Role of Stefan-Maxwell fluxes in the dynamics of concentrated electrolytes

被引:24
作者
Balu, Bhavya [1 ]
Khair, Aditya S. [1 ]
机构
[1] Carnegie Mellon Univ, Dept Chem Engn, Pittsburgh, PA 15213 USA
关键词
DOUBLE-LAYER CAPACITANCE; LI-ION BATTERIES; MULTICOMPONENT DIFFUSION; CHALLENGES; LIQUIDS;
D O I
10.1039/c8sm01222a
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
This theoretical analysis quantifies the effect of coupled ionic fluxes on the charging dynamics of an electrochemical cell. We consider a model cell consisting of a concentrated, binary electrolyte between parallel, blocking electrodes, under a suddenly applied DC voltage. It is assumed that the magnitude of the applied voltage is small compared to the thermal voltage scale, RT/F, where R is the universal gas constant, T is the temperature and F is the Faraday's constant. We employ the Stefan-Maxwell equations to describe the hydrodynamic coupling of ionic fluxes that arise in concentrated electrolytes. These equations inherently account for asymmetry in the mobilities of the ions in the electrolyte. A modified set of Poisson-Nernst-Planck equations, obtained by incorporating Stefan-Maxwell fluxes into the species balances, are formulated and solved in the limit of weak applied voltages. A long-time asymptotic analysis reveals that the electrolyte dynamics occur on two distinct time scales. The first is a faster "RC" time, (RC) = k(-1)L/D-E, where k(-1) is the Debye length, L is the length of the half-cell, and D-E is an effective diffusivity, which characterizes the evolution of charge density at the electrode. The effective diffusivity, D-E, is a function of the ambi-polar diffusivity of the salt, D-a, as well as a cross-diffusivity, D+-, of the ions. This time scale also dictates the initial exponential decay of current in the external circuit. At times longer than (RC), the external current again decays exponentially on a slower, diffusive time scale, tau(D) similar to L-2/D-a, where D-a is the ambi-polar diffusivity of the salt. This diffusive time scale is due to the unequal ion mobilities that result in a non-uniform bulk concentration of the salt during the charging process. Finally, we propose an approach by which our theory may be used to measure the cross-diffusivity in concentrated electrolytes.
引用
收藏
页码:8267 / 8275
页数:10
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