101. X-ray magnetic circular dichroïsm provides strong evidence for tetrahedral iron in ferrihydrite
- Author
-
Yohan Guyodo, Philippe Sainctavit, Marie-Anne Arrio, Claire Carvallo, R. Lee Penn, Jasmine J. Erbs, Brady S. Forsberg, Guillaume Morin, Fabien Maillot, France Lagroix, Pierre Bonville, Fabrice Wilhelm, and Andrei Rogalev
- Subjects
010504 meteorology & atmospheric sciences ,Extended X-ray absorption fine structure ,Magnetic circular dichroism ,010502 geochemistry & geophysics ,01 natural sciences ,Magnetic field ,Crystallography ,Ferrihydrite ,Geophysics ,Nuclear magnetic resonance ,Octahedron ,X-ray magnetic circular dichroism ,Geochemistry and Petrology ,Absorption (chemistry) ,Earth (classical element) ,Geology ,0105 earth and related environmental sciences - Abstract
[1] Ferrihydrite is an important iron oxyhydroxide for earth and environmental sciences, biology, and technology. Nevertheless, its mineral structure remains a matter of debate. The stumbling block is whether a significant amount of tetrahedrally coordinated iron is present. Here we present the first X-ray magnetic circular dichroism (XMCD) measurements performed on a well characterized synthetic sample of 6-line ferrihydrite, at both K and L2,3energy edges of iron. XMCD results demonstrate unambiguously the presence of tetrahedrally coordinated Fe(III) in the mineral structure, in quantities compatible with the latest extended X-ray absorption fine structure (EXAFS) analyses suggesting a concentration of 20–30%. Moreover, we find an antiferromagnetic coupling between tetrahedral and octahedral sublattices, with the octahedral sublattice parallel to the external magnetic field.
- Published
- 2012