“…Geochemical reactions depend on several factors such as reservoir temperature, pressure, brine salinity, rock mineralogy, fluid injection rates, and time-scale of geological storage (Fang et al, 2010;van der Meer, 2005). In addition to the potential geomechanical risks associated with CO 2 injection that are discussed later in this section, it has been reported that chemical interactions of CO 2 -enriched brine with caprock minerals at the reservoir and caprock interface in the long-term might reduce rock strength, increase damage risks, and alter the flow properties of the caprock layer (Hangx et al, 2010a).…”