English

Nature of the spin dynamics and 1/3 magnetization plateau in azurite

Statistical Mechanics 2009-11-13 v1

Abstract

We present a specific heat and inelastic neutron scattering study in magnetic fields up into the 1/3 magnetization plateau phase of the diamond chain compound azurite Cu3_3(CO3_3)2_2(OH)2_2. We establish that the magnetization plateau is a dimer-monomer state, {\it i.e.}, consisting of a chain of S=1/2S = 1/2 monomers, which are separated by S=0S = 0 dimers on the diamond chain backbone. The effective spin couplings Jmono/kB=10.1(2)J_{mono}/k_B = 10.1(2) K and Jdimer/kB=1.8(1)J_{dimer}/k_B = 1.8(1) K are derived from the monomer and dimer dispersions. They are associated to microscopic couplings J1/kB=1(2)J_1/k_B = 1(2) K, J2/kB=55(5)J_2/k_B = 55(5) K and a ferromagnetic J3/kB=20(5)J_3/k_B = -20(5) K, possibly as result of dz2d_{z^2} orbitals in the Cu-O bonds providing the superexchange pathways.

Keywords

Cite

@article{arxiv.0709.2560,
  title  = {Nature of the spin dynamics and 1/3 magnetization plateau in azurite},
  author = {K. C. Rule and A. U. B. Wolter and S. Süllow and D. A. Tennant and A. Brühl and S. Köhler and B. Wolf and M. Lang and J. Schreuer},
  journal= {arXiv preprint arXiv:0709.2560},
  year   = {2009}
}

Comments

5 pages, 4 figures