The Steady State Fluctuation Relation for the Dissipation Function

Debra J. Searles, Lamberto Rondoni, Denis J. Evans

INTRODUCTION

Steady state fluctuation relations provide information about the probability distribution of time averages of certain phase variables for systems in nonequilibrium steady states: they express the ratio of the probabilities of observing positive and negative values of time averages of such variables. These relationships have received much attention over the past decade (see e.g. ). In fact, they are among the few exact results regarding nonequilibrium systems; close to equilibrium they lead to the Green-Kubo relations for linear transport coefficients ; they provide information about fluctuations in nanoscale systems and they show how irreversibility can emerge from time reversible dynamics.

The first such fluctuation relation (FR) for a nonequilibrium particle system was given in Ref., in 1993. It concerned fluctuations of time averages of the energy dissipation or equivalently the phase space contraction rate, for an isoenergetic shearing interacting particle system. In the isoenergetic dissipative system of Ref., the instantaneous energy dissipation equals the instantaneous phase space contraction rate. The form of the relation was the following:

where AA and −A-A were the time averaged values of the dissipation on steady state trajectory segments of duration τ\tau, and Pτ(A)P_{\tau}{\scriptscriptstyle{\displaystyle(A)}} is the steady state probability of observing the average value A (with some tolerance), in a time τ\tau. In analogy with the periodic orbit expansion for dynamical systems , the relation was derived heuristically using the “Lyapunov weights” in the long τ\tau limit, and was not expected to work at short τ\tau’s.

Paper motivated a number of works, in which various derivations of formulae formally similar to Eq.(1) were given for different systems, although for non-isoenergetic systems the phase space contraction rate and the energy dissipation are no longer instantaneously equal. Beginning in 1994, a series of papers by Evans and Searles focussed on the fluctuation properties of the “dissipation function” Ω\Omega, cf. Refs., while Gallavotti and Cohen, in 1995 et.seq.\mathit{et.}seq., considered the fluctuations of the time-averaged phase space contraction rate, −Λ-\Lambda, under the assumption that the dynamics is time reversible, transitive and Anosov or that the system satisfies the Chaotic Hypothesis (i.e.\mathit{i.e.} although the dynamics is not Anosov, for the purposes of this FR, it behaves as if it was Anosov), cf. Refs.. Various generalizations and extensions of these relations have been produced by different authors, see e.g. Refs..

In the literature, FR’s which superficially resemble the form of Eq.(1), are often collectively referred to as the Gallavotti-Cohen Fluctuation Relations, or instances of the Gallavotti-Cohen symmetry, although they may have subtly different meanings. Therefore, for the sake of clarity, we refer to the relation for the phase space contraction rate of Refs., as the Λ\Lambda-FR, while we refer to the relation for the dissipation function of Refs., as the Ω\Omega-FR. In the cases in which Ω=−Λ\Omega=-\Lambda, like those of , the two relations have the same content.

Ω\Omega-FR’s have been widely used and tested numerically and experimentally, for various transient as well as steady state systems (see e.g. ). Although the transient Ω\Omega-FR’s have been proven more than a decade ago, beginning with Ref., there has been some question over the derivation of the corresponding steady state relations . Therefore, we present a derivation of the Ω\Omega-FR’s which is more thorough than the ones that have appeared thus far in the literature . The purpose is to shed light on the mechanisms which allow the Ω\Omega-FR’s to hold, and which may be used to better understand properties of nonequilibrium systems. In particular, we are interested in nonequilibrium steady states where the dissipation function takes the form

where JJ is the dissipative flux in the system of interest, VV is the volume of the system of interest, kBk_{B} is Boltzmann’s constant, TT is the equilibrium thermodynamic temperature of the thermal reservoir with which the system of interest is in contact, and Σ\Sigma is the generalized entropy production (or energy dissipation) induced by the dissipative field FeF_{e} applied to the system of interest . For the equality Ω=Σ\Omega=\Sigma to hold, we require that the unthermostatted (i.e. adiabatic) field dependent dynamics preserves phase space volumes instantaneously, and that the initial distribution of phases could in principle be generated by a single (exceedingly long) zero-field phase space trajectory. Systems that satisfy the condition of the adiabatic incompressibility of phase space are called AIΓAI\Gamma in Ref. (cf. Appendix A).

When referring to steady state systems, we only consider systems which relax to a unique steady state. The necessary and sufficient conditions for the system of interest to relax to a unique steady state are unknown. Certainly, it is known that under certain circumstances nonequilibrium steady states are not possible . If the systems of interest are near equilibrium, where the thermodynamic notions of temperature and entropy can be used, then as is shown in the theory of linear irreversible thermodynamics the time or ensemble average of Ω\Omega is equal to leading order in the dissipative field, to the average so-called spontaneous entropy production rate . Outside this local equilibrium regime, the entropy production rate cannot be defined. While the notions of a thermodynamic temperature, thermodynamic entropy or an entropy production rate cannot be defined outside the local thermodynamic equilibrium regime, in a nonequilibrium steady state the ensemble or time averaged phase space contraction rate is equal to the steady state time derivative of the fine grained Gibbs entropy. The fact that the fine grained Gibbs entropy is not constant in a steady state (unlike the pressure or the energy), is the reason why it is so difficult to attach meaning to standard thermodynamic quantities such as temperature, in steady states outside the local equilibrium regime.

In the derivation of a relation like (1), one may follow different approaches. The one which has led to the Λ\Lambda-FR requires the full knowledge of the physical measure of the dynamics, which is then assumed to be of the Anosov type, hence to have a Sinai-Ruelle-Bowen (SRB) measure, μSRB\mu_{SRB} . This is the mathematical approach, which aims to identify the class of dynamical systems for which a relation like (1) can be rigorously obtained, regardless of the physical relevance of such dynamical systems or of the quantities appearing in (1). How far one can go along this line and which other condition could replace the the Anosov condition are highly nontrivial and interesting mathematical questions, which do not have an answer, at present.

The explicit knowledge of the physical measure gives the maximum possible amount of information about the phase space distribution: all statistical properties of the dynamics can be obtained from it. However, if one is only interested in why the FR holds, less detailed knowledge of the phase space distribution is likely to suffice, and special features of the dynamics, such as the Anosov property, need not play a role. This may explain why many physical systems have an observable which obeys a relation like (1). As a matter of fact, hardly any particle system of physical interest is of the Anosov kind, therefore it is interesting to ask whether a physical system obeying a fluctuation relation does so because it shares certain properties with Anosov systems, or whether it obeys such relations for other reasons. To investigate this question, which is part of the physical approach, we follow Evans and Searles , since they do not require the invariant phase space probability measure to be explicitly determined. This will lead to transient fluctuation relations for Σ\Sigma as well as for many other functions of phase, including Λ\Lambda. If ϕ\phi is the observable of interest, we speak of ϕ\phi-FR.

The purpose of the present paper is to understand why the Σ\Sigma-FR holds for many physically interesting systems, and why this can be observed within physically relevant time scales. This is useful to further develop the present theory.

Remark. This issue is not completely unrelated to, but is quite different from the identification of the class of dynamical systems which allow a rigorous mathematical derivation of the Λ\Lambda-FR. One may say that the two issues are as much related as Khinchin’s approach to the ergodic hypothesis is related to ergodic theory.

In Section 2 we derive transient FR’s for time reversal invariant dynamics. These relations are called “transient” because they describe the time evolving statistics of an ensemble of finite time averages of given phase functions. They hold under very general conditions, similarly to other transient relations, like the Jarzynski and the Crooks relations . In particular, the transient relations hold even if a steady state with positive and negative fluctuations of the observable under consideration is not reached. If a fluctuating steady state is not reached, the transient relations hold and express properties of evolving ensembles of phase space trajectories, while the Anosov structure cannot characterize the dynamics.

In Section 3, we show how the results of Section 2 can be used to derive asymptotic FR’s for reversible systems, under the technical assumption that Ω\Omega is bounded. In Section 4, the decay of the Ω\Omega-autocorrelation is shown to be sufficient for the steady state Ω\Omega-FR to hold. Furthermore, in isoenergetic systems which enjoy AIΓAI\Gamma (e.g. systems whose adiabatic evolution is Hamiltonian), the phase space contraction rate and the dissipation function are instantaneously equal. In these cases, the predictions of the Λ\Lambda-FR and of the Ω\Omega-FR can be compared directly, and the Ω\Omega-FR at high dissipation implies a different behavior from the one predicted by the Λ\Lambda-FR under the axiom-C condition of Ref., but which agrees with the results of . This is possible because the conjectures of are not necessarily verified by particle systems. The approach followed in Sections 2, 3 and 4 leads to a number of ϕ\phi-FR’s and to various other relations. In Section 5 we discuss our results. Appendix A contains a detailed description of the dissipation function for the common cases. Appendix B discusses the problem of axiom-C systems and the decay of correlations, and explains that our approach is based on exact relations, which are then valid even when the conditions of Section 4 are not met. Our conclusions are that:

to satisfy the steady state Ω\Omega-FR, the time reversal invariance of the dynamics and the decay of the Ω\Omega-autocorrelations, with respect to the initial (non-singular) probability measure, suffice. This decay of correlations is not the one characterizing the steady states of axiom-C systems, which concerns all observables and is referred to the invariant (singular) measure.

