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Thermodynamic databases suited for calculating phase equilibria in Earth sciences mostly contain only silicates and oxides.
Firstly, dynamical properties about this model are discussed by numerically calculating phase portraits, Lyapunov exponents and bifurcation diagram.
This separation process can be investigated quantitatively by calculating phase equilibria for the measured pressure and temperatures.
The van der Waals contribution of force fields designed for calculating phase equilibria and thermodynamic properties are usually adjusted to experimental data of pure components.
In addition, the calculation results are compared with those obtained by the PC-SAFT EoS, which is known to be useful for calculating phase equilibria of polymer systems.
A comprehensive thermodynamic model has been applied to calculating phase equilibria, speciation, and other thermodynamic properties of systems that are of geochemical importance.
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We measured inter-regional phase synchronization by calculating phase-locking values.
Shuffling was performed by randomizing the order of trials and, then, calculating phase-locking between events not recorded at the same time.
The calculated phase diagrams agreed well with the experimental ones.
The calculated phase equilibria are compared with experiments.
A phase diagram construction algorithm based on the calculated phase reaction data in PandaT was developed.
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