Existence and Uniqueness of Solutions to the Generalized Hydrodynamics Equation
Friedrich H\"ubner, Benjamin Doyon

TL;DR
This paper proves the existence and uniqueness of solutions to the generalized hydrodynamics equation for integrable models, ensuring well-posedness and absence of shocks under broad initial conditions.
Contribution
It establishes the first rigorous proof of existence and uniqueness for the full GHD equation, including differentiable and weak solutions, using a novel fixed-point approach.
Findings
Solutions exist and are unique for a large class of initial conditions.
Differentiable initial conditions lead to differentiable solutions at all times.
Weak initial conditions like the Riemann problem have unique weak solutions that preserve entropy.
Abstract
The generalized hydrodynamics (GHD) equation is the equivalent of the Euler equations of hydrodynamics for integrable models. Systems of hyperbolic equations such as the Euler equations usually develop shocks and are plagued by problems of uniqueness. We establish for the first time the existence and uniqueness of solutions to the full GHD equation and the absence of shocks, from a large class of initial conditions with bounded occupation function. We assume only absolute integrability of the two-body scattering shift. In applications to quantum models of fermionic type, this includes all commonly used physical initial states, such as locally thermal states and zero-entropy states. We show in particular that differentiable initial conditions give differentiable solutions at all times and that weak initial conditions such as the Riemann problem have unique weak solutions which preserve…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsAquatic and Environmental Studies · Differential Equations and Numerical Methods · Arctic and Antarctic ice dynamics