For Ω\Omega to equal Σ\Sigma, hence to obtain a steady state Σ\Sigma-FR, AIΓAI\Gamma must hold and the initial distribution of phases must in principle be obtainable form a single field free (Fe=0F_{e}=0) phase space trajectory. In such a case, we say that the initial distribution is ergodically consistent with the field free dynamics .

The Ω\Omega-FR’s avoid the difficulties encountered by the Λ\Lambda-FR close to equilibrium. The Λ\Lambda-FR, requires ever longer convergence times, the closer the steady state is to equilibrium . The Ω\Omega-FR’s hold in a range which does not shrink for decreasing fields, and are verified within the physically relevant (Ω\Omega-autocorrelation) times, both for systems far and close to equilibrium.

The direct derivation of the steady state Σ\Sigma-FR’s avoids the difficulties connected with obtaining a relation for the energy dissipation via the Λ\Lambda-FR, justifies the convergence rates, and leads to new testable relations. However, the class of dynamical systems which enjoy the required decay of correlations remains to be identified.

It goes without saying that the steady state relations require that a steady state is reached (hence that the correlations decay with respect to the initial state), and that fluctuations of opposite sign in the dissipation function should be observable. If such a steady state is not attained or if the steady state is sufficiently far from equilibrium that negative values of the dissipation function cannot be observed, the steady state FR’s cannot be applied, but the transient FR’s (including their asymptotic forms) remain valid as properties of the evolving ensembles, because they only require time reversibility.

In this sense, our relations are like the usual thermodynamic relations which are extraordinarily general, being independent of the nature of interparticle interactions and dynamics. All that is required of the dynamics is that it should be time reversible and, for steady state FR’s, that the autocorrelation of Ω\Omega decays and that the steady state is uniqueThis is analogous to the equilibrium thermodynamic requirement of a unique allotrope.. Furthermore our derivation explains why the Ω\Omega-FR is verified within times which can be expressed in terms of material properties.

TRANSIENT FLUCTUATION RELATION

Because we will be interested in thermodynamic systems which possibly relax to a nonequilibrium steady state, our dynamics will consist of the Hamiltonian dynamics of an NN-particle system of interacting particles to which a dissipative field is applied. The resultant equations of motion may or may not be derivable from a Hamiltonian . In order for such a system to be capable of relaxing to a nonequilibrium steady state, the system must be allowed on average, to loose heat. This can be accomplished by surrounding the system of interest with thermostatting walls which serve two purposes: to confine the system of interest and also to remove dissipative heat generated (on average) by the dissipative field applied to it. It has been shown that any loss of heat from a Hamiltonian system requires that the dynamics over the degrees of freedom in the system of interest is no longer volume preserving . These details are explained further in the Appendix. In what follows however, we will consider a more general setting that is time reversible and does not necessarily preserve the phase space volumes.

Given the phase space M{\cal M} of a particle system, consider a probability measure μ\mu on M{\cal M}, with density ff, i.e.{\it i.e.} dμ(Γ)=f(Γ)dΓd\mu(\Gamma)=f(\Gamma)d\Gamma for every point Γ∈M\Gamma\in{\cal M}. The measure μ\mu does not need to be produced by any dynamics on M{\cal M}, although it could represent, for instance, the initial equilibrium distribution of the system. Further, given a (sufficiently well behaved) phase function ϕ:M→IR\phi:{\cal M}\rightarrow I\hskip-3.6ptR, the probability that it takes values in the interval (a,b)⊂IR(a,b)\subset I\hskip-3.6ptR, according to μ\mu, is given by

is the set of points of the phase space for which ϕ\phi takes values in (a,b)(a,b).ϕ∣(a,b)\phi|_{(a,b)} is assumed to be μ\mu-measurable, like all sets in this paper.

Let Sτ:M→MS^{\tau}:{\cal M}\rightarrow{\cal M} be the time evolution operator, which takes any point Γ∈M{\Gamma}\in{\cal M} to its evolved image SτΓS^{\tau}\Gamma, under some dynamics applied for the time τ\tau.In particular, the dynamics could be determined by the equations of motion of a particle system subjected to a dissipative field FeF_{e}, and to a deterministic thermostat meant to remove the excess energy pumped into the system by the field, so that a nonequilibrium steady state can be reached . In this case, Γ=(q,p)\Gamma=(\mathbf{q{\textstyle{\textstyle,}\mathbf{p}}}) denotes the generalized coordinates and momenta of all the particles comprising the system. We refer to time reversal invariant dynamics, i.e. dynamics which obey

where i:M→Mi:{\cal M}\rightarrow{\cal M}, which obeys ii=i2=ii=i^{2}= identity, is an involution representing the time inversion operator (e.g. iΓ≡i(q,p)≡(q,−p)i{{\Gamma}}\equiv i(\mathbf{q},\mathbf{p})\equiv(\mathbf{q},-\mathbf{p})) for the dynamics. Consider the phase functions defined by:

Take δ>0\delta>0, t0=0t_{0}=0, introduce the sets Aδ+=(A−δ,A+δ)A_{\delta}^{+}=(A-\delta,A+\delta), Aδ−=(−A−δ,−A+δ)A_{\delta}^{-}=(-A-\delta,-A+\delta) and, for an odd phase variable ϕ\phi (i.e. ϕ(iΓ)=−ϕ(Γ)\phi(i\Gamma)=-\phi(\Gamma)), consider the ratio

i.e. the probability according to μ\mu that ϕ‾0,τ∈Aδ+\overline{\phi}_{0,\tau}\in A_{\delta}^{+}, divided by the probability according to the same μ\mu that ϕ‾0,τ∈Aδ−\overline{\phi}_{0,\tau}\in A_{\delta}^{-}.

To compute this quantity, observe that the points of M{\cal M} which fall in ϕ‾0,τ∣Aδ−\overline{\phi}_{0,\tau}|_{A^{-}_{\delta}} are those, and only those, obtained by doing the time inversion of the evolution, for a time τ\tau, of the points in ϕ‾0,τ∣Aδ+\overline{\phi}_{0,\tau}|_{A^{+}_{\delta}}, i.e.

Indeed, take any Γ∈ϕ‾0,τ∣Aδ−\Gamma\in\overline{\phi}_{0,\tau}|_{A^{-}_{\delta}}, invert it and evolve it backward for a time τ\tau; the resulting point Y=S−τiΓY=S^{-\tau}i\Gamma is the initial condition of a trajectory segment of duration τ\tau over which one obtains ϕ‾0,τ∈Aδ+\overline{\phi}_{0,\tau}\in A_{\delta}^{+}, hence Y∈ϕ‾0,τ∣Aδ+Y\in\overline{\phi}_{0,\tau}|_{A^{+}_{\delta}}. Moreover, there are no points of iSτϕ‾0,τ∣Aδ+iS^{\tau}\overline{\phi}_{0,\tau}|_{A^{+}_{\delta}} which do not lie in ϕ‾0,τ∣Aδ−\overline{\phi}_{0,\tau}|_{A^{-}_{\delta}}. This allows us to compute the denominator of Eq.(7) in terms of ϕ‾0,τ∣Aδ+\overline{\phi}_{0,\tau}|_{A^{+}_{\delta}}, through the coordinate transformation

Here, the quantity Λ\Lambda is the phase space expansion rate (the opposite of the contraction rate) which, for dynamics Γ˙=G(Γ)\dot{\Gamma}=G(\Gamma) on M{\cal M}, is defined by

A necessary condition for the derivation of the transient fluctuation relations is that

This condition is satisfied by appropriate choices of μ\mu, for the given SτS^{\tau}. For example, μ\mu could be selected to be the probability distribution generated by the field-free (equilibrium) dynamics of a particle system, S0τS_{0}^{\tau} say, for which SτS^{\tau} is the nonequilibrium dynamics; i.e. μ\mu could be generated by S0τS_{0}^{\tau}, obtained by setting the dissipative field of the nonequilibrium dynamics SτS^{\tau} to zero. In fact, this selection ensures that f(iSτΓ)≠0f(iS^{\tau}\Gamma)\neq 0 whenever f(Γ)≠0f(\Gamma)\neq 0.Here, it is assumed that equilibrium dynamics corresponds to no net dissipation, and that typical trajectories explore all the phase space. Then, assuming that ff is also time reversal invariantThe assumption that ff be time reversal invariant is not necessary for our main results. A different choice will simply result in a alternative definition of the dissipation function, . However, if μ\mu is selected to be an equilibrium measure, then this condition is guaranteed, and relying on it makes the calculations more elegant. (i.e. that f(Γ)=f(iΓ)f(\Gamma)=f(i\Gamma) for every Γ∈M\Gamma\in{\cal{M}}) the ratio of probabilities (7) becomes:

The restriction on the choice of μ\mu for the given SτS^{\tau}, i.e. that f(iSτΓ)≠0f(iS^{\tau}\Gamma)\neq 0 whenever f(Γ)≠0f(\Gamma)\neq 0, is referred to as ergodic consistency of ff with SτS^{\tau} . The main quantity used below can now be introduced.

