ABSTRACT:  The colloidal stability of suspensions of hematite/yttria core/shell particles is investigated in this work and compared with that of the pure hematite cores.  The different electrical surface characteristics of yttrium and iron oxides, as well as the diameters of both types of spherical particles, dominate the overall process of particle aggregation.  The aggregation kinetics of the suspensions was followed by measuring their optical absorbance as a function of time.  By previously calculating the extinction cross section of particle doublets, it was demonstrated that for both core and core/shell particles the turbidity of the suspensions should increase on aggregation.  Such an increase was in fact found in the sustems in spite of the ever-present tendency of the particles to settle under gravity.  The authors used the initial slope of the turbidity increment time plots as a measure of the ease of aggregation between  particles.  Thus, they found that the essential role played by pH on the charge generation on the two oxides and the shift of one pH unit between the isoelectric points of hematite and yttria manifest in two features: (i) the stability decreases on approaching the isoelectric point from either the acid or basic side and (ii) the maximum instability is found for hematite at pH 7 and for hematite/yttria at pH 8, that is, close to the isoelectric points of alpha-Fe2O3 and Y2O3, respectively.  The role of added electrolyte is simply to yield the suspensions of either type more unstable.  Using the surface free energy of the particles, the authors could estimate their Hamaker constants in water.  From these and their zeta potentials, the DLVO theory of stability was used to quantitatively explain their results.