Thermodynamic integration: Difference between revisions

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'''Thermodynamic integration''' is used to calculate the difference in the [[Helmholtz energy function]] between two states.
'''Thermodynamic integration''' is used to calculate the difference in the [[Helmholtz energy function]], <math>A</math>, between two states.
The path must be ''continuous'' and ''reversible''.
The path must be ''continuous'' and ''reversible''.
One has a  continuously variable energy function <math>U_\lambda</math> such that
One has a  continuously variable energy function <math>U_\lambda</math> such that
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:<math>\left.U_\lambda\right.=(1-\lambda)U_0 + \lambda U</math>.
:<math>\left.U_\lambda\right.=(1-\lambda)U_0 + \lambda U</math>.
==Isothermal integration==
Ref. 1 Eq. 5:
:<math>\frac{A(\rho_2,T)}{Nk_BT} = \frac{A(\rho_1,T)}{Nk_BT} + \int_{\rho_1}^{\rho_2} \frac{p(\rho)}{k_B T \rho^2} ~\mathrm{d}\rho </math>
==Isobaric integration==
Ref. 1 Eq. 6:
:<math>\frac{G(T_2,p)}{Nk_BT_2} = \frac{G(T_1,p)}{Nk_BT_1} - \int_{T_1}^{T_2} \frac{H(T)}{Nk_BT^2} ~\mathrm{d}T </math>
where <math>G</math> is the [[Gibbs energy function]] and <math>H</math> is the [[enthalpy]].
==Isochoric integration==
Ref. 1 Eq. 7:
:<math>\frac{A(T_2,V)}{Nk_BT_2} = \frac{A(T_1,V)}{Nk_BT_1}  - \int_{T_1}^{T_2} \frac{U(T)}{Nk_BT^2} ~\mathrm{d}T </math>
where <math>U</math> is the [[internal energy]].
==See also==
==See also==
*[[Gibbs-Duhem integration]]
*[[Gibbs-Duhem integration]]
==References==
==References==
#[http://dx.doi.org/10.1088/0953-8984/20/15/153101  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)
[[category:classical thermodynamics]]
[[category:classical thermodynamics]]

Revision as of 12:11, 4 August 2008

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)