Abstract
Effects of l-aspartic acid ( l-Asp) on dissolution of calcite were investigated. The step retreat velocity and dissolution rate of calcite were measured simultaneously using an AFM flow-through system. The etch-pit morphology of calcite was observed using confocal laser scanning microscopy. Results show that the etch-pit morphologies changed drastically depending on the l-Asp concentration ([ l-Asp]) in the order of rhomboidal, pentagonal, and triangular (not perfectly, but retaining an extra step). The change in obtuse step directions and appearance of the [0 1 0] step triggered these morphological changes. Addition of l-Asp accelerated all step retreats at [ l-Asp]<0.01 M, which implied the effect of l-Asp on the diffusive barrier. In contrast, at [ l-Asp]>0.01 M, l-Asp inhibited the retreats of obtuse steps and [0 1 0] step, although the retreat velocities of acute steps were constant irrespective of [ l-Asp]. These results suggest that the directional changes and the inhibition of retreat velocities of obtuse steps were attributed to the generation of [ 4 1 1] and [4 5 1] steps caused by l-Asp. Moreover, we confirmed the preferential effects of l-Asp on the [4 8 1] + to [ 4 4 1] ± step edge, and proposed the preferential effects of l-Asp on the [ 4 1 1] to [4 5 1] step edge.
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