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A new approach to assignment of infra-red absorption bands in layer-structure silicates
Published/Copyright:
July 28, 2010
Abstract
The infra-red spectra of layer structures synthesized under controlled high-temperature, high-pressure conditions in sealed noble-metal systems have been examined in the region 400–5000 cm−1 (25–2 μ). By complete replacement of an ion, e.g., Mg2+ by Ni2+ or Fe2+, Al3+ by Ga3+ or Fe3+, and Si4+ by Ge4+ it was possible to assign the main absorption bands of layer-structure silicates. Bands involving various OH-vibrations were located by complete replacement of OH− by OD−.
The results obtained in this study suggest certain other relations between the bonds involved and IR spectra of the complex crystalline phases.
Published Online: 2010-07-28
Published in Print: 1961-08
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Articles in the same Issue
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- On the measurement of integrated intensities
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- Refinement of the crystal structure of andalusite
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- Supplementary note on “False symmetry, the Templeton effect, in lawsonite”
- Note on the false symmetry effect (“Templeton effect”)
- The crystal structure of andalusite
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