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Susceptibility of the Surrounding Soil and Rock by the Electrical Resistivity Method

JURNAL GEOCELEBES · Vol. 7 No. 1 (2023) · pp. 29–36

DOI
10.20956/geocelebes.v7i1.23889
ISSN
2579-5546, 2579-5821
Published
2023-02-14
Publisher
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Language
en

Abstract

The research area is located in Banga, Soppeng Regency, South Sulawesi Province. The purpose and intent of this research is to determine the resistivity value of the material layer, identify the characteristics of the slip plane and its relationship to the plasticity properties and the characteristics of the clay minerals contained in the soil. The method used to collect field data includes surface geological data and subsurface geology, which are the electrical resistivity data and surface soil data, then interpreted by combining topographiccross-sectional data and subsurface geoelectrical data along the measurement path. The first slip plane is curved as well as the second slip plane is the residual soil resulting from weathering of limestone which is still above the less dense and thick parent rock (in situ). The geochemistry of the soil samples showed that the mineral content in each layer had the largest percentage of illite 54.4% - 69.9%, and montmorillonite 6.1% - 13.6%, these two clay minerals have large shrinkage properties. Plasticity Index 29.8% - 35.8%, causing vulnerability to the soil, so that the mass movement on the sliding plane is moderate and active in slow motion. The mass movement in the slip plane can be categorized into creep type.

Keywords

Collaboration network of the authors

25 authors · 48 co-authorship links

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

  • University of Mataram
  • Institut Agama Islam Negeri Kendari
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Busthan AzikinAffiliation unknown3
Agung Budi MuljonoUniversity of Mataram1
I Made GinarsaUniversity of Mataram1
I Made Ari NrarthaUniversity of Mataram1
Sabar NababanUniversity of Mataram1
La RiandaAffiliation unknown1
Dhian HerdhiansyahAffiliation unknown1
Muhammad Faturrachman SY.Affiliation unknown1
Regina AprialniAffiliation unknown1
Lutfi Fadhel MubaraqAffiliation unknown1
Suryanto ArifinAffiliation unknown1
Nurmiati NurmatiAffiliation unknown1
Mansyur RadjabAffiliation unknown1
Nurfadilla NurfadillaAffiliation unknown1
Ibriza SabrinaAffiliation unknown1
Kezia PatasikAffiliation unknown1
Erin Savitri GawingAffiliation unknown1
Sri IndriatiAffiliation unknown1
Muhammad IqbalInstitut Agama Islam Negeri Kendari1
Asmita AhmadAffiliation unknown1
Rohaya LangkokeAffiliation unknown1
Meinarni ThamrinAffiliation unknown1
Syarifullah BundangAffiliation 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">Susceptibility of the Surrounding Soil and Rock by the Electrical Resistivity Method</dc:title>
	<dc:creator xml:lang="en">Husain, Ratna</dc:creator>
	<dc:creator xml:lang="en">Sultan, Sultan</dc:creator>
	<dc:subject xml:lang="en">plasticity index</dc:subject>
	<dc:subject xml:lang="en">resistivity</dc:subject>
	<dc:subject xml:lang="en">slip plan</dc:subject>
	<dc:subject xml:lang="en">XRD</dc:subject>
	<dc:description xml:lang="en">The research area is located in Banga, Soppeng Regency, South Sulawesi Province. The purpose and intent of this research is to determine the resistivity value of the material layer, identify the characteristics of the slip plane and its relationship to the plasticity properties and the characteristics of the clay minerals contained in the soil. The method used to collect field data includes surface geological data and subsurface geology, which are the electrical resistivity data and surface soil data, then interpreted by combining topographiccross-sectional data and subsurface geoelectrical data along the measurement path. The first slip plane is curved as well as the second slip plane is the residual soil resulting from weathering of limestone which is still above the less dense and thick parent rock (in situ). The geochemistry of the soil samples showed that the mineral content in each layer had the largest percentage of illite 54.4% - 69.9%, and montmorillonite 6.1% - 13.6%, these two clay minerals have large shrinkage properties. Plasticity Index 29.8% - 35.8%, causing vulnerability to the soil, so that the mass movement on the sliding plane is moderate and active in slow motion. The mass movement in the slip plane can be categorized into creep type.</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2023-02-14</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/23889</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v7i1.23889</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 7 No. 1: April 2023; 29-36</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/23889/9323</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2023 JURNAL GEOCELEBES</dc:rights>
</oai_dc:dc>