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PLD of Fe3O4 thin films: Influence of background gas on surface morphology and magnetic properties

机译:Fe3O4薄膜的PLD:背景气体对表面形态和磁性的影响

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Ablation of Fe3O4 targets has been performed using a pulsed UV laser (KrF, gimel = 248 nm, 30 ns pulse duration) onto Si(100) substrates, in reactive atmospheres of O-2 and/or Ar, with different oxygen partial pressures. The as-deposited films were characterised by atomic force microscopy (AFM), X-ray diffraction (XRD), conversion electron Mossbauer spectroscopy (CEMS) and extraction magnetometry, in order to optimise the deposition conditions in the low temperature range. The results show that a background mixture of oxygen and argon improves the Fe:O ratio in the films as long as the oxygen partial pressure is maintained in the 10(-2) Pa range. Thin films of almost stoichiometric single phase polycrystalline magnetite, Fe2.99O4, have been obtained at 483 K and working pressure of 7.8 x 10-2 Pa, with a high-field magnetization of similar to 490 emu/cm(3) and Verwey transition temperature of 112 K, close to the values reported in the literature for bulk magnetite. (c) 2005 Elsevier B.V. All rights reserved.
机译:在O-2和/或Ar的反应性气氛中,使用不同的氧气分压,已使用脉冲UV激光(KrF,gimel = 248 nm,脉冲持续时间30 ns)对Fe3O4靶进行了烧蚀。通过原子力显微镜(AFM),X射线衍射(XRD),转换电子Mossbauer光谱(CEMS)和萃取磁法对沉积后的薄膜进行表征,以优化低温范围内的沉积条件。结果表明,只要氧气分压保持在10(-2)Pa范围内,氧气和氩气的本底混合物就能改善薄膜中的Fe:O比。在483 K和7.8 x 10-2 Pa的工作压力下获得了几乎化学计量的单相多晶磁铁矿Fe2.99O4薄膜,其高磁场磁化强度接近490 emu / cm(3),并发生了Verwey转变温度为112 K,接近文献中报道的块状磁铁矿的值。 (c)2005 Elsevier B.V.保留所有权利。

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