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Magnetic Transitions in Chemically Synthesized Nanoparticles of CoCr2O4

机译:化学合成CoCr 2 O 4 纳米粒子的磁跃迁

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Bulk CoCr2O4 undergoes a transition from paramagnetic to long-range ferrimagnetic phase at $T_{c}$ (94 K) to a long-range and/or short-range spiral order at $T_{s}$ ( $sim 24$ K), and finally shows a lock-in-transition below 15 K. The spiral component induces an electric polarization and also a spontaneous magnetization for which it is said to be multiferroic. Reducing the size of a CoCr2O4 multiferroic material to $sim 50$ nm by a coprecipitation method, we obtain a pure cubic phase with space group, Fd3m and lattice parameter (8.334 ± 0.003 °A). A rich sequence of magnetic transitions are examined by measuring temperature and field-dependent magnetization and diffused neutron scattering (DNS) using polarized neutron at different temperatures. While paramagnetic to ferrimagnetic transition is enhanced from 97 K in bulk to 99 K at 0.5 kOe field, followed by a decrease in lock-in-transition ( $T_{L}$ ) from 15 K in bulk to 8 K, spiral ordering temperature does not show a significant change. A strong disagreement between paramagnetic moment obtained from the fitting of $chi ^{-1}=({T}/{C})+({1}/{chi _{o}})-({b}/{T-theta })$ and ferrimagnetic moment obtained from the $M$ versus $H$ loop taken at 2 K, nonsaturated magnetization at 50–100 kOe field, two order of magnitude higher coercivity ( $H_{c}$ ), and splitting of ac susceptibly confirm the core–shell structure of the particles. Furthermore, a magnetic scattering analysis clearly shows that while the paramagnetic to ferrimagnetic transition is continuous, the spiral ordering is sharp, short range, and commensurate in contrast to incommensurate spiral order observed single crystal of CoCr2O4.
机译:块状CoCr2O4经历了从顺磁性到长距离铁磁相的转变,转变温度为$ T_ {c} $(94 K),转变为远距离和/或短程螺旋形转变,转变为$ T_ {s} $($ sim 24 $ K ),最后显示出低于15 K的过渡锁定。螺旋形成分会引起电极化,并引起自发磁化,据称该磁化作用是多铁性的。通过共沉淀法将CoCr2O4多铁性材料的尺寸减小至$ sim 50 $ nm,我们获得了具有空间群,Fd3m和晶格参数(8.334±0.003°A)的纯立方相。通过在不同温度下使用极化中子测量温度和与场有关的磁化强度和扩散中子散射(DNS),可以检查一系列丰富的磁跃迁。在0.5 kOe的磁场下,顺磁性到亚铁磁性的跃迁从97 K增大到了99 K,随后,转变锁定($ T_ {L} $)从15 K减小到8 K,螺旋有序温度没有明显的变化。通过拟合$ chi ^ {-1} =({T} / {C})+({1} / {chi _ {o}})-({b} / {T -theta})$和从$ M $与$ H $环路在2 K下获取的铁磁矩,在50–100 kOe磁场下的非饱和磁化强度,矫顽力高两个数量级($ H_ {c} $),以及分裂ac证实了粒子的核-壳结构。此外,磁散射分析清楚地表明,尽管顺磁至亚铁磁的过渡是连续的,但与观察到的CoCr2O4单晶的螺旋序不等时相比,螺旋序是尖锐的,短程的和相称的。

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