Calcite
dissolution and Ca–Mg ion exchange on carbonate
rock surfaces have been proposed as potential mechanisms occurring
during smart waterflooding in carbonate reservoirs. However, there
is still a lack of fundamental understanding of these reactions to
quantitatively evaluate their effects in the reservoir flooding process.
Especially, the data on precipitation and dissolution kinetics are
insufficient. In this work, the equilibration kinetics of calcite
dissolution and Ca–Mg exchange was experimentally studied.
The behavior of three powders was compared: pure calcium carbonate,
Stevns Klint outcrop chalk, and North Sea reservoir chalk. It was
found that the equilibration time for calcite dissolution was of the
order of seconds for a given surface-area-to-liquid-volume ratio.
The existing theory of calcite dissolution could well reproduce our
observations. The Ca–Mg exchange showed two-step kinetics:
the first step was fast, and it dominated the process within the first
hour of reaction; the second step was slow, and it continued longer
than the time of observation (2 weeks). Characteristic times for the
two steps were extracted by fitting the experimental curves. A two-layer
adsorption model was proposed to characterize the kinetic process
and successfully matched with experimental data. The findings were
further extended to flow-through scenarios. By comparing with literature
data and surface complexation models, it was concluded that calcite
dissolution alone was unlikely to be able to explain the additional
recovery reported in the literature. The Ca–Mg exchange process
could dominate the fluid–rock interactions at a high temperature
in pure calcium carbonate rocks, while competitive adsorption of cations
appeared to control the process at a lower temperature. Different
carbonate rocks possess different properties with regard to the ion-exchange
process.