Definition.The time averaged dissipation function Ω‾t0,t0+τ:M→IR\overline{\Omega}_{t_{0},t_{0}+\tau}:\mathcal{M}\to I\hskip-3.6ptR, for a time reversal invariant phase space probability density ff is defined by :

provided ff is ergodically consistent with StS^{t}. The instantaneous dissipation function Ω(Γ)\Omega(\Gamma) is obtained from differentiation with respect to τ\tau of Ω‾0,τ\overline{\Omega}_{0,\tau}, for sufficiently regular ff.

Here the condition of ergodic consistency plays an important role, although it may not be so evident in general. Indeed, given a particle system with certain conserved quantities under its equilibrium dynamics S0τS_{0}^{\tau}, the nonequilibrium dynamics SτS^{\tau} may not conserve the same quantities, and a trajectory SτΓS^{\tau}\Gamma may wander outside the support of μ\mu, making the corresponding Ω\Omega unusable in the following derivations. Thus, in physical applications ff must be chosen with care, although many phase space densities are acceptable from a mathematical point of view. Using Eq.(13), Eq.(12) implies what has been referred to as the

Here ⟨exp⁡(−Ω0,τ)⟩ϕ‾0,τ∈Aδ+\left\langle\exp\left(-\Omega_{0,\tau}\right)\right\rangle_{\overline{\phi}_{0,\tau}\in A_{\delta}^{+}} is the ensemble average of exp⁡[−Ω0,τ(X)]\exp[-\Omega_{0,\tau}(X)], over the set of trajectories which satisfy the constraint that ϕ‾0,τ∈Aδ+\overline{\phi}_{0,\tau}\in A_{\delta}^{+} . In the case that ϕ‾0,τ=Ω‾0,τ\overline{\phi}_{0,\tau}=\overline{\Omega}_{0,\tau} the fluctuation relation assumes the particularly elegant form, called

Here, ε\varepsilon is an error term of magnitude ∣ε∣≤δ|\varepsilon|\leq\delta, which depends on δ,A\delta,A and τ\tau, and appears because Ω‾0,τ\overline{\Omega}_{0,\tau} is not necessarily constant and equal to AA. Therefore, ε(δ,A,τ)→0\varepsilon(\delta,A,\tau)\rightarrow 0 as δ→0\delta\rightarrow 0, for all AA for which the ratio of Eq.(15) exists .

Remark. Different choices of ff are possible, which lead to different Ω\Omega-FR’s. In particular, equilibrium probability densities of many-particle systems which obey AIΓAI\Gamma lead to an Ω\Omega-FR which concerns the entropy production, or the energy dissipation rate Σ\Sigma (cf. Appendix A). The uniform density in a compact phase space, f(Γ)=1/∣M∣f(\Gamma)=1/|{\cal M}| say, yields Ω=−Λ\Omega=-\Lambda. A density such that fdΓfd\Gamma approximates as accurately as desired the (possibly singular) steady state measure is also allowed.

The above relations are called “transient” because, independently of the length of τ\tau, they express properties of the measure μ\mu and not of the possible steady state. The time τ\tau, indeed, enters the ϕ\phi-FR only in the definition of the observable ϕ‾0,τ\overline{\phi}_{0,\tau}, and not of the phase space probability density. Equations (14,15) are exact and do not need any limit to be taken either on τ\tau or on δ\delta. As the calculation shows, the only properties that are required for Eqs.(14,15) to hold are that the dynamics SτS^{\tau} be time reversal invariant, to ensure that, for odd ϕ\phi, −A-A can be observed if AA can, and that f(iSτΓ)≠0f(iS^{\tau}\Gamma)\neq 0 for any Γ\Gamma for which f(Γ)≠0f(\Gamma)\neq 0. The range of AA’s that can be observed depends both on SτS^{\tau} and ϕ\phi.

If the initial distribution can be generated by a single field free phase space trajectory, and AIΓAI\Gamma holds, the dissipation function Ω\Omega takes the form given in (2) and at equilibrium (where Fe=0F_{e}=0), Ω=0\Omega=0, hence

as it should be for the equilibrium measure μ\mu, and for any odd variable ϕ\phi (for instance, ϕ\phi could be the instantaneous current JJ, which does not need to vanish at equilibrium, although its mean certainly does). For symmetric intervals (−δ,δ)(-\delta,\delta), one also has A=0A=0 and can write

In the limit that δ\delta tends to infinity, the second equality in (17) tends to a full phase space average, and produces the NonEquilibrium Partition Identity (also referred to as the Kawasaki normalization). This identity can be used to test the accuracy of the numerical simulations, and has even been used to calibrate experimental equipment . The highly asymmetric convergence of numerical estimates to unity means that estimating the statistical uncertainty of experiments is problematic without this relationship . If the dissipation function is bounded (i.e. ∣Ω∣≤Ω∗|\Omega|\leq\Omega^{*}, for some Ω∗>0\Omega^{*}>0), one obtains

for all odd ϕ\phi. Because different dissipation functions are allowed and the above ratio holds for all of them, a sharp bound can be given for all ϕ\phi and independently of the physically relevant dissipation function, by taking the smallest possible Ω∗\Omega^{*}. This constitutes a new prediction, which may be interesting to test in nonequilibrium systems.

ASYMPTOTIC FLUCTUATION RELATIONS

In order to derive steady state fluctuation relations, one may develop further the transient ϕ\phi-FR’s obtained in Section 2, considering the time averaged phase variable ϕ‾t0,t0+τ\overline{\phi}_{t_{0},t_{0}+\tau} (cf. Eq.(6)), where the time averaging begins at a time t0>0t_{0}>0, rather than at time 0:

Here, ϕ‾t0,t0+τ∣E={Γ∈M:ϕ‾t0,t0+τ(Γ)∈E}\overline{\phi}_{t_{0},t_{0}+\tau}|_{E}=\{\Gamma\in{\cal M}:\overline{\phi}_{t_{0},t_{0}+\tau}(\Gamma)\in E\} is the set of all phase points which are initial conditions of trajectory segments of duration t0+τt_{0}+\tau, over which ϕ‾t0,t0+τ\overline{\phi}_{t_{0},t_{0}+\tau} takes values in EE, and E=Aδ+E=A_{\delta}^{+} or Aδ−A_{\delta}^{-}. The calculation of the ratio (19) requires that the points of M{\cal M} lying in ϕ‾t0,t0+τ∣Aδ−\overline{\phi}_{t_{0},t_{0}+\tau}|_{A^{-}_{\delta}} be identified. To do that, consider a trajectory of length t=2t0+τt=2t_{0}+\tau, and take WW in ϕ‾t0,t0+τ∣Aδ+\overline{\phi}_{t_{0},t_{0}+\tau}|_{A^{+}_{\delta}}. Then, let X=St0WX=S^{t_{0}}W, Y=St0+τWY=S^{t_{0}+\tau}W, Z=S2t0+τW=StWZ=S^{2t_{0}+\tau}W=S^{t}W, and Γ=iZ=iStW\Gamma=iZ=iS^{t}W (see Figure 1). The trajectory segment between iYiY and iXiX produces the opposite of the average produced between XX and YY, in the time interval (t0,t0+τ)(t_{0},t_{0}+\tau), so that

where J=∣dΓdW∣=exp⁡[Λ0,t(W)]J=\left|\frac{d\Gamma}{dW}\right|=\exp[\Lambda_{0,t}(W)] and we use time reversal invariance of ff.

Note that the integral defining JJ is along the full trajectory of duration tt, although ϕ‾t0,t0+τ\overline{\phi}_{t_{0},t_{0}+\tau} concerns only one of its parts of duration τ\tau. From the definition of Ω‾0,t\overline{\Omega}_{0,t} (Eq.(13)), one obtains:

The probability ratio of Eq.(19) can then be written as:

which is the inverse of the average of exp⁡(−Ω0,t)\exp(-\Omega_{0,t}), conditioned to the constraint ϕ‾t0,t0+τ∈Aδ+\overline{\phi}_{t_{0},t_{0}+\tau}\in A_{\delta}^{+}; and the special case ϕ=Ω\phi=\Omega, yields

The right hand side of this expression can be written as:

Taking the logarithm, and dividing by τ\tau one then obtains:

where the correction term ε\varepsilon depends on δ,t0,A\delta,t_{0},A and τ\tau and, like in Section 2, ∣ε∣≤δ|\varepsilon|\leq\delta. This result is exact, and holds for all t0t_{0}, τ\tau and δ\delta, and for any AA for which both the probabilities in the left hand side of (27) do not vanish. It rests only on the time reversibility of StS^{t}, and on the ergodic consistency of ff with StS^{t}.

