Physico-chemical and mineralogical changes of lithic xerorthent soils on volcanic rocks under semi-arid ecological conditions

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dc.authoridDemir, Sinan/0000-0002-1119-1186
dc.authoridAlaboz, Pelin/0000-0001-7345-938X
dc.contributor.authorDemir, Sinan
dc.contributor.authorAlaboz, Pelin
dc.contributor.authorDengiz, Orhan
dc.contributor.authorSenol, Huseyin
dc.contributor.authorYilmaz, Kamil
dc.contributor.authorBaskan, Oguz
dc.date.accessioned2024-12-24T19:30:11Z
dc.date.available2024-12-24T19:30:11Z
dc.date.issued2022
dc.departmentSiirt Üniversitesi
dc.description.abstractThis study investigates the mineralogical changes and soil development processes of young soils formed on va-rious bedrocks of volcanic origin under the same land use/land cover and climate conditions. The current study was conducted in Lithic Xerorthent soils formed on tuff, trachybasalt, and trachyandesite bedrock between San-dikli-Suhut districts of Afyonkarahisar. The three soil profiles excavated in the study area were classified in Enti-sols order based on Soil taxonomy. The primary minerals, sanidine and muscovite, and the clay minerals, smec-tite, kaolinite, and illite, were widely determined in three soil profiles which were named Profile I (PI), Profile II (PII), and Profile III (PIII). According to the chemical alteration index (CIA) values, which indicate weathering, the soils formed on the tuff bedrock were slightly weathered (77.04%). The chemical weathering index (CIW) in the soils' surface horizons formed on the trachybasalt and trachyandesite bedrock are classified as non -weathe-ring rocks with 24.43% and 33.88%. Basic cations are found at high levels in the tuff bedrock. The determination of phillipsite, gismondin and calcite minerals is an indication that the mineral content of the bedrock and the bedrocks have a significant effect on soil formation. The relationship between the bedrock and the soil has been revealed. As a result of the study, it was concluded that there were significant differences in their physico-chemical characteristics, weathering rates, and mineralogical properties. However, they were characterized as young soils since they do not contain any subsurface diagnostic horizons on the volcanic bedrock under the same climatic and land use/land cover conditions.
dc.identifier.doi10.15446/esrj.v26n4.96571
dc.identifier.endpage301
dc.identifier.issn1794-6190
dc.identifier.issn2339-3459
dc.identifier.issue4
dc.identifier.scopus2-s2.0-85149499209
dc.identifier.scopusqualityQ3
dc.identifier.startpage291
dc.identifier.urihttps://doi.org/10.15446/esrj.v26n4.96571
dc.identifier.urihttps://hdl.handle.net/20.500.12604/7425
dc.identifier.volume26
dc.identifier.wosWOS:000992820500003
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherUniv Nacional De Colombia
dc.relation.ispartofEarth Sciences Research Journal
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_20241222
dc.subjectVolcanites
dc.subjectWeathering rates
dc.subjectSoil development
dc.subjectLithic Xerorthent
dc.titlePhysico-chemical and mineralogical changes of lithic xerorthent soils on volcanic rocks under semi-arid ecological conditions
dc.title.alternativeCambios físicoquímicos y mineralógicos de suelos xerortentes líticos en rocas volcánicas bajo condiciones ecológicas semiáridas
dc.typeArticle

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