Kolmogorov Turbulent Cascade

Energy cascades from large eddies to small scales — E(k) ∝ k⁻⁵/³

Parameters


K41 theory (Kolmogorov 1941):
E(k) = C_K ε²/³ k⁻⁵/³

Energy injected at large scales (small k) cascades through inertial range to Kolmogorov microscale η=(ν³/ε)^(1/4) where viscous dissipation occurs.

Inertial range: eddies break up without direct viscous effect — universal scaling.

Exact result: ⟨(δu)³⟩ = −4/5 εℓ (4/5 law)