There
is a limited understanding of the microscale interactions
between fluid–oil–solid interfaces, which could be a
stumbling block to the development of relevant technologies and industries.
With this in mind, we applied an in situ method, quartz crystal microbalance
with dissipation (QCM-D), on the interactions among the fluid–oil–solid
phases and investigated the desorption process of the asphaltene model
molecule from silica surfaces during a flow of LSW at the conditions
of different ion types, salinities, or pH values. The salinity effect
plays a bigger role than that of the pH effect on the asphaltene desorption
and, furthermore, the divalent ions (such as SO4
2–, Mg2+, or Ca2+) show a stronger effect than
that of monovalent ions (such as Cl–, Na+, or K+). Our study provides a new strategy for the investigation
of the interactions between fluid–oil–solid interfaces.