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
, between two states.
The path must be continuous and reversible.
One has a  continuously variable energy function  such that
 such that
 ,
,   and
 and  ,
,  
 
where
 . .
Isothermal integration
Ref. 1 Eq. 5:
 
Isobaric integration
Ref. 1 Eq. 6:
 
where  is the Gibbs energy function and
 is the Gibbs energy function and  is the enthalpy.
 is the enthalpy.
Isochoric integration
Ref. 1 Eq. 7:
 
where  is the internal energy.
 is the internal energy.
See also
References
- 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)