Magnetic order and fluctuations in the presence of quenched disorder in the kagome staircase system (Co1xMgx)3V2O8

K. Fritsch, Z. Yamani, S. Chang, Y. Qiu, J. R. D. Copley, M. Ramazanoglu, H. A. Dabkowska, and B. D. Gaulin
Phys. Rev. B 86, 174421 – Published 21 November 2012
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Abstract

Co3V2O8 is an orthorhombic magnet in which S=3/2 magnetic moments reside on two crystallographically inequivalent Co2+ sites, which decorate a stacked, buckled version of the two-dimensional kagome lattice, the stacked kagome staircase. The magnetic interactions between the Co2+ 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 T6.2 K. Here we report magnetization measurements on single- and polycrystalline samples of (Co1xMgx)3V2O8 for x<0.23, as well as elastic and inelastic neutron scattering measurements on single crystals of magnetically dilute (Co1xMgx)3V2O8 for x=0.029 and x=0.194, in which nonmagnetic Mg2+ ions substitute for magnetic Co2+. 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 (Co1xMgx)3V2O8 (x=0.029), similar to that of the pure x=0 material, and by broad diffuse scattering at temperatures below 10 K in (Co1xMgx)3V2O8 (x=0.194). 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.

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  • Received 21 June 2012

DOI:https://doi.org/10.1103/PhysRevB.86.174421

©2012 American Physical Society

Authors & Affiliations

K. Fritsch1, Z. Yamani2, S. Chang3, Y. Qiu3,4, J. R. D. Copley3, M. Ramazanoglu1, H. A. Dabkowska5, and B. D. Gaulin1,5,6

  • 1Department of Physics and Astronomy, McMaster University, Hamilton, Ontario, Canada L8S 4M1
  • 2Canadian Neutron Beam Centre, National Research Council, Chalk River Laboratories, Chalk River, Ontario, Canada K0J 1P0
  • 3NIST Center for Neutron Research, NIST, Gaithersburg, Maryland 20899-8102, USA
  • 4Department of Materials Science and Engineering, University of Maryland, College Park, Maryland 20742, USA
  • 5Brockhouse Institute for Materials Research, Hamilton, Ontario, Canada L8S 4M1
  • 6Canadian Institute for Advanced Research, 180 Dundas Street West, Toronto, Ontario, Canada M5G 1Z8

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Issue

Vol. 86, Iss. 17 — 1 November 2012

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