Proceedings of the 4th International Seminar on Science and Technology (ISST 2022)

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Determination of Aquifer System Using Resistivity Method in Pekalongan City and Surrounding Areas, Central Java, Indonesia

Authors
Meitharisha F. Hasani1, 2, *, Heru Hendrayana1, Ahmad Taufiq2
1Geological Engineering Department, Universitas Gadjah Mada, Yogyakarta, Indonesia
2Ministry of Public Works and Housing, Jakarta, Indonesia
*Corresponding author. Email: meitharishafakhdiyarhasani@mail.ugm.ac.id
Corresponding Author
Meitharisha F. Hasani
Available Online 22 August 2023.
DOI
10.2991/978-94-6463-228-6_12How to use a DOI?
Keywords
Resistivity Method; Subsurface Lithology; Aquifer System
Abstract

The increasing population growth and rapid development of Pekalongan in recent years have caused an increase in clean water needs that cannot be fulfilled from surface water due to pollution problems, so people prefer to use groundwater. Therefore, it is necessary to determine the aquifer system to know groundwater sustainability in this area. This study investigates subsurface lithology and aquifer layer thickness to determine the aquifer system. The investigation determined the subsurface lithology using the 1 Dimension Electrical Resistivity method with Schlumberger Configuration. Based on the investigation results, the rock layers in the northern part have resistivity values below 3 Ωm and 11–60 Ωm. The value is predicted by the loose and unconsolidated materials derived from the river and coastal deposits, predominantly sand-clay grain-sized. This layer is interpreted as the primary aquifer in the northern part. The other layer in the northern part, with a resistivity value of 3–10 Ωm, is interpreted as sandy clay and acts as an aquiclude. A layer with a resistivity value of 11–60 Ωm in the south is tuff sand. The tuff sand originates from volcanic rock debris and acts as an aquifer. The layer with a resistivity value of 3–10 Ωm is interpreted as a tuff clay. The tuff clay acts as an aquiclude layer. The layer with a resistivity value of more than 60 Ωm is known as the tuff breccia. The layer is an aquitard and base of the aquifer system.

Copyright
© 2023 The Author(s)
Open Access
Open Access This chapter is licensed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/), which permits any noncommercial use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made.

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Volume Title
Proceedings of the 4th International Seminar on Science and Technology (ISST 2022)
Series
Advances in Physics Research
Publication Date
22 August 2023
ISBN
10.2991/978-94-6463-228-6_12
ISSN
2352-541X
DOI
10.2991/978-94-6463-228-6_12How to use a DOI?
Copyright
© 2023 The Author(s)
Open Access
Open Access This chapter is licensed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/), which permits any noncommercial use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made.

Cite this article

risenwbib
TY  - CONF
AU  - Meitharisha F. Hasani
AU  - Heru Hendrayana
AU  - Ahmad Taufiq
PY  - 2023
DA  - 2023/08/22
TI  - Determination of Aquifer System Using Resistivity Method in Pekalongan City and Surrounding Areas, Central Java, Indonesia
BT  - Proceedings of the 4th International Seminar on Science and Technology (ISST 2022)
PB  - Atlantis Press
SP  - 100
EP  - 108
SN  - 2352-541X
UR  - https://doi.org/10.2991/978-94-6463-228-6_12
DO  - 10.2991/978-94-6463-228-6_12
ID  - Hasani2023
ER  -