The Dynamical Matching Mechanism in Phase Space for Caldera-Type Potential Energy Surfaces
arXiv:1911.09644 · doi:10.1016/j.cplett.2020.137199
Abstract
Dynamical matching occurs in a variety of important organic chemical reactions. It is observed to be a result of a potential energy surface (PES) having specific geometric features. In particular, a region of relative flatness where entrance and exit to this region is controlled by index-one saddles. Examples of potential energy surfaces having these features are the so-called caldera potential energy surfaces. We develop a predictive level of understanding of the phenomenon of dynamical matching in a caldera potential energy surface. We show that the phase space structure that governs dynamical matching is a particular type of heteroclinic trajectory which gives rise to trapping of trajectories in the central region of the caldera PES. When the heteroclinic trajectory is broken, as a result of parameter variations, then dynamical matching occurs.
9 pages, 2 figures
References in corpus (3)
Cited by in corpus (3)
- The Nature of Reactive and Non-reactive Trajectories for a Three Dimensional Caldera Potential Energy Surface
- The Influence of a Pitchfork Bifurcation of the Critical Points of a Symmetric Caldera Potential Energy Surface on Dynamical Matching
- From Poincare Maps to Lagrangian Descriptors: The Case of the Valley Ridge Inflection Point Potential