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Mineral Tanah sebagai Indikator Stabilitas Tanah pada Daerah Berlereng: Studi Kasus Tombolopao Kabupaten Gowa

Jurnal Ecosolum · Vol. 7 No. 1 (2018) · pp. 33–37

DOI
10.20956/ecosolum.v7i1.5214
ISSN
2654-430X, 2252-7923
Published
2018-10-11
Publisher
Universitas Hasanuddin
Language
en

Abstract

Soil forming process can influence soil stability, especially on a sloping area, which is currently related to landslides. This research aims to study mineral content in the soil as an indicator to evaluate soil stability in slope area. Soil texture analyzed with hydrometer and soil mineral analyzed with Kerr method. Soil parent rock comes from Tpbv (Tertiary Pliocene Baturape Volcanic) Formation that consists of lava, breccia, tuff, and conglomerate. Soil texture in A horizon dominated with silty clay loam and in B horizon with silty clay. Clay content in A horizon to B horizon increase ranges from 2-6%. Soils mineral have been weathering on the physical and chemical, which caused cracking on minerals lattice and formed clay minerals inside it. The presence of clay minerals between soil mineral particles can cause mutual repulsion force and cause friction particles that triggering the movement of particles in a small scale when soil saturated by water and triggers soil movement (landslide).

Keywords

Collaboration network of the authors

39 authors · 85 co-authorship links

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  • Universitas Halu Oleo
  • 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
Syamsul Arifin LiasAffiliation unknown2
Indriyani BaliAffiliation unknown2
Meutia FaridaAffiliation unknown2
Moh. Junaedy BurhanAffiliation unknown2
Hamid UmarAffiliation unknown2
Nur IkhwanaAffiliation unknown2
Aminuddin Mane KandariUniversitas Halu Oleo1
Ambo AlaAffiliation unknown1
KaimuddinAffiliation unknown1
Masria MasriaAffiliation unknown1
Hazairin ZubairAffiliation unknown1
Burhanuddin RasyidAffiliation unknown1
Hariyati HariyatiAffiliation unknown1
Bachrul IbrahimAffiliation unknown1
Rismaneswati RismaneswatiAffiliation unknown1
Rachmad WunangkoluAffiliation unknown1
Nur IsraAffiliation unknown1
Muhammad Fitrah Khairul AnamiAffiliation unknown1
RismaneswatiAffiliation unknown1
Tania PatandungAffiliation unknown1
Zulkarnain ChairuddinAffiliation unknown1
Pratama PutraAffiliation unknown1
Risma NeswatiAffiliation unknown1
Hasri SulfaniAffiliation unknown1
Muh. JayadiAffiliation unknown1
Fify Nuril AfniAffiliation unknown1
Fhadly S.MAffiliation unknown1
Ahmad Fauzan AdzimaAffiliation unknown1
Muhammad IqbalInstitut Agama Islam Negeri Kendari1
Rohaya LangkokeAffiliation unknown1
Ratna HusainAffiliation unknown1
Meinarni ThamrinAffiliation unknown1
ZaenalAffiliation unknown1
Zulkarnain ChaeruddinAffiliation unknown1
Aulia Luhtfyah AsbarAffiliation 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/ecosolum/oai, first harvested 2 Nov 2026, last seen 2 Nov 2026.
Original metadata (oai_dc) 
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	<dc:title xml:lang="en">Mineral Tanah sebagai Indikator Stabilitas Tanah pada Daerah Berlereng: Studi Kasus Tombolopao Kabupaten Gowa</dc:title>
	<dc:creator xml:lang="en">Ahmad, Asmita</dc:creator>
	<dc:creator xml:lang="en">Lopulisa, Christianto</dc:creator>
	<dc:creator xml:lang="en">Imran,, A.M</dc:creator>
	<dc:creator xml:lang="en">Baja, Sumbangan</dc:creator>
	<dc:subject xml:lang="en">mineral</dc:subject>
	<dc:subject xml:lang="en">slope</dc:subject>
	<dc:subject xml:lang="en">landslide</dc:subject>
	<dc:subject xml:lang="en">clay</dc:subject>
	<dc:description xml:lang="en">Soil forming process can influence soil stability, especially on a sloping area, which is currently related to landslides. This research aims to study mineral content in the soil as an indicator to evaluate soil stability in slope area. Soil texture analyzed with hydrometer and soil mineral analyzed with Kerr method. Soil parent rock comes from Tpbv (Tertiary Pliocene Baturape Volcanic) Formation that consists of lava, breccia, tuff, and conglomerate. Soil texture in A horizon dominated with silty clay loam and in B horizon with silty clay. Clay content in A horizon to B horizon increase ranges from 2-6%. Soils mineral have been weathering on the physical and chemical, which caused cracking on minerals lattice and formed clay minerals inside it. The presence of clay minerals between soil mineral particles can cause mutual repulsion force and cause friction particles that triggering the movement of particles in a small scale when soil saturated by water and triggers soil movement (landslide).</dc:description>
	<dc:publisher xml:lang="en">Universitas Hasanuddin</dc:publisher>
	<dc:date>2018-10-11</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/ecosolum/article/view/5214</dc:identifier>
	<dc:identifier>10.20956/ecosolum.v7i1.5214</dc:identifier>
	<dc:source xml:lang="en">Jurnal Ecosolum; Vol. 7 No. 1 (2018): JUNI; 33-37</dc:source>
	<dc:source>2654-430X</dc:source>
	<dc:source>2252-7923</dc:source>
	<dc:source>10.20956/ecosolum.v7i1</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/ecosolum/article/view/5214/2820</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2018 Jurnal Ecosolum</dc:rights>
</oai_dc:dc>