Equations (24) and (27) are valid for all τ\tau, hence also in the limit τ→∞\tau\to\infty, but remain transient relations because no matter how large τ\tau is; they refer to the initial measure μ\mu, even if the dynamics makes μ\mu evolve into μτ\mu_{\tau}. However, the above derivation suggests that for systems that reach a steady state, it may be possible to derive steady state FR’s from the transient FR’s. The idea is that for sufficiently large times t0t_{0}, Eqs.(24,27) should concern trajectory segments of length τ\tau distributed according to the invariant measure, or very close to that. Furthermore, taking τ\tau long, and δ\delta small, should make the last two terms in Eq.(27) negligible.

To investigate this possibility, we firstly transform Eqs.(24) and (27) by transferring the time evolution up to t0t_{0} from the sets of phase space points ϕ‾t0,t0+τ∣(a,b)\overline{\phi}_{t_{0},t_{0}+\tau}|_{(a,b)}, to the phase space probability distributions. Given an initial phase space probability density f0f_{0}, and the corresponding probability measure μ0\mu_{0}, we denote their evolved counterparts after a time t0t_{0} by ft0f_{t_{0}}, and μt0\mu_{t_{0}} respectively:

for every t0∈IRt_{0}\in I\hskip-3.6ptR and E⊂ME\subset{\cal M}, where St0ES^{t_{0}}E is the set of points reached by all points of EE after an evolution of duration t0t_{0}. Equations (28) are consequences of the conservation of probability by time evolution.They merely state that the initial probability of EE becomes the probability of the evolved set St0ES^{t_{0}}E after a time t0t_{0}. Physically, they are an instance of what is referred to as the Heisenberg-Schrödinger equivalence, while mathematically they are the result of the coordinate transformations X=St0WX=S^{t_{0}}W and W=S−t0XW=S^{-t_{0}}X. The Jacobian of this transformation is given by

In Eqs.(30,31), we could have integrated over any measurable set EE, hence, equating (30) and (31) finally gives:

This is known as the Lagrangian form of the Kawasaki distribution function .This can also be written, ft0(St0W)=f0(W)e−Λ0,t0(W)f_{t_{0}}(S^{t_{0}}W)=f_{0}(W)e^{-\Lambda_{0,t_{0}}(W)}. From Eq.(22), which yields

and gives the evolution of the phase space probability density f0f_{0}. This well known exact result for the time dependent phase space density ft0(X)f_{t_{0}}(X), was first derived for thermostatted particle dynamics where the dissipation function takes the form given in Eq.(2) by Evans and Morriss in 1984 . Observe that

because ϕ\phi is a phase variable, hence does not explicitly depend on time, and because we assume the dynamics to be autonomous. Indeed, a point X∈St0ϕ‾t0,t0+τ∣(a,b)X\in S^{t_{0}}\overline{\phi}_{t_{0},t_{0}+\tau}|_{(a,b)} is the evolution by a time t0t_{0} of a point Γ\Gamma for which ϕ‾t0,t0+τ\overline{\phi}_{t_{0},t_{0}+\tau} takes the same value of ϕ‾0,τ(X)\overline{\phi}_{0,\tau}(X), i.e.

Thus, Eq.(31) expresses the time evolving probability of the fixed set ϕ‾0,τ∣(a,b)\overline{\phi}_{0,\tau}|_{(a,b)},

Provided convergence to the steady state occurs, this equation yields a more and more accurate approximation to the steady state measure of ϕ‾0,τ∣(a,b)\overline{\phi}_{0,\tau}|_{(a,b)}, as t0t_{0} grows, at fixed τ\tau.

Equation (24), which is expressed in terms of the initially chosen phase space probability distribution, and of evolving phase space sets, can now be given in terms of the evolving PDF, since

Relation (39) is exact and holds for all t0,τt_{0},\tau and possible pairs AA and −A-A (whose range must be determined case by case). Letting ϕ‾t0,t0+τ=Ω‾t0,t0+τ\overline{\phi}_{t_{0},t_{0}+\tau}=\overline{\Omega}_{t_{0},t_{0}+\tau} and rearranging, Eq.(27) yields the

where the conditional ensemble average in the last term is computed with respect to the initial distribution ff.

Let us consider some direct consequences of the above relations. For A=0A=0, δ>0\delta>0, t0,τ∈IRt_{0},\tau\in I\hskip-3.6ptR, and any odd ϕ\phi, the conditional average of Eq.(39) yields

which, in the δ→∞\delta\to\infty limit, leads again to the NonEquilibrium Partition Identity (17), for the full ensemble average.

which shows that this particular conditional average is uniformly bounded in t0t_{0}, and tends to 1 when δ→0\delta\to 0, at fixed τ\tau. Equation (41) with ϕ=Ω\phi=\Omega differs from (42) because of the integration times in the argument of the exponential function. For fixed δ\delta and τ\tau, such that δτ≪1\delta\tau\ll 1, one can write

even for t0→∞t_{0}\to\infty, which is interesting for the validity of the steady state Ω\Omega-FR. Indeed, the last term in Eq.(40) ought not to dominate over the others, if the steady state Ω\Omega-FR is to hold. Exchanging the roles of Aδ+A_{\delta}^{+} and Aδ−A_{\delta}^{-} in Eq.(40), one obtains

One last property that is worthwhile to consider is the following asymptotic result, which is particularly close to a steady state FR. As it happens in many situations of interest, let ∣Ω∣|\Omega| be bounded by some Ω∗>0\Omega^{*}>0, so that:

for all τ\tau. Then, taking δ<γ\delta<\gamma, which implies ∣ε∣<γ|\varepsilon|<\gamma, and

Recalling the connection between Ω\Omega and the physical dissipation, which holds under proper choices of the initial ff, the above condition can be written as

where J∗J^{*} is the maximum of the flux. This shows that, differently from the case of the steady state Λ\Lambda-FR, the convergence time of the Ω∞\Omega_{\infty}-FR does not increase when the dissipative field tends to 0; to the contrary, it may decrease.

As in the transient case, an asymptotic ϕ\phi-FR holds for AA in a range which depends on the dynamics and on the observable, but for large τ\tau it remains close to (−Ω∗,Ω∗)(-\Omega^{*},\Omega^{*}). Indeed, one has

and taking any γ>0\gamma>0 and letting tt grow, with τ(t)≫t\tau(t)\gg t, one can write

for any odd ϕ\phi, and with the smallest Ω∗\Omega^{*}, among the upper bounds of the allowed dissipation functions.

Because at equilibrium the dissipation function given by Eq.(2) is Ω=−FeJV/kBT=0\Omega=-F_{e}JV/k_{{}_{B}}T=0, one has

whatever odd variable ϕ\phi is considered, Ω\Omega, Λ\Lambda or JJ for instance. This yields the usual equilibrium symmetry, in the full range of JJ, not just in 0, and without the need for long convergence times.

for large t0t_{0}, all τ\tau and all allowed AA. Then, as far as the asymptotic fluctuation relations are concerned, the different dissipation functions are equivalent.

Let us note that Eq.(47) does not necessarily imply the steady state Ω\Omega-FR, even when there is a single steady state and all initial measures μ0\mu_{0} with density f0f_{0} are attracted by the same μ∞\mu_{\infty}, because the limit in Eq.(50) could be singular. Although this is not impossible, it is not the typical situation of particle systems of physical interest (cf. Section 4 and Appendix B), and Eq.(47) is a result rather close to the steady state Ω\Omega-FR.

In Section 4 we discuss the conditions under which Eq.(47) describes the statistics of trajectory segments sampled from a single steady state trajectory. Before we do this, we note that whereas in Sections 2 and 3, the initial distribution f0f_{0} can have arbitrary form, provided it is ergodically consistent with the dynamics considered, a further condition on f0f_{0} is imposed, in order to obtain the steady state Ω\Omega-FR: the decay of the Ω\Omega-autocorrelation, with respect to f0f_{0}. This is necessary for the initial state to relax to a steady state. The further requirement that the ensemble is not only invariant under S0tS^{t}_{0}, but that is also generated by a single trajectory, has the purpose to avoid the presence of distinct steady states, selected by different choices of the initial conditions. These states, indeed, would have different properties, and a unique μ∞\mu_{\infty} would not be possible. For instance, if f0f_{0} was selected to be a uniform distribution (so that Ω=−Λ\Omega=-\Lambda) and isokinetic dynamics was carried out, a distinct μ∞\mu_{\infty} would be expected for each distinct value of the kinetic energy.

