Fig. 8 Relationship between the rate of change in alkalinity in dolomite-seeded Ca–Mg–HCO₃/CO₃ solutions and pIAP_dolomite. Control lines are 95% confidence and prediction lines from the unseeded Ca–Mg–HCO₃/CO₃ solutions, corresponding with the hypothesis of no alkalinity change due to dolomite dissolution. Lines connect individual dolomite-seeded solutions from 0 to 672 d

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