Investigating the Phase Space Dynamics of Hamiltonian Systems by the Origin-Fate Map
Ferris Moser
TL;DR
This work tackles how phase-space transport in a two-degree-of-freedom caldera potential organizes itself when multiple exit channels are present. It combines the Origin--Fate Map (OFM) framework with Lagrangian Descriptors (LDs) to classify transport outcomes across a tunable stretching parameter $\lambda$, analyzed on two Poincaré surfaces. The main contributions show that at $\lambda=1.0$ the system exhibits highly symmetric OFM patterns, while for smaller $\lambda$ channel imbalance, figure-eight transport loops, and fractal-like transport boundaries emerge; LD ridges align with OFM boundaries, revealing the invariant-manifold skeleton driving transport. The results demonstrate that OFM and LD offer complementary, high-resolution tools for mapping transport in Hamiltonian systems and motivate applying the approach to other multi-channel potentials and time-dependent dynamics.
Abstract
We investigate phase space transport in a two-dimensional stretched caldera potential using the Origin-Fate Map (OFM) framework, complemented by Lagrangian Descriptor (LD) analysis. The caldera potential, a model for reaction dynamics with multiple exit channels, is adjusted by a stretching factor lambda that controls the directional bias of the four-saddle landscape. Several OFMs are constructed for two Poincare surfaces of section using forwards and backwards symplectic integration to assign each initial condition a channel of origin and fate. Our results reproduce the highly symmetric lambda = 1.0 patterns reported in Hillebrand et al. (Phys. Rev. E 108, 024211, 2023), and reveal, for smaller lambda, pronounced channel imbalance, figure-eight transport loops, and complex mixed-channel chaotic regions. Long-time integrations show a reduction of trapped regions with boundaries that exhibit self-similarity under deep zoom, revealing fractal-like structures. High-resolution OFMs and LD gradient maps uncover lobe dynamics and manifold structures that govern transport, showing near-perfect alignment between LD ridges and OFM boundaries.
