Thermodynamic integration: Difference between revisions

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'''Related reading'''
'''Related reading'''
*[http://dx.doi.org/10.1063/1.3023062 Enrique de Miguel "Estimating errors in free energy calculations from thermodynamic integration using fitted data", Journal of Chemical Physics '''129''' 214112 (2008)]
*[http://dx.doi.org/10.1063/1.3023062 Enrique de Miguel "Estimating errors in free energy calculations from thermodynamic integration using fitted data", Journal of Chemical Physics '''129''' 214112 (2008)]
*[http://dx.doi.org/10.1063/1.4921884 Maria Concetta Abramo, Carlo Caccamo, Dino Costa, Paolo V. Giaquinta, Gianpietro Malescio, Gianmarco Munaò, and Santi Prestipino "On the determination of phase boundaries via thermodynamic integration across coexistence regions", Journal of Chemical Physics '''142''' 214502 (2015)]
[[category:classical thermodynamics]]
[[category:classical thermodynamics]]

Revision as of 12:08, 23 June 2015

Thermodynamic integration is used to calculate the difference in the Helmholtz energy function, , between two states. The path must be continuous and reversible, i.e., the system must evolve through a succession of equilibrium states (Ref. 1 Eq. 3.5)

Isothermal integration

At constant temperature (Ref. 2 Eq. 5):

Isobaric integration

At constant pressure (Ref. 2 Eq. 6):

where is the Gibbs energy function and is the enthalpy.

Isochoric integration

At constant volume (Ref. 2 Eq. 7):

where is the internal energy.

See also

References

  1. J. A. Barker and D. Henderson "What is "liquid"? Understanding the states of matter ", Reviews of Modern Physics 48 pp. 587 - 671 (1976)
  2. 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)

Related reading