Thermoluminescence studies of calcite conducted by bacterial CaCO3 precipitation in organic soil

dc.contributor.authorToktamış, Hüseyin
dc.contributor.authorHatib, Muhammed
dc.contributor.authorKılıç, H. İbrahim
dc.contributor.authorÇanakçı, Hanifi
dc.contributor.institutionauthorÇanakçı, Hanifi
dc.date.accessioned2022-12-20T11:05:08Z
dc.date.available2022-12-20T11:05:08Z
dc.date.issued2022en_US
dc.departmentHKÜ, Mühendislik Fakültesi, İnşaat Mühendisliği Bölümüen_US
dc.description.abstractIn this study, the thermoluminescence (TL) properties of the calcite conducted by bacterial calcium carbonate (CaCO3) precipitation (BCCP) in organic soils were investigated. The bacterial calcium carbonate (CaCO3) precipitation (BCCP) is a popular technique and has been applied in a variety of civil and geotechnical engineering applications. For example, bacterial calcium carbonate precipitation fills the gaps on the organic ground and makes cementing it with the biological method using bacteria. The study reveals that the calcium carbonate mineral called as calcite has a clear TL glow curve with four main peaks located around 90, 140, 210 and 240 °C, a wide linear dose response region between 140Gy and 2.3 kGy is observed. In addition, a good reusability is seen in the high temperature peaks. The TL glow curve peaks are not affected by reusability. Although the dosimetric peaks at 210 and 240 °C appear to be nearly constant, the TL peak intensities at 90 °C and 140 °C completely faded after 24 and 336 h storage time, respectively. The activation energies (Ea) and frequency factors (s) for peaks at 90 °C, 140 °C, 210 °C and 240 °C were evaluated via variable heating rate (VHR). The activation energy of the peaks in the TL glow curve is lying between 0.57eV and 1.04 eV. © 2022 Elsevier Ltden_US
dc.identifier.citationToktamış, H., Hatib, M., Kılıç, H. İ., Çanakçı, H. (2022). Thermoluminescence studies of calcite conducted by bacterial CaCO3 precipitation in organic soil. Applied Radiation and Isotopes: Cilt, 190, s. 1-8.en_US
dc.identifier.doi10.1016/j.apradiso.2022.110462
dc.identifier.endpage8en_US
dc.identifier.issn09698043
dc.identifier.orcid0000-0002-1392-1701en_US
dc.identifier.pmid36174334
dc.identifier.scopus2-s2.0-85138486282
dc.identifier.scopusqualityQ2
dc.identifier.startpage1en_US
dc.identifier.urihttps://hdl.handle.net/20.500.11782/3004
dc.identifier.urihttps://doi.org/10.1016/j.apradiso.2022.110462
dc.identifier.volume190en_US
dc.identifier.wosWOS:000868625100005
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakPubMed
dc.language.isoen
dc.publisherElsevieren_US
dc.relation.ispartofApplied Radiation and Isotopes
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectthermoluminescenceen_US
dc.subjectcalciteen_US
dc.subjectbacterial calcium carbonate (CaCOen_US
dc.subjectprecipitationen_US
dc.titleThermoluminescence studies of calcite conducted by bacterial CaCO3 precipitation in organic soil
dc.typeArticle

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