The current flow for a local electrolytic cell with rectangular anode and cathode is calculated as a function of a polarization parameter, electrolyte thickness and conductivity, anode and cathode size, and zero current potential difference. The total current is obtained from the numerical computation (with error analysis) of a series solution of Laplace's equation assuming a linear polarization relation at the electrode-electrolyte interface. For high values of the polarization parameter and sufficiently thick electrolytes an asymptotic formula obtains for the current approximately proportional to the anodic fraction, as was found by Waber et al. However, in general the cell geometry greatly influences the amount of current flow, especially for anode shapes near to linear rather than near to square. This effect can be greater than an order of magnitude. The calculated results are compared with experimental data obtained by Ogburn and Schlissel and are shown to be in good agreement. Corrosion currents in randomly pitted surfaces may be estimated from the above results.
Electrodeposited lead dendrites were grown and examined by x-ray diffraction and metallographically. Their structure was essentially that of two crystals having a twist relation about a common [111] pole which was normal to the flat surface of the two-dimensional dendrites. Each dendrite contained many small voids or channels. The direction of growth was either about halfway between a <211> direction of one crystal and a neighboring <211> direction of the second crystal or halfway between <110> directions.Electrodeposited dendrites 2 have been described and reviewed extensively by Wranglen (1). He examined dendrites of lead, tin, silver, cadmium, and copper microscopically and by x-ray diffraction and described them as single crystals. Faust and Johns (2) examined electrodeposited dendrites of lead, silver, copper, gold, and aluminum, and by metallography found at least one grain boundary in each of the dendrites growing in <211> or
Isolated faces of copper single crystals were plated with copper from copper sulfate‐sulfuric acid solutions. Deposits on {100} and {110} faces, despite the presence of grain boundaries, gave x‐ray diffraction patterns showing uniform lattice orientation. The grain boundaries were associated with topographic features of the deposits. Over‐all metal distribution showed a tendency to deviate from that of poly crystal deposits on polycrystalline bases.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
customersupport@researchsolutions.com
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
This site is protected by reCAPTCHA and the Google Privacy Policy and Terms of Service apply.
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.