K. Inoue et C. Satoh, SURFACE-CHARGE CHARACTERISTICS OF HYDROXYALUMINOSILICATE AND HYDROXYALUMINUM MONTMORILLONITE COMPLEXES, Soil Science Society of America journal, 57(2), 1993, pp. 545-552
The electric charge and surface characteristics of montmorillonite (Mt
) complexed with hydroxy-Al (HyA) or hydroxyaluminosilicate (HAS) ions
were studied in the pH range of 4 to 8. The HAS or HyA ions were prep
ared from solutions containing HyA ions and orthosilicic acid at an Al
concentration of 4 mmol L-1; Si/Al atomic ratios of 0, 0.25, 0.5, and
1.0; and NaOH/Al molar ratios of 1.0, 2.0, and 2.5. At pH 4 to 6, the
negative charge of Mt was drastically reduced by interlayer formation
with HAS or HyA ions. At pH 7 to 8, the magnitude of negative charge
of RAS-Mt or HyA-Mt complexes was close to that of Mt, suggesting that
HAS or HvA ions were excluded from the interlayer spaces of Mt. A sig
nificant positive charge was developed on RAS-Mt complexes formed at N
aOH/Al molar ratios of 2.0 and 2.5. The fixation of HAS or HyA ions on
Mt caused a significant reduction in total and internal surface areas
but a slight increase in external surface area. Our results reveal th
at the complexation of Mt with HAS or HyA ions changed the electric ch
arge and surface characteristics of Mt, and suggest that RAS and HyA i
ons fixed on expansible 2:1 layer silicates contribute as active Al co
mponents to humus accumulation and phosphate retention in acidic and n
onallophanic Andisols and related soils. Our data also indicate that t
he fixation of RAS and HyA ions on Mt can influence the levels of solu
tion Al species that cause some toxicological problems in terrestrial
and aquatic environments.