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The Feynman path integral formulation of non-dispersive Airy wave packets and their applications to the heavy meson mass spectra and ultra-cold neutrons

Paul Ferrante, Connor Donovan, Chueng-Ryong Ji

TL;DR

This work links the non-dispersive evolution of Airy wave packets in linear potentials to practical quantum systems by deriving the linear kernel via the Feynman path integral and solving Airy eigenstates for several linear-potentials. The authors map Airy function zeros to the confinement contribution in heavy-meson 1S-2S mass gaps within a 1+1D absolute linear potential, introducing a vacuum-energy offset $a\approx 141$ MeV that yields agreement with light-front calculations in the heavy-quark regime. They also apply the Airy solutions to ultra-cold neutrons bouncing in Earth's gravity, predicting quantized heights $h_n$ that align with experimental data and WKB results. Overall, the paper provides a unified 1+1D framework connecting Airy function mathematics to hadron spectroscopy and gravitational quantum states, with clear avenues for incorporating relativistic corrections and broader QCD-inspired models.

Abstract

We demonstrate the non-spreading behavior of Airy wave packets utilizing the Feynman path integral formulation of a linear potential, the Airy functions' zeros correspondence to heavy-meson mass spectroscopy, and their implications to the eigenstates of ultra-cold neutrons in Earth's gravitational field. We derive the linear kernel, and utilize the Feynman path integral time evolution to show that Airy function wave packets are non-dispersive in free space. We then model the confining contribution to 1S - 2S heavy meson mass gaps as a 1+1D absolute linear potential and look at the correspondence of the Airy function zeros. In doing so, we predicted the confining contribution to the mass gap of heavy mesons with a good accuracy when compared to calculations performed in the light front. Furthermore, we used these Airy function solutions to model the quantum states of a neutron under Earth's gravity. We show that the measured heights of a neutron can be modeled by the zeros of the Airy function, and compare to experimental data and predictions utilizing the WKB approximation.

The Feynman path integral formulation of non-dispersive Airy wave packets and their applications to the heavy meson mass spectra and ultra-cold neutrons

TL;DR

This work links the non-dispersive evolution of Airy wave packets in linear potentials to practical quantum systems by deriving the linear kernel via the Feynman path integral and solving Airy eigenstates for several linear-potentials. The authors map Airy function zeros to the confinement contribution in heavy-meson 1S-2S mass gaps within a 1+1D absolute linear potential, introducing a vacuum-energy offset MeV that yields agreement with light-front calculations in the heavy-quark regime. They also apply the Airy solutions to ultra-cold neutrons bouncing in Earth's gravity, predicting quantized heights that align with experimental data and WKB results. Overall, the paper provides a unified 1+1D framework connecting Airy function mathematics to hadron spectroscopy and gravitational quantum states, with clear avenues for incorporating relativistic corrections and broader QCD-inspired models.

Abstract

We demonstrate the non-spreading behavior of Airy wave packets utilizing the Feynman path integral formulation of a linear potential, the Airy functions' zeros correspondence to heavy-meson mass spectroscopy, and their implications to the eigenstates of ultra-cold neutrons in Earth's gravitational field. We derive the linear kernel, and utilize the Feynman path integral time evolution to show that Airy function wave packets are non-dispersive in free space. We then model the confining contribution to 1S - 2S heavy meson mass gaps as a 1+1D absolute linear potential and look at the correspondence of the Airy function zeros. In doing so, we predicted the confining contribution to the mass gap of heavy mesons with a good accuracy when compared to calculations performed in the light front. Furthermore, we used these Airy function solutions to model the quantum states of a neutron under Earth's gravity. We show that the measured heights of a neutron can be modeled by the zeros of the Airy function, and compare to experimental data and predictions utilizing the WKB approximation.

Paper Structure

This paper contains 15 sections, 83 equations, 6 figures, 1 table.

Figures (6)

  • Figure 1: Graph of Airy $\mathsf{Ai}(x)$ and $\mathsf{Bi}(x)$ functions.
  • Figure 2: The probability density $\rho(q=x/x_0,t)$ of an Airy wave packet at 3 different times. The probability density shows no dispersion, but instead accelerates along the $q$ axis. Here, $t$ is in units of $2m x_0^2/\hbar$.
  • Figure 3: Graph of $\mathsf{Ai}(x)$, with marked zeroes for $\mathsf{Ai}(x)$ and $\mathsf{Ai}'(x)$.
  • Figure 4: The first four eigenstates of the absolute linear potential, scaled to prevent overlap.
  • Figure 5: The first four eigenstates of the one sided linear potential, scaled to prevent overlap.
  • ...and 1 more figures