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IN-SITU OBSERVATION OF DIFFUSION AND SEGREGATION OF Fe ATOMS IN Si CRYSTALS AT HIGH TEMPERATURE BY MOESSBAUER SPECTROSCOPY

机译:晶体中Fe原子在高温下的扩散和偏析的穆斯堡尔光谱原位观察

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We perform "high-temperature" Moessbauer experiments on silicon wafers with 30 at. ppm ~(57)Fe in the temperature range from 20°Cto 1100°C using an UHV-furnace. Different phases of Fe-silicides such as ξ_β and ξ_α-FeSi_2 are identified in the spectra at elevating experimental temperatures. At 1100°C, the precipitates of ξ_α-FeSi_2 dissolve completely, leading to an "Fe solid solution" in Si matrix. This component is tentatively assigned to "substitutional Fe", which performs atomic jumps with the jump frequency of 10~7 s~(-1) at 1000°C, although the concentration of 30 at.ppm Fe is far above the reported solubility.
机译:我们在30 at。的硅晶圆上执行“高温” Moessbauer实验。使用UHV炉在20°C至1100°C的温度范围内达到ppm〜(57)Fe。在升高的实验温度下,在光谱中鉴定出诸如ξ_β和ξ_α-FeSi_2之类的硅化铁的不同相。在1100°C,ξ_α-FeSi_2的沉淀完全溶解,从而在Si基体中形成“铁固溶体”。该成分暂定为“取代的铁”,它在1000°C时以10〜7 s〜(-1)的跳变频率发生原子跳变,尽管30 at.ppm Fe的浓度远高于所报道的溶解度。

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