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arXiv 0804.2966cond-mat.str-el
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自旋链化合物CoV2O6的变磁性和1/3平台

Metamagnetism and 1/3 Plateau in the Spin Chain Compound CoV2O6

Simon A. J. Kimber, Dimitri N. Argyriou, J. Paul Attfield

摘要:

在1.8 < T < 300 K温度范围和高达9 T的外加磁场下,通过磁化强度和热容测量研究了准一维铁钒石型化合物CoV_2O_6。我们的测量结果表明,交换相互作用的不寻常的平衡(CW= 2.8(2)K)和一个单一的反铁磁转变在TN = 7 K。M(H)等温线记录低于5 K显示变磁性转变和1/3磁化平台。在5-7 K温度范围内,只观察到变磁转变。对于T < TN < ~ 25 K,我们的热容和磁化强度测量显示出强低维铁磁涨落的证据。我们提出了一个简单的相图,讨论的原则特点,并强调伊辛各向异性的重要性。

英文摘要:

The pseudo-one dimensional brannerite type compound CoV2O6 has been studied by magnetisation and heat capacity measurements in the temperature range 1.8 < T < 300 K and in applied fields of up to 9 T. Our measurements show an unusual balance of exchange interactions (CW= 2.8(2) K) and a single antiferromagnetic transition at TN = 7 K. M(H) isotherms recorded below 5 K show a metamagnetic transition and a 1/3 magnetisation plateau. From 5-7 K, only the metamagnetic transition is observed. For T < TN < ~ 25 K, our heat capacity and magnetisation measurements show evidence for strong low dimensional ferromagnetic fluctuations. We propose a simple phase diagram, discuss the principle features and emphasise the importance of Ising anisotropy.

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。

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