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Silicon for use as a transmissive material in the far IR

机译:在远红外中用作透射材料的硅

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Abstract: 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.!8
机译:摘要:硅在光谱的中红外(IR)区域被广泛用作透射光学器件。由于远在约9微米的吸收带,它尚未用于远红外。这种吸收是固有晶格吸收和由于氧(O $ -2 $ /)引起的杂质带吸收的结果。通过减少或消除杂质带成分,可以使吸收最小化。在这项工作中,我们报告通过透射扫描获得的低氧“ O $ -2 $ /游离”硅的结果。我们将这些结果与典型Czochralski(CZ)硅获得的结果进行比较。吸收系数由透射数据计算得出。表格数据和数据图形表示在光谱的8至12微米区域中!8

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