In this paper, the characteristics of natural manganese mineral collected f
rom Guangxi Province. China, including crystalline properties, elemental co
mposition, organic substrates content (0.17%) and BET surface area (29.8 m(
2)/g), were determined. By X-ray powder diffraction and fluorescence spectr
ograph analysis, it is shown that manganese oxide in the natural mineral ex
ists in the crystal structure of alpha-Mn2O3 and the contents of manganese
(II) and manganese (IV) oxides are 4.6 and 42.6%, respectively. The solubil
ity experiments show that manganese dissolved in solution can be ignored at
a higher pH value, but its significant solubility is observed with the dec
rease of pH value. Moreover. the decolorization properties of direct light
red F3B dye on natural manganese mineral surface were studied by batch tech
nique. The effects of pH value, temperature, inert electrolyte, light, part
icles concentration and size, the presence of calcium and phosphate as well
as oxygen on the decolorization efficiency of the dye were investigated in
detail. The results show that the decolorization of the dye is strongly de
pendent on pH value, with lower decolorization percentage at higher pH valu
es, and the higher concentration of inert electrolyte and temperature favor
the decolorization reaction of the dye on the particle surface. By Arrheni
us Equation. the apparent activation energy is found to be at 71.7 kJ/mol,
indicating the surface chemical reaction as a rate-limiting step in the ove
rall interface process. The illumination enhances the surface chemical reac
tion of the dye on manganese mineral particles. The decolorization rate of
the dye compound is increased with the increase of particle concentration a
nd the decrease of size since the available surface sires grow in number. T
he presence of phosphate greatly inhibits the decolorization reaction by co
mpetitive adsorption on the mineral surface with the dye anion, while the a
ddition of calcium promotes the decolorization rate of direct light red F3B
dye. (C) 2000 Elsevier Science Ltd. All rights reserved.