Premium
Low‐Temperature Formation of Aluminum Orthophosphate
Author(s) -
Bothe James V.,
Brown Paul W.
Publication year - 1993
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1151-2916.1993.tb03793.x
Subject(s) - anhydrous , crystallinity , tridymite , crystallite , cristobalite , chemistry , dehydration , crystallography , phase (matter) , chemical engineering , mineralogy , inorganic chemistry , materials science , organic chemistry , quartz , biochemistry , engineering , composite material
Factors influencing the low‐temperature formation of AIPO 4 and its precursor phases, AIPO 4 · x H 2 O (1 x 2), were investigated. AIPO 4 formed by reaction between 33.3 wt% H 3 PO 4 solution and alumina. Five aluminas (three anhydrous and two hydrated) were utilized. Each differed in particle size, surface area, and crystallinity. The reaction temperatures investigated were 113°, 123°, and 133°C. The high‐surface‐area aluminas were sufficiently reactive in the phosphoric acid solution at these temperatures to produce crystalline reaction products. However, only hydrated forms of AIPO 4 , AIPO 4 · x H 2 O (1 x 2), crystallized directly out of solution. x generally decreased as the curing temperature was increased. Upon dehydration of these hydrated reaction products, anhydrous AIPO 4 was formed, primarily in the berlinite and/or cristobalite modifications. Both the temperature of reaction and the alumina used influence the hydrates that form. In turn, the hydrates which form, the macroscopic assemblages into which they may crystallize, and the morphologies of the crystallites all affect the polymorphic form and the crystallinity of the anhydrous AIPO 4 phase ultimately produced on dehydration. Phase‐pure and highly crystalline AIPO 4 ‐cristobalite (the high‐temperature modification) was formed by the dehydration of AIPO 4 ·H 2 O at a temperature as low as 113°C.