Environ. Sci. Technol., 39 (17), 6420 -6428, 2005. 10.1021/es050470z S0013-936X(05)00470-0
Web Release Date: July 27, 2005

Copyright © 2005 American Chemical Society

Inhibition of Calcite Precipitation by Natural Organic Material: Kinetics, Mechanism, and Thermodynamics

Yi-Pin Lin, Philip C. Singer,* and George R. Aiken

Department of Environmental Sciences and Engineering, University of North Carolina, CB #7431, Chapel Hill, North Carolina 27599-7431, and U.S. Geological Survey, 3215 Marine Street, Boulder, Colorado 80303

Received for review March 9, 2005

Revised manuscript received July 19, 2005

Accepted July 20, 2005

Abstract:

The inhibition of calcite precipitation by natural organic material (NOM) in solutions seeded with calcite was investigated using a pH-stat system. Experiments were carried out using three NOMs with different physical/chemical properties. For each of the materials, inhibition was found to be more effective at lower carbonate/calcium ratios and lower pH values. The reduction in the precipitation rate could be explained by a Langmuir adsorption model using a conditional equilibrium constant. By identification of the type of site on the NOM molecules that is involved in the adsorption reaction, the "conditional" equilibrium constants obtained at different solution compositions converged to a single "nonconditional" value. The thermodynamic data determined at 25 C and 1 atm suggest that the interaction between NOM molecules and the calcite surface is chemisorptive in nature and that adsorption is an endothermic reaction driven by the entropy change. The greatest degree of inhibition was observed for the NOM with the highest molecular weight and aromatic carbon content. For a given type of NOM, the degree of inhibition of calcite precipitation was dictated by the balance between the enthalpy change and the entropy change of the adsorption reaction.


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