“…The acid naturally reacts with various minerals in the rock, for example, albite, K‐feldspar, and glauconite (Ketzer et al, ; Lebedev, Zhang, Sarmadivaleh, et al, ; Mangane et al, ) when exposed to live brine more than 3 hr (Baker et al, ; Yasuda et al, ). Fines migration and solid reprecipitation change the pore size distribution and pore connectivity, which again significantly influence reservoir‐scale fluid dynamics (Al‐Khdheeawi et al, , ; Hangx et al, ), dramatically affect permeability (Al‐Yaseri et al, , , ; Liu et al, ; Reynolds et al, ), and storage capacity (Iglauer et al, ; Iglauer & Lebedev, ). This porosity and permeability modification thus pose a significant risk, particularly when permeability is decreased dramatically (formation damage), and as a consequence, CO 2 injectivity may be very poor (Iglauer et al, ; Lamy‐Chappuis et al, ; Mangane et al, ).…”