Abstract

Many complex fluids can be described by continuum hydrodynamic field equations, to which noise must be added in order to capture thermal fluctuations. In almost all cases, the resulting coarse-grained stochastic partial differential equations carry a short-scale cutoff, which is also reflected in numerical discretisation schemes. We draw together our recent findings concerning the construction of such schemes and the interpretation of their continuum limits, focusing, for simplicity, on models with a purely diffusive scalar field, such as ‘Model B’ which describes phase separation in binary fluid mixtures. We address the requirement that the steady-state entropy production rate (EPR) must vanish for any stochastic hydrodynamic model in a thermal equilibrium. Only if this is achieved can the given discretisation scheme be relied upon to correctly calculate the nonvanishing EPR for ‘active field theories’ in which new terms are deliberately added to the fluctuating hydrodynamic equations that break detailed balance. To compute the correct probabilities of forward and time-reversed paths (whose ratio determines the EPR), we must make a careful treatment of so-called ‘spurious drift’ and other closely related terms that depend on the discretisation scheme. We show that such subtleties can arise not only in the temporal discretisation (as is well documented for stochastic ODEs with multiplicative noise) but also from spatial discretisation, even when noise is additive, as most active field theories assume. We then review how such noise can become multiplicative via off-diagonal couplings to additional fields that thermodynamically encode the underlying chemical processes responsible for activity. In this case, the spurious drift terms need careful accounting, not just to evaluate correctly the EPR but also to numerically implement the Langevin dynamics itself.

Highlights

  • Numerous complex fluid systems can be described by continuum equations formulated at the hydrodynamic level

  • We have further extended these ideas and embedded a large class of active field theories in a thermodynamically consistent setting that accounts for their driving mechanism, in which case, the irreversibility of the enlarged system capture the actual rate of heat production

  • By accounting for the driving mechanism, we find that the rate of heat production for the active system follows from the full entropy production rate (EPR) measuring the irreversibility of both the active and driving fields, which can be evaluated from the fluctuations of active fields only

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Summary

Introduction

Numerous complex fluid systems can be described by continuum equations formulated at the hydrodynamic level. In our studies of active field theories, we have found interesting physics to be laid bare when one considers the way the IEPR (and the heat rate) depends on the spatial configuration of the system and the way different contributions to it (e.g., bulk or interfacial) scale with the noise level To address these issues by computer simulation, it is clearly crucial to have a numerical implementation in which the calculated entropy production arises solely by virtue of the active, detailed-balance-breaking terms, unpolluted by any failure of the numerical discretisation scheme to respect detailed balance even in thermal equilibrium.

Langevin Equation
Discretised Langevin Equation
Fokker–Planck Equation
Transition Probability
Path Integral Suppose that, initially, the particle is at x0 at time t0
Entropy Production
Evaluation via Discretised Action
Non-Equilibrium Steady State
Stochastic Calculus for d > 1 Degrees of Freedom
Conversion from Stratonovich to Itô Integral
Dynamical Action
Scalar Active Field Theories with Additive Noise
Informatic Entropy Production
Spatial Discretisation
Computing the IEPR
Tt t 0
Thermodynamics of Active Field Theories
Onsager Coupling in Two-Dimensional System
Spatial Discretisation in Stochastic Field-Theories
Thermodynamics of a Conserved Active Scalar Field
Concluding Remarks
Full Text
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