Calcite dissolution kinetics in the system CaCO3 H2O CO2 at high undersaturation

Details Calcite dissolution kinetics in the system CaCO3 H2O CO2 at high undersaturation Calcite dissolution kinetics in the system CaCO3 H2O CO2 at high undersaturation

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007gecoa..71.1398k&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 71, Issue 6, p. 1398-1410.

Computer Science

4

Scientific paper

Dissolution rates of limestone covered by a water film open to a CO2-containing atmosphere are controlled by the chemical composition of the CaCO3 H2O CO2 solution at the water-mineral interface. This composition is determined by the Ca2+-concentration at this boundary, conversion of CO2 into H+ and HCO3- in the solution, and by diffusional mass transport of the dissolved species from and towards the water limestone interface. A system of coupled diffusion reaction equations for Ca2+, HCO3-, and CO2 is derived. The Ca2+ flux rates at the surface of the mineral are defined by the PWP-empirical rate law. These flux rates by the rules of stoichiometry must be equal to the flux rates of CO2 across the air water interface. In the solution, CO2 is converted into H+ and HCO3-. At low water-film thickness this reaction becomes rate limiting. The time dependent diffusion reaction equations are solved for free drift dissolution by a finite-difference scheme, to obtain the dissolution rate of calcite as a function of the average calcium concentration in the water film. Dissolution rates are obtained for high undersaturation. The results reveal two regimes of linear dissolution kinetics, which can be described by a rate law F = αi(miceq - c), where c is the calcium concentration in the water film, ceq the equilibrium concentration with respect to calcite. For index i = 0, a fast rate law, which here is reported for the first time, is found with α0 = 3 × 10-6 m s-1 and m0 = 0.3. For c > m0ceq, a slow rate law is valid with α1 = 3 × 10-7 m s-1 and m1 = 1, which confirms earlier work. The numbers given above are valid for film thickness of several tenths of a millimetre and at 20 °C. These rates are proven experimentally, using a flat inclined limestone plate covered by a laminar flowing water film injected at an input point with known flow rate Q and calcium concentration. From the concentration measured after flow distance x the dissolution rates are determined. These experiments have been performed at a carbon-dioxide pressure of 0.00035 atm and also of 0.01 atm. The results are in good agreement to the theoretical predictions.

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