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Subsurface Profile Analysis for Aquifer Layer Identification: Analisis Profil Bawah Permukaan untuk Identifikasi Lapisan Pembawa Air

JURNAL GEOCELEBES · Vol. 6 No. 2 (2022) · pp. 194–202

DOI
10.20956/geocelebes.v6i2.21911
ISSN
2579-5546, 2579-5821
Published
2022-10-31
Publisher
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Language
en

Abstract

Bungaiya village is a village located in Gowa Regency which has volcanic rock lithology with one of the problems faced in volcanic rocks is that the rock porosity is small so that this layer cannot be an aquifer zone. But the water needs needed by the community for agriculture are very large. Geoelectric is a geophysical method that can be used to describe subsurface profiles, especially aquifer layers. The purpose of this study is to interpret using the geoelectric resistivity method, is the Wenner configuration method as many as 2 lines with a length of 470 m and a space of 10 m. The interpretation results on Line 1, there are 3 layers, are volcanic breccia with resistivity values ​​of 85.6 – 2.2013.19 Ωm and depths between 1.2 – 68 m, layer 2 of tuff with resistivity values ​​of 9.82 – 59.68 Ωm, depth of 12 – 76 m and the third layer is a volcanic breccia, resistivity value is 85.6 – 176 Ωm. Line 2 has 2 layers, are the first layer with a depth of 1.2 – 42 m with a resistivity value of 93 – 490.41 Ωm which is a volcanic breccia. The second layer at a depth of 1.2 – 78.8 m with a resistivity value of 30.9 – 77, 67 Ωm is tuff. Layers 1 and 2 show a similar subsurface profile. Based on these results, it can be concluded that the layer that functions as a water-carrying layer is tuff with a resistivity value of 9.82 – 77.67 Ωm.

Keywords

Collaboration network of the authors

40 authors · 139 co-authorship links · 11 across different organisations · showing the 40 most connected

Hover or tap a name to highlight its co-authors. Double-click to open the author's page.

  • Tadulako University
  • Universitas Halu Oleo
  • Universitas Balikpapan
  • Institut Teknologi dan Sains Mandala
  • Universitas Muhammadiyah Prof Dr Hamka
  • Universitas Raharja
  • Universitas Syiah Kuala
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Abdul WahidInstitut Teknologi dan Sains Mandala3
Andi AmriUniversitas Muhammadiyah Prof Dr Hamka2
Muhammad Dalvi MustafaAffiliation unknown2
Andi Adri AriefAffiliation unknown2
Sitti FakhriyyahAffiliation unknown2
Mardiana E. FachryAffiliation unknown2
M. Chasyim HasaniAffiliation unknown2
Jamaluddin JamaluddinAffiliation unknown2
Argitha Jessica PutriUniversitas Balikpapan1
Bambang SardiTadulako University1
Moh Ghifta HentuTadulako University1
Anti A JakariaTadulako University1
Nur Anisa KarimTadulako University1
Auliandari AuliandariTadulako University1
Thazkira AuliaTadulako University1
Sari ZulhijaTadulako University1
Fidya Tri WulandariTadulako University1
Nur AirinTadulako University1
Diva AvicennaTadulako University1
Wulan Mutiara SabaniTadulako University1
Nur AzizahUniversitas Raharja1
Fajar SarananiAffiliation unknown1
Laode SabaruddinUniversitas Halu Oleo1
La BacoAffiliation unknown1
Peribadi PeribadiUniversitas Halu Oleo1
Syaifudin Suhri KasimUniversitas Halu Oleo1
Rety Reka MerlinsAffiliation unknown1
Abdul Rahim Sya’banAffiliation unknown1
Wa Ode Nova Noviyanti RAffiliation unknown1
Andi Mauliana TAffiliation unknown1
Muhammad HasbiUniversitas Syiah Kuala1
Prinob AksarUniversitas Halu Oleo1
Rezki Inta FawaidAffiliation unknown1
Benny Audy Jaya GosariAffiliation unknown1
Febri Yanti PanjaitanAffiliation unknown1
Endah Murpi NingrumAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/geocelebes/oai, first harvested 3 Nov 2026, last seen 3 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en">Subsurface Profile Analysis for Aquifer Layer Identification: Analisis Profil Bawah Permukaan untuk Identifikasi Lapisan Pembawa Air</dc:title>
	<dc:creator xml:lang="en">Bundang, Syarifullah</dc:creator>
	<dc:creator xml:lang="en">Massinai, Muhammad Fawzy Ismullah</dc:creator>
	<dc:creator xml:lang="en">Firman, Firman</dc:creator>
	<dc:creator xml:lang="en">Hidayat, Wahyu</dc:creator>
	<dc:creator xml:lang="id">Bundang, Syarifullah</dc:creator>
	<dc:subject xml:lang="en">aquifers</dc:subject>
	<dc:subject xml:lang="en">geoelectric</dc:subject>
	<dc:subject xml:lang="en">tuff</dc:subject>
	<dc:subject xml:lang="en">volcanic breccia</dc:subject>
	<dc:subject xml:lang="en">Wenner</dc:subject>
	<dc:description xml:lang="en">Bungaiya village is a village located in Gowa Regency which has volcanic rock lithology with one of the problems faced in volcanic rocks is that the rock porosity is small so that this layer cannot be an aquifer zone. But the water needs needed by the community for agriculture are very large. Geoelectric is a geophysical method that can be used to describe subsurface profiles, especially aquifer layers. The purpose of this study is to interpret using the geoelectric resistivity method, is the Wenner configuration method as many as 2 lines with a length of 470 m and a space of 10 m. The interpretation results on Line 1, there are 3 layers, are volcanic breccia with resistivity values ​​of 85.6 – 2.2013.19 Ωm and depths between 1.2 – 68 m, layer 2 of tuff with resistivity values ​​of 9.82 – 59.68 Ωm, depth of 12 – 76 m and the third layer is a volcanic breccia, resistivity value is 85.6 – 176 Ωm. Line 2 has 2 layers, are the first layer with a depth of 1.2 – 42 m with a resistivity value of 93 – 490.41 Ωm which is a volcanic breccia. The second layer at a depth of 1.2 – 78.8 m with a resistivity value of 30.9 – 77, 67 Ωm is tuff. Layers 1 and 2 show a similar subsurface profile. Based on these results, it can be concluded that the layer that functions as a water-carrying layer is tuff with a resistivity value of 9.82 – 77.67 Ωm.</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2022-10-31</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.unhas.ac.id/index.php/geocelebes/article/view/21911</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v6i2.21911</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 6 No. 2: October 2022; 194 – 202</dc:source>
	<dc:source>2579-5546</dc:source>
	<dc:source>2579-5821</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/geocelebes/article/view/21911/8799</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2022 JURNAL GEOCELEBES</dc:rights>
</oai_dc:dc>