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  4. High-field magnetic ground state in S = 1/2 kagome lattice antiferromagnet ZnCu[subscript 3](OH)[subscript 6]Cl[subscript 2<]

High-field magnetic ground state in S = 1/2 kagome lattice antiferromagnet ZnCu[subscript 3](OH)[subscript 6]Cl[subscript 2<]

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Author(s)
Asaba, Tomoya
•
Han, Tianheng
•
Lawson, B. J.
•
Yu, F.
•
Tinsman, C.
•
Xiang, Z.
•
Li, G.
•
Lee, Young S.
•
Li, Lu
Date Issued
August 2014
Journal
Physical Review B
Publisher
American Physical Society
Citation
Asaba, Tomoya, et al. "High-field magnetic ground state in S = 1/2 kagome lattice antiferromagnet ZnCu[subscript 3](OH)[subscript 6]Cl[subscript 2<]." Phys. Rev. B 90, 064417 (August 2014). © 2014 American Physical Society
Version
Final published version
Abstract
Herbertsmithite ZnCu[subscript 3](OH)[subscript 6]Cl[subscript 2] is a kagome lattice antiferromagnet with spin-1/2 and has been demonstrated to be a likely candidate of spin liquid by a number of recent experiments. The high-field magnetization of the kagome lattice is complicated due to the presence of a few percent of extra Cu impurities sitting on the interlayer metallic sites. To determine the magnetic ground state of the kagome lattice, we measured the magnetization of a single crystalline ZnCu[subscript 3](OH)[subscript 6]Cl[subscript 2] using torque magnetometry down to the base temperatures 20 mK in intense magnetic field as high as 31 T. The high-field intrinsic magnetization from the kagome lattice turns out to be linear with magnetic field, and the magnetic susceptibility is independent of temperature at 20 mK ≤ T ≤ 5 K. Moreover, below 2 K, several field-induced anomalies are observed in between 7 T and 15 T.
MIT Department
Massachusetts Institute of Technology. Department of Physics
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
http://hdl.handle.net/1721.1/88970
DOI of Published Version
https://doi.org/10.1103/PhysRevB.90.064417
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