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dc.contributor.authorChawalit Chankhanthaen_US
dc.contributor.authorPanjawan Thanasuthipitaken_US
dc.contributor.authorPinit Kidkhunthoden_US
dc.date.accessioned2018-09-05T03:15:23Z-
dc.date.available2018-09-05T03:15:23Z-
dc.date.issued2016-12-01en_US
dc.identifier.issn2228835Xen_US
dc.identifier.issn16863933en_US
dc.identifier.other2-s2.0-84994507709en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84994507709&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/56350-
dc.description.abstract© 2016, Walailak University. All rights reserved. Rough green beryls from Madagascar were studied for their gemological characteristics after heat treatment. The conversion of the iron oxidation state after heating was studied using the modern technique of X-ray absorption spectroscopy. The X-ray absorption near edge spectroscopy (XANES) results are in conclusively agreement with the traditional Ultraviolet-visible-near infrared (UV-Vis-NIR) technique, where Fe3+in an octahedral site is changed into Fe2+after heat treatment. The undesirable yellow tinge in the stone, therefore, is expelled and, thus, an attractive blue color is developed. The green beryls contained moderate amounts of chromophore iron (up to 1.08 wt.% FeO (total)), and relatively low amounts of Cs and Na. Fourier transform infrared (FTIR) spectroscopic features and chemical analyses are consistent with alkali-poor beryl. The gemological characterization of Malagasy green beryl is also presented in detail.en_US
dc.subjectMultidisciplinaryen_US
dc.titleIron K-edge xanes study of heated green beryl from Madagascaren_US
dc.typeJournalen_US
article.title.sourcetitleWalailak Journal of Science and Technologyen_US
article.volume13en_US
article.stream.affiliationsThailand Ministry of Industryen_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsSynchrotron Light Research Institute (Public Organization)en_US
Appears in Collections:CMUL: Journal Articles

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