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Parent Volatiles in Comet 9P/Tempel 1: Before and After Impact
Michael J. Mumma,1*Michael A. DiSanti,1Karen Magee-Sauer,2Boncho P. Bonev,1,3Geronimo L. Villanueva,1Hideyo Kawakita,4Neil Dello Russo,5Erika L. Gibb,6Geoffrey A. Blake,7James E. Lyke,8Randall D. Campbell,8Joel Aycock,8Al Conrad,8Grant M. Hill8
We quantified eight parent volatiles (H2O, C2H6, HCN, CO, CH3OH,H2CO, C2H2, and CH4) in the Jupiter-family comet Tempel 1 usinghigh-dispersion infrared spectroscopy in the wavelength range2.8 to 5.0 micrometers. The abundance ratio for ethane was significantlyhigher after impact, whereas those for methanol and hydrogencyanide were unchanged. The abundance ratios in the ejecta aresimilar to those for most Oort cloud comets, but methanol andacetylene are lower in Tempel 1 by a factor of about 2. Theseresults suggest that the volatile ices in Tempel 1 and in mostOort cloud comets originated in a common region of the protoplanetarydisk.
1 Solar System Exploration Division, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA. 2 Department of Physics and Astronomy, Rowan University, Glassboro, NJ 080281701, USA. 3 Ritter Astrophysical Research Center, Department of Physics and Astronomy, University of Toledo, Toledo, OH 43606, USA. 4 Department of Physics, Kyoto Sangyo University, Motoyama, Kamigamo, Kita-ku, Kyoto 603-8555, Japan. 5 Space Department, Planetary Exploration Group, Applied Physics Laboratory/Johns Hopkins University, 11100 Johns Hopkins Road, Laurel, MD 207236099, USA. 6 Department of Physics and Astronomy, University of Missouri, St. Louis, MO 631214499, USA. 7 Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA. 8 W. M. Keck Observatory, 65-1120 Mamalahoa Highway, Kameula, HI 96743, USA.
* To whom correspondence should be addressed. E-mail: michael.j.mumma{at}nasa.gov
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