwse.20190503.11
    AB  - Background: The condition of the land in Kawatuna Sub-district is dry, with vegetation overgrown only with shrubs. Dry land condition makes people difficult to get clean water sources for their daily needs. Purpose: This research aims to find out the existence of an aquifer and the depth of the aquifer in Kawatuna Sub-district. Method: The method used in this research is Vertical Electrikal Soundin (VES) with Sclumberger Configuration. The measurement is conducted on 10 measuring points. Data is processed using IP2WIN. Result: The result shown by the program is in the form of distribution of resistivity(ρ), thickness (h), and depth (d) of each subsurface layer. Aquifer layer is shown by the resistivity value of 32.15Ωm-48.03 Ωm and formation factor value of 2-5. This layer consists of sands, pebbles, and sandstones. The upper limit of this later is in the depth of 50.05-72.75m, while the lower limit is undetectable. Conclusion: Aquifer layer is distributed to the east and to the west. It can be seen from the depth of aquifer in the west which tends to be shallower than that in the east. Commonly, this layer is located below the impermeable clay layer.
    VL  - 5
    IS  - 3
    ER  - 

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Author Information
  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Physics, Tadulako University, Palu, Indonesia

  • Department of Geography Education, Tadulako University, Palu, Indonesia

  • Department of Information Technology, Tadulako University, Palu, Indonesia

  • Department of Information Technology, Tadulako University, Palu, Indonesia

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