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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A Raman Spectroscopic Study of the Uranyl Selenite Mineral Haynesite
TL;DR: In this paper, the position of the antisymmetric stretching vibration occurs at lower wavenumbers than the symmetric stretching mode of the (UO2)2+ and (SeO3)2-2-units respectively.
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A Raman spectroscopic study of the uranyl phosphate mineral parsonsite
TL;DR: In this article, the UO bond lengths in uranyl were calculated from the Raman and infrared spectra, which were in agreement with those from the available X-ray single crystal structure analysis of parsonsite.
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The effect of mechanochemical activation upon the intercalation of a high-defect kaolinite with formamide
TL;DR: The effect of mechanochemical activation upon the intercalation of formamide into a high-defect kaolinite has been studied using a combination of X-ray diffraction, thermal analysis, and DRIFT spectroscopy to reduce the capacity of the Kaolinite to be intercalated with formamide.
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Thermal behavior and decomposition of kaolinite–potassium acetate intercalation composite
TL;DR: In this paper, a series of kaolinite-potassium acetate intercalation composite was prepared and the thermal behavior and decomposition of these composites were investigated by simultaneous differential scanning calorimetry-thermogravimetric analysis (DSC-TGA), X-ray diffraction (XRD) and Fourier-transformation infrared (FT-IR).
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Thermal decomposition of jarosites of potassium, sodium and lead
TL;DR: In this paper, the authors used thermal analysis coupled with mass spectrometry to study three Australian jarosites which are predominantly K, Na and Pb, and found that the first mass loss step for Na-jarosite is attributed to deprotonation.