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Journal of Electroanalytical Chemistry
Volume 407, Issues 1-2, 10 May 1996, Pages 61-73
 
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doi:10.1016/0022-0728(95)04477-9    How to Cite or Link Using DOI (Opens New Window)
Copyright © 1996 Published by Elsevier Science B.V.

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A quantitative study of gravity-induced convection in two-dimensional parallel electrodeposition cells

J. -N. Chazalviela, M. Rossoa, Corresponding Author Contact Information, E. Chassaingb and V. Fleurya

a Laboratoire de Physique de la Matière Condensée, CNRS-Ecole Polytechnique, 91128, Palaiseau Cedex, France b Centre d'Etudes de Chimie Métallurgique, CNRS, 15 Rue Georges Urbain, 94407, Vitry-sur-Seine Cedex, France

Received 15 September 1995; 
revised 16 November 1995. 
Available online 11 December 1998.

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Abstract

Even in thin horizontal cells, electrodeposition of tree-like metal aggregates is accompanied by a gravity-induced fluid flow at the electrodes. This flow has been calculated and the resulting map of the salt concentration has been deduced. Two extreme flow regimes are found: at shorter times, fluids with different densities behave as immiscible liquids and the extent of the perturbed zone near the electrode is found to vary with time as t4/5. For longer times, fluid motion is sufficiently slow that diffusion tends to equalize the concentrations vertically (i.e. along the direction normal to the cell). In this regime, the extent of the perturbed zone varies as t1/2. These two types of behaviour account quantitatively for experimental measurements on Cu electrodeposition in copper sulphate electrolytes.

Author Keywords: Electrodeposition; Convection; Buoyancy; Optical absorption

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