『Abstract
We present evidence of inhibition of calcite dissolution by dissolved
magnesium through direct observation of the (104) surface using
force microscopy (AFM) and vertical scanning interferometry (VSI).
Far from equilibrium, the pattern of magnesium inhibition is dependent
on solution composition and specific to surface step geometry.
In CO2-free solutions (pH 8.8), dissolved
magnesium brings about little inhibition even at concentrations
of 0.8×10-3 molal. At the same pH, magnesium concentrations
of less than 0.05×10-3 molal in carbonate -buffered
solutions generate significant inhibition, although no changes
in surface and etch pit morphology are observed. As concentrations
exceed magnesite saturation, the dissolution rate shows little
additional decrease; however, selective pinning of step edges
results in unique etch pit profiles, seen in both AFM and VSI
datasets. Despite the decrease in step velocity, magnesium addition
in carbonated solutions also appears to activate the surface by
increasing the nucleation rate of new defects. These relationships
suggest that the modest depression of the bulk rate measured by
VSI reflects a balance between competing reaction mechanisms that
simultaneously depress the rate through selective inhibition of
step movement, but also enhance reactivity on terraces by lowering
the energy barrier to new etch pit formation.』
1. Introduction
2. Methods
3. Results
3.1. VSI experiments
3.2. AFM experiments
4. Discussion
4.1. Control of step morphology
4.2. Step velocities and enhanced defect nucleation rates
5. Summary and conclusions
Acknowledgments
References