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首页> 外文期刊>Applied Surface Science >500 keV Ar2+ ion irradiation induced anatase to brookite phase transformation and ferromagnetism at room temperature in TiO2 thin films
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500 keV Ar2+ ion irradiation induced anatase to brookite phase transformation and ferromagnetism at room temperature in TiO2 thin films

机译:室温下500 keV Ar2 +离子辐照诱导TiO2薄膜中锐钛矿到板钛矿相变和铁磁性

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摘要

In our earlier report, where we have demonstrated ferromagnetic behavior at room temperature (RT) in TiO2 thin films deposited through electron beam evaporation technique followed by annealing either in Ar or O-2 atmosphere [Mohanty et al., Journal of Magnetism and Magnetic Materials 355 (2014) 240-245], here we have studied the evolution of structure and magnetic properties after irradiating the TiO2 thin films with 500 keV Ar2+ ions. The pristine film while exhibits anatase phase, the films become amorphous after irradiating at fluence in the range 1 x 10(14) to 1 x 10(16) ions/cm(2). Increasing the fluence up to 5 x 10(16) ions/cm(2), amorphous to crystalline phase transformation occurs and the structure becomes brookite. Although anatase to rutile phase transformation is usually reported in literatures, anatase to brookite phase transformation is an unusual feature which we have reported here for the first time. Such anatase to brookite phase transformation is accompanied with grain growth without showing any change in film thickness evidenced from Rutherford's Back Scattering (RBS) measurement. From scanning probe micrographs (SPM), roughness is found to be more in amorphous films than in the crystalline ones. Anatase to brookite phase transformation could be realized by considering the importance of intermediate amorphous phase. Because due to amorphous phase, heat deposited by energetic ions are localized as dissipation of heat is less and as a result, the localized region crystallizes in brookite phase followed by grain growth as observed in highest fluence. Further, we have demonstrated ferromagnetic behavior at RT in irradiated films similar to pristine one, irrespective of their phase and crystallinity. Origin for room temperature ferromagnetism (RTFM) is attributed to the presence of oxygen vacancies which is confirmed by carrying out XPS measurement. (C) 2017 Elsevier B.V. All rights reserved.
机译:在我们先前的报告中,我们已经证明了通过电子束蒸发技术沉积的TiO2薄膜在室温(RT)下的铁磁行为,然后在Ar或O-2气氛中进行了退火[Mohanty等,《磁性与磁性材料学报》 355(2014)240-245],这里我们研究了用500 keV Ar2 +离子辐照TiO2薄膜后结构和磁性能的演变。原始膜虽然表现出锐钛矿相,但以1 x 10(14)到1 x 10(16)离子/ cm(2)的通量辐照后,它们变成非晶态。将通量提高到5 x 10(16)离子/ cm(2),发生非晶态到结晶态的相变,结构变成板钛矿。尽管在文献中通常报道了锐钛矿相向金红石相的转变,但是锐钛矿相向板钛矿相的转变是一个不寻常的特征,这是我们首次在此报道。这种锐钛矿到板钛矿的相变伴随晶粒的生长,而没有显示出卢瑟福的反向散射(RBS)测量所证明的膜厚变化。根据扫描探针显微照片(SPM),发现非晶薄膜的粗糙度大于结晶薄膜的粗糙度。考虑到中间非晶相的重要性,可以实现锐钛矿到板钛矿的相变。由于归因于非晶相,高能离子所沉积的热量由于热量的散失而被局部化,结果,局部区域在板钛矿相中结晶,随后以最高的通量观察到晶粒长大。此外,我们已经证明了在与原始的原始膜相似的辐照膜中,在室温下的铁磁行为,无论其相和结晶度如何。室温铁磁(RTFM)的起源归因于氧空位的存在,通过执行XPS测量可以确认氧空位的存在。 (C)2017 Elsevier B.V.保留所有权利。

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