If the system under investigation does not converge to a steady state with positive and negative fluctuations, there is no need for a steady state relation, but the Ω\Omega-FR, the ϕ\phi-FR, the Ω∞\Omega_{\infty}-FR and the ϕ∞\phi_{\infty}-FR remain valid for the given ensemble of trajectories.

STEADY STATE FLUCTUATION RELATIONS

We assume the steady state exists and that it is unique. This will not always be the case, for example if we start from a canonical phase space distribution at time zero and have isokinetic dynamics subsequently, there will be distinct steady state attractors for each trajectory with a different kinetic energy. Each of the steady state attractors will have different properties because they are at different kinetic temperatures. By saying that the steady state is unique we mean that, apart from a set of measure zero, the statistics generated by each trajectory is independent of the initial phase, in the relevant equilibrium phase space.

Equations (27) and (40) are both exact, but contain information on the trajectories before the steady state is reached. To be of practical use in the description of the steady state fluctuations of the dissipation function, the last two terms in the equation have to be negligible. Therefore, for A≠0A\neq 0, some assumption on the nature of the logarithmic term of Eq.(40) is necessary since, in principle, this term could be of order O(t0/τ)O(t_{0}/\tau), and t0t_{0} should tend to infinity, in order to reach the steady state, before τ\tau does . We argue that, in most cases of interest, the dynamics of particle systems used to model nonequilibrium fluids satisfy the following:

Steady state Ω\Omega-FR. For any tolerance γ>0\gamma>0, there exists δγ,τγ>0\delta_{\gamma},\tau_{\gamma}>0 such that

holds for 0<δ≤δγ0<\delta\leq\delta_{\gamma} and τ≥τγ\tau\geq\tau_{\gamma}, if both the values AA and −A-A are δ\delta-possible.

Here, the following definition has been used:

Definition. The value A∈IRA\in I\hskip-3.6ptR is called δ\delta-possible if, given δ>0\delta>0, there exists τA,δ>0\tau_{A,\delta}>0 such that

for all τ>τA,δ\tau>\tau_{A,\delta}.Because of the finiteness of τ\tau, this can be the case even though μ∞(Ω‾0,τ∣Aδ+)→0\mu_{\infty}(\overline{\Omega}_{0,\tau}|_{A^{+}_{\delta}})\to 0, for τ→∞\tau\to\infty, as it does if the steady state ensemble average of Ω\Omega, ⟨Ω⟩∞\langle\Omega\rangle_{\infty} say, does not belong to Aδ+A^{+}_{\delta}.

It follows that, for AA to be δ\delta-possible, μ∞(Ω‾0,τ∣Aδ+)\mu_{\infty}(\overline{\Omega}_{0,\tau}|_{A_{\delta}^{+}}) must decay with τ\tau more slowly than the error term [ε(δ,t0,A,τ)−1τln⁡⟨e−Ω0,t0−Ωt0+τ,2t0+τ⟩Ω‾t0,t0+τ∈Aδ+]\left[\varepsilon(\delta,t_{0},A,\tau)-\frac{1}{\tau}\ln\left\langle e^{-\Omega_{0,t_{0}}-\Omega_{t_{0}+\tau,2t_{0}+\tau}}\right\rangle_{\overline{\Omega}_{t_{0},t_{0}+\tau}\in A^{+}_{\delta}}\right] of Eq.(40). Indeed, given δ>0\delta>0, a pair (−A,A)(-A,A) and a fixed τ\tau, the logarithmic term in the right hand side of Eq.(40) may either take arbitrarily large values or be bounded, in the t0→∞t_{0}\to\infty limit. In the first case, because A,δA,\delta and τ\tau are fixed real numbers and ∣ε∣≤δ|\varepsilon|\leq\delta, the corresponding divergence is reflected on the measures μt0(Ω‾0,τ∣Aδ+))\mu_{t_{0}}(\overline{\Omega}_{0,\tau}|_{A^{+}_{\delta}})) and μt0(Ω‾0,τ∣Aδ−)\mu_{t_{0}}(\overline{\Omega}_{0,\tau}|_{A_{\delta}^{-}}), one of which at least either tends to zero or does not converge at all. Indeed, if for every R,τ,t^0>0R,\tau,\hat{t}_{0}>0 there is t0>t^0t_{0}>\hat{t}_{0} such that

which corresponds either to μ∞(Ω‾0,τ∣Aδ−)=0\mu_{\infty}(\overline{\Omega}_{0,\tau}|_{A^{-}_{\delta}})=0, or to the μ∞\mu_{\infty} non-measurability of Ω‾0,τ∣Aδ−\overline{\Omega}_{0,\tau}|_{A^{-}_{\delta}}. In either case, −A-A is not δ\delta-possible, and similarly one may treat AA.

Clearly, AA is of no interest for a steady state FR, i.e. it does not belong to the domain of the steady state Ω\Omega-FR with tolerance γ\gamma, if AA and −A-A are not both δ\delta-possible; in a number of cases that domain may even be empty.There are various reasons for which AA or −A-A might not be in the the domain of the steady state Ω\Omega-FR. For example, AA could be larger than the largest value of Ω\Omega, or there could be no fluctuations in the steady state (cf. Appendix B). Therefore, we focus only on the AA values with bounded logarithmic term in Eq.(40), and let M(A,δ,τ)M(A,\delta,\tau) be the real number to which the conditional average in Eq.(40) tends, in the t0→∞t_{0}\to\infty limit. We may then write

If (1/τ)ln⁡M(A,δ,τ)(1/\tau)\ln M(A,\delta,\tau) tends to zero, for the given A,δA,\delta and growing τ\tau, the steady state Ω\Omega-FR holds for AA. This is the case if correlations decay, so that the thermodynamic behavior sets in. In particular, if the Ω\Omega-autocorrelation function is a δ\delta-function (as e.g. in Ref.), one can write:

because of the NonEquilibrium Partition Identity (17). Then, (1/τ)ln⁡M(A,δ,τ)(1/\tau)\ln M(A,\delta,\tau) identically vanishes for all τ\tau. This is an idealized situation and, indeed, the tests performed on molecular dynamics systems,The conditional average of Eq.(40) can, of course, be computed independently of the other terms in Eq.(40), although this is not strictly necessary, because Eq.(40) is an exact identity. cf. Ref., indicate that typically there exists a constant KK (often not too far from 1), such that

which may be understood as follows. In the first place, the conditional average is limited for growing t0t_{0}, if −A,A-A,A are δ\delta-possible, and equals 1 for τ=0\tau=0. Then, if the Ω\Omega-autocorrelation decays with time scale tMt_{M},This time is called Maxwell time; its order of magnitude is that of the mean free time. The Maxwell time expresses a physical property of the system and depends only mildly on the external field; usually, tM(Fe)=tM(0)+O(Fe2)t_{M}(F_{e})=t_{M}(0)+O(F_{e}^{2}) one expects ln⁡K\ln K to be of order O(tM)O(t_{M}). Taking τ\tau sufficiently larger than tMt_{M}, and letting cAc_{A} be a natural number dependent on the given AA, one may write

with an accuracy which improves with increasing t0t_{0} and τ\tau, if cAc_{A} is the number of Maxwell times necessary to obtain the desired decorrelation at the chosen AA. Indeed, one would eventually obtain t0,τ≫cAtMt_{0},\tau\gg c_{A}t_{M}.

If Eq.(4) holds, the t0→∞t_{0}\to\infty limit of ⟨e−Ωt0+τ+cAtM,2t0+τ⟩\left\langle e^{-\Omega_{t_{0}+\tau+c_{A}t_{M},2t_{0}+\tau}}\right\rangle is finite for all δ\delta-possible pairs (−A,A)(-A,A), and is insensitive to variations of τ\tau above a certain threshold. Indeed, let τ^=τ+cAtM\hat{\tau}=\tau+c_{A}t_{M} and observe that

is the average of e−Ω0,t0−cAtMe^{-\Omega_{0,t_{0}-c_{A}t_{M}}} computed with the probability distribution obtained from the evolution of the initial one, for the time t=t0+τ^t=t_{0}+\hat{\tau}. The value of this average may be estimated noting that, for δ\delta-possible pairs (−A,A)(-A,A), and growing t0t_{0}, it converges approximately to the positive number M(A,δ,τ^)M(A,\delta,\hat{\tau}), if Eq.(4) holds. Furthermore, for fixed t0>0t_{0}>0 and for tt of the order of the Maxwell time, ⟨e−Ω0,t0−cAtM⟩t\left\langle e^{-\Omega_{0,t_{0}-c_{A}t_{M}}}\right\rangle_{t} approaches its steady state mean value, ⟨e−Ω0,t0−cAtM⟩∞\left\langle e^{-\Omega_{0,t_{0}-c_{A}t_{M}}}\right\rangle_{\infty} which is equal to 1 at equilibrium for all t0t_{0} and cAc_{A}. Then, for sufficiently large t0t_{0} and t=t0+τ^t=t_{0}+\hat{\tau}, one may write

thanks also to the fact that τ^\hat{\tau} is by itself larger than the decorrelation time. Because the left hand side of Eq.(63) does not depend on t0t_{0} while the right hand side does not depend on τ\tau, one concludes that further growths of t0t_{0} or of τ\tau do not cause any substantial changes in the conditional average in the middle. Close to equilibrium, this term should only have a correction of order O(Fe2)O(F_{e}^{2}) to its equilibrium average, 1. Numerical studies show that this is precisely what happens to the quantities in Eqs.(60,4,62), .

