Abstract
CoVO is an orthorhombic magnet in which magnetic moments reside on two crystallographically inequivalent Co sites, which decorate a stacked, buckled version of the two-dimensional kagome lattice, the stacked kagome staircase. The magnetic interactions between the Co moments in this structure lead to a complex magnetic phase diagram at low temperature, wherein it exhibits a series of five transitions below 11 K that ultimately culminate in a ferromagnetic ground state below K. Here we report magnetization measurements on single- and polycrystalline samples of (CoMg)VO for , as well as elastic and inelastic neutron scattering measurements on single crystals of magnetically dilute (CoMg)VO for and , in which nonmagnetic Mg ions substitute for magnetic Co. We find that a dilution of 2.9 leads to a suppression of the ferromagnetic transition temperature by 15 while a dilution level of 19.4 is sufficient to destroy ferromagnetic long-range order in this material down to a temperature of at least 1.5 K. The magnetic excitation spectrum is characterized by two spin wave branches in the ordered phase for (CoMg)VO (), similar to that of the pure material, and by broad diffuse scattering at temperatures below 10 K in (CoMg)VO (). Such a strong dependence of the transition temperatures on long-range order in the presence of quenched nonmagnetic impurities is consistent with two-dimensional physics driving the transitions. We further provide a simple percolation model that semiquantitatively explains the inability of this system to establish long-range magnetic order at the unusually low dilution levels which we observe in our experiments.
6 More- Received 21 June 2012
DOI:https://doi.org/10.1103/PhysRevB.86.174421
©2012 American Physical Society