Thermodynamic integration

From Wikipedia, the free encyclopedia

Thermodynamic integration is a method used to compare the difference in free energy between two given macroscopic states (e.g., A and B) whose potential energies and have different dependences on the spatial coordinates. Because the free energy of a system is not simply a function of the phase space coordinates of the system, but is instead a function of the Boltzmann-weighted integral over phase space (i.e. a partition function), the free energy difference between two macroscopic states cannot be calculated directly from the potential energy of just two coordinate sets (for state A and B respectively). In thermodynamic integration, the free energy difference is calculated by defining a thermodynamic path between the states and integrating over ensemble-averaged enthalpy changes along the path. Such paths can either be real chemical processes or alchemical processes. An example alchemical process is the Kirkwood's coupling parameter method.[1]

See also

References

Related Articles

Wikiwand AI