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Path integral based calculations of symmetrized time correlation functions. I.
S Bonella1, M Monteferrante, C Pierleoni
1Dipartimento di Fisica and CNISM, Università La Sapienza, Piazzale Aldo Moro 5, 00185 Rome, Italy. sara.bonella@roma1.infn.it
This study explores approximating quantum evolution with classical dynamics for correlation functions. We show how quantum delocalization complicates this approximation, even in the semiclassical limit.
Area of Science:
- Quantum mechanics
- Statistical mechanics
- Computational chemistry
Background:
- Calculating correlation functions is crucial in many areas of physics and chemistry.
- Approximating quantum evolution with classical dynamics offers computational advantages.
- Schofield's symmetrized time correlation function is a key quantity for such studies.
Purpose of the Study:
- To investigate the conditions and methods for approximating quantum evolution using classical dynamics.
- To analyze the role of quantum delocalization in the accuracy of these approximations.
- To provide a path integral-based derivation of Schofield's quantum correction factor.
Main Methods:
- Expressing Schofield's correlation function as a path integral in complex time.
- Utilizing sum and difference path variables.
- Performing Taylor series expansion of the path integral exponent to first and second order.
Main Results:
- A novel, path integral-based derivation of Schofield's quantum correction factor was achieved via first-order expansion.
- Second-order expansion revealed how quantum mechanical delocalization impacts correlation function approximations.
- The study demonstrates limitations in interpreting propagators as classical trajectories due to quantum effects.
Conclusions:
- Classical dynamics approximations for quantum evolution in correlation functions are feasible but have limitations.
- Quantum delocalization inherently complicates the semiclassical interpretation of propagators.
- Further theoretical development is needed to fully reconcile quantum and classical descriptions in these calculations.
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