Low-salinity
waterflooding (LSWF) has proven to improve oil recovery
in carbonate formations through rock wettability alteration, although
the underlying mechanism remains elusive. Multivalent ionic exchange
and calcite dissolution have usually been investigated using geochemical
analysis in secondary coreflooding. In this work, coreflooding, in
tertiary mode, coupled with a surface reactivity analysis approach
was employed to investigate the interplay of wettability alteration
mechanisms such as mineral dissolution, electrostatic bond attraction,
and the effect of pH at in situ conditions. Improved oil recovery
(IOR) in tertiary mode observed by coreflooding in Indiana limestone
rocks showed an ionic strength dependence, that is, reducing brine
ionic strength resulted in an increase in oil recovery. Coreflooding
results showed that the seawater and low-salinity brines deprived
of Mg2+ ions resulted in the lowest IOR in tertiary mode,
indicating the significance of Mg2+ on IOR in limestone
rocks. Similar results were observed through the contact angle measurement
showing the limestone rock wettability state dependence on ionic strength
and the effect of Mg2+ ions. Surface reactivity analysis
showed an increase in solution pH, Ca2+ and Mg2+ ions concentration in the effluent solution from the coreflooding
in tertiary mode using low salinity brines (about 40 and 20% increase
in the effluent composition for Ca2+ and Mg2+, respectively). These changes in solution composition were used
to calculate the in situ oil–brine and rock–brine zeta
potential using a validated surface complexation model, showing the
changes of zeta potential as brine is injected into limestone rocks.
The results show that using seawater-like brine in tertiary mode resulted
in no mineral dissolution or ionic exchange. However, improved oil
recovery (IOR) using such seawater-like brine was due to wettability
alteration caused by reduced electrostatic bond attraction associated
with Mg2+ ions [from 2.6 × 10–13 (mol/m2)2 for formation water salinity to
1.5 × 10–13 (mol/m2)2 for seawater salinity]. Using low-salinity brines in tertiary mode
improved oil recovery by mineral dissolution, resulting in oil desorption
and an increase in solution pH. The increase in solution pH also resulted
in reduced electrostatic bond attraction which lead to rock wettability
alteration using low-salinity brines.