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Effective Temperature

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A few rambling thoughts before we begin: I've been feeling increasingly weak lately[1], but after exercising today I feel refreshed and clear-headed, and my thinking has become noticeably more active. It seems like a good time to sort out a physics concept that has been bothering me recently (my memory really is poor, so this is as much for my future self as anyone else).

Introduction ​

The effective temperature discussed here refers to a concept that arises in the non-equilibrium states of ordinary classical systems: it allows certain properties of a non-equilibrium system to be mapped onto the same properties of an equilibrium system at a higher temperature.

From the fundamental laws of thermodynamics, the Gibbs relation, the FDR, kinetic energy, and potential energy, one can compute a "temperature" for a non-equilibrium system, called the effective temperature; different approaches yield different effective temperatures[2]. The fact that different methods give inconsistent effective temperatures makes the concept elusive.[3]

Vaguely, the effective temperature seems to be just a parameter, and one without a clear, universal meaning — even though the motion of a non-equilibrium system is unlikely to be the same in every direction and at every scale.

I would venture that at the end of the last century[4] the concept of effective temperature was not very clear, but it can broadly be divided into two types: those computed from dynamical quantities and those computed from thermodynamic quantities. These days, fluctuation-dissipation relations (FDRs) are widely used. Who first computed it from FDRs remains to be verified, but Professor Ludovic Berthier has done a considerable amount of research in this area. This article will more or less center on the FDRs method throughout.

FDRs Method ​

In a non-equilibrium system under steady-state simple shear, for any two physical quantities A(t) and B(t), one can write their correlation (cross-correlation) function:

CAB(t)=⟨A(t+t0)B(t0)⟩−⟨A(t0)⟩⟨B(t0)⟩

The response function:

RAB(t)≡δA(t+t0)δhB(t0)

Here hB(t0) is a perturbing field (acting on some of the particles) at time t0 that is conjugate to B(t). If one takes A(t)=⟨1N′∑jϵiexp⁡(ikri(t))⟩ and B(t)=⟨2∑jϵjcos⁡(ikri(t))⟩, then CAB(t) can be shown to be the Self-Intermediate Scattering Function (ISF), a quantity generally used to characterize relaxation among particles.

In equilibrium, the correlation function and the response function satisfy the fluctuation-dissipation theorem:

TRAB(t)=dCAB(t)dt

Meanwhile, the susceptibility (I could not find a Chinese translation for this, so let us call it the "sensitization rate" for now) can be obtained by integrating the response function:

χAB(t)≡∫0tdt′RAB(t′)

If the field h_{B} is not too large and linear response holds, then the susceptibility can be used to write

TχAB(t)=CAB(0)−CAB(t)

The effective temperature TeffAB satisfies RAB(t)=−1TeffABdCAB(t)dt, and on a plot of χAB−CAB the effective temperature appears as the linear relation of the curve, as shown in the figure:

One glance at this figure makes it clear that there are a great many tricks involved in computing it. In theory the effective temperature is unique and independent of the chosen observable. This holds at the mean-field level, and Professor Ludovic Berthier's paper proves that it also holds, at least, in the Kob-Anderson supercooled liquid model[5].

References ​


  1. Most likely caused by staying up late, which inevitably brings to mind a certain protagonist from a recent anime whose mental state is very similar ↩︎

  2. Although I think this is entirely normal ↩︎

  3. https://doi.org/10.1126/sciadv.abg6766 ↩︎

  4. Among the old papers I have seen and still remember ↩︎

  5. https://doi.org/10.1103/PhysRevLett.89.095702 ↩︎