Thermodynamic integration

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Thermodynamic integration is used to calculate the difference in the Helmholtz energy function, , between two states. The path must be continuous and reversible. One has a continuously variable energy function such that , and ,

where

.

Isothermal integration

Ref. 1 Eq. 5:

Isobaric integration

Ref. 1 Eq. 6:

where is the Gibbs energy function and is the enthalpy.

Isochoric integration

Ref. 1 Eq. 7:

where is the internal energy.

See also

References

  1. C. Vega, E. Sanz, J. L. F. Abascal and E. G. Noya "Determination of phase diagrams via computer simulation: methodology and applications to water, electrolytes and proteins", Journal of Physics: Condensed Matter 20 153101 (2008) (section 4)