Abstract
The magnetic properties of FeCl2·2H2O have been investigated by means of single-crystal magnetic susceptibility, high-field magnetization, and proton nuclear-magnetic-resonance (nmr) measurements. A transition to an antiferromagnetic state is observed at TN23°K. The magnetic susceptibility tensor in the paramagnetic state has uniaxial symmetry about an axis (α) lying in the ac plane (α=α*+58°). In the range 30-100°K the measured susceptibilities follow a Curie-Weiss relation with gα=2.4, gβgγ=1.9, and effective Weiss constants Δα=12°K, ΔβΔγ=5°K. The zero-field proton nmr in the ordered state consists of a single spin-spin doublet with extrapolated center frequency at 0°K ν0=9.231±0.001 Mc/sec. Proton nmr measurements in weak external magnetic fields at 4.0°K give four symmetry-related proton local-field directions. The magnetic susceptibility and proton nmr experiments give evidence for a magnetic structure (Pc2m) in which ferromagnetic chains, parallel to the c axis, are coupled antiferromagnetically to adjacent chains. The direction of sublattice magnetization coincides with the α axis. The magnetization behavior at 4.0°K and with Hα exhibits two metamagnetic transitions, Hc1=39±1 kOe and Hc2=46±1 kOe. The corresponding magnetic moments are M1=1.4±0.1μB and M2=4.25±0.05μB. The first magnetization discontinuity is shown to result from an antiferromagnetic intrasublattice interaction which makes the two-sublattice zero-field configuration unstable with respect to a six-sublattice modification in sufficiently strong external fields.