The thermal change of anodic alumina (AA), particularly the exothermic peak
followed by the endothermic peak at ca 950 degreesC was studied in detail
by mainly using simultaneous TG-DTA/FTIR. The gradual loss of mass up to ca
910 degreesC is attributed to dehydration. When heated at a constant rate
by using TG-DTA, an exothermic peak with subsequent endothermic peak is obs
erved at ca 950 degreesC, but the exothermic peak becomes less distinct wit
h decreasing heating rate. It has been found that gaseous SO2 accompanying
a small amount of CO2 is mainly discharged at this stage. The reaction in t
his stage can be considered roughly in two schemes. The first scheme can be
said collectively as crystallization, in which the migration of S or C tra
pped inside the crystal lattice of the polycrystalline phase (gamma-, delta
-, and theta -Al2O3, which presumably accompanies a large amount of amorpho
us or disordered phase) occurs. In the second scheme, the initial polycryst
alline (+amorphous) phase crystallizes into a quasi-crystalline gamma -Al2O
3-like metastable phase after amorphization. Conclusively, after the distin
ct exo- and endothermic reactions, the amorphous phase crystallizes into ga
mma -Al2O3, presumably accompanying small amount of delta -Al2O3. It is als
o found that, when maintained isothermally, the metastable phases undergo t
ransformation into the stable alpha -Al2O3 at 912 degreesC.