Year-end Sale % OFF 
Abstract
Measurements of the quadrupole splitting in the pyrite-structure compounds FeS2, Fe0.01Co0.99S2, and Fe0.01Ni0.99S2 are reported. These splittings, and those of the similar compounds FeS2, FeSe2, and FeTe2 of the marcasite structure, are shown to correlate well with the electric field gradient at the Fe site, calculated on the point-charge model. Deviations of the calculated quadrupole splitting from that observed in these compounds are in the directions to be expected from covalent effects and from distortion of the local environment of the Fe atoms.
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.
