Bentkamp, Lalescu and Wilczek (Nat. Commun. 10, 3550, 2019) showed that conditioning Lagrangian tracer statistics in homogeneous isotropic turbulence on the squared particle acceleration coarse-grained over a viscous time scale Θ\Theta decomposes the strongly intermittent single-particle statistics into close-to-Gaussian subensembles. Their characteristic-functional framework reproduces acceleration, velocity-increment, and dispersion statistics across Rλ≈210R_{\lambda}\approx210–509509, but only by taking the PDF f(α)f(\alpha) of the coarse-grained squared acceleration and the conditional velocity autocorrelations Cα(τ)C_{\alpha}(\tau) directly from direct numerical simulation (DNS) data — the framework is descriptive, not predictive. The open problem is to supply theoretically grounded, non-DNS-fed models for f(α)f(\alpha) and Cα(τ)C_{\alpha}(\tau) that make the framework fully predictive, together with the auxiliary open issue the same authors raise: whether the optimal coarse-graining time Θ\Theta approaches a Reynolds-number-independent asymptote at very high RλR_{\lambda}.

Background

In the Lagrangian description of turbulence one follows individual fluid tracers — idealized point particles advected with the flow — rather than the velocity field at fixed points. Single-particle Lagrangian statistics govern turbulent dispersion and mixing and are paradigmatic examples of intermittency: tracer accelerations a(t)\mathbf{a}(t) display extended quiescent periods interrupted by violent, short-lived bursts when the particle passes through intense small-scale structures such as vorticity filaments. As a consequence, the probability density function (PDF) of a single acceleration component has very heavy (nearly exponential-to-stretched-exponential) tails, with a flatness — the normalized fourth moment ⟨a4⟩/⟨a2⟩2\langle a^4\rangle/\langle a^2\rangle^2, equal to 3 for a Gaussian — far above the Gaussian value, and this non-Gaussianity relaxes only slowly with time scale. Quantitative studies rely on direct numerical simulation (DNS, i.e., fully resolved numerical solution of the Navier–Stokes equations) and on high-resolution particle-tracking experiments, typically reported as functions of the Taylor-scale Reynolds number RλR_{\lambda} (the standard dimensionless measure of the intensity of turbulence, formed from the root-mean-square velocity fluctuation, the mean energy dissipation rate, and the kinematic viscosity; larger RλR_{\lambda} means a wider separation between the largest and smallest flow scales), with τη\tau_{\eta} the Kolmogorov viscous time scale setting the smallest temporal scale of the flow.

Classical reductionist attempts — multifractal models (models in which the local scaling exponents of the small-scale statistics form a whole spectrum of values rather than a single number, reflecting the spotty spatial structure of intense dissipation), superstatistics (modeling non-Gaussian statistics as a superposition of simpler distributions with a fluctuating parameter), and refined-similarity formulations in terms of locally averaged dissipation — had not produced a practically useful decomposition of the full Lagrangian ensemble into simple subensembles. Bentkamp, Lalescu and Wilczek (2019) introduced the persistent acceleration: the squared acceleration coarse-grained over a viscous time window, α(t)≡∫−∞∞dτ FΘ(τ) a2(t+τ),\alpha(t)\equiv\int_{-\infty}^{\infty}\mathrm{d}\tau\,F_{\Theta}(\tau)\,\mathbf{a}^2(t+\tau), with FΘF_{\Theta} a Gaussian filter of standard deviation Θ\Theta (in practice Θ≈2\Theta\approx2–3 τη3\,\tau_{\eta}). Conditioning on α\alpha partitions trajectories into subensembles of different local small-scale activity, and — remarkably — the conditional single-component acceleration statistics within each subensemble are close to Gaussian, with the conditional variance growing roughly linearly in α\alpha.

This observation yields a closed kinematic framework. The complete statistical information of a one-component Lagrangian velocity time series u(t)u(t) is encoded in its characteristic functional ϕ[ϑ]=⟨exp⁡(i∫dt ϑ(t)u(t))⟩\phi[\vartheta]=\langle\exp(\mathrm{i}\int\mathrm{d}t\,\vartheta(t)u(t))\rangle (the generating object of the functional formalism of turbulence, from which all multi-time statistics follow by functional differentiation). The authors show that ϕ\phi is well approximated by a probabilistic superposition of Gaussian characteristic functionals conditioned on α\alpha, ϕ[ϑ]=∫0∞dα f(α) ϕαG[ϑ]\phi[\vartheta]=\int_0^\infty\mathrm{d}\alpha\,f(\alpha)\,\phi_{\alpha}^{\mathrm{G}}[\vartheta], where the Gaussian subensemble functional is fully determined by the conditional single-component velocity autocorrelation function Cα(τ)=⟨u(t0−τ/2) u(t0+τ/2)∣α(t0)=α⟩C_{\alpha}(\tau)=\langle u(t_0-\tau/2)\,u(t_0+\tau/2)\mid\alpha(t_0)=\alpha\rangle. Projecting this functional gives explicit superposition formulas for the velocity PDF (mixture of Gaussians with variances Cα(0)C_{\alpha}(0)), the acceleration PDF (variances −Cα′′(0)-C_{\alpha}''(0)), and the velocity-increment PDFs (variances given by the conditional second-order structure function), and by construction the framework is consistent with the kinematic evolution equations of these PDFs. Fed with DNS-extracted f(α)f(\alpha) (extremely broad, spanning more than six orders of magnitude, with an approximately log-normal right tail) and Cα(τ)C_{\alpha}(\tau) (larger variance and faster decorrelation at larger α\alpha, with a secondary oscillatory maximum at the largest α\alpha, attributed to particle trapping in vortical structures), the framework accurately reproduces acceleration, increment, velocity, correlation, and dispersion statistics at Rλ≈210R_{\lambda}\approx210–509509.