Note that cAc_{A} may vary with AA, as the set of trajectories involved in the conditional average changes with AA; cAc_{A} could then even diverge. However, close to equilibrium at least, the existence of the transport coefficients implies that the conditional correlation functions must not grow too much (cf. Appendix B).

Note also that, for the steady state Ω\Omega-FR to hold, it suffices that (1/τ)ln⁡M(A,δ,τ)(1/\tau)\ln M(A,\delta,\tau) can be made as small as one wishes, by taking sufficiently large τ\tau and small δ\delta. Thus, it is not necessary that Eq.(60) holds; it suffices that M(A,δ,τ)M(A,\delta,\tau) grows less than exponentially fast with τ\tau, or even that it grows exponentially fast, with a rate which tends to zero when δ\delta does, as in Eq.(42), where A=0A=0. However, the numerical tests performed so far indicate that Eq.(60) is usually satisfied in the full range of numerically or experimentally accessible AA’s.

If the Ω\Omega-autocorrelation decays, and Eq.(60) holds with the condition on Ω\Omega replaced by an equivalent one for another observable ϕ\phi, one obtains the

Steady State ϕ\phi-FR. For sufficiently large τ\tau,

This expression states that the ratio of the probabilities that ϕ‾0,τ∈Aδ+\overline{\phi}_{0,\tau}\in A^{+}_{\delta} and ϕ‾0,τ∈Aδ−\overline{\phi}_{0,\tau}\in A^{-}_{\delta} is determined by the average of the exponential of the values taken by Ω\Omega in the same time intervals in which ϕ\phi has average in Aδ+A_{\delta}^{+}. Because ϕ\phi can be any odd observable, Ω\Omega appears to be a rather special function of phase.

One may wonder how the above could be reconciled with the modifications of the steady state Λ\Lambda-FR suggested for a special kind of non-transitive dynamical systems . As explained in Appendix B, Eq.(60) is not in contradiction to the scenarios of Refs., because the decay of correlations enjoyed by their dynamical systems concern the invariant measures, while the conditional average in Eq.(60) is computed with respect to the initial measure. Therefore, the arguments of this section and those of Refs. are compatible, since Eq.(60) would not hold if the cases of Refs. were realized. The scenarios under which the approximation (60) does not hold, appear however quite peculiar, and this section explains why quite commonly the steady state Ω\Omega-FR does hold: time reversibility and the decay of the Ω\Omega-autocorrelation characterize the most common deterministic models of nonequilibrium statistical mechanics. Through the connection with the Maxwell time tMt_{M}, this approach also justifies why the convergence times of the steady state Ω\Omega-FR do not grow with decreasing dissipation: the fact is that the Ω\Omega-FR depends only on material properties of the system, and these do not change much around equilibrium. This is quite different from the case of the Λ\Lambda-FR, whose convergence times increase as the driving is decreased, and typically diverge in the equilibrium limit. As stated above, the calculations of this section hold for any regular density ff, i.e. for all possible dissipation functions Ω\Omega, but the Ω\Omega-FR turns into the Σ\Sigma-FR only when the initial distribution can be generated by single field free trajectories, and AIΓAI\Gamma holds.

CONCLUSIONS

In this paper we have investigated the mechanisms underlying the validity of the transient and steady state FR’s, following the prescriptions given by Evans and Searles over the last decade. As already evidenced in the literature, the transient relations hold under very general conditions; it suffices that the dynamics of the particle systems at hand be deterministic, autonomous, and time reversal invariant. If the initial state is properly selected, the corresponding Ω\Omega equals the energy dissipation rate Σ\Sigma. Different initial densities ff are allowed, for any given dynamics SτS^{\tau}; they are not completely equivalent, as in general they generate different dissipation functions Ω\Omega, but to some extent they are interchangeable (cf. Eq.(52)). The transient relations describe the properties of evolving ensembles of systems, even in their asymptotic form.

The steady state fluctuation relations need further assumptions. Firstly and quite obviously the system must relax to a nonequilibrium steady state. This requirement is nontrivial. The necessary and sufficient conditions for this to occur are unknown, but necessarily involve some loss of memory of the initial state, and the corresponding decay of correlations. Certainly there are examples of dissipative particle systems in contact with a thermal heat bath that do not relax to a steady state. Also, there may be distinct basins of attraction in M{\cal M} with distinct steady state measures. For example if M{\cal M} is taken to be all of phase space with an energy less than some bound and the initial ensemble is canonical, but the dynamics is isoenergetic, then obviously there will be no mixing between trajectories that have different initial energies, and the subensemble members will generate distinctly different energy dependent steady states. Different steady states may coexist also when dissipation is too high . Transitivity (i.e. that a typical trajectory explores the whole phase space relevant to the given dynamics) avoids these difficulties.

As a matter of fact, most of the molecular dynamics studies performed so far indicate that convergence to a steady state independent of the initial phase is a very common situation. This convergence is consistent with laboratory experiments where for systems with low Reynolds/Raleigh numbers the nonequilibrium steady state (if such a state exists) is quite independent of the initial starting state or the preparative history of the system. The low shear rate viscosity of fluids is empirically observed to be a function of the temperature and density (or pressure) of the fluid. The independence of the initial phase or preparative history is the nonequilibrium analogue of the situation where at equilibrium thermodynamic free energies are commonly observed to be thermodynamic state functions. Even at equilibrium the conditions required for this to be the case are not known (they are violated in glassy systems for example).

If a single steady state is approached, its statistics may be recovered from an individual trajectory, and this may have no knowledge of the initial ensemble ff. This loss of knowledge of the initial ensemble amounts to a decay of correlations, which may be further weakened. It must be stressed that the decay of correlations required by the validity of the Ω\Omega-FR reduces to the Ω\Omega-autocorrelation decay, with respect to the initial ensemble ff. As is well known, this is required, close to equilibrium, for the existence of the transport coefficients.

In the case that transitivity and boundedness of Ω\Omega suffice to obtain the steady state Ω\Omega-FR (something that needs further study), we observe that these are much weaker conditions than the Anosov assumption, which also implies the boundedness of the phase space contraction rate.Recall that the Anosov assumption was considered appropriate for the particle system of , in which −Λ=Ω-\Lambda=\Omega, although Ω\Omega was not bounded. This is interesting, because one can name a number of cases which do have bounded Ω\Omega, like the isokinetic (or isoenergetic) hard particle systems; the isokinetic or Nosé-Hoover thermostatted systems for heat current and shear flow systems with bounded interaction potentials; the color conductivity isokinetic systems with unbounded potentials etc. Transitivity, in turn, is almost always verified.

We note that in order to obtain a steady state Σ\Sigma-FR, the initial distribution, f0f_{0}, must be obtainable from a single the field free evolution, and AIΓAI\Gamma must hold. These conditions are easily obtainable for systems of physical interest.

The Σ\Sigma-FR’s directly refer to the dissipative fluxes or to quantities simply related to them, rather than to the phase space contraction rate. This avoids the difficulty of justifying how a Λ\Lambda-FR can speak of the fluctuations of the entropy production rate. As discussed in , these difficulties are more evident close to equilibrium, where one observes that the convergence times of the Λ\Lambda-FR typically diverge as the dissipative applied field decreases and the system approaches equilibrium. This is due to the fact that Λ\Lambda contains undesirable terms, which have to average to zero. As one approaches equilibrium the dissipation decreases as the square of the dissipative field while the undesirable terms remain constant (to leading order in the field). Therefore, longer and longer averaging times are required before the Λ\Lambda-FR converges. It has been argued that the Σ\Sigma-FR can be obtained from the Λ\Lambda-FR because the time averages of Σ\Sigma and −Λ-\Lambda become equivalent in the long time limit. However, this argument can not explain the satisfaction of the Σ\Sigma-FR at physically accessible times in non-isoenergetic systems at low fields. Moreover, if the Van Zon - Cohen picture applies to deterministic particle systems, as argued in Refs., the asymptotic equivalence between Σ\Sigma-FR and Λ\Lambda-FR is restricted to a limited fraction of the possible fluctuation values. As a matter of fact, Σ\Sigma equals −Λ-\Lambda only if ff is uniform in M\mathcal{M}, which requires M\mathcal{M} to be compact. When this is not the case, Σ\Sigma and Λ\Lambda are substantially different quantities, as even Ref. shows. The difficulties with the weak field convergence of Λ\Lambda-FR make the derivation of Green-Kubo relations from Λ\Lambda-FR, highly problematic . Differently, if a relation for the dissipation is obtained independently, this difficulty is not present. In particular, the convergence times are understood in terms of material properties related to known, physical properties of the system (e.g. the Maxwell time is related to the infinite frequency shear modulus and the zero shear rate shear viscosity), and the derivation of the Green-Kubo relations from the steady state Σ\Sigma-FRs is reasonably straightforward .

