Comprehensive Inorganic Chemistry II 2013
DOI: 10.1016/b978-0-08-097774-4.00731-2
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Cited by 28 publications
(18 citation statements)
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“…Pore formation is likely a consequence of the molar volume change accompanying the reaction. That is, the molar volume of amorphous C is 8.01 cm 3 /mol (based on a mass density of 1.50 g/cm 3 ) 12 while those of Si and β‐SiC are 12.06 and 12.50 cm 3 /mol, respectively. Therefore, reaction of 1 cm 3 of amorphous C with the equivalent molar amount of Si (1.51 cm 3 ) yields 1.56 cm 3 of SiC, a contraction of 38% relative to the combined volume of the reactants (a similar scenario is expected for graphitic C, where the reaction involves a volume contraction of ~27%.…”
Section: Discussionmentioning
confidence: 99%
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“…Pore formation is likely a consequence of the molar volume change accompanying the reaction. That is, the molar volume of amorphous C is 8.01 cm 3 /mol (based on a mass density of 1.50 g/cm 3 ) 12 while those of Si and β‐SiC are 12.06 and 12.50 cm 3 /mol, respectively. Therefore, reaction of 1 cm 3 of amorphous C with the equivalent molar amount of Si (1.51 cm 3 ) yields 1.56 cm 3 of SiC, a contraction of 38% relative to the combined volume of the reactants (a similar scenario is expected for graphitic C, where the reaction involves a volume contraction of ~27%.…”
Section: Discussionmentioning
confidence: 99%
“…Therefore, reaction of 1 cm 3 of amorphous C with the equivalent molar amount of Si (1.51 cm 3 ) yields 1.56 cm 3 of SiC, a contraction of 38% relative to the combined volume of the reactants (a similar scenario is expected for graphitic C, where the reaction involves a volume contraction of ~27%. The difference arises from the difference in density of amorphous C and that of graphite, 12 namely 2.26 g/cm 3 , owing to the highly convoluted turbostratic structure of the former 13 ). The inference is that the volume contraction drives the formation of pores at the surface as C is progressively replaced by SiC.…”
Section: Discussionmentioning
confidence: 99%
“…Molecular sieves are a class of porous materials with very narrow PSDs, which make them useful in gas separation applications wherein species are separated according to their size. [165][166][167][168][169] These materials are derivatives of porous materials such as silicates and zeolites. 166,[170][171] While activated carbons typically have heterogeneous PSDs, if they are synthesised or adapted to change pore entrance dimensions to a single pore size they are known as carbon molecular sieves (CMSs).…”
Section: Carbon Molecular Sievesmentioning
confidence: 99%
“…166,[170][171] While activated carbons typically have heterogeneous PSDs, if they are synthesised or adapted to change pore entrance dimensions to a single pore size they are known as carbon molecular sieves (CMSs). 169,172 Prior to the explosion in ZTC research, templated carbons were often referred to as CMSs, 90 however the term is now restricted to non-templated carbons with narrow PSDs. On an industrial scale, CMSs are typically synthesised by depositing pyrolytic carbon at the mouth of the pores in activated carbons, resulting in uniform pore entrances.…”
Section: Carbon Molecular Sievesmentioning
confidence: 99%
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