The framework is thus descriptive by construction: both ingredients, the PDF f(α)f(\alpha) and the conditional correlations Cα(τ)C_{\alpha}(\tau), are extracted from DNS. The authors state explicitly that only when theoretical models for these two ingredients become available does the framework become fully predictive — which they identify as an exciting direction for future work. A further issue is raised: the only free parameter, the coarse-graining time Θ\Theta, shows data-set-dependent optimal values (near 3 τη3\,\tau_{\eta} at Rλ≈210R_{\lambda}\approx210 and 350350, near 2 τη2\,\tau_{\eta} at Rλ≈509R_{\lambda}\approx509) without a clear trend, with large-scale intermittency suspected to play a role; whether Θ\Theta reaches an asymptotic, Reynolds-number-independent viscous value at very high RλR_{\lambda} is posed as a question for the next generation of experiments and simulations. In addition, while second-order and many finite-dimensional statistics are captured essentially exactly (some by design), the authors document moderate deviations in higher-order measures, most visibly the acceleration flatness, which is systematically overestimated for too small Θ\Theta and underestimated for too large Θ\Theta.

Problem Statement

Turn the persistent-acceleration decomposition of Lagrangian turbulence from a descriptive into a predictive framework. Specifically, for homogeneous isotropic turbulence:

  1. (Core) Derive or construct theoretically grounded models — not extracted or calibrated from DNS of the target statistics — for (i) the PDF f(α)f(\alpha) of the coarse-grained squared Lagrangian acceleration α(t)=∫−∞∞dτ FΘ(τ) a2(t+τ)\alpha(t)=\int_{-\infty}^{\infty}\mathrm{d}\tau\,F_{\Theta}(\tau)\,\mathbf{a}^2(t+\tau) (with FΘF_{\Theta} a Gaussian filter of width Θ∼\Theta\sim a few τη\tau_{\eta}), including its broad, near-log-normal right tail and its Reynolds-number dependence, and (ii) the conditional single-component velocity autocorrelation functions Cα(τ)C_{\alpha}(\tau), including the growth of Cα(0)C_{\alpha}(0) with α\alpha, the faster decorrelation at larger α\alpha, and the secondary oscillatory maximum at the largest α\alpha. A successful answer must, when inserted into the superposition formulas f(u)=∫dα f(α) g(u;Cα(0))f(u)=\int\mathrm{d}\alpha\,f(\alpha)\,g(u;C_{\alpha}(0)), f(a)=∫dα f(α) g(a;−Cα′′(0))f(a)=\int\mathrm{d}\alpha\,f(\alpha)\,g(a;-C_{\alpha}''(0)), and the corresponding increment and dispersion expressions — where g(x;σ2)g(x;\sigma^2) denotes a zero-mean Gaussian probability density of variance σ2\sigma^2, consistent with the near-Gaussianity of the conditional subensembles — reproduce measured (DNS or experimental) single-particle statistics — acceleration PDF and flatness, velocity-increment PDFs across time lags, velocity and acceleration autocorrelations, and mean-squared displacement — quantitatively and across at least two Reynolds numbers, with all model parameters fixed a priori from theory or from measurements independent of the validation data.

  2. (Auxiliary, raised by the same authors) Determine, empirically and/or theoretically, whether the optimal coarse-graining time Θ\Theta approaches an asymptotic, Reynolds-number-independent value (in units of the Kolmogorov time τη\tau_{\eta}) at very high RλR_{\lambda}, and in particular disentangle the roles of Reynolds number and large-scale intermittency in the observed data-set dependence of the optimal Θ\Theta.

Both components are required for a complete answer. The two are scientifically linked aspects of one objective: they supply the missing ingredients and settle the only free parameter of the same characteristic-functional decomposition, and a complete answer establishes the first fully predictive, self-consistent statistical theory of Lagrangian single-particle turbulence within this framework. (A natural further generalization — extending the decomposition to multi-particle statistics or to non-isotropic, inhomogeneous flows — is not part of the author-declared problem and is not required.)

References

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