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在9P/坦普尔1号彗星表面暴露的水冰沉积物。

Exposed water ice deposits on the surface of comet 9P/Tempel 1.

作者信息

Sunshine J M, A'Hearn M F, Groussin O, Li J-Y, Belton M J S, Delamere W A, Kissel J, Klaasen K P, McFadden L A, Meech K J, Melosh H J, Schultz P H, Thomas P C, Veverka J, Yeomans D K, Busko I C, Desnoyer M, Farnham T L, Feaga L M, Hampton D L, Lindler D J, Lisse C M, Wellnitz D D

机构信息

Science Applications International Corporation (SAIC), Chantilly, VA 20151, USA.

出版信息

Science. 2006 Mar 10;311(5766):1453-5. doi: 10.1126/science.1123632. Epub 2006 Feb 2.

Abstract

We report the direct detection of solid water ice deposits exposed on the surface of comet 9P/Tempel 1, as observed by the Deep Impact mission. Three anomalously colored areas are shown to include water ice on the basis of their near-infrared spectra, which include diagnostic water ice absorptions at wavelengths of 1.5 and 2.0 micrometers. These absorptions are well modeled as a mixture of nearby non-ice regions and 3 to 6% water ice particles 10 to 50 micrometers in diameter. These particle sizes are larger than those ejected during the impact experiment, which suggests that the surface deposits are loose aggregates. The total area of exposed water ice is substantially less than that required to support the observed ambient outgassing from the comet, which likely has additional source regions below the surface.

摘要

我们报告了对深度撞击任务观测到的彗星9P/坦普尔1号表面暴露的固态水冰沉积物的直接探测。根据其近红外光谱显示,三个颜色异常的区域含有水冰,这些光谱在波长1.5和2.0微米处有诊断性的水冰吸收峰。这些吸收峰可以很好地模拟为附近非冰区域与直径为10至50微米的3%至6%水冰颗粒的混合物。这些颗粒尺寸大于撞击实验中喷出的颗粒尺寸,这表明表面沉积物是松散的聚集体。暴露的水冰总面积远小于支持观测到的彗星周围气体逸出所需的面积,这表明表面之下可能还有其他气源区。

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