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The influence of surface state and saturation state on the dissolution kinetics of biogenic aragonite in seawater

American Journal of Science (1989) 289(9) 1098-1116
DOI: 10.2475/ajs.289.9.1098
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Abstract

Uses several realistic partial molar volume changes (ΔV) for aragonite dissolution in seawater. Indicates that the molar volume change for aragonite dissolution is within the bounds -37 cm3/mole ≤ΔV ≤ -39.5 cm3/mole. -from Authors

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Acker, J. G., & Byrne, R. H. (1989). The influence of surface state and saturation state on the dissolution kinetics of biogenic aragonite in seawater. American Journal of Science, 289(9), 1098–1116. https://doi.org/10.2475/ajs.289.9.1098

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