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On the “Matsubara heating” of overtone intensities and Fermi splittings

Raz L. Benson, Stuart C. Althorpe

2021The Journal of Chemical Physics20 citationsDOIOpen Access PDF

Abstract

Classical molecular dynamics (MD) and imaginary-time path-integral dynamics methods underestimate the infrared absorption intensities of overtone and combination bands by typically an order of magnitude. Plé et al. [J. Chem. Phys. 155, 104108 (2021)] have shown that this is because such methods fail to describe the coupling of the centroid to the Matsubara dynamics of the fluctuation modes; classical first-order perturbation theory (PT) applied to the Matsubara dynamics is sufficient to recover most of the lost intensity in simple models and gives identical results to quantum (Rayleigh–Schrödinger) PT. Here, we show numerically that the results of this analysis can be used as post-processing correction factors, which can be applied to realistic (classical MD or path-integral dynamics) simulations of infrared spectra. We find that the correction factors recover most of the lost intensity in the overtone and combination bands of gas-phase water and ammonia and much of it for liquid water. We then re-derive and confirm the earlier PT analysis by applying canonical PT to Matsubara dynamics, which has the advantage of avoiding secular terms and gives a simple picture of the perturbed Matsubara dynamics in terms of action-angle variables. Collectively, these variables “Matsubara heat” the amplitudes of the overtone and combination vibrations of the centroid to what they would be in a classical system with the oscillators (of frequency Ωi) held at their quantum effective temperatures [of ℏΩi coth(βℏΩi/2)/2kB]. Numerical calculations show that a similar neglect of “Matsubara heating” causes path-integral methods to underestimate Fermi resonance splittings.

Topics & Concepts

Path integral formulationOvertoneQuantum dynamicsQuantumPhysicsQuantum mechanicsSpectral lineQuantum, superfluid, helium dynamicsSpectroscopy and Quantum Chemical StudiesAtmospheric Ozone and Climate
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