Jp. Jalava et al., Structural investigation of hydrous titanium dioxide precipitates and their formation by small-angle X-ray scattering, IND ENG RES, 39(2), 2000, pp. 349-361
The mechanisms of formation and structure of precipitates hydrolyzed from a
queous solutions of titanium tetrachloride and titanium sulfate were studie
d by small-angle X-ray scattering (SAXS). SAXS was found a powerful method
for that purpose. The small colloidal primary particles that were present i
n the solutions at room temperature started to aggregate when thermal preci
pitation started. The aggregated particles coalesced until their radius was
approximately 1 nm depending of the precipitation conditions to some exten
t. After that, the aggregation continued producing either mass fractal or s
urface fractal structures. The structure was mass fractal when primary part
icle concentration was high enough and surface fractal when concentrations
were closer to the equilibrium state. With a delay ionic titanium started t
o precipitate. Because of its rather slow precipitation rate in the conditi
ons of this study, only surface fractal aggregates were formed. The mass fr
actal structure was found X-ray amorphous and the surface fractal aggregate
s nano crystalline. The mass and surface fractal dimensions of these aggreg
ates were 2.2 (1 s +/- 0.1) and 2.7 (1 s +/- 0.2), respectively. The "titan
ic acids" were found to be aggregates of small titanium dioxide particles t
hat have mass fractal structure in ortotitanic acid and surface fractal str
ucture in metatitanic acid. The loose structure of the mass fractal aggrega
tes causes the relatively easy solubility and the X-ray amorphous state fou
nd in ortotitanic acid. On the contrary, the more compact structure of meta
titanic acid explains its nano crystallinity and insolubility. The changing
of ortotitanic acid to metatitanic acid upon aging is obviously a conseque
nce of the restructuring of the primary titanium dioxide particles toward t
he close-packed porous structure.