Solution composition-sensitive
disjoining pressure acting between
the mineral surfaces in fluid-filled granular rocks and materials
controls their cohesion, facilitates the transport of dissolved species,
and may sustain volume-expanding reactions leading to fracturing or
pore sealing. Although calcite is one of the most abundant minerals
in the Earth’s crust, there is still no complete understanding
of how the most common inorganic ions affect the disjoining pressure
(and thus the attractive or repulsive forces) operating between calcite
surfaces. In this atomic force microscopy study, we measured adhesion
acting between two cleaved (104) calcite surfaces in solutions containing
low and high concentrations of Ca
2+
ions. We detected only
low adhesion between calcite surfaces, which was weakly modulated
by the varying Ca
2+
concentration. Our results show that
the more hydrated calcium ions decrease the adhesion between calcite
surfaces with respect to monovalent Na
+
at a given ionic
strength, and thus Ca
2+
can sustain relatively thick water
films between contacting calcite grains even at high overburden pressures.
These findings suggest a possible loss of cohesion and continued progress
of reaction-induced fracturing for weakly charged minerals in the
presence of strongly hydrated ionic species.