arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1306.4269cond-mat.str-el
收藏

S=1/2氟氧化钒可果美反铁磁体[ NH4 ]2[ C7H14N ][ V7O6F18 ]的无隙自旋液体基态

Gapless spin liquid ground state in the S=1/2 vanadium oxyfluoride kagome antiferromagnet [NH4]2[C7H14N][V7O6F18]

L. Clark, J. C. Orain, F. Bert, M. A. de Vries, F. H. Aidoudi, R. E. Morris, P. Lightfoot, J. S. Lord, M. T. F. Telling, P. Bonville, J. P. Attfield, 1 P. Mendels, A. Harrison

摘要:

氟氧化钒[NH 4]2[C7 H14 N][V7 O 6 F18](DQVOF)是一种几何阻挫磁性双层材料。该结构由V4+ d1离子的S=1/2 kagome平面和位于kagome层之间的S=1 V3+ d2离子组成。μ子自旋弛豫测量表明,尽管反铁磁交换相互作用的能量标度为60 K,但在40 mK以下没有自旋冻结。从磁化强度和热容量的测量,我们得出结论,S=1自旋的面间V 3+离子是弱耦合到kagome层,DQVOF可以被看作是一个实验模型S=1/2 kagome物理,它显示了一个无隙自旋液体基态。

英文摘要:

The vanadium oxyfluoride [NH4]2[C7H14N][V7O6F18] (DQVOF) is a geometrically frustrated magnetic bilayer material. The structure consists of S=1/2 kagome planes of V4+ d1 ions with S=1 V3+ d2 ions located between the kagome layers. Muon spin relaxation measurements demonstrate the absence of spin freezing down to 40 mK despite an energy scale of 60 K for antiferromagnetic exchange interactions. From magnetization and heat capacity measurements we conclude that the S=1 spins of the interplane V3+ ions are weakly coupled to the kagome layers, such that DQVOF can be viewed as an experimental model for S=1/2 kagome physics, and that it displays a gapless spin liquid ground state.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