Entropy of pure-silica molecular sieves

被引:46
作者
Piccione, PM
Woodfield, BF
Boerio-Goates, J
Navrotsky, A
Davis, ME [1 ]
机构
[1] CALTECH, Pasadena, CA 91125 USA
[2] Brigham Young Univ, Dept Chem & Biochem, Provo, UT 84602 USA
[3] Univ Calif Davis, Thermochem Facil, Dept Chem Engn & Mat Sci, Davis, CA 95616 USA
关键词
D O I
10.1021/jp010491p
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The entropies of a series of pure-silica molecular sieves (structural codes *BEA, FAU, MFI, and MTT) are obtained by calorimetric measurements of low-temperature heat capacity. The third law entropies at 298.15 K are (on the basis of 1 mol of SiO2): *BFA, 44.91 +/- 0.11 J .K-1 mol(-1); FAU, 44.73 +/- 0.11 J .K-1. mol(-1); MFI, 45.05 +/- 0.11 J .K-1 mol(-1); MTT, 45.69 +/- 0.11 J .K-1. mol(-1) while the corresponding entropies of transition from quartz at 298.15 K are *BEA, 3.4 J .K-1. mol(-1): FAU, 3.2 J .K-1 mol(-1); MFI, 3.6 J .K-1. mol(-1); MTT, 4.2 J .K-1 mol(-1). The entropies span a very narrow range at 3.2-4.2 J .K-1 mol(-1) above quartz, despite a factor of 2 difference in molar volume. This confirms that there are no significant entropy barriers to transformations between SiO2 polymorphs. Finally, the Gibbs free energy of transformation with respect to quartz is calculated for eight SiO2 phases and all are found to be within twice the available thermal energy of each other at 298.15 K.
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收藏
页码:6025 / 6030
页数:6
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