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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XRD, TEM, and thermal analysis of Arizona Ca-montmorillonites modified with didodecyldimethylammonium bromide.
TL;DR: This work shows that the dialkyl surfactant can be directly intercalated into the montmorillonite without first undergoing Na(+) exchange and indicates that the prepared organoclay is stable to significantly high temperatures.
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Fourier transform infrared spectrometry: a versatile technique for real world samples.
Llewellyn Rintoul,Helen Panayiotou,Serge Kokot,Graeme A. George,Gregory Cash,Ray L. Frost,Thuy Bui,Peter M. Fredericks +7 more
TL;DR: The versatility of FTIR spectrometry was explored by considering a variety of samples drawn from industrial applications, materials science and biomedical research, which included polymeric insulators, bauxite ore, clay, human hair and human skin.
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Raman spectroscopic study of the magnesium carbonate mineral hydromagnesite (Mg5[(CO3)4(OH)2]· 4H2O)
TL;DR: In this article, a combination of Raman and infrared spectroscopy has been used to study the mineral hydromagnesite, which is important for understanding the concept of geosequestration.
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Synthesis and characterisation of clay-supported titania photocatalysts
TL;DR: This study examines the use of laponite, a synthetic smectite, which forms exfoliated silicate layers when dispersed in water, as an inorganic support for titania nanocrystals.
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Thermal decomposition of humboldtine - a high resolution thermogravimetric and hot stage Raman spectroscopic study
Ray L. Frost,Matt L. Weier +1 more
TL;DR: In this paper, three Raman bands were observed at 1470, 1465 and 1432 cm-1 attributed the CO symmetric stretching mode, which supports the concept of multiple iron(II) oxalate phases.