Zeta potential measurements
and microscopic surface characterization
and imaging were conducted on calcite and dolomite crystals aged in
stearic acid model oil and exposed to different synthetic brines representing
different potential scenarios of injected seawater from the Arabian
Gulf. Calcite particles were negatively charged in deionized water
and maintained negative surface charges in all tested brines, except
in diluted Arabian Gulf seawater that contained higher concentration
of Ca2+ and Mg2+ ions. Dolomite particles were
positively charged in deionized water as well as in all tested brines,
except in diluted Arabian Gulf seawater that contained four times
higher concentration of SO4
2– ions. Scanning
electron microscopy and atomic force microscopy experiments on cleaved
calcite and dolomite chips showed different morphological changes
when both samples were aged in model oil and then treated with brines.
Calcite surface dissolution was observed in addition to stearic acid
deposition. Surface elemental analysis using energy-dispersive spectroscopy
showed Mg2+ and SO4
2– ions
adsorb preferably on locations where stearic acid is deposited. The
finding that stearic acid was adsorbing more strongly on dolomite
than on calcite could indicate why the tested brines were less efficient
to change the zeta potential of the dolomite systems. The current
study concludes that manipulating the concentration of potential-determining
ions present in the Arabian Gulf seawater, especially Mg2+ and SO4
2– ions, will alter the surface
charges of aged calcite and dolomite samples as well as their surface
morphology.