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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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Thermal decomposition of the natural hydrotalcites carrboydite and hydrohonessite

TL;DR: A combination of high-resolution thermogravimetric analysis coupled with a gas evolution mass spectrometer combined with infrared emission spectroscopy has been used to study the thermal decomposition of two Australian hydrotalcites carrboydite (Ni6Al2(SO4,CO3)(OH)16.4H2O) and hydrohonessite.
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Vibrational spectroscopy of the sorosilicate mineral hemimorphite Zn4(OH)2Si2O7 · H2O

TL;DR: In this paper, the authors used a Libowitzky type formula to assign the Raman spectra of the mineral hemimorphite from different origins to different vibrational properties, such as out-of-plane bending vibrations of the Si2O7 units.
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Raman spectroscopy of the arsenates and sulphates of the tsumcorite mineral group

TL;DR: In this paper, the structure of a selection of arsenate and sulphate based minerals of the======¯¯¯¯tsumcorite group has been studied by the combination of Raman and infrared spectroscopy.
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Changes in the surfaces of adsorbed p-nitrophenol on methyltrioctadecylammonium bromide organoclay - An XRD, TG, and infrared spectroscopic study

TL;DR: In this paper, it is proposed that the p-nitrophenol penetrates the siloxane layer of the clay and bonds through the ditrigonal space of the hexagonal units to the inner OH units.
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The basic copper arsenate minerals olivenite, cornubite, cornwallite, and clinoclase: An infrared emission and Raman spectroscopic study

TL;DR: In this article, the molecular structures of the basic copper arsenate minerals olivenite, cornubite and clinoclase were studied using a combination of infrared emission spectroscopy and Raman Spectroscopy.