Crovisier J, Leech K, Bockelée-Morvan D, Brooke T Y, Hanner M S, Altieri B, Keller H U, Lellouch E
Observatoire de Paris-Meudon, F-92195 Meudon, France.
Science. 1997 Mar 28;275(5308):1904-7. doi: 10.1126/science.275.5308.1904.
Comet Hale-Bopp (C/1995 O1) was observed at wavelengths from 2.4 to 195 micrometers with the Infrared Space Observatory when the comet was about 2.9 astronomical units (AU) from the sun. The main observed volatiles that sublimated from the nucleus ices were water, carbon monoxide, and carbon dioxide in a ratio (by number) of 10:6:2. These species are also the main observed constituents of ices in dense interstellar molecular clouds; this observation strengthens the links between cometary and interstellar material. Several broad emission features observed in the 7- to 45-micrometer region suggest the presence of silicates, particularly magnesium-rich crystalline olivine. These features are similar to those observed in the dust envelopes of Vega-type stars.
当海尔-波普彗星(C/1995 O1)距离太阳约2.9天文单位(AU)时,利用红外空间天文台在2.4至195微米的波长范围内对其进行了观测。从彗核冰中升华出来的主要挥发性物质是水、一氧化碳和二氧化碳,其数量比为10:6:2。这些物质也是在致密星际分子云中观测到的冰的主要成分;这一观测结果加强了彗星物质与星际物质之间的联系。在7至45微米区域观测到的几个宽发射特征表明存在硅酸盐,特别是富含镁的结晶橄榄石。这些特征与在织女星型恒星尘埃包层中观测到的特征相似。