The
effectiveness of water flooding oil recovery depends to an
important extent on the competitive wetting of oil and water on the
solid rock matrix. Here, we use macroscopic contact angle goniometry
in highly idealized model systems to evaluate how brine salinity affects
the balance of wetting forces and to infer the microscopic origin
of the resultant contact angle alteration. We focus, in particular,
on two competing mechanisms debated in the literature, namely, double-layer
expansion and divalent cation bridging. Our experiments involve aqueous
droplets with a variable content of chloride salts of Na+, K+, Ca2+, and Mg2+, wetting surfaces
of muscovite and amorphous silica, and an environment of ambient decane
containing small amounts of fatty acids to represent polar oil components.
By diluting the salt content in various manners, we demonstrate that
the water contact angle on muscovite, not on silica, decreases by
up to 25° as the divalent cation concentration is reduced from
typical concentrations in seawater to zero. Decreasing the ionic strength
at a constant divalent ion concentration, however, has a negligible
effect on the contact angle. We discuss the consequences for the interpretation
of core flooding experiments and the identification of a microscopic
mechanism of low salinity water flooding, an increasingly popular,
inexpensive, and environment-friendly technique for enhanced oil recovery.