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The physical relevance of fluctuations in a probabilistic language demands the illustration of basic mathematical tools, including the central limit theorem and the theory of large deviations. A short summary about random matrix theory precedes the model of generalized random walks, which includes Levy flights and walks as representations of anomalous diffusive processes. Einstein's approach to the role of fluctuations in thermodynamic processes is detailed for both an isolated and a thermalized thermodynamic system. An introduction to stochastic thermodynamics and to generalized fluctuation theorems is finally discussed.
An interface is rough if the mean square fluctuations of its position diverge at large times and system sizes. This may occur when the interface is driven out of equilibrium in the presence of some noise and the way roughness diverges defines suitable critical exponents. We introduce and discuss extensively two important universality classes: the Edwards–Wilkinson and the Kardar–Parisi–Zhang. The latter has been the subject of renewed interest since it was possible to determine analytically the whole spectrum of fluctuations and it was found an experimental system satisfying such predictions with great accuracy. The last part of the chapter is devoted to nonlocal models, specifically the celebrated Diffusion Limited Aggregation.
The phenomenological theory proposed by Einstein for interpreting the phenomenon of Brownian motion is described in detail. The alternative approaches due to Langevin and Fokker–Planck are also illustrated. The theory of Markov chains is also reported as a basic mathematical approach to stochastic processes in discrete space and time; various of its applications, for example, the Monte Carlo method, are also illustrated. The theory of stochastic equations, as a representation of stochastic processes in continuous space–time, is discussed and used for obtaining a generalized, rigorous formulation of the Langevin and Fokker–Planck equations for generalized fluctuating observables. The Arrhenius formula as an example of the first exit-time problem is also derived.
We explore a reduced-order model (ROM) of plane Couette flow with a view to performing near-wall turbulence control. The ROM is derived through Galerkin projections of the incompressible Navier–Stokes system onto a basis of controllability modes. Such ROMs were found to reproduce key aspects of turbulence dynamics in Couette flow with only a few hundred degrees of freedom, and here we use them to devise a control strategy. We consider a ROM with an extra forcing term whose structure is given by a combination of eigenfunctions of a linear viscous diffusion equation, optimised in order to minimise the total fluctuation energy. The optimisation is performed at Reynolds numbers $Re=1000, 2000, 3000$, and produces a novel control mechanism wherein the optimal forcing leads the flow to laminarisation in all cases. The forcing acts by reducing the shear in a large portion of the channel, hindering the main energy input mechanism. The forced flow possesses a new laminar solution which is linearly stable at $Re=1000$ and unstable at higher $Re$, but whose transient growth of streaky structures is substantially lower than that of laminar Couette flow, leading the flow to full laminarisation when the forcing is removed. Forcings optimised in the ROM are subsequently applied in direct numerical simulations (DNS). The same control mechanisms are observed in the DNS, where laminarisation is also achieved. We show that the ROMs provide an effective framework to design turbulence control strategies, despite the high degree of truncation, which opens up interesting possibilities for turbulence control.
Based on data from pore-resolved direct numerical simulation of turbulent flow over mono-disperse random sphere packs, we evaluate the budgets of the double-averaged turbulent kinetic energy (TKE) and the wake kinetic energy (WKE). While TKE results from temporal velocity fluctuations, WKE describes the kinetic energy in spatial variations of the time-averaged flow field. We analyse eight cases which represent sampling points within a parameter space spanned by friction Reynolds numbers $Re_\tau \in [150, 500]$ and permeability Reynolds numbers $Re_K \in [0.4, 2.8]$. A systematic exploration of the parameter space is possible by varying the ratio between flow depth and sphere diameter $h/D \in \{ 3, 5, 10 \}$. With roughness Reynolds numbers of $k_s^+ \in [20,200]$, the simulated cases lie within the transitionally or fully rough regime. Revisiting the budget equations, we identify a WKE production mechanism via viscous interaction of the flow field with solid surfaces. The scaling behaviour of different processes over $Re_K$ and $Re_\tau$ suggests that this previously unexplored mechanism has a non-negligible contribution to the WKE production. With increasing $Re_K$, progressively more WKE is transferred into TKE by wake production. A near-interface peak in the TKE production, however, primarily results from shear production and scales with interface-related scales. Conversely, further above the sediment bed, the TKE budget terms of cases with comparable $Re_\tau$ show similarity under outer-scaling. Most transport processes relocate energy in the near-interface region, whereas pressure diffusion propagates TKE and WKE into deeper regions of the sphere pack.
This final chapter is a short introduction to pattern-forming systems, which highlights a few concepts and models rather than pretending to give a general overview (which is impossible in 40 pages). We focus on stationary bifurcations, distinguishing between scenarios where the critical wavevector vanishes and where it is a finite value, because they have different nonlinear behaviors. A few pages are devoted to describe some different experimental setups: thermal convection (a fluid heated from below, showing the rising of convection cells); unstable growth process (under particle deposition, with the formation of mounds); and a rotating mixture of granular systems (with their phase separation).
This chapter essentially faces the following question: If at equilibrium a system has a phase transition between a disordered phase and an ordered phase, how does it relax to equilibrium if it is quenched from the former to the latter phase? Quenching means that an external parameter, typically the temperature, is suddenly changed. The answer depends on some relevant factors: if dynamics conserves or not the order parameter; if the order parameter is a scalar or a vector; if long-range interactions are present or not. We devote special attention to the short-range Ising model, but we also consider nonscalar systems. If the order parameter is conserved, its value before quenching is also an important parameter, allowing to distinguish between two different trigger mechanisms of the relaxation process: spinodal decomposition and thermally activated nucleation.