The Relationship of the Change in Hydrogeochemical Features and Lithium Values of Kızılırmak Basin (Nevsehir-Central Anatolia) Water with Tectonic Fields

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dc.contributor.authorDemircioğlu, Ramazan
dc.contributor.authorElhatip, Hatim
dc.date.accessioned2025-04-11T07:08:58Z
dc.date.available2025-04-11T07:08:58Z
dc.date.issued2024
dc.departmentSağlık Bilimleri Fakültesi
dc.description.abstractIn this study, in particular, the relationship between high lithium values and geological environments was examined. To determine this, the geology, structural geology, hydrogeology, and hydrogeochemistry of the area in the north of the Gülşehir-Yeşilöz sub-basin of the Kızılırmak Basin were investigated. For hydrogeological studies, 19 water samples were collected in May and September. Tectonically, this area has a horst-graben structure. The relationships between the water analysis values of the study area and the tectonic areas were investigated. In particular, the lithium content of the waters in the study area was investigated. Hydrogeochemical properties and seasonal changes in water resources were studied in detail, and their relationship with tectonic areas was evaluated. Water analyses were carried out during wet and dry periods to determine temporal hydrogeochemical changes. According to the analysis, the waters in the area are of Ca-HCO3 and Ca-Mg-HCO3 facies. In addition, there are water samples with high lithium content in the study area. IDW and Kernel diagrams of these were prepared. It was found that these high values were influenced by the rocks formed in the ancient sea and saline lake environments. The region with the highest lithium value is in the formations that represent the former salt lake environment. High lithium (Li) values are generally higher in the region within the Kızılırmak graben. Lithium values in this area were determined as 241.3 µg/L, 154.5 µg/L, 155.2 µg/L, 156.8 µg/L, and 155.6 µg/L.
dc.identifier.doi10.46544/AMS.v29i2.11
dc.identifier.endpage383
dc.identifier.issn13351788
dc.identifier.issue2
dc.identifier.scopus2-s2.0-85207828644
dc.identifier.scopusqualityQ2
dc.identifier.startpage367
dc.identifier.urihttps://dx.doi.org/10.46544/AMS.v29i2.11
dc.identifier.urihttps://hdl.handle.net/20.500.12451/13008
dc.identifier.volume29
dc.identifier.wos001362055200011
dc.identifier.wosqualityQ2
dc.indekslendigikaynakScopus
dc.indekslendigikaynakWeb of Science
dc.institutionauthorDemircioğlu, Ramazan
dc.institutionauthorElhatip, Hatim
dc.language.isoen
dc.publisherTechnical University of Kosice
dc.relation.ispartofActa Montanistica Slovaca
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectHydrogeology
dc.subjectLithium
dc.subjectSalt Lake
dc.subjectWater Analyses
dc.titleThe Relationship of the Change in Hydrogeochemical Features and Lithium Values of Kızılırmak Basin (Nevsehir-Central Anatolia) Water with Tectonic Fields
dc.typeArticle

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