Orthophosphates. Part II. The transformations brushite → fluoroapatite and monetite → fluoroapatite in aqueous potassium fluoride solution

E. J. Duff
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引用次数: 34

Abstract

The transformations brushite → fluoroapatite and monetite → fluoroapatite have been investigated at 25 °C in aqueous acidic KF solutions, ca. 10–1M in F–. The transformations involve a first-order uptake of F– by the secondary orthophosphates, followed by a solid-state rearrangement to fluoroapatite with the second-order release of H2PO4–. The ΔGf° for fluoroapatite has been calculated from the brushite → apatite transformation as –1524·1 kcal mol–1, and confirmed by calculation of the ΔGf° value for monetite as –401·1 kcal mol–1. From these results, the ΔGf° values of hydroxyapatite, Ca5OH(PO4)2, Ca3(PO4)2, and Ca(H2PO4)2, and Ca(H2PO4)2,H2O were calculated as –1494·2, –925·1, –677·8, and –729·5 kcal mol–1. The possibility of K substitution for Ca in fluoroapatite is discussed.
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分析。第二部分。在氟化钾水溶液中,电刷石→氟磷灰石和铁云母→氟磷灰石发生转化
在25℃的酸性KF水溶液中,研究了电刷石→氟磷灰石和铁云母→氟磷灰石的转变。转化包括二级正磷酸盐对F -的一级吸收,随后是固体重排为氟磷灰石,二级释放H2PO4 -。由电刷石→磷灰石相变计算出氟磷灰石的ΔGf°为-1524·1 kcal mol-1,通过计算确定了氟磷灰石的ΔGf°为-401·1 kcal mol-1。根据这些结果,计算出羟基磷灰石、Ca5OH(PO4)2、Ca3(PO4)2、Ca(H2PO4)2和Ca(H2PO4)2、H2O的ΔGf°值分别为-1494·2、-925·1、-677·8和-729·5 kcal mol-1。讨论了氟磷灰石中以K取代Ca的可能性。
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