R
Ray L. Frost
Researcher at Queensland University of Technology
Publications - 1359
Citations - 45933
Ray L. Frost is an academic researcher from Queensland University of Technology. The author has contributed to research in topics: Raman spectroscopy & Infrared spectroscopy. The author has an hindex of 86, co-authored 1356 publications receiving 41053 citations. Previous affiliations of Ray L. Frost include University of Western Sydney & Southwest University of Science and Technology.
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Raman spectroscopy of halogen‐containing carbonates
Ray L. Frost,Marilla J. Dickfos +1 more
TL;DR: Raman spectra of carbonates from different origins including bastnasite, parisite and northupite have been used to study a series of selected natural halogenated carbonates as discussed by the authors.
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Raman spectroscopy and characterisation of α-gallium oxyhydroxide and β-gallium oxide nanorods
Yanyan Zhao,Ray L. Frost +1 more
TL;DR: Raman spectroscopy was used to characterize both gallium oxyhydroxide (α-GaO(OH)) and gallium oxide (β-Ga2O3) nanorods synthesised with and without the surfactants using a soft chemical methodology at low temperatures.
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Purity evaluation of carbon nanotube materials by thermogravimetric, TEM, and SEM methods.
João Paulo C. Trigueiro,Glaura G. Silva,Rodrigo L. Lavall,Clascídia A. Furtado,Sergio C. Oliveira,Andre S. Ferlauto,Rodrigo G. Lacerda,Luiz Orlando Ladeira,Jiangwen Liu,Ray L. Frost,Graeme A. George +10 more
TL;DR: In this paper, the authors applied conventional and high resolution thermogravimetry to quantify different fractions of carbonaceous and metallic materials in raw and moderately purified single walled and multiwalled carbon nanotubes.
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The effect of varying synthesis conditions on zinc chromium hydrotalcite: a spectroscopic study
TL;DR: In this article, Zn/Cr hydrotalcites were synthesised by coprecipitation, with varying pH values and divalent/trivalent metal ion ratio.
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Infrared and infrared emission spectroscopic study of typical Chinese kaolinite and halloysite.
TL;DR: The infrared emission spectra of halloysite were found to be considerably different to that of kaolinite at lower temperatures, attributed to the fundamental difference in the structure of the two minerals.