首页> 外文OA文献 >Dzyaloshinsky-Moriya interaction and the ground state in S=3/2 perfect kagome lattice antiferromagnet $\mathbf{KCr_3(OH)_6(SO_4)_2}$ (Cr-jarosite) studied by X-band and high-frequency ESR
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Dzyaloshinsky-Moriya interaction and the ground state in S=3/2 perfect kagome lattice antiferromagnet $\mathbf{KCr_3(OH)_6(SO_4)_2}$ (Cr-jarosite) studied by X-band and high-frequency ESR

机译:Dzyaloshinsky-moriya的相互作用和s = 3/2的基态完美无缺   kagome lattice antiferromagnet $ \ mathbf {KCr_3(OH)_6(sO_4)_2} $(Cr-jarosite)   通过X波段和高频EsR进行研究

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摘要

A single crystal S=3/2 perfect kagome lattice antiferromagnet$\mathrm{KCr_3(OH)_6(SO_4)_2}$ (Cr-jarosite) has been studied by X-band andhigh-frequency electron spin resonance (ESR). The g-values perpendicular to thekagome plane (c-axis) and in the plane are determined to be $g_c=1.9704 \pm0.0002$ and $g_\xi=1.9720 \pm 0.0003$, respectively, by high-frequency ESRobserved at 265 K. Antiferromagnetic resonances (AFMR) with theantiferromagnetic gap of 120 GHz are observed at 1.9 K, which is below$T_N$=4.5 K. The analysis of AFMR modes by the conventional molecular fieldtheory shows $d_p=0.27$ K and $d_z=0.07$ K, where $d_p$ and $d_z$ are in-planeand out-of-plane components of DM d vector, respectively. From these resultsand the estimated exchange interaction J=6.15 K by Okuta et al., the groundstate of Cr-jarosite is discussed in connection with the Monte Carlosimulations result with classical Heisenberg spins on the kagome lattice byElhajal et al. Finally, the angular dependence of linewidth and the lineshapeobserved at 296 K by X-band ESR show typical behavior of a two-dimensionalHeisenberg antiferromagnet, suggesting a good two-dimensionality ofCr-jarosite.
机译:通过X波段和高频电子自旋共振(ESR)研究了单晶S = 3/2完美的kagome晶格反铁磁体$ \ mathrm {KCr_3(OH)_6(SO_4)_2} $(铬铁铁矿)。垂直于thekagome平面(c轴)和该平面中的g值,通过高频ESRob分别确定为$ g_c = 1.9704 \ pm0.0002 $和$ g_ \ xi = 1.9720 \ pm 0.0003 $。 265K。在1.9 K处观察到反铁磁隙为120 GHz的反铁磁共振(AFMR),低于$ T_N $ = 4.5K。传统分子场论对AFMR模式的分析表明$ d_p = 0.27 $ K和$ d_z = 0.07 $ K,其中$ d_p $和$ d_z $分别是DM d向量的平面内和平面外分量。根据这些结果和Okuta等人估计的交换相互作用J = 6.15 K,结合Elhajal等人对经典的海森堡自旋在kagome晶格上进行的蒙特卡洛模拟结果,讨论了铬铁矿的基态。最后,线宽的角度依赖性和X波段ESR在296 K下观察到的线形显示出二维Heisenberg反铁磁体的典型行为,表明Cr黄铁矿具有良好的二维性。

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