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 mesoporous structure for efficient photocatalysts: Anatase nanocrystals attached to leached clay layers / Microporous Mesoporous Mat.
Xuzhuang Yang,Huaiyong Zhu,Jiangwen Liu,Xueping Gao,Wayde N. Martens,Ray L. Frost,Yuenian Shen,Zhangfu Yuan +7 more
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Raman spectroscopic study of the mixed anion sulphate–arsenate mineral parnauite Cu9[(OH)10|SO4|(AsO4)2]·7H2O
TL;DR: The mixed anion mineral parnauite Cu9[(OH)10|SO4|(AsO4)2]·7H2O has been studied by Raman spectroscopy.
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Raman microscopy at 77 K of natural gypsum CaSO4·2H2O
Jacob Kloprogge,Ray L. Frost +1 more
TL;DR: The effectiveness of low-temperature Raman microscopy in characterizing the changes in gypsum was examined in this paper, where changes observed in the Raman activity and the appearance of a new band in the OH stretching region were correlated to the changes observed for the SO modes in the low frequency region.
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Identification of intracellular calcium oxalate crystals in Chamelaucium uncinatum (Myrtaceae)
Andrew J. Macnish,Donald E. Irving,Daryl C. Joyce,V. Vithanage,A. H. Wearing,Richard I. Webb,Ray L. Frost +6 more
TL;DR: Intracellular inclusions in the pedicel and calyx-tube tissues of Chamelaucium uncinatum Schauer (Myrtaceae) flowers are irregular in shape and crystals shown to be birefringent may function to regulate soluble calcium concentrations in C. unc inatum tissues near sites where calcium is unloaded from the xylem.
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Modification of the Kaolinite Hydroxyl Surfaces through the Application of Pressure and Temperature, Part III
TL;DR: X-ray diffraction shows that some of the layers of kaolinite hydroxyl surfaces are expanded, and it is hypothesized that this expansion occurs at the edges of the crystals due to the intercalation of water.