Understanding of Long-Term CO₂-Brine-Rock Geochemical Reactions Using Numerical Modeling and Natural Analogue Study

Figure 5

Variations in abundance (in volume fraction of medium) of albite and anorthite (a); K-feldspar (b); chlorite (c); illite (d); calcite, siderite, ankerite, and dawsonite (e); smectite-Na and smectite-Ca (f); kaolinite (g); and quartz (h) after flooding by CO₂.

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