Global dissipative solutions of the 3D Naiver-Stokes and MHD equations
Alexey Cheskidov, Zirong Zeng, Deng Zhang
TL;DR
The paper establishes the global existence and nonuniqueness of dissipative weak solutions to the 3D Navier–Stokes and MHD equations for divergence-free initial data in the critical space $H_x^{1/2}$, while also obtaining continuous-energy solutions for rough $L_x^2$ data. It introduces a telescoping convex integration framework built around a $ vLambda(t)$-dependent (the $ vLambda$-MHD) approximation, a frequency-truncation scheme, and heat correctors that leverage dissipation to achieve energy decay along prescribed channels. By constructing backward/forward time sequences and carefully balancing energy and cross helicity profiles, the method produces infinitely many solutions with distinct energy trajectories, including energy-decreasing ones, thereby violating uniqueness in the dissipative class. The approach extends to stochastic settings and provides a detailed, technically involved pathway to control Reynolds and magnetic stresses through a layered perturbation scheme with precise estimates for perturbations, heat corrections, and various error terms. The results have implications for the understanding of turbulence-like behaviors and nonuniqueness phenomena in viscous, dissipative fluid and MHD models, highlighting the nuanced roles of dissipation and frequency interactions in weak solution theory.
Abstract
For any divergence free initial data in $H^\frac12$, we prove the existence of infinitely many dissipative solutions to both the 3D Navier-Stokes and MHD equations, whose energy profiles are continuous and decreasing on $[0,\infty)$. If the initial data is only $L^2$, our construction yields infinitely many solutions with continuous energy, but not necessarily decreasing. Our theorem does not hold in the case of zero viscosity as this would violate the weak-strong uniqueness principle due to Lions. This was achieved by designing a convex integration scheme that takes advantage of the dissipative term.
