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 in | Russian journal of inorganic chemistry Vol. 59; no. 11; pp. 1219 - 1227 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Moscow
Pleiades Publishing
01.11.2014
|
Subjects | |
Online Access | Get full text |
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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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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0036-0236 1531-8613 |
DOI: | 10.1134/S0036023614110084 |