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首页> 外文期刊>The Astrophysical journal >CASSINI VISUAL AND INFRARED MAPPING SPECTROMETER OBSERVATIONS OF IAPETUS: DETECTION OF CO_2
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CASSINI VISUAL AND INFRARED MAPPING SPECTROMETER OBSERVATIONS OF IAPETUS: DETECTION OF CO_2

机译:蛇麻草的卡西尼视觉和红外映射光谱仪观测:CO_2的检测

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摘要

The Visual and Infrared Mapping Spectrometer (VIMS) instrument aboard the Cassini spacecraft obtained its first spectral map of the satellite Iapetus in which new absorption bands are seen in the spectra of both the low-albedo hemisphere and the H_2O ice-rich hemisphere. Carbon dioxide is identified in the low-albedo material, probably as a photochemically produced molecule that is trapped in H_2O ice or in some mineral or complex organic solid. Other absorption bands are unidentified. The spectrum of the low-albedo hemisphere is satisfactorily modeled with a combination of organic tholin, poly-HCN, and small amounts of H_2O ice and Fe_2O_3. The high-albedo hemisphere is modeled with H_2O ice slightly darkened with tholin. The detection of CO_2 in the low-albedo material on the leading hemisphere supports the contention that it is carbon-bearing material from an external source that has been swept up by the satellite's orbital motion.
机译:卡西尼号航天器上的视觉和红外映射光谱仪(VIMS)仪器获得了其Iapetus卫星的第一张光谱图,其中在低反照率半球和H_2O富冰半球的光谱中都看到了新的吸收带。在低反照率物质中识别出二氧化碳,可能是由光化学产生的分子困在H_2O冰或某些矿物质或复杂的有机固体中。其他吸收带尚未确定。低反照率半球的光谱通过有机索林,聚HCN以及少量H_2O冰和Fe_2O_3的组合令人满意地建模。高反照率的半球以H_2O冰为模型,并用索林稍微变暗。在超前半球的低反照率物质中检测到CO_2支持这样一种论点,即它是来自外部来源的含碳物质,该来源已被卫星的轨道运动所扫除。

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