Iron
minerals are hydrophobic minerals predominately found in sandstone
formations with their role in wettability alteration not fully understood.
With the reservoir rock being a complex system of multiple minerals,
the control of wettability alterations becomes difficult to manage
due to the different surface chemistry of constituent minerals. This
study presents for the first time the surface charge development of
pyrite, magnetite, and hematite minerals in native reservoir environments
and the effect of oilfield operations such as acidizing, water injection,
polymerization, surfactant flooding, and alkaline flooding on iron
minerals, surface charge development. This was achieved using zeta
potential measurement, which depicts the type of surface charge and
infers the propensity of precipitation. The experimental results show
that pyrite, magnetite, and hematite behave similarly under reservoir
conditions with all the minerals being positively charged although
pyrite and hematite are negatively charged in seawater (SW). Results
also show that the surface charge development is controlled by the
electrical double-layer effect and ion adsorption on the mineral surfaces.
These findings provide key insights into the role of iron minerals
in wettability alteration as they provide surfaces that serve as a
precursor for polar crude component adsorption. Also, the design of
an ion-engineered fluid to control the surface charge of iron minerals
was implemented, and the results showed that they behave differently.
Furthermore, the effect of low-salinity water on the mineral surface
charge was examined. The findings revealed that low-salinity water
can produce a negatively charged surface, however, cannot mitigate
the iron mineral precipitation challenge as the observed zeta potential
values are near zero. Finally, slug and continuous injection of the
ethylenediaminetetraacetic acid chelating agent was implemented as
an iron mineral precipitation control strategy, with the continuous
injection observed to significantly improve the colloidal stability
of the iron minerals in the reservoir native state and after SW injection.