Meier R, Owen T C, Jewitt D C, Matthews H E, Senay M, Biver N, Bockel e-Morvan D, Crovisier J, Gautier D
University of Hawaii, Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA.
Science. 1998 Mar 13;279(5357):1707-10. doi: 10.1126/science.279.5357.1707.
Deuterated hydrogen cyanide (DCN) was detected in a comet, C/1995 O1 (Hale-Bopp), with the use of the James Clerk Maxwell Telescope on Mauna Kea, Hawaii. The inferred deuterium/hydrogen (D/H) ratio in hydrogen cyanide (HCN) is (D/H)HCN = (2.3 +/- 0.4) x 10(-3). This ratio is higher than the D/H ratio found in cometary water and supports the interstellar origin of cometary ices. The observed values of D/H in water and HCN imply a kinetic temperature >/=30 +/- 10 K in the fragment of interstellar cloud that formed the solar system.
利用位于夏威夷莫纳克亚山的詹姆斯·克拉克·麦克斯韦望远镜,在彗星C/1995 O1(海尔-波普彗星)中检测到了氘代氰化氢(DCN)。推断出氰化氢(HCN)中的氘/氢(D/H)比为(D/H)HCN =(2.3±0.4)×10⁻³。该比值高于在彗星水冰中发现的D/H比,这支持了彗星冰的星际起源。在水冰和HCN中观测到的D/H值意味着形成太阳系的星际云碎片中的动力学温度≥30±10 K。