It has previously been suggested that a local pH increase
at pore
surfaces is responsible for desorption of polar oil components and
wettability alteration in sandstone reservoirs, leading to increased
oil recovery during smart water or low salinity injection. The pH
increase can be a result of cation exchanges at clay surfaces or at
other mineral surfaces present in sandstone reservoirs, such as feldspars,
which is the topic of this paper. In this study, static batch tests
and dynamic sandpack flooding tests have been performed to investigate
the pH development in the brine phase in contact with three common
feldspars, Ab-feldspar (albite), An-feldspar (anorthite), and Or-feldspar
(microcline). Temperature varied between 23 and 130 °C, and brine
salinity varied from 0 ppm (deionized water) to 100 000 ppm
NaCl in batch tests. The sandpacks were composed of 10 wt % feldspar
and 90 wt % quartz and flooded with 100 000 and 1000 ppm brines.
In all tests, equilibrated brine pH was monitored to study cation-exchange
reactions between the feldspars and the brine phase. The main results
in this study showed that all three feldspars tested, Ab-feldspar,
An-feldspar, and Or-feldspar, caused a pH increase in the brine phase
at all temperatures and salinities tested and can therefore influence
pH during waterflooding of sandstone reservoirs. There was a general
decrease in ion exchange and pH increment when the test temperature
increased for all three feldspars. The least stable feldspar, or the
most reactive feldspar, in cation-exchange processes seemed to be
An-feldspar, causing the highest pH at most conditions, also being
least affected by increasing brine salinity.