Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 69 4 b Solution Created 2026-10-03 Updated 2026-10-14
Take a positive initial separation . In the dissipation range, the velocity field is smooth, so the difference of the two Lagrangian trajectories obeys the linearized separation equation . Chaotic stretching gives a positive Lyapunov exponent of order and a typical separationThis needs a nonzero initial separation: exactly coincident particles remain coincident in a smooth flow.
Once lies in the inertial range, the Kolmogorov 1941 theory gives a relative speed of order . A scale-local typical-separation estimate integrates toAfter loss of the entry-scale memory, the statistical Richardson pair dispersion law is . Thus the characteristic separation grows as while . This is a statistical scaling closure, rather than a deterministic equation for every pair.
For , the particle velocities become approximately independent. If their Lagrangian velocity autocorrelations have a finite Lagrangian integral time , the diffusive large-scale pair dispersion has effective relative diffusivity of order . After a further velocity-decorrelation transient,This is the long-time mechanism of Taylor turbulent dispersion applied to the difference of two decorrelated trajectories. The root mean square separation eventually loses memory of the term.
Reaching at the end of the inertial range takesOrder-one coefficients depend on the dispersion closure. The initial exponential stage can take a long time if is extremely small, but the inertial-range stage is of order one outer eddy turnover time.
The three-regime turbulent pair-separation model in the sketch matches the regimes continuously for illustration. Its coefficients are schematic; the universal claims here are the scaling powers under the stated stretching, locality and decorrelation assumptions.
Three-regime turbulent pair-separation model 2026-10-14
For positive initial separation below the Kolmogorov length scale, a phenomenological pair-dispersion model has smooth-flow exponential stretching, inertial-range Richardson pair dispersion, and diffusive large-scale pair dispersion beyond the integral scale of turbulence. A positive Lyapunov exponent is needed for the first regime, scale locality and initial-memory loss for the second, and integrable relative-velocity autocorrelation for the third. The inertial-range crossing time is of order , one outer eddy turnover time.
