Magnetic order and lattice anomalies in the J1-J2 model system VOMoO4
Physical Review B Condensed Matter and Materials Physics 71:22 (2005)
Abstract:
High-resolution x-ray and neutron powder-diffraction measurements were performed on polycrystalline VOMoO4. Below ≃ 40K the system orders in a simple Néel antiferromagnetic state (propagation vector k =0), indicating a dominant role of the nearest-neighbor interactions. The order is three dimensional but the reduced saturated magnetic moment m of 0.41 (1) μ V4+ at 2K indicates strongly two-dimensional character and enhanced quantum fluctuations. On cooling, there is no evidence of a reduction of the crystal symmetry. However, neutron diffraction indicates an anomalous evolution of the lattice parameters, which can be related to the onset of magnetic correlations. © 2005 The American Physical Society.Orbital ordering in transition-metal spinels
New Journal of Physics 7 (2005)
Abstract:
Transition-metal spinels (general formula ABSpin structure and magnetic frustration in multiferroic RMn2O5 (R = Tb, Ho, Dy)
(2005)
Spin structure and magnetic frustration in multiferroic RMn2O5 (R = Tb, Ho, Dy)
ArXiv cond-mat/0501382 (2005)
Abstract:
We have studied the crystal and magnetic structures of the magnetoelectric materials RMn2O5 (R = Tb, Ho, Dy) using neutron diffraction as a function of temperature. All three materials display incommensurate antiferromagnetic ordering below 40 K, becoming commensurate on further cooling. For R = Tb, Ho, a commensurate-incommensurate transition takes place at low temperatures. The commensurate magnetic structures have been solved and are discussed in terms of competing exchange interactions. The spin configuration within the ab plane is essentially the same for each system, and the radius of R determines the sign of the magnetic exchange between adjacent planes. The inherent magnetic frustration in these materials is lifted by a small lattice distortion, primarily involving shifts of the Mn3+ cations and giving rise to a canted antiferroelectric phase.Structural evolution of natrolite during over-hydration: A high-pressure neutron diffraction study
European Journal of Mineralogy 17:2 (2005) 305-313