Abstract
The first study of noncramers Fe 2+ substitutional center in YAG by acoustic EPR is presented. Symmetry of the crystal field in the site of Fe 2+ localization was determined. Magnetic properties of the Fe 2+ ion ground state were measured: g ∥ = 4.815 ± 0.08, ΔB 1 2 = 75 ± 6 G . Using the measured g-factor, the value of the trigonal field constant δ was estimated. A simple theory of the Fe 2+ ground state is presented.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
