作者: H. Catherine , W. Skinner
DOI: 10.1016/0025-5408(70)90083-8
关键词: Inorganic chemistry 、 Pyrophosphate 、 Dehydration 、 Transition temperature 、 Calcium orthophosphate 、 Ion 、 Chemistry 、 Mechanical engineering 、 General Materials Science 、 Mechanics of Materials 、 Condensed 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.