1976
DOI: 10.1016/0016-7037(76)90162-9
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Thermochemistry of some pyroxenes and related compounds

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Cited by 101 publications
(12 citation statements)
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“…In our previous study [7], we used the same method of hightemperature oxide melt solution calorimetry and determined the enthalpy of formation of the natural magnesian chrysotile asbestos of the composition Mg 3 Si 2 O 5 (OH) 4 : ∆ f, el H 0 (298.15 K) = -4353 ± 17 kJ/mol. This value agrees well with the results obtained from acid (HF) calorimetry (-4364.6 ± 3.3 kJ/mol) [8], as well as with the data calculated from the equilibria for this mineral (-4363.35 kJ/mol [9] and -4358.46 ± 2.50 kJ/mol [10]).…”
Section: Resultsmentioning
confidence: 99%
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“…In our previous study [7], we used the same method of hightemperature oxide melt solution calorimetry and determined the enthalpy of formation of the natural magnesian chrysotile asbestos of the composition Mg 3 Si 2 O 5 (OH) 4 : ∆ f, el H 0 (298.15 K) = -4353 ± 17 kJ/mol. This value agrees well with the results obtained from acid (HF) calorimetry (-4364.6 ± 3.3 kJ/mol) [8], as well as with the data calculated from the equilibria for this mineral (-4363.35 kJ/mol [9] and -4358.46 ± 2.50 kJ/mol [10]).…”
Section: Resultsmentioning
confidence: 99%
“…The corresponding parameters of the Ni 3 Si 2 O 5 (OH) 4 nanotubes synthesized under the same conditions are as follows: length, 10 µ m; outer diameter, 10-15 nm; and inner diameter, 2-3 nm. The dehydration temperatures of the Mg 3 Si 2 O 5 (OH) 4 and Ni 3 Si 2 O 5 (OH) 4 nanotubes are equal to 953 to 993 K, respectively. Table 1 presents the results of the chemical analysis, which was carried out by the analyst L.A. Doronina (Grebenshchikov Institute of Silicate Chemistry, Russian Academy of Sciences, St. Petersburg, Russia).…”
Section: Sample Preparation and Experimental Techniquementioning
confidence: 99%
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“…Maresch and Mottana, 1976;Chopin, 1978). The change in the slope of reaction (1) resulting from the presence of rhodonite instead of pyroxmangite is probably small, because the AS and A V of the rhodonite-pyroxmangite transition is small (Navrotsky and Coons, 1976).…”
Section: Discussionmentioning
confidence: 99%