Mardi 24 juin, Centre de Physique Théorique, Luminy
Journée de Dynamique Non Linéaire
Résumé du séminaire de Stefano Ruffo I will discuss the problem of "ensemble inequivalence": the disagreement in the value of averages (energy, temperature, etc.) in different statistical ensembles which persists in the thermodynamic limit. This can appear when the interaction is long-range, i.e., potentials decay at large distances with a power less or equal than the Euclidean space dimension. A large class of long-range interactions that is frequently introduced in statistical physics is the one of mean-field models. We have solved exactly some mean-field models (e.g. the Blume-Emery-Griffiths model), both in the canonical and in the microcanonical ensemble and proven that these give inequivalent predictions when the system is inhomogeneous, for instance at a first-order phase transition. In particular, we have shown that "negative specific heat" and "temperature jumps" can arise in the microcanonical ensemble. Both these phenomena are potentially observable in nature: recently signals of the presence of a negative specific heat have been observed in the melting process of atomic clusters, where the range of the interaction is of the order of the size of the system, mimicking the effect of long-range interactions. We have also shown that these peculiar effects are not specific of the mean-field limit, but can be present also when the interaction is weakly decaying in space. I will briefly discuss also the appearence of coherent structures in the dynamics of systems with long-range interaction, whose lifetime increases with system size.
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Résumé du séminaire de Dmitri Volchenkov Energy E dissipated in a mass of turbulent fluid per second in an isotropic homogeneous fully developed turbulent flow is constant in the inertial range of scales [Kolmogorov, 1941]. Swirling eddies of an immiscible fluid injected into the flow provoke it into turbulence damping, since the energy dissipation rate E(k) acquires a minimum selecting the eddies of an optimal size l, while the others are damped out. The flow with a finite gyrotropy of order 1/l is unstable and responses with bursts for any small perturbation. However, it can be stabilized by a spatially homogeneous "mean" magnetic field.
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