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Dehydration of goethite and diaspore*

Veröffentlicht/Copyright: 28. Juli 2010
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Abstract

The dehydration of goethite and diaspore is studied in detail by single-crystal and powder x-ray methods, and also by the use of the electron microscope. By variation of the temperature of dehydration and duration of heating it has been possible to observe intermediate states in the process.

These intermediate states are revealed by satellite reflections which at certain temperatures occur close to the developed hematite or corundum diffraction spots. At higher temperatures these satellites are replaced by diffuse intensity regions, which disappear on further heating. The satellites could correspond to a sinusoidal structure-amplitude modulation along the c axis of the hematite or corundum crystallites, before dehydration is complete. The wavelength of the modulation was 32 Å for the hematite formed from goethite, and 39 Å for the corundum formed from diaspore.

Non-uniform broadening of the lines on powder photographs of the developed hematite, or corundum, was observed only when the original goethite or diaspore showed a particular texture. This effect is ascribed to stacking faults.

A well developed system of pores was observed on heated diaspore. The activation energies involved in the dehydration have been determined (19.8 kcal/mole for goethite, and 24.1 kcal/mole for diaspore). The inhomogeneous mechanism is confirmed for this type of dehydration, and a structural explanation for the formation of the satellites is presented.

Published Online: 2010-07-28
Published in Print: 1963-12
Heruntergeladen am 10.1.2026 von https://www.degruyterbrill.com/document/doi/10.1524/zkri.1963.119.3-4.176/pdf
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