“…When low-salinity brine is injected into porous media, this equilibrium is disturbed and, as a result, clay particles are detached and mobilized by the drag forces caused by the displacing phase. ,,− Migration of fines leads to the aforementioned fines straining in the rock. As a result, water-permeable channels are plugged and the flow is directed toward unswept zones where residual oil is trapped. ,,− This microscale flux diversion causes a decline in water relative permeability and an increase in pressure drop, which improves microscopic sweep efficiency by mobility control, resulting in enhanced oil recovery. ,− …”