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首页> 外文期刊>The Astrophysical journal >The SPECTRAL Ice Chamber: Application to Titan’s Stratospheric Ice Clouds
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The SPECTRAL Ice Chamber: Application to Titan’s Stratospheric Ice Clouds

机译:SPECTRAL冰室:在土卫六平流层冰云中的应用

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An ice chamber for obtaining thin-film transmission spectra of Titan-relevant organic ices between 50 and 11,700 cm?1 (200–0.85 μm) is described in detail in this work. The ice chamber, called the SPECtroscopy of Titan-Related ice AnaLogs chamber, is located in the Spectroscopy for Planetary ICes Environments laboratory at NASA Goddard Space Flight Center. Organic vapors are typically deposited between 30 and 150 K via a variable leak valve onto a chemical vapor deposition diamond substrate, where condensation directly into the solid state occurs. Quantitative thin-film infrared transmission spectra of the given ice or ice mixture are then measured, from which optical constants (complex indices of refraction) are computed. These optical constants in turn provide the necessary input for interpreting radiative transfer analyses of Cassini's Composite InfraRed Spectrometer observations of Titan's organic stratospheric ice clouds to determine their chemical compositions, abundances, and vertical distributions as functions of Titan latitude and season.
机译:在这项工作中详细描述了一个冰室,该冰室用于获得与泰坦有关的有机冰的薄膜透射光谱,介于50至11700 cm?1(200-0.85μm)之间。该冰室称为“与泰坦有关的冰AnaLogs的SPECtroscopy”,位于NASA戈达德太空飞行中心行星IC环境光谱实验室中。有机蒸气通常通过可变泄漏阀在30 K和150 K之间沉积到化学气相沉积金刚石基材上,在其中直接凝结成固态。然后测量给定冰或冰混合物的定量薄膜红外透射光谱,从中计算光学常数(复折射率)。这些光学常数反过来为解释卡西尼号的复合红外光谱仪对泰坦的有机平流层冰云的辐射传递分析提供了必要的输入,以确定其化学成分,丰度和垂直分布是泰坦纬度和季节的函数。

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