论文标题
蜂窝晶格磁铁cotio $ _3 $中的自旋轨道激子:揭示稀土与过渡金属磁性之间的联系
Spin-Orbit Exciton in a Honeycomb Lattice Magnet CoTiO$_3$: Revealing Link Between Rare Earth and Transition Metal Magnetism
论文作者
论文摘要
我们进行了非弹性中子散射,以研究cotio $ _3 $的单晶样品中的自旋(SO)激子作为温度的函数。 cotio $ _3 $是具有主导XY型磁相互作用的蜂窝磁铁,A-Type抗铁磁订单以下$ \ mathrm {t_n} \大约38 $ 〜k。我们发现,与磁性相比,SO激子变得更柔软,但是在顺磁相中获得了更大的带宽。此外,仅在中间温度范围内观察到一个额外的模式,因为样品在低于$ \ mathrm {t_n} $以下的最低温度高于最低的可访问温度以上。这种材料中观察到的这种异常的温度依赖性表明其基础状态($ s _ {\ mathrm {eff}} = \ frac {1} {1} {2} $ doublet)和激发态多重链的多重在强烈耦合,因此不能像在Pseudo-Spin模型中独立处理,因此无法独立处理。我们的观察结果可以通过随机相位近似中的多级理论来解释,该理论明确考虑了地面和激发的多重组。最初开发的理论的成功是为了解释稀土磁铁中磁激发的温度依赖性,突出了稀土系统中的磁激发与具有强旋转轨道耦合的过渡金属系统中的磁激发之间的相似性。
We carried out inelastic neutron scattering to study the spin-orbital (SO) exciton in a single crystal sample of CoTiO$_3$ as a function of temperature. CoTiO$_3$ is a honeycomb magnet with dominant XY-type magnetic interaction and an A-type antiferromagnetic order below $\mathrm{T_N} \approx 38$~K. We found that the SO exciton becomes softer, but acquires a larger bandwidth in the paramagnetic phase, compared to that in the magnetically ordered phase. Moreover, an additional mode is only observed in the intermediate temperature range, as the sample is warmed up above the lowest accessible temperature below $\mathrm{T_N}$. Such an unusual temperature dependence observed in this material suggests that its ground states (an $S_{\mathrm{eff}}=\frac{1}{2}$ doublet) and excited states multiplets are strongly coupled, and therefore cannot be treated independently, as often done in a pseudo-spin model. Our observations can be explained by a multi-level theory within random phase approximation that explicitly takes into account both the ground and excited multiplets. The success of our theory, which is originally developed to explain temperature dependence of magnetic excitations in the rare-earth magnets, highlight the similarity between the magnetic excitations in rare-earth systems and those in transition metal systems with strong spin orbit coupling.