1977
DOI: 10.1002/pssa.2210430249
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Induced crystallization of amorphous silicon oxide

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Cited by 4 publications
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“…By contrast, the oxidation of the elemental Si particles began at ≈750 °C in air by the formation of an amorphous and dense SiO 2 scale. [55][56][57][58][59][60][61] The passive oxidation of elemental Si is limited by the inward diffusion of oxygen through the forming SiO 2 scale, exhibiting a parabolic rate at constant temperatures, which increases linearly with a rising temperature. [55] This explains the rapid mass gain of 25 wt% detected up to 1415 °C and the final yield of ≈128 wt% after further annealing at 1415 °C for 5 h in air, corresponding to a conversion of 25 mol% of Si to SiO 2 .…”
Section: Pyrolysis Behavior Of the Yb(2:1) Composite Powdermentioning
confidence: 99%
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“…By contrast, the oxidation of the elemental Si particles began at ≈750 °C in air by the formation of an amorphous and dense SiO 2 scale. [55][56][57][58][59][60][61] The passive oxidation of elemental Si is limited by the inward diffusion of oxygen through the forming SiO 2 scale, exhibiting a parabolic rate at constant temperatures, which increases linearly with a rising temperature. [55] This explains the rapid mass gain of 25 wt% detected up to 1415 °C and the final yield of ≈128 wt% after further annealing at 1415 °C for 5 h in air, corresponding to a conversion of 25 mol% of Si to SiO 2 .…”
Section: Pyrolysis Behavior Of the Yb(2:1) Composite Powdermentioning
confidence: 99%
“…Nevertheless, the oxidation of the Si particles was accompanied by a molar volume expansion by a factor of 2.2, which can partially compensate the shrinkage of the silazane up to 900 °C reducing the porosity. [55][56][57][58][59][60][61] Despite the formation of ytterbium silicate and secondary phases above 1000 °C, no apparent change in the porosity content was measured up to 1100 °C, which remained constant at ≈33 vol%. In this regard, the formation of β-Yb 2 Si 2 O 7 (6.15 g cm −3 ) [67] and I2/a-Yb 2 SiO 5 (7.28 g cm −3 ) [31] phases from Yb 2 O 3 (9.17 g cm −3 ) [31] and SiO 2 (α-cristobalite, 2.33 g cm −3 ) [68] should lead to a volume shrinkage of up to 11.5%, by considering the total volume of Yb 2 O 3 and α-cristobalite before and after the stoichiometric conversion in ytterbium mono-or disilicate.…”
Section: Composition and Microstructure Of The Yb(2:1) Monolithsmentioning
confidence: 99%