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The Yellow Color of Silver-Containing Zeolite A.
Roland Seifert1, Andreas Kunzmann1, Gion Calzaferri1
1Department for Chemistry and Biochemistry, Freiestrasse 3, CH-3012 Berne (Switzerland), Fax: (+41) 31-6313994.
Angewandte Chemie (International Ed. in English)
|May 2, 2018
Summary
The yellow color in silver-containing zeolite A originates from oxygen atoms, not silver clusters. This color is caused by a charge-transfer transition from oxygen to silver ions.
Area of Science:
- Materials Science
- Solid-State Chemistry
- Spectroscopy
Background:
- Silver-containing zeolite A exhibits a yellow coloration, a phenomenon observed since 1962.
- The precise origin of this yellow color has been a long-standing question in the field.
Purpose of the Study:
- To elucidate the fundamental cause of the yellow color in silver-containing zeolite A.
- To identify the specific atomic or electronic interactions responsible for the observed optical properties.
Main Methods:
- Spectroscopic analysis to probe electronic transitions.
- Theoretical calculations to model charge transfer processes.
- Characterization of silver-zeolite A structures.
Main Results:
- The yellow color is attributed to oxygen atoms within the zeolite lattice, not silver clusters.
- A charge-transfer transition from lattice oxygen atoms to the silver ions' 5s orbital is identified as the cause.
- This finding resolves a decades-old scientific mystery.
Conclusions:
- The electronic structure and interactions of lattice oxygen are critical for the optical properties of silver-zeolite A.
- Understanding these charge-transfer mechanisms provides insights into the color of related materials.
- This work clarifies the origin of color in silver-containing zeolites.
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