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Factors That Govern the Formation of Multi-Domainic Goethites

Published online by Cambridge University Press:  02 April 2024

R. M. Cornell  and
R. Giovanoli
R. M. Cornell
Affiliation:
Institute of Inorganic Chemistry, University of Berne, CH-3000 Berne 9, Switzerland
R. Giovanoli
Affiliation:
Laboratory of Electron Microscopy, University of Berne, CH-3000 Berne 9, Switzerland
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Abstract

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Transmission electron microscopic (TEM) examination has shown that multi-domainic crystals of synthetic goethite consist of almost parallel intergrowths, each of which is slightly misoriented with respect to its neighbors. These intergrowths emanate from a central nucleus within the crystal. They can nucleate along both the x and y crystal axes, but subsequent growth is mainly in the z direction.

The formation of multi-domainic goethites from ferrihydrite was favored by high pH (≥ 13) and, at lower pHs, by the addition of NaNO3 to the system. Decreasing the temperature of synthesis from 70° to 20°C also enhanced domain formation. The nucléation of domains was confined to the initial stage of goethite formation. Domains probably formed when crystal growth was very rapid or when adsorbed species blocked the appropriate sites on the nucleus material.

Keywords

DomainsGoethiteIntergrowthsIronSynthesisTransmission electron microscopy
Type
Research Article
Information
Clays and Clay Minerals , Volume 34 , Issue 5 , October 1986 , pp. 557 - 564
Copyright
Copyright © 1986, The Clay Minerals Society

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