A Mössbauer study of ferric iron in olivine |
| |
Authors: | I Shinno |
| |
Institution: | 1. Institute of Earth Science, College of General Education, Kyushu University, 810, Fukuoka, Japan
|
| |
Abstract: | Natural and synthetic olivines with ferrous and ferric iron have been studied by Mössbauer spectroscopy. Their spectra exhibit three superimposed quadrupole-split doublets corresponding to Fe2+ at M1 and M2 sites and Fe3+ at an unidentified position, which is probably M2. The hyperfine parameters of Fe3+ at temperatures between 300°C and 450°C are: Δ=0.67–1.23 mm/s, δ=0.04–0.23 mm/s relative to metallic iron, and the full width at half height, HW=0.15–0.43 mm/s. The Fe2+ populations of M2 decrease with increasing Fe3+ content. However, Fe2+ prefers M1 in synthetic olivines, even at high temperatures (800°–1,400°C). In kirschsteinite, Fe2+ and Fe3+ are exclusively in M1. Fe2+/Fe3+ ratios estimated from the peak areas are consistent with chemical analyses. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|