J. Chorover et al., COMPARISON OF HEMATITE COAGULATION BY CHARGE SCREENING AND PHOSPHATE ADSORPTION - DIFFERENCES IN AGGREGATE STRUCTURE, Clays and clay minerals, 45(5), 1997, pp. 690-708
The formation and structure of hematite aggregates were examined by dy
namic and static light scattering techniques. A large range in coagula
tion kinetics was studied by varying either indifferent electrolyte (K
CI) concentration or surface complexing anion (H2PO4-) concentration,
P-T, at pH 6.0 +/- 0.1. Diffusion limited aggregation (DLA) was induce
d by counterion screening at [KCl] > 80 mM or by surface charge neutra
lization at P-T = 31 mu M (and ionic strength = 1.0 mM). In DLA, the f
ractal dimension, d(f), of aggregates formed by either surface charge
neutralization or counterion screening was 1.7 +/- 0.1. A reduction in
the rate of coagulation in KCl for [KCI] < critical coagulation conce
ntration (CCC) produced an increase in d(f) to 2.1 +/- 0.1. For aggreg
ation induced by phosphate adsorption at constant ionic strength, ther
e was no apparent trend in d(f) with coagulation rate. The value of d,
was consistently less than 1.8 when reaction limited aggregation (RLA
) resulted from surface charge neutralization rather than counterion s
creening. TEM observations of aggregates formed in the presence or abs
ence of phosphate confirm that, when RLA is induced by phosphate adsor
ption, resulting aggregates we much looser in structure than those for
med by counterion screening. The results suggest that the high-affinit
y binding of phosphate to hematite may result in a nonrandom distribut
ion of surface charge that facilitates the coalescence of positive and
negative charge crystal faces.