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Ab initio surface phase diagram of the {104} calcite surface
Sebastien Kerisit1, Arnaud Marmier, Stephen C Parker
1Department of Chemistry, University of Bath, Claverton Down, Bath BA2 7AY, UK.
The Journal of Physical Chemistry. B
|July 21, 2006
Summary
Calcite surfaces can change their structure under humid atmospheric conditions, forming nonstoichiometric terminations. This finding is crucial for understanding the surface chemistry of calcite, a common mineral.
Area of Science:
- Geochemistry
- Materials Science
- Surface Chemistry
Background:
- Calcite surfaces are critical in geological and industrial processes.
- Understanding calcite surface termination is key to predicting its reactivity.
- Previous studies have not fully explored calcite surface behavior under varying environmental conditions.
Purpose of the Study:
- To investigate the surface termination of the {104} calcite surface.
- To determine how temperature, pressure, and gas composition affect calcite surface structure.
- To explore the potential for nonstoichiometric terminations under atmospheric conditions.
Main Methods:
- Utilized electronic structure calculations at the density functional theory level.
- Generated a surface phase diagram to map termination changes.
- Simulated calcite surface interactions with water and carbon dioxide.
Main Results:
- Identified conditions under which nonstoichiometric calcite terminations can form.
- Demonstrated that high relative humidity can induce nonstoichiometric surfaces.
- The {104} calcite surface is susceptible to changes in termination.
Conclusions:
- Nonstoichiometric calcite surfaces can form under ambient atmospheric conditions.
- These nonstoichiometric surfaces likely play a significant role in calcite surface chemistry.
- The findings have implications for understanding mineral weathering and carbon capture technologies.
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