Published January 1988 | Version v1
Journal article

Interpreting the optical spectra of trace Fe2+ in layer silicates

  • 1. Dumanskii Institute of Colloid and Water Chemistry (USSR)

Description

Estimates have been made of Fe2+ term splittings in axial crystalline fields. It is found that all three long-wave bands in the optical spectrum are due to Fe2+ α Fe3+ charge transfer, while the splitting of 5T/sub 2g/ and 5E/sub g/ occurs in low-symmetry fields. Experimental evidence is presented for these calculations

Additional details

Publishing Information

Journal Title
Theoretical and Experimental Chemistry (English Translation)
Journal Volume
23
Journal Issue
4
Series
Theor. Exp. Chem. (Engl. Transl.).
Journal Page Range
435-438
ISSN
0040-5760
CODEN
TEXCA

Optional Information

Notes
Translated from Teoret. Eksper. Khimiya; 23: No. 4, 464-468(Jul-Aug 1987). Cover-to-cover translation of Teoreticheskaya i Ehksperimental'naya Khimiya (USSR).