Substantially enhanced oil recoveries
from carbonate reservoirs
have been accredited to the modification of ionic content and salinity
of the injection water and subsequent alteration of reservoir rock
wettability toward more water-wet. Modification of surface charges
at rock/oil/water interfaces is believed to be the main mechanism
that controls the process of wettability alteration. This paper presents
a systematic zeta-potential measurement study that investigates the
individual and relative impacts of Ca2+, Mg2+, and SO4
2– ions on a limestone rock
from the Middle East. The main target of the study is to understand
the impact of each potential determining ion individually and in the
presence of another ion for insightful explanations of the overall
impact of injection water during ionically controlled waterflooding
in carbonate reservoirs. The novelty of the current study is the comprehensive
investigation of the interplay between potential determining ions
and the resultant impact on limestone surface charges. Different modified
brines were prepared based on the ionic composition of Arabian Gulf
seawater, which is the main source of injection water in the region.
Model oil, containing carboxylic acid, was used to represent the oil
phase in aging procedures. Interactions at the rock/oil/water interfaces
were assessed using zeta-potential measurements of unaged and aged
limestone particles. The results show that Ca2+, Mg2+, and SO4
2– are potential determining
ions that can alter surface charges of unaged and aged limestone.
SO4
2– ions were found to have a profound
impact on the generation of negative surface charges on limestone
as well as in suppressing the preferential ability of Ca2+ and Mg2+ ions to generate positive surface charges. Results
also showed that limestone possesses negative surface charges when
conditioned in unmodified seawater and twice diluted seawater. Comparing
the obtained results from this study with the literature suggests
that similarities in the mineralogical composition of carbonates rocks
do not necessarily reflect in similar electrokinetic behavior, even
under the same experimental conditions. Moreover, this study shows
that the zeta-potential of limestone is not linearly correlated with
decreased salinity. Furthermore, it is shown that conditioning limestone
in sequentially diluted seawater will result in an increase in the
magnitude of the negative charges up to twice diluted seawater, after
which the magnitude of the negative surface charges will start to
decrease. This finding suggests that a different mechanism is responsible
for the modification of carbonate surface charges during late stages
of sequential low-salinity waterflooding than the mechanism that controls
the modification of surface charges during early stages of the process.