The present study addressed the investigation of the basic fundamental
s of the behaviour of celestite (SrSO4), strontianite (SrCO3) and calc
ite (CaCO3) in aqueous solutions in the presence and absence of sodium
oleate. The results showed that the isoelectric point (IEP((aq))) of
aqueous suspensions of strontianite and calcite takes place at pH 8 an
d 8.2, respectively; from thermodynamics, the IEP((aq)) of the mineral
s takes place at pH 8 and 8.3, respectively. Similarly, a thermodynami
c analysis of the celestite-aqueous solution equilibrium open to the a
tmosphere showed celestite transforms to strontium carbonate in alkali
ne slurries (pH greater than or equal to 7.75). This phenomenon is due
to the chemical reaction of celestite with the carbonate ion that for
ms in the solution as a result of the dissolution of the atmospheric C
O2. The results of the mineral-aqueous solution equilibrium, electroki
netic and infrared spectroscopy studies appear to confirm such a super
ficial transformation. The electrokinetic studies showed the isoelectr
ic point (IEP) of celestite and strontianite takes place at pH 5.4 and
7.4, respectively. The floatability of the minerals was investigated
in the pH range 5 to 11 and varying the concentration of sodium oleate
from 10(-6) to 10(-4) M. The results showed that celestite floatabili
ty had a maximum in the pH range 7 to 9; at higher pH values its float
ability tended to decrease as a result of its surface transformation t
o strontium carbonate. The floatability of strontianite and calcite wa
s substantially lower than that of celestite and tended to increase wi
th the pH (pH greater than or equal to 7) and concentration of sodium
oleate. It is proposed that in alkaline slurries sodium oleate was ads
orbed on the celestite, strontianite and calcite surfaces by a chemiso
rption mechanism.