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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 Spectroscopic Study of the Mineral Thorikosite Pb3(OH)(SbO3,AsO3)Cl2: A Mineral of Archaeological Significance

TL;DR: In this article, Raman spectra of antimonite-bearing mineral thorikosite Pb3(OH)(SbO3,AsO3)Cl2 were studied and were related to the structure of the mineral.
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Characterisation of Ni carbonate-bearing minerals by UV–Vis–NIR spectroscopy

TL;DR: In this paper, four nickel carbonate-bearing minerals from Australia have been investigated to study the effect of Ni for Mg substitution, and the crystal field stabilization energy (CFSE) of Ni2+ in the four carbonates is calculated from the observed 3A2g (3F) → 3T2g(3F), transition.
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A vibrational spectroscopic study of the phosphate mineral vantasselite Al4(PO4)3(OH)3·9H2O.

TL;DR: In this paper, a combination of SEM with EDX and Raman and infrared spectroscopy was used to study the phosphate mineral vantasselite Al4(PO4)3(OH)3·9H2O.
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Influence of smectite suspension structure on sheet orientation in dry sediments: XRD and AFM applications

TL;DR: Investigation of how smectite clay platelets were oriented on silicon wafer substrate when dried from suspension range of methods like SEM, XRD and AFM concluded that high clay concentrations and larger particle diameters in suspension result in random orientation of platelets in the substrate.
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Raman spectroscopy of potassium acetate‐intercalated kaolinites over the temperature range 25–300,°C

TL;DR: In this article, the Raman spectra of the hydroxyl-stretching region of potassium acetate-intercalated kaolinite were obtained under an atmosphere of both air and nitrogen using a thermal stage over the temperature range 25-300 °C.