1983
DOI: 10.1080/0371750x.1983.10822648
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Thermal Decomposition of Vermiculites: Kinetics of Dehydration and Dehydroxylation Processes

Abstract: The thermal decomposition reactions of some homoionic clay minerals, viz. vermiculite, in air in the temperature range 30°-l000°C by thermo-analytical methods are reported. The reaction kinetic of iso· thermal dehydration and dehydroxylation is found to obey first order reaction rate.

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Cited by 3 publications
(3 citation statements)
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“…Dehydroxylation, elimination of water from hydroxyl groups, is an important thermal dissociation reaction among those occurring in the kaolinite group minerals and in natural or synthesized silicate materials [19]. Non-isothermal kinetics of this process, which occurs at temperature quite higher than dehydration due to the presence of stronger hydrogen bonds between the OH groups, was extensively studied for different types of KAOs [18,[20][21][22][23][24][25][26], but little is known about the same process occurring in HNTs where early papers used questionable methods under isothermal conditions [27,28].…”
Section: Introductionmentioning
confidence: 99%
“…Dehydroxylation, elimination of water from hydroxyl groups, is an important thermal dissociation reaction among those occurring in the kaolinite group minerals and in natural or synthesized silicate materials [19]. Non-isothermal kinetics of this process, which occurs at temperature quite higher than dehydration due to the presence of stronger hydrogen bonds between the OH groups, was extensively studied for different types of KAOs [18,[20][21][22][23][24][25][26], but little is known about the same process occurring in HNTs where early papers used questionable methods under isothermal conditions [27,28].…”
Section: Introductionmentioning
confidence: 99%
“…It is also worth noting that the m LOSS,250 °C values of the three friction materials exceed the 7% value, indicating that other constituents of the friction materials over the resins (e.g. rubber, aramid fibre, vermiculite and mica [54,55]) are also degrading.…”
Section: Air Atmospherementioning
confidence: 96%
“…The mass loss can be explained by the degradation of other ingredients present in the friction material mixture, e.g. vermiculite, graphite and coke [54,56,57], which also contribute to the maximum mass loss rate in the case of R6_fm and R7_fm. The mass increase observed above 800 °C is related to the oxidation of metallic constituents present in the friction material like Fe fibres.…”
Section: Friction Materials In Air Atmospherementioning
confidence: 99%