Wettability alteration toward a favorable
wetting condition is
one major mechanism of enhancing oil recovery in carbonates. Obtaining
the desired wettability stipulates that a clear understanding of the
original wetting properties of the rock surface be provided. In fact,
the aim of this study is to elucidate the effect of acid and base
upon the wettability alteration of a calcite surface by investigating
the individual effects of an organic acid (stearic acid) and a base
(N,N-dimethyldodecylamine, N,N-DMDA) at different concentrations as
well as their combinations on calcite wetting properties. Contact
angle, ζ-potential, Fourier transform infrared spectroscopy,
and thermogravimetric analysis (TGA) were conducted to determine changes
in wetting properties of the calcite surface. Moreover, interfacial
tension (IFT) measurements were used to evaluate the interfacial activity
of the model oil systems. Overall, the results revealed that by increasing
the acid concentration, wettability of a calcite surface shifted toward
more oil-wetness and adsorption of stearic acid on a calcite surface
increased. Treating calcite surfaces with the base revealed that a
low concentration of N,N-DMDA was
able to shift the calcite wettability from a water-wet state to a
slightly oil-wet state. In addition, TGA results showed low adsorption
of the base with a high surface area occupied by the base molecule,
indicating a horizontal orientation of the base on the calcite surface.
For acid–base mixtures, at a constant acid concentration, the
wettability alteration toward oil-wetness increased in the presence
of the base, as the base-to-acid ratio increased up to 1, as a result
of which oil-wetness decreased. Moreover, IFT measurements indicated
lower IFT of acid–base mixtures compared to those of individual
acidic and basic model oil solutions, which could be attributed to
the synergistic effect between the acid and base by forming acid–base
complexes. The presence of the base hindered acid adsorption on the
calcite surface. However, the basic component could contribute to
wettability alteration by forming acid–base complexes. These
complexes could adsorb on the calcite surface and affect its wetting
preferences. In addition, the base molecules may adsorb on the calcite
surface at high base-to-acid ratios. The results suggested that the
ratio of base to acid would determine the contribution of acid molecules,
base molecules, and acid–base complexes in wettability alteration
of calcite surfaces. Hence, possible mechanisms of wettability alteration
by acid–base combinations were proposed at different base-to-acid
ratios.