Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/handle/123456789/8913
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dc.contributor.authorTestasicca, Leonardo Pena-
dc.contributor.authorFrost, Ray Leslie-
dc.contributor.authorRuan, Xiuxiu-
dc.contributor.authorLim, Jéssica-
dc.contributor.authorBelotti, Fernanda Maria-
dc.contributor.authorCipriano, Ricardo Augusto Scholz-
dc.date.accessioned2017-10-10T13:44:57Z-
dc.date.available2017-10-10T13:44:57Z-
dc.date.issued2016-
dc.identifier.citationTESTASICCA, L. P. et al. The application of high-temperature X-ray diffraction and infrared emission spectroscopy to the thermal decomposition of krohnkite. Journal of Thermal Analysis and Calorimetry, v. 126, p. 1089-1095, 2016. Disponível em: <https://link.springer.com/article/10.1007/s10973-016-5644-y>. Acesso em: 25 ago. 2017.pt_BR
dc.identifier.issn1588-2926-
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/8913-
dc.description.abstractHigh-temperature X-ray diffraction and infrared emission spectroscopy have been applied to measure the thermal stability of the sulphate mineral kro¨hnkite Na2Cu(SO4)2 2H2O. Kro¨hnkite shows a low thermal stability. The mineral decomposes into a complex mixture of sulphates below 500 C and sulphides below 650 C, before melting. Broad emission infrared bands at 3350 and 3105 cm-1 are assigned to the stretching vibration of the water units. The intensity of these two bands decreases as the temperature is raised. The intensity of these bands is lost by 250 C. The sharp IES band at 992 cm-1 is assigned to the m1 SO4 2- symmetric stretching vibration. Intensity in this band is lost by 200 C. New IES bands are noted. The important aspect of this work is the use of hightemperature X-ray diffraction to determine the thermal decomposition of a mineral, in this case krohnkite.pt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.subjectKrohnkitept_BR
dc.subjectInfrared emission spectroscopypt_BR
dc.subjectSulphatept_BR
dc.subjectThermal stabilitypt_BR
dc.titleThe application of high-temperature X-ray diffraction and infrared emission spectroscopy to the thermal decomposition of krohnkite.pt_BR
dc.typeArtigo publicado em periodicopt_BR
dc.identifier.uri2https://link.springer.com/article/10.1007/s10973-016-5644-ypt_BR
dc.identifier.doihttps://doi.org/10.1007/s10973-016-5644-y-
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