4.6 Article

Anisotropy: Spin order and magnetization of single-crystalline Cu4(OH)6FBr barlowite

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PHYSICAL REVIEW B
卷 93, 期 21, 页码 -

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AMER PHYSICAL SOC
DOI: 10.1103/PhysRevB.93.214416

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  1. Department of Physics, University of Chicago
  2. Department of Energy (DOE) [DE-FG02-99ER45789, DE-AC02-06CH11357]
  3. NSF Independent Research/Development program
  4. NSF [DMR-1157490]
  5. State of Florida
  6. DOE
  7. DOE Basic Energy Science Field Work Proposal Science in 100 T
  8. U.S. Department of Energy (DOE) [DE-FG02-99ER45789] Funding Source: U.S. Department of Energy (DOE)

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Despite decades-long fascination, the difficulty of maintaining high lattice symmetry in frustrated nonbipartite S = 1/2 materials that can also be made into high-quality single crystals has been a persistent challenge. Here we report magnetization studies of a single-crystal sample of barlowite, Cu-4(OH)(6)FBr, which has a geometrically perfect kagome motif. At T <= 4.2 K and 35 <= mu H-0 <= 65 T, the interlayer spins are fully polarized, and the kagome-intrinsic magnetization is consistent with a Heisenberg model having J/k(B) = -180 K. Several field-driven anomalies are observed, having varied scalings with temperature. At an applied field, kagome disorder caused by the interlayer spins is smaller than that in herbertsmithite. At T <= 15 K, the bulk magnetic moment comes from the interlayer spins. An almost coplanar spin order suggests that the magnitude of in-plane Dzyaloshinskii-Moriya interaction is smaller than 0.006(6) J. On the other hand, the possibility of a spin-liquid state in the kagome lattice coexisting with ordered interlayer spins is left open.

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