An investigation of the deposition and in situ transformation of scale
found in a Bayer process plant has been carried out using X-ray powde
r diffraction and FTIR studies. Scale samples were analysed as a funct
ion of their position in the Bayer process circuit. Scale precipitated
during bauxite digestion at approximately 255 degrees C was found to
be mostly cafetite but also contained haematite. At 120 degrees C boeh
mite has been identified as the main scale phase formed from ''spent''
liquor (i.e. liquors from which Al(OH)(3) crystallisation has previou
sly occurred). Three sodium aluminosilicate phases were found to form
between 150 and 255 degrees C, sodalite(1), sodalite(2) and cancrinite
although thermonatrite (Na2CO3 . H2O) and calcite (CaCO3) were also o
bserved periodically. The ratios of cancrinite to sodalite(1) and soda
lite(2) to sodalite(1) were observed to increase with the temperature
of formation, The scale phases found in a cross section of plant scale
formed at 150 degrees C show a similar trend on increasing the in sit
u age of the scale. Comparison with precipitation from synthetic solut
ions has indicated that the aging mechanism of the sodium aluminosilic
ate deposits is the same in both cases: sodalite(1) (cubic, a approxim
ate to 8.98 Angstrom) --> sodalite(2) (cubic, a approximate to 8.89 An
gstrom) --> cancrinite (hexagonal, a approximate to 12.70 Angstrom, c
approximate to 5.18 Angstrom). The transformation from sodalite(2) to
cancrinite has been shown to be the rate determining step in cancrinit
e formation.