1993
DOI: 10.1007/bf02546561
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The α-β inversion in submilligram particles of natural quartz

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Cited by 4 publications
(3 citation statements)
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“…In the second stage (300-750°C, a minimum at 516.6°C), the mass loss of 3.8% corresponds to the dehydroxylation of the clay and the thermal polymorph transition (a ? b) of quartz [42,43].…”
Section: Thermal Characterization Of Sorption Productsmentioning
confidence: 99%
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“…In the second stage (300-750°C, a minimum at 516.6°C), the mass loss of 3.8% corresponds to the dehydroxylation of the clay and the thermal polymorph transition (a ? b) of quartz [42,43].…”
Section: Thermal Characterization Of Sorption Productsmentioning
confidence: 99%
“…6. The peaks originating from the -CH 3 radical (M/Z = 15), amines (43), -N(CH 3 ) 2-CH 2 (58), and CH 3 Br(58), appearing in the region between 200 and 450°C, provide evidence for the defragmentation of surfactant molecules [45][46][47] Ion Current/A HDTMA(0.01)-P(V)- (44), and NO 2 (46) represent surfactant oxidation, which proceeds in two steps, between 200 and 400°C and between 400 and 800°C. The first step regards the surfactant sorbed on the mineral surface via electrostatic and covalent forces, whereas the second one relates to the surfactant present in the interior of the mineral structure, bound by electrostatic forces.…”
Section: Thermal Characterization Of Sorption Productsmentioning
confidence: 99%
“…Quartz undergoes crystalline transition at 573 °C and 870 °C and both alters the volume of quartz. At 573 °C α-quartz form undergoes structural change to β-quartz with associated 5% volume expansion, whereas at 870 °C β-quartz form changes to β-squamous quartz with a 12 % volume expansion (Balitsky et al, 1996;Moore, 1993). Due to a difference of the expansion rate between impurity and quartz, the rapid change in temperature can cause a large number of cracks at the junction of impurity and quartz matrix.…”
Section: Advanced Purification Of Industrial Quartz Using Calcinationmentioning
confidence: 99%