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Measurement of residual stresses by X-ray diffraction techniques in pyrite films prepared by magnetron sputtering

机译:通过X射线衍射技术测量磁控溅射制备的黄铁矿薄膜中的残余应力

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摘要

Pyrite films were prepared by magnetron sputtering and sulphuration treatment. The residualnstresses in the pyrite films were studied as a function of sulphuration temperature. Thenmicrostructure was investigated by atomic force microscopy (AFM). The measurement wasnperformed with a h–2h mode glancing incidence X-ray diffraction (XRD) instrument. The residualnstresses were calculated by using sin2 y method. The intrinsic stresses were estimated from thendifference of the sulphurised pyrite films lattice constant and stress free pyrite films latticenconstant. The thermal stresses were obtained from the empirical formula. The experimental resultsnindicate that residual stresses stored in the pyrite films are compressive and the value of residualnstresses decreases from 100 to 79 MPa with increasing sulphuration temperature from 623 ton873 K. The intrinsic stresses in the pyrite films are comprehensive and decrease with increasingnsulphuration temperature. In contrast, the thermal stresses in pyrite films are tensile and tend tonincrease with sulphuration temperature.
机译:通过磁控溅射和硫化处理制备黄铁矿薄膜。研究了黄铁矿薄膜中的残余应力与硫化温度的关系。然后通过原子力显微镜(AFM)研究了微观结构。使用h–2h模式扫掠入射X射线衍射(XRD)仪器进行测量。残余应力通过sin2y法计算。根据硫化黄铁矿薄膜晶格常数和无应力黄铁矿薄膜晶格常数的差异估算了本征应力。从经验公式获得热应力。实验结果表明,随着硫化温度从623 ton873 K升高,黄铁矿薄膜中存储的残余应力为压缩应力,残余应力值从100 MPa降低至79 MPa。黄铁矿薄膜中的固有应力是全面的,随着硫化温度的升高而降低。相反,黄铁矿膜中的热应力是拉伸的,并且随着硫化温度的升高趋于单调增加。

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