Phase equilibria in the tricalcium phosphate-mixed calcium sodium (potassium) phosphate systems

Phase equilibria in the quasi-binary sections Ca 3 (PO 4 ) 2 -CaMPO 4 (M = Na, K) are distinguished by high-temperature isomorphism of glaserite-like phases α’-Ca 3 (PO 4 ) 2 and α-CaMPO 4 . The main differences of the Ca 3 (PO 4 ) 2 -CaKPO 4 system from the Ca 3 (PO 4 ) 2 -CaNaPO 4 system are a shi...

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Published inRussian journal of inorganic chemistry Vol. 59; no. 11; pp. 1219 - 1227
Main Authors Evdokimov, P. V., Putlyaev, V. I., Ivanov, V. K., Garshev, A. P., Shatalova, T. B., Orlov, N. K., Klimashina, E. S., Safronova, T. V.
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.11.2014
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Summary:Phase equilibria in the quasi-binary sections Ca 3 (PO 4 ) 2 -CaMPO 4 (M = Na, K) are distinguished by high-temperature isomorphism of glaserite-like phases α’-Ca 3 (PO 4 ) 2 and α-CaMPO 4 . The main differences of the Ca 3 (PO 4 ) 2 -CaKPO 4 system from the Ca 3 (PO 4 ) 2 -CaNaPO 4 system are a shift of invariant equilibria toward higher temperatures, deceleration of phase transformations, and the emergence of polymorphism of an intermediate phase of an ordered solid solution based on α-CaKPO 4 . The low-temperature modification of this phase of a composition near Ca 8 K 2 (PO 4 ) 6 has the apatite structure with unoccupied hexagonal channels.
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content type line 23
ISSN:0036-0236
1531-8613
DOI:10.1134/S0036023614110084