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Magnetic properties of the spin-1/2 deformed kagome antiferromagnet edwardsite

机译:自旋1/2变形的Kagome反铁磁铁变质铁矿的磁性

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We prepared a powder sample of edwardsite Cd_2Cu_3(SO_4)_2(OH)_6·4H_2O, which is a new candidate compound for the spin-1/2 kagome antiferromagnet, and studied its magnetic properties by magnetic susceptibility and heat capacity measurements. Edwardsite has a deformed kagome lattice with an average antiferromagnetic interaction of 51K between nearby spins and shows an antiferromagnetic order accompanied by a small ferromagnetic moment below 4.3 K. The weak ferromagnetism is likely due to spin canting caused by sizable Dzyaloshinsky-Moriya interactions, which may stabilize the long-range magnetic order instead of a spin-liquid state expected for the kagome antiferromagnet.
机译:我们制备了作为自旋1 / 2kagome反铁磁体的新候选化合物的磷铝石Cd_2Cu_3(SO_4)_2(OH)_6·4H_2O的粉末样品,并通过磁化率和热容测量研究了其磁性能。 Edwardsite的变形的kagome晶格在附近的自旋之间平均具有51K的反铁磁相互作用,并且显示出反铁磁有序并伴随着一个低于4.3 K的小铁磁矩。弱的铁磁可能是由于Dzyaloshinsky-Moriya相互作用较大而引起的自旋倾斜。稳定远距离的磁序,而不是针对Kagome反铁磁体所期望的自旋液态。

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