Abstract
The magnetic properties of vermiculite (V) intercalated with 3d-transition-metal ions (, , , and ) as interlayer cations have been studied by measuring the dc magnetic susceptibilities of these compounds. The Landé g factors of the magnetic ions in V with and without water molecules coexisting in the gallery have been analyzed by using crystal-field theory. A substantial decrease in the crystal-field strength has been observed when water is removed from the gallery. V and V are found to be paramagnetic for temperatures down to 2 K regardless of the hydration conditions. Dehydrated V and V show signatures of an antiferromagnetic phase transition at a few degrees Kelvin (∼5 and ∼3 K, respectively), whereas they do not exhibit any magnetic ordering while water is present in the gallery.
- Received 23 November 1992
DOI:https://doi.org/10.1103/PhysRevB.47.16486
©1993 American Physical Society