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The wet state GF matching the pipe geometry was produced.
However, still a significant wettability change toward less oil-wet state or neutral wet state is expected to occur.
In the wet state (water saturated state), ionic conduction dominates.
Figure 2b shows the multilayered film of nanosilver particles in its initial wet state.
All rocks containing clay minerals (in wet state) exhibit abnormally high conductivity in this account.
The difference is remarkable in dry state and is less in wet state.
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Wettability study showed that at zero salinity surfactin can change original oil-wet state to water-wet state, but in seawater salinity it cannot modify the wettability significantly.
This means that the rock surface alters from oil-wet state to water-wet state as the surface charge increases from negative values to positive values.
Surfactant flooding enhances the relative permeability of oil as the oil-wet state of the sand pack is altered to a water-wet state.
The main recovery mechanism behind low salinity waterflooding is wettability alteration to more water-wet state.
Water finds the path to move forward along the pore wall with water-wet state and reaches the center of the pores in the oil-wet state during the surfactant flooding.
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