It is also important to consider the consistency of the results obtained in this manuscript with those obtained for the axiom C systems postulated in Refs.. As discussed in Appendix B, these systems may satisfy the decay of correlations of all observables, with respect to an invariant measure supported on a surface Mr\mathcal{M}_{r}, of dimension lower than that of the phase space M\mathcal{M}. Then, assuming as in Ref., that Λ\Lambda is proportional to the contraction rate of volumes in Mr\mathcal{M}_{r}, Λr\Lambda_{r} say, Λ\Lambda should obey a modified FR. So far there is no direct evidence, in particle systems, of the validity of that assumption (supported by numerical studies of certain hydrodynamic models ). In fact, in the case considered in Ref., the dissipation is sufficiently high that the dynamics is not transitive yet the Σ\Sigma-FR holds without the modifications conjectured in . In other words, our work and Refs. usually consider different observables, and when they consider the same observable, it is not necessary that they lead to the same conclusions of Refs.. If, on the other hand, the treatment of Refs. applies, the decay of correlations of Section 4 is compatible with it, as explained in Appendix B, because it is referred to the initial measure, and not the invariant one.One should also observe that Eq.(40) is exact, hence cannot lead to any contradiction about reversible dynamical systems. The energy dissipation Σ\Sigma remains related to Λ\Lambda, not to Λr\Lambda_{r}, even if the steady state is confined inside a lower dimensional manifold Mr\mathcal{M}_{r}.

As pointed out by one of the anonymous referees, the existence of a unique stationary measure may be considered a strong assumption, and the necessary and sufficient condition required for it to hold are not known. Therefore, the study of Anosov systems constitutes a natural starting point for the purpose of classifying the dynamical systems that verify some kind of FR. The purpose of the present paper is different: it amounts to analyzing systems which cannot be chosen at will, but are selected by physical conditions, in order to understand further their properties as well as the physical mechanism responsible for FR’s to hold in natural systems. We have found that time reversibility and ergodic consistency imply, without further assumptions, a number of transient and asymptotic FRs (cf. Sections 2 and 3), which are amenable to experimental verification. If the system of interest does not reach a unique steady state, assuming that it is Anosov does not help of course, but those relations remain valid. When present, convergence to a unique steady state is the manifestation of a certain decay of correlations of the observables, which typically are required to relax to a steady state. The approach proposed in this paper thus makes it clear that the details of the microscopic dynamics (like the very strong hypothesis of uniform hyperbolicity) do not play any role in the validity of the FR’s, as appropriate for thermodynamic relations. The class of dynamical systems which obey Eq.(60) cannot be determined, however, by this approach.

These facts may help in developing further the theory of nonequilibrium phenomena, as the derivation of the novel relations given above indicates.

ACKNOWLEDGMENTS

We wish to thank the Australian Research Council, and the Italian Embassy in Canberra for support. We also thank the Erwin Schrödinger Institute for support for the "Workshop on Stochastic and Deterministic Dynamics in Equilibrium and Nonequilibrium Systems" where this work was discussed. We thank Barbara Johnston for her input to this work, and Stephen Williams, Emil Mittag, Angelo Vulpiani, E.G.D. Cohen, Federico Bonetto and Carlos Mejia Monasterio for their comments. Thanks are in order also to the anonymous referees, for useful remarks on the purpose of our work.

APPENDIX A

Using the general definition of the dissipation function (13), it can be shown that the instantaneous value of the dissipation function is directly related to the instantaneous dissipative flux for a wide class of systems. Here we consider three cases: isoenergetic, isokinetic and Nosé-Hoover thermostatted dynamics.

A general form of the equations of motion for a field-driven N-particle, thermostatted nonequilibrium system is

where Fe{\bf F}_{e} is the applied field that is coupled to the system via the phase functions Ci(Γ){\bf C}_{i}(\Gamma) and Di(Γ){\bf D}_{i}(\Gamma). The term −αpi-\alpha{\bf p}_{i} is a deterministic, time reversible term used to add or remove heat from the system . The adiabatic equations of motion

simply lack the thermostatting term. If Eqs.(66) are Hamiltonian, the phase space expansion rate Λ\Lambda obviously vanishes, a condition referred to as adiabatic incompressibility of phase space, AIΓAI\Gamma , but AIΓAI\Gamma may hold even if the general adiabatic equations are not Hamiltonian. Here, for simplicity, we concentrate on systems which satisfy AIΓAI\Gamma, because their dissipative flux and dissipation function are simply related. In the other cases, the relationship between dissipative flux and dissipation function is only more complicated. We also assume that the initial distribution of phases f0f_{0} may in principle be generated by a single field-free (Fe=0F_{e}=0) thermostatted dynamics. By this we mean that f0f_{0} must not only be preserved by the equilibrium dynamics, but also that a single field free trajectory may explore all of its support. In other words, that this support is not the union of disjoint invariant sets, like the constant energy surfaces corresponding to different initial energies of Hamiltonian systems. This is consistent with nonlinear response theory that shows that if one is interested in the statistics of the physically relevant steady state observables, f0f_{0} should be that which corresponds to the field free dynamics . The possible difficulties that might be encountered if f0f_{0} is not selected to be the distribution function generated by the field free dynamics can easily be seen by considering the distribution of ϕ‾0,τ\overline{\phi}_{0,\tau} along an equilibrium trajectory. In this case the correct physical picture requires the right hand side of Eq.(39) to be 1 for all A,t0,δA,t_{0},\delta and τ\tau. This can only be the case if Ω(Γ)=0\Omega(\Gamma)=0 for all Γ\Gamma. Using Eq.(34), this implies that f0(S0tΓ)=ft(S0tΓ)f_{0}(S^{t}_{0}\Gamma)=f_{t}(S^{t}_{0}\Gamma) under the field free dynamics S0tS^{t}_{0}, and that f0=ftf_{0}=f_{t} must be preserved by the field free dynamics. Note that a single trajectory can’t possibly generate the ensemble in physically relevant times, in any system made of more than a few particles, but it may do it, in principle, allowing it to evolve for exceedingly long. This is needed for the possible initial equilibrium state to be uniquely determined.

In general, the dissipative flux, J{\bf J}, is obtained from the adiabatic time-derivative of the internal energy, H0=∑i=1Npi⋅pi2m+Φ(q)H_{0}=\sum_{i=1}^{N}\frac{{\bf p}_{i}\cdot{\bf p}_{i}}{2m}+\Phi({\bf q}), i.e. from the derivative of the internal energy under the dynamics of Eqs.(66):

while the full dynamics of Eqs.(65) yields

were KK is the kinetic energy of the system. Consider now three widely used deterministic, reversible thermostatting methods.

Gaussian isoenergetic (ergostatted) system. In this case H0H_{0} is fixed, i.e. H˙0=0\dot{H}_{0}=0, and Eq.(68) gives

For the ergostatted system described by equations (65), the phase space expansion rate is,

where AIΓAI\Gamma is used to obtain the final equality, and ON(1)O_{N}(1) is a correction which is order 1 in NN. The ON(1)O_{N}(1) term can be explicitly determined from the partial derivative of the Gaussian ergostatting term with respect to p{\bf p}. The equilibrium phase space distribution function is microcanonical on a surface H0=H_{0}=const, hence f(iSτΓ)=f(SτΓ)=f(Γ)f(iS^{\tau}\Gamma)=f(S^{\tau}\Gamma)=f(\Gamma), and Eq.(13) yields:

where β(Γ)=(dN−d−1)/(2K(Γ))\beta(\Gamma)=(dN-d-1)/(2K(\Gamma)).

