The effect of uniform constant magnetic fields on free‐convective ion transport in magnetoelectrolytic cells employing parallel vertical plate electrodes has been investigated in experiments with CuSO 4 / H 2 SO 4 and K 3 Fe ( CN ) 6 / K 4 Fe ( CN ) 6 / KOH electrolytes. A modified free‐convective diffusion model, developed from fundamental principles of magnetohydrodynamics and classical convective diffusion theory, offers a reasonable approximation to experimentally observed transport rates in horizontal magnetic fields.
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Kim et al. (1995) studied this question.