Atomistic simulations provide a meaningful way to determine the
physico-chemical properties of liquids in a consistent theoretical framework.
This approach takes on particular usefulness for the study of molten
carbonates, in a context where thermodynamic and transport data are crucially
needed over a large domain of temperatures and pressures (to ascertain the role
of these melts in geochemical processes) but are very scarce in the literature,
especially for the calco-magnesian compositions prevailing in the Earth's
mantle. Following our work on Li2CO3-Na2CO3-K2CO3 melts, we extend our force
field to incorporate Ca and Mg components. The empirical interaction potentials
are benchmarked on the density data available in the experimental literature
(for the crystals and the K2Ca(CO3)2 melt) and on the liquid structure issued
from ab initio molecular dynamics simulations. Molecular dynamics simulations
are then performed to study the thermodynamics, the microscopic structure, the
diffusion coefficients, the electrical conductivity and the viscosity of molten
Ca, Mg-bearing carbonates up to 2073 K and 15 GPa. Additionally, the equation
of state of a Na-Ca-K mixture representative of the lavas emitted at Ol Doinyo
Lengai (Tanzania) is evaluated. The overall agreement between the MD results
and the existing experimental data is very satisfying and provides evidence for
the ability of the force field to accurately model any
MgCO3-CaCO3-Li2CO3-Na2CO3-K2CO3 melt over a large T - P range. Moreover it is
the first report of a force field allowing to study the transport properties of
molten magnesite (MgCO3) and molten dolomite (CaMg(CO3)2)