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Silicon for use as a transmissive material in the far IR

机译:硅作为远程IR中的透射材料

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Silicon is used extensively as a transmissive optic in the mid infrared (IR) region of the spectrum. It has not been used in the far IR primarily due to an absorption band at about nine microns. This absorption is the result of both intrinsic lattice absorption and an impurity band absorption due to oxygen (O$-2$/). The absorption can be minimized by reducing or eliminating the impurity band component. In this work we report results obtained from transmission scans for low oxygen 'O$-2$/ Free' silicon. We compare these results with those obtained for typical Czochralski (CZ) silicon. Absorption coefficients are calculated from the transmission data. Tabular data and graphical representations of the data are shown in the eight to twelve micron region of the spectrum.
机译:硅被广泛用于光谱中红外(IR)区域中的透射光学器件。它尚未在远程中使用,主要是由于约9微米的吸收带。这种吸收是由于氧气引起的固有晶格吸收和杂质带吸收的结果(O $ -2 $ /)。通过减少或消除杂质带组分可以最小化吸收。在这项工作中,我们向低氧气-2美元/免费'硅的传输扫描提供的结果报告结果。我们将这些结果与典型的Czochralski(CZ)硅的硅进行比较。从传输数据计算吸收系数。数据的表格数据和图形表示在频谱的八到十二微米区域中示出。

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