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The partition function and pressure estimators

The partition function for the isotropic isothermal-isobaric ensemble (NPT) is given by [39, 5]

  eqnarray597

where tex2html_wrap_inline4896 is the canonical partition function at volume V, tex2html_wrap_inline4900 is its discrete path integral counterpart Eq. (2.1), tex2html_wrap_inline4902 and tex2html_wrap_inline4904 is the external applied pressure. If the transformation tex2html_wrap_inline4906 is applied to Eq. (2.1) to make the volume dependence explicit, then the expression for the partition function becomes:

  eqnarray609

In Appendix B, the general problem of writing a path integral expression for a system in a finite size parallelpiped is reviewed. Inserting Eq. (3.2) into Eq. (3.1) yields the discrete Feynman path integral expression for the isotropic isothermal-isobaric partition

  eqnarray630

Again, the path integral formalism effectively replaces each classical point particle with a cyclic chain ``molecule'' [30]. Therefore, the quantum mechanical isothermal isobaric ensemble is analogous to the classical isothermal isobaric treatment of cyclic chain molecules.

The standard thermodynamic connection formula, tex2html_wrap_inline4908 , can be used to prove two important identities in the isothermal isobaric ensemble. The first is the pressure virial theorem [39, 15]

eqnarray652

and the second is work virial theorem[39, 15]

eqnarray659

Note, the internal work plus kT balances the external work. The excess factor of kT can be thought of as the work done by the ``piston'' to maintain the pressure balance. (Others favor a formulation where the work balances and the pressures are different by an additive factor of tex2html_wrap_inline4914 .)

The pressure connection formula can also be used to derive a discrete path integral expression for the average pressure in a quantum mechanical system. Using the relation

  equation665

and performing the volume derivative of tex2html_wrap_inline4916 Eq.(3.2), it is straightforward to show

eqnarray670

where tex2html_wrap_inline4918 tex2html_wrap_inline4920 is the derivative of the potential with respect to the explicit volume dependence present in the potential energy, only and

  equation689

Equation (3.8) will be referred to as the primitive pressure estimator. Note, this formula must be made consistent with periodic boundary conditions before it can be applied, in analogy with standard classical procedures[32]. Also, the specific definition of tex2html_wrap_inline4920 is complicated by the approximations made in truncating the potential energy function (see Appendix C).

The primitive pressure estimator can be manipulated to produce another pressure estimator in the same manner as the path integral virial kinetic energy estimator is obtained from the primitive kinetic energy estimator [13, 6]. The identity which can be proved via integration by parts [13, 6]

  equation699

is inserted into Eq.(3.8) to yield

  equation713

where where tex2html_wrap_inline4924 is the path centroid and tex2html_wrap_inline4926 is the centroid force. This pressure estimator, the virial pressure estimator, also must be made consistent with periodic boundary conditions before it can be applied. The path integral manifests quantum mechanical effects by replacing classical point particles with cyclic polymeric pseudomolecules [30]. The virial pressure estimator, tex2html_wrap_inline4928 , is the center of mass pressure virial of the pseudomolecular system[32, 35]. Finally, the derivation assumes the ``size'' of the pseudomolecules is small compared to the volume (i.e. surface terms are neglected). This approximation is already embodied in the form of path integral expression utilized in the derivation. If this approximation is not valid, the image approximation to the free particle propagator must be introduced (see Appendix B)[40, 41]. Finally, the virial expression can also be derived by assuming that only the particle centroid is scaled by the volume or the limits of integration of the other normal modes are not bound by the volume (see below).


next up previous
Next: Equations of motion Up: Isothermal-isobaric ensemble: Isotropic volume Previous: Isothermal-isobaric ensemble: Isotropic volume

Mark Tuckerman
Fri May 2 11:23:33 EDT 1997