This research program develops a spectral-fractal approach to tackle global regularity in fluid equations, suggesting significant implications for mathematics.
We develop a spectral-fractal approach to the 3D incompressible Navier-Stokes global regularity problem — one of the Clay Millennium Prize Problems — combining four innovations that exploit the fine structure of the nonlinear term, satisfying the Tao supercriticality barrier. The first innovation is the intrinsic emergence of √2 from incompressibility: when a vortex tube stretches by factor λ, incompressibility forces transverse contraction by 1/√λ. For one-octave doubling (λ = 2), the contraction ratio is 1/√2. This is geometry, not assumption — verifiable from ∇·u = 0 alone. The second is a visco-elastic analogy: viscous dissipation acts as a super-Hookean restoring force in the enstrophy cascade, with dissipation dominance scaling as (1/2)^n per cascade level — exponential suppression without any parameter choice. The third is a fractal-temporal reparametrization exploiting the bounded enstrophic time budget from the energy identity: the total time during which enstrophy can be large is unconditionally finite. The fourth is the Kesten-Stigum reconstruction threshold applied to the enstrophy cascade tree, showing that the cascade is in the disordered phase (b·η² ≪ 1) and no coherent enstrophy concentration can survive. What is proved unconditionally: √2 emergence from incompressibility; exponential dissipation dominance (1/2)^n; bounded enstrophic time budget; super-Hookean structure; bootstrap closure conditional on d_eff < 2; the cascade attractor d* = √2 with viscous contractivity |Φ_ν'(d*)| < 1; KS disordered phase. What remains conditional: Path A (attractor bootstrap) requires the fractal support theorem, which involves a standard PDE bootstrap circularity (smooth → damping → d* < 2 → regularity → smooth). Path B (KS threshold) requires the passage from BKM blow-up criterion to cascade coherence, which is proposed but not proved, and the cascade is not an exact tree due to Biot-Savart non-locality. A crucial dichotomy distinguishes NS from Euler: for Euler (ν = 0), Φ₀'(d*) ≈ 1.02 > 1 (unstable — blow-up possible). For NS (ν > 0), Φ_ν'(d*) < 1 (stable — regularity forced). Viscosity is the mechanism, consistent with the Clay problem asking about NS, not Euler. Empirical support: DNS measurements of vorticity fractal dimension D ≈ 1.3–1.5 (She et al. 1990, Jiménez et al. 1993), consistent with √2 ≈ 1.414. Independent contributions (√2 emergence, elastic analogy, enstrophic time budget, NS/Euler distinction) are valuable regardless of whether the full program succeeds.
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Thierry Marechal (2026) studied this question.
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