Twinning and homo‐epitaxy cooperation in the already rich growth morphology of CaCO3 polymorphs. II. Calcite

The two most abundant CaCO3 polymorphs, calcite and aragonite, are universally recognized for the richness of their morphology to which different twins make relevant contributions. The epitaxial transformation calcite ↔ aragonite has long been debated. While the twinning has been thoroughly treated, the homo‐epitaxy occurring within each of these minerals has, inexplicably, been overlooked to date, both experimentally and theoretically. Twinning can be deceptive to the point where it can be mistaken for homo‐epitaxy, thus making the proposed growth mechanism in the crystal aggregate wrong. Within the present work, the first aim is a theoretical investigation of the homo‐epitaxies among the three {10.4}‐cleavage, {01.2}‐steep and {01.8}‐flat rhombohedra of calcite. Accordingly, the specific adhesion energies were calculated between facing crystal forms, unequivocally showing that the {01.2}/{01.8} homo‐epitaxy competes with the generation of both {01.2} and {01.8} contact twins. Secondly, the calculation of the specific adhesion energy was extended to consider homo‐epitaxy for the {10.4} rhombohedron. The two‐dimensional geometric lattice coincidence has been tried for the {00.1} pinacoidal form as well. A theoretical investigation is presented of the homo‐epitaxies among the three {10.4}‐cleavage, {01.2}‐steep and {01.8}‐flat rhombohedra of calcite.