Abstract

The character of the most important crystallographic forms of calcite crystal is quantitatively reviewed according to the Hartman and Perdok theory. Specific surface and edge energies of the cleavage {1 0 4} rhombohedron are calculated in the crystal–vacuum system by means of a semi-empirical potential function and following Stranski’s definition of the total surface energy of a finite crystal. A comparison is made between the calculated value and the experimental quantities entering the Dupré formula (specific crystal–solution interface energy, specific vapour–solution surface energy): the crystal–vacuum specific surface energy is proved to be quite reasonable, and for the first time, the specific crystal–solution adhesion energy for the {1 0 4} form is estimated.

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