Fluctuating hydrodynamics of dilute electrolyte solutions: systematic perturbation calculation of effective transport coefficients governing large-scale dynamics

TL;DR

This paper develops a systematic perturbation approach using fluctuating hydrodynamics to calculate frequency-dependent transport coefficients like diffusion, viscosity, and conductivity in dilute electrolyte solutions, revealing new insights into their large-scale dynamics.

Contribution

It introduces a novel perturbation calculation method for effective transport coefficients in electrolyte solutions, including frequency dependence and electrophoretic effects, extending classical theories.

Findings

Frequency dependence of viscosity and conductivity analyzed in one-loop approximation.

Derived the electrophoretic contribution to finite-frequency conductivity.

Predicted the maximum in real conductivity at a specific frequency proportional to salt density.

Abstract

We study the transport properties of dilute electrolyte solutions on the basis of the fluctuating hydrodynamic equation, which is a set of nonlinear Langevin equations for the ion densities and flow velocity. The nonlinearity of the Langevin equations generally leads to effective kinetic coefficients for the deterministic dynamics of the average ion densities and flow velocity; the effective coefficients generally differ from the counterparts in the Langevin equations and are frequency-dependent. Using the path-integral formalism involving auxiliary fields, we perform systematic perturbation calculations of the effective kinetic coefficients for ion diffusion, shear viscosity, and electrical conductivity, which govern the dynamics on the large length scales. As novel contributions, we study the frequency dependence of the viscosity and conductivity in the one-loop approximation. Regarding the conductivity at finite frequencies, we derive the so-called electrophoretic part in addition to the relaxation part, where the latter has been obtained by Debye and Falkenhagen; it is predicted that the combination of these two parts gives rise to the frequency $\omega_{\rm max}$ proportional to the salt density, at which the real part of the conductivity exhibits a maximum. The zero-frequency limits of the conductivity and shear viscosity coincide with the classical limiting laws for dilute solutions, derived in different means by Debye, Falkenhagen, and Onsager. As for the effective kinetic coefficients for slow ion diffusions in large length scales, our straightforward calculation yields the cross kinetic coefficient between cations and anions. Further, we discuss the possibility of extending the present study to more concentrated solutions.