The impact of solution stoichiometry, upon formation
of BaSO4 crystals in 0.02 M NaCl suspensions, on the development
of
particle size was investigated using dynamic light scattering (DLS).
Measurements were performed on a set of suspensions prepared with
predefined initial supersaturation, based on the quotient of the constituent
ion activity product {Ba2+}{SO4
2–} over the solubility product K
sp (Ωbarite = {Ba2+}{SO4
2–}/K
sp = 100, 500, or 1000–11,000
in steps of 1000), and ion activity solution stoichiometries (r
aq = {Ba2+}:{SO4
2–} = 0.01, 0.1, 1, 10 and 100), at circumneutral pH of 5.5–6.0,
and ambient temperature and pressure. DLS showed that for batch experiments,
crystal formation with varying r
aq was
best investigated at an initial Ωbarite of 1000 and
using the forward detection angle. At this Ωbarite and set of r
aq, the average apparent
hydrodynamic particle size of the largest population present in all
suspensions increased from ∼200 to ∼700 nm within 10–15
min and was independently confirmed by transmission electron microscopy
(TEM) imaging. Additional DLS measurements conducted at the same conditions
in flow confirmed that the BaSO4 formation kinetics were
very fast for our specifically chosen conditions. The DLS flow measurements,
monitoring the first minute of BaSO4 formation, showed
strong signs of aggregation of prenucleation clusters forming particles
with a size in the range of 200–300 nm for every r
aq. The estimated initial bulk growth rates from batch
DLS results show that BaSO4 crystals formed fastest at
near-stoichiometric conditions and more slowly at nonstoichiometric
conditions. Moreover, at extreme SO4-limiting conditions,
barite formation was slower compared to Ba-limiting conditions. Our
results show that DLS can be used to investigate nucleation and growth
at carefully selected experimental and analytical conditions. The
combined DLS and TEM results imply that BaSO4 formation
is influenced by solution stoichiometry and may aid to optimize antiscalant
efficiency and regulate BaSO4 (scale) formation processes.