Transition of calcium orthophosphate to pyrophosphate at elevated pressures

作者: H. Catherine , W. Skinner

DOI: 10.1016/0025-5408(70)90083-8

关键词: Inorganic chemistryPyrophosphateDehydrationTransition temperatureCalcium orthophosphateIonChemistryMechanical engineeringGeneral Materials ScienceMechanics of MaterialsCondensed matter physics

摘要: The equilibrium transition temperature of 2 CaHPO4 ⇄ Ca2P2O7 + H2O was determined as 322.5 ± 2.5°C. at 2000 bars pressure and 342.5 4000 pressure. monetite dehydration is extremely sluggish due to the large structural change anion groups, orthophosphate (PO4′′′) pyrophosphate (P2O7″″). A stersochemical mechanism suggested based on crystallo-graphic investigations.

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