Phases of CaCO3 stabilized
at high pressures and temperatures
are the potential agents of the global carbon cycle, transferring
oxidized carbon in deep Earth’s interiors and thus are of special
interest for the Earth sciences. Here, we report finding of the new
phase, named disarag, which is dynamically disordered aragonite with
freely rotating CO3 groups, similar to that in the CaCO3-V phase with a calcite-like structure. Disarag has a stability
field expanding from 3 to 10 GPa and from 1600 to 2000 K. Consideration
of twinned structure enlarges this field, decreasing the transition
temperature from aragonite to disarag at 100–300 K. At P–T parameters corresponding to
the transition from aragonite to disarag, the marked disappearance
of the diffraction peaks is observed in in situ experiments.
We show that, among known phases of CaCO3, disarag is the
best candidate for the explanation of this reconstruction of diffraction
pattern. Also, for the first time, using ab initio molecular dynamics technique, we determine equilibrium curves between
calcite and its disordered phases CaCO3-IV and CaCO3-V. We show that the transitions of alkaline-earth carbonates
CaCO3, SrCO3, and BaCO3 to the disordered
states start when the critical angle of librations of the CO3 group about the axis perpendicular to the molecular three-fold axis
exceeds 45°. The calcite-like structure of CaCO3 is
characterized by more intense librations than the aragonite-like structure
of this compound and reaches the critical angle at lower temperatures.
As a result, calcite transforms into the disordered state at lower
temperatures than aragonite.