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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Thermal decomposition of hydrotalcite with molybdate and vanadate anions in the interlayer
TL;DR: In this article, carbonate hydrotalcites containing carbonate, vanadate, and molybdate were prepared by coprecipitation and the resulting materials were characterized by XRD, and TG/DTA to determine the stability of the synthesized synthesized.
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Raman spectroscopy of selected borate minerals of the pinakiolité group
TL;DR: In this paper, the Raman spectra of a series of related minerals of the pinakiolite group have been collected and the spectra related to the mineral structure are assigned to the ν1 BO33− symmetric stretching mode.
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Vibrational spectroscopy of formamide-intercalated kaolinites
TL;DR: The vibrational spectroscopy of low and high defect kaolinites fully and partially intercalated with formamide have been determined using a combination of X-ray diffraction, DRIFT and Raman spectroscopic.
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A Raman spectroscopic study of the uranyl sulphate mineral johannite.
TL;DR: Raman spectroscopy can contribute significant knowledge in the study of uranyl minerals because of better band separation with significantly narrower bands, avoiding the complex spectral profiles as observed with infrared spectroscopic.
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Infrared spectroscopic study of potassium and cesium acetate-intercalated kaolinites
TL;DR: In this paper, three near-IR spectral regions are identified: (a) the high frequency region between 6400 and 7400 cm−1 attributed to the first overtone of the hydroxyl stretching mode, (b) the 4800-5400 cm− 1 region attributed to water combination modes and (c) the 4000-4800 cm −1 region attributed by the combination of the stretching and deformation modes of the AlOH units of the kaolinite.