AN EXAFS STUDY OF THE LOCAL STRUCTURAL ENVIRONMENTS OF FE, CO, ZN ANDMG IN NATURAL AND SYNTHETIC STAUROLITES

Citation
Cmb. Henderson et al., AN EXAFS STUDY OF THE LOCAL STRUCTURAL ENVIRONMENTS OF FE, CO, ZN ANDMG IN NATURAL AND SYNTHETIC STAUROLITES, Mineralogical Magazine, 61(5), 1997, pp. 613-625
Citations number
40
Categorie Soggetti
Mineralogy
Journal title
ISSN journal
0026461X
Volume
61
Issue
5
Year of publication
1997
Pages
613 - 625
Database
ISI
SICI code
0026-461X(1997)61:5<613:AESOTL>2.0.ZU;2-N
Abstract
X-ray absorption spectroscopy (XAS) has been used to study the local s tructures of Fe, Co, Zn, and Mg in synthetic and natural staurolites. Results for the near-edge features (XANES) and refined EXAFS were used to deduce the crystallographic site(s) occupied for each element. The least squares refined, mean first shell metal-O bond lengths, coordin ation numbers, and Debye-Waller factors are in the ranges: Fe 1.97-1.9 9 Angstrom, 3.5-4.1, 0.013-0.023 Angstrom(2); Co 1.97-1.98 Angstrom, 3 .5-3.9, 0.009-0.014 Angstrom(2); Zn 1.95-1.96 Angstrom, 3.7-3.8, 0.008 -0.009 Angstrom(2); and Mn 1.99 Angstrom, 3.8, 0.012 Angstrom(2). No s ignificant differences were found which depended on element concentrat ion or whether the sampes are synthetic or natural. The refined bond l ength for Mg in end-member Mg-staurolite is 2.00 Angstrom but EXAFS da ta did not allow refinement to give reliable coordination number and D ebye-Waller factor estimates. The EXAFS data, together with staurolite and model compound XANES features, suggest that > about 90% of Fe, Co , Zn and Mn are concentrated in the tetrahedral T2 site, while in Mg-s taurolite > about 75% of the total Mg is in T2 with the remainder in o ctahedral sites. In natural staurolite from Pizzo Forno (PF2), a great er proportion of Mg appears to be in octahedral coordination.