“…This argument is supported by the work of Sternbeck [45], who concluded that dehydration of MnCO 0 3 on {MnHCO 0 3 and {MnCO 3 À sites was the rate determining process for rhodochrosite growth. Similarly, Terjesen et al [18] demonstrated that adsorption of Cu(II) to calcite decreased with decreasing solution pH, indicating that Cu(II) adsorbed mainly as CuHCO 3 + or CuCO 3 0 . Alternatively, if successive stepwise reactions such as (4)-(6) are indeed important, especially at pH$8.8, the surface would require an induction period of some time before adsorption imposed a significant influence on the dissolution process.…”