Gaussian isokinetic system. In this case the kinetic energy is fixed K(Γ)=K0=(dN−d−1)kBT=(dN−d−1)/βK(\Gamma)=K_{0}=(dN-d-1)k_{B}T=(dN-d-1)/\beta. Equation (68) can therefore be used to show,

while the phase space expansion rate Λ\Lambda is still expressed by (70) to order N, with a different ON(1)O_{N}(1) term. The equilibrium phase space distribution function takes the form f(Γ)∼e−βH0δ(K(Γ)−K0)f(\Gamma)\sim e^{-\beta H_{0}}\delta(K(\Gamma)-K_{0}), on a surface K(Γ)=K(\Gamma)=const, hence f(Γ)/f(iSτΓ)=eβ∫0τH˙0(Γ(s))dsf(\Gamma)/f(iS^{\tau}\Gamma)=e^{\beta\int_{0}^{\tau}{\dot{H}}_{0}(\Gamma(s))ds}, and Eq.(13) leads to:

for all τ\tau. Combining this with Eqs.(73) and (70), one obtains

Nosé-Hoover thermostat. In this case, equations (65) are supplemented with the equation,

where Q is a constant related to the relaxation time of the thermostat, and TT is the imposed average temperature. In this case,

The equilibrium phase space distribution function is the Nosé-Hoover extended canonical distribution f(Γ)∼e−β(H0+12Qα2)f(\Gamma)\sim e^{-\beta(H_{0}+\frac{1}{2}Q\alpha^{2})}, hence f(Γ)/f(iSτΓ)=eβ∫0τ(H˙0Γ(s)+Qαα˙)dsf(\Gamma)/f(iS^{\tau}\Gamma)=e^{\beta\int_{0}^{\tau}({\dot{H}}_{0}\Gamma(s)+Q\alpha\dot{\alpha})ds}. So equation (13) can be used to show that:

Therefore, for field driven nonequilibrium systems whose equations of motion satisfy AIΓAI\Gamma, the dissipation function and the dissipative flux are simply related. In fact, for thermostatted systems with a constant field, Σ(Γ)=kJ(Γ)\Sigma(\Gamma)=kJ(\Gamma) where kk is a constant.

It is straightforward to show that the same expressions (72), (75),(80) can be obtained even if only a fraction of the system’s particles is subjected to a thermostat (e.g. the wall particles), see , for example. Furthermore, if the walls are large, the results are not sensitive to the details of the thermostatting mechanism .

APPENDIX B

The derivation of the steady state relations from transient ones needs a careful analysis of the conditional average

which appears in Eqs.(27,40), and of its limit

which is needed for the transient states μt0\mu_{t_{0}} to eventually reach the steady state μ∞\mu_{\infty}. In particular, M(A,δ,τ)M(A,\delta,\tau) must exist and be positive for τ\tau larger than a certain τA,δ\tau_{A,\delta}, for the pair (−A,A)(-A,A) to be δ\delta-possible, i.e. for fluctuations of size close to AA to occur, and for AA to be in the domain of the fluctuation relation with some tolerance γ>δ\gamma>\delta.

As observed in the text, Eqs.(27) and (40) are exact, hence cannot contradict any correct result on deterministic, reversible dynamical systems. The question is whether one can extract sufficient information from them, that they can be of practical use for the description of the statistics of steady state trajectories. This requires that either the dynamics of interest be explicitly given, or that the possible situations be explored. In section 4, we have considered the possibility that the Ω\Omega-autocorrelation decays in time, as the most common for the deterministic reversible particle models of nonequilibrium fluids. In fact, less is needed for the steady state Ω\Omega-FR to hold for AA; it suffices that M(A,δ,τ)M(A,\delta,\tau) does not grow too fast with τ\tau: subexponential growths, and exponential growths with rate not larger than δ\delta (as for A=0A=0) are all acceptable.

In the linear regime, the decay of correlations in the steady state can be well approximated by their decay at equilibrium, and for this reason, in the linear regime, the transport coefficients are given by the integral of the equilibrium time correlation function, multiplied by the field . Lack of decay of correlations of Ω\Omega corresponds to the non-existence of the transport coefficient associated with Ω\Omega. Further away from equilibrium, nonlinear response theory applies. Now the time correlation function is still determined with respect to the initial measure μ\mu, but the dynamics used to compute the nonlinear transport coefficients is the nonequilibrium one (cf. the Transient Time Correlation Function ). This is analogous to what is done in calculations of M(A,δ,τ)M(A,\delta,\tau), and if the nonlinear transport coefficients exist in the nonlinear regime, then there should be a decay of the Ω\Omega-autocorrelation, with respect to the equilibrium measure. Note also that the growth of τ\tau increases the separation of the end of the integral in the first exponential of Eq.(81) from the beginning of the integral in the second exponential, hence that the growth of τ\tau should contribute to the decorrelation.

Therefore, it looks quite plausible that, in most cases, one of the above considerations on the decay of correlations be satisfied. There is, however, one competing effect, which may become important in particular circumstances: the set of trajectories over which the conditional average (81) is computed changes with τ\tau, and this may balance the decorrelation phenomena in some cases.

To illustrate these facts, consider a simple model that has been discussed in connection to the fluctuation theorems in the past , and apply the procedure described in this manuscript to that example. The model consists of a particle moving in empty space, under the action of a constant external force Fe{\bf F_{e}} and a Gaussian thermostat:

where the kinetic energy K=p⋅p/2K={\bf p\cdot p}/2 is a constant of motion. The dynamics of this particle is rather simple: for initial conditions with p{\bf p} pointing in the direction opposite to Fe{\bf F}_{e}, p{\bf p} is a constant of motion; for all other initial conditions the direction of p{\bf p} tends to the direction of Fe{\bf F_{e}}, while the magnitude of p{\bf p}, 2K\sqrt{2K}, is constant. The treatment of Sections 2 and 3 applies to this system, since it is reversible and an initial distribution that is ergodically consistent with the final distribution can be selected. However there are various reasons why the treatment in Section 4 cannot be applied to produce a steady state Σ\Sigma-FR in this case. For instance, the distribution generated by the field free equations of motion is not ergodically consistent with the steady state dynamics (see Appendix A). In addition, the attractor is a fixed point in p{\bf p}-space, and the time-dependence of q\bf q is irrelevant; so, for any Ω\Omega that is a function of p\bf p only, there are no steady state fluctuations - that is for small δ\delta, no pair (−A,A)(-A,A) is δ\delta-possible, hence that the domain of the steady state Ω\Omega-FR is empty. The theory outlined in this paper also anticipates these facts, since correlations for any phase function do not decay, and therefore the term MM diverges in the t0→∞t_{0}\to\infty limit. In particular, selecting the dissipation function that would correspond to a uniform initial distribution, we obtain Ω=−Λ=(d−1)Fe⋅p/2K\Omega=-\Lambda=(d-1){\bf F}_{e}\cdot{\bf p}/2K where dd is the number of dimensions in configuration space. The range of values of this Ω\Omega is [−(d−1)2K∣Fe∣,(d−1)2K∣Fe∣][-(d-1)\sqrt{2K}|{\bf F_{e}}|,(d-1)\sqrt{2K}|{\bf F_{e}}|] and any smooth probability distribution in it (e.g. the uniform one) evolves in time in such a way that

As all trajectories, except those with initial condition p(0)=−(d−1)2KFe/∣Fe∣{\bf p}(0)=-(d-1)\sqrt{2K}{\bf F}_{e}/|{\bf F}_{e}|, tend to have Ω=(d−1)2KFe/∣Fe∣\Omega=(d-1)\sqrt{2K}{\bf F}_{e}/|{\bf F_{e}}|, this means that the integrals Ω0,t0\Omega_{0,t_{0}} and Ωt0+τ,2t0+τ\Omega_{t_{0}+\tau,2t_{0}+\tau} diverge linearly with t0t_{0}.

Therefore, Eq.(60) does not apply in this case. This will be the case for any steady state that has no fluctuations. Nevertheless, the transient and asymptotic relations remain valid for the evolving ensembles. The transient Ω\Omega-FR expresses the rate at which the initial probability of observing −A-A vanishes, compared to the initial probability of AA, and the Ω∞\Omega_{\infty}-FR expresses the corresponding asymptotic rate; but the domain of the steady state Ω\Omega-FR is empty. A similar situation, with no fluctuations of opposite sign in the steady state, may be produced in more realistic models by applying extremely high fields, making the motion ordered. In these cases, the domain of the steady state Ω\Omega-FR would also be empty. However, intermediate situations are possible, like those of Ref., in which the attractors have small dimension, but the initial correlations decay, and the steady state Ω\Omega-FR holds.

References consider systems with steady states confined within manifolds Mr\mathcal{M}_{r} of dimension smaller than M\mathcal{M}, whose volumes fluctuate in time, so that the corresponding phase space contraction rate, Λr\Lambda_{r}, obeys the standard fluctuation relation. In these systems, correlations of all observables decay with respect to the invariant measure μ∞\mu_{\infty}, supported on Mr\mathcal{M}_{r}. Furthermore, if the phase space contraction rate Λ\Lambda, in the space of the field-free dynamics M\mathcal{M}, is proportional to Λr\Lambda_{r}, as assumed in , a modified FR holds for it, which can be expressed as

with c<1c<1. The relevance of such a possibility for particle systems is not obvious, but no difficulty emerges with the theory developed here, since the decay of correlations with respect to μ∞\mu_{\infty} does not imply the decay of correlations with respect to a non-singular measure supported on M\mathcal{M}. Many different scenarios are possible, and should be analyzed case by case, but this goes beyond the purpose of the present paper. Here it suffices to observe that no scenario that can be realized can contradict the framework of the present paper; to the contrary, it could be explained in it, through the analysis of the conditional average (81).

References