Dissolution kinetics of calcium carbonate minerals in H2OCO2 solutions in turbulent flow: The role of the diffusion boundary layer and the slow reaction H2O + CO2 → H+ + HCO3−
- 31 July 1997
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 61 (14), 2879-2889
- https://doi.org/10.1016/s0016-7037(97)00143-9
Abstract
No abstract availableKeywords
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