La0.8Sr0.2MnO3纳米锰矿铁磁性向超顺磁性转变的合成及ESR研究

Mondher Yahya, F. Hosni, A. Hamzaoui
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引用次数: 2

摘要

采用电子自旋共振(ESR)光谱法测定了La0.8Sr0.2MnO3纳米晶在室温下的磁态跃迁随晶粒尺寸的变化规律。采用两步法自燃烧法制备了平均晶粒尺寸为9 ~ 57 nm的铁磁性纳米颗粒。ESR谱线形状、共振场(Hr)、g因子、线宽(∆Hpp)和低场微波吸收(LFMA)信号的显著变化表明,随着晶粒尺寸的增大,磁畴结构从超顺磁性转变为单畴和多畴铁磁性。晶粒尺寸小于24.5 nm的样品处于超顺磁状态。在24.5到32nm之间,它们是由单畴铁磁形成的。对于较大的尺寸,会出现多域状态。在超顺磁区,g因子的值基本不变,表明磁芯尺寸随晶粒尺寸的减小而不变。这种与核壳模型相矛盾的观察结果可以用相分离现象来解释,这种现象导致了一种新的磁态的形成,我们称之为多核超顺磁态。
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Synthesis and ESR Study of Transition from Ferromagnetism to Superparamagnetism in La0.8Sr0.2MnO3 Nanomanganite
Electron spin resonance (ESR) spectroscopy was used to determine the magnetic state transitions of nanocrystalline La0.8Sr0.2MnO3 at room temperature, as a function of crystallite size. Ferromagnetic nanoparticles having an average crystallite size ranging from 9 to 57 nm are prepared by adopting the autocombustion method with two-step synthesis process. Significant changes of the ESR spectra parameters, such as the line shape, resonance field (Hr), g-factor, linewidth (∆Hpp), and the low-field microwave absorption (LFMA) signal, are indicative of the change in magnetic domain structures from superparamagnetism to single-domain and multi-domain ferromagnetism by increase in the crystallite size. Samples with crystallite sizes less than 24.5 nm are in a superparamagnetic state. Between 24.5 and 32 nm, they are formed by a single-domain ferromagnetic. The multi-domain state arises for higher sizes. In superparamagnetic region, the value of g-factor is practically constant suggesting that the magnetic core size is invariant with decreasing crystallite size. This contradictory observation with the core-shell model was explained by the phenomenon of phase separation that leads to the formation of a new magnetic state that we called multicore superparamagnetic state.
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