2009
DOI: 10.1016/j.gca.2009.03.041
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Aluminum speciation, vibrational entropy and short-range order in calcium aluminosilicate glasses

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Cited by 21 publications
(18 citation statements)
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References 25 publications
(51 reference statements)
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“…Spline fits made to these data have been used to derive the smoothed values and thermodynamic functions of Tables II–IV. For silicates, C p is a linear function of composition at low temperature provided that the used components refer to well‐defined structural species, namely cations with fixed anion coordinations 11,24 . In this case, partial molar heat capacities C p,i ° can be considered as being independent of composition, viz where x i is the mole fraction of component i .…”
Section: Resultsmentioning
confidence: 99%
“…Spline fits made to these data have been used to derive the smoothed values and thermodynamic functions of Tables II–IV. For silicates, C p is a linear function of composition at low temperature provided that the used components refer to well‐defined structural species, namely cations with fixed anion coordinations 11,24 . In this case, partial molar heat capacities C p,i ° can be considered as being independent of composition, viz where x i is the mole fraction of component i .…”
Section: Resultsmentioning
confidence: 99%
“…In spite of such experimental differences, the coherence of the results obtained with both kinds of procedures has been noted in a comprehensive study of calcium aluminosilicate glasses. 26 We thus assume that our calculations are not af- fected by significant bias resulting in particular from systematic differences in thermal history and fictive temperature. In binary alkaline earth silicate melts, liquid immiscibility may be a concern.…”
Section: Methodsmentioning
confidence: 99%
“…Table 3 Molar thermodynamic functions of NS 2 Fe red glass. whether Ca 2+ is ''free" or acting as a charge-compensating cation for tetrahedrally coordinated Al 3+ because the coordination of Ca 2+ is about the same in both instances (de Ligny et al, 1996;Richet et al, 2009). But for Na 2 O different entropy values of 85 and 96.7 J/mol K were derived depending on whether Na + is ''free" or charge-compensating tetrahedral Al 3+ , respectively, the difference resulting from the large increase in coordination number from about 5 to about 9 induced by the association of sodium with aluminum (Richet et al, 1993).…”
Section: Discussionmentioning
confidence: 99%
“…For Al 2 O 3 we have used the value of 69.1 J/mol K derived from entropies of alkali and alkaline earth aluminosilicate glasses (Richet et al, 1993). For calcium aluminosilicates, this figure actually represents the weighted average of the values for Al 2 O 3 components in which Al is in four-and five-fold coordination, whose entropies are 72.8 and 48.5 J/mol K, respectively (Richet et al, 2009). Interestingly, fits made with the 72.8 J/mol K derived for IV Al 2 O 3 yield entropies that are too high compared to those obtained from the data of Table 6.…”
Section: Discussionmentioning
confidence: 99%