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Use este identificador para citar ou linkar para este item: https://ri.ufs.br/jspui/handle/riufs/21389
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Campo DCValorIdioma
dc.contributor.authorCampos, Simara Santos-
dc.contributor.authorAlmeida, Geângela Menezes-
dc.contributor.authorCardoso, Leandro Xavier-
dc.contributor.authorLima, Leonardo Lelis de-
dc.contributor.authorA., Carlos-
dc.contributor.authorSouza, Susana Oliveira de-
dc.date.accessioned2025-03-19T19:56:50Z-
dc.date.available2025-03-19T19:56:50Z-
dc.date.issued2010-
dc.identifier.citationCAMPOS, S. S. et al. Thermoluminescent dose reconstruction using quartz extracted from unfired buildings. Journal of Physics: Conference Series, v. 249, 2010. Trabalho apresentado em 16º International Conference on Defects in Insulating Materials, 2008, [Aracaju]. Disponível em: https://iopscience.iop.org/article/10.1088/1742-6596/249/1/012031/pdf. Acesso em: 19 mar. 2025.pt_BR
dc.identifier.issn1742-6596-
dc.identifier.issn1742-6588-
dc.identifier.urihttps://ri.ufs.br/jspui/handle/riufs/21389-
dc.languageengpt_BR
dc.publisherIOP Publishingpt_BR
dc.relation.ispartofJournal of Physics: Conference Seriespt_BR
dc.subjectThermoluminescenceeng
dc.subjectQuartzeng
dc.subjectKinetic parameterseng
dc.subjectRetrospective dosimetryeng
dc.titleThermoluminescent dose reconstruction using quartz extracted from unfired buildingspt_BR
dc.typeTrabalhos em Eventospt_BR
dc.identifier.licenseCreative Commons Atribuição 4.0 Internacional (CC BY 4.0)pt_BR
dc.description.resumoThe use of thermoluminescence (TL) is very useful for application in retrospective dosimetry, that is, for inference of the dose of radiation undergone for some material. The calculation of the lifetime of TL peaks can help to clarify which TL intensity is due to the dose of environmental radiation and which is proceeding from the accident with radiation. In this work, the kinetic order (b), activation energy (Et) and the frequency factor (s) were obtained for quartz samples that had been extracted from unfired buldings. It was observed the occurrence of peaks in the 150 ºC – 250 ºC range, that corresponds to a range commonly used in retrospective dosimetry, due to its shorter lifetime when compared with TL geological signal. The analysis of the peaks was done through several well known methods, namely the peak shape (PS), curve fitting (CF) and heating rate (HR) methods. To confirm the structure of the sample, additional X-ray diffraction was made.pt_BR
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