Constraints on the nucleus and dust properties from mid-infrared imaging of comet Hyakutake.
We use Mie scattering theory to determine the expected thermal emission from dust grains in cometary comae and apply these results to mid-infrared images of comet Hyakutake (C/1996 B2) obtained preperihelion in 1996 March. Calculations were performed for dust grains in the size range from 0.1 to 10 micrometers for two different compositions: amorphous olivine (a silicate glass) and an organic residue mixture. The resulting emission efficiencies are complicated functions of wavelength and particle size and are significantly different for the two materials in question. The Hyakutake data set consists of three nights of high-resolution imaging (100-150 km pixel-1 at the comet) of the inner coma at 8.7, 11.7, 12.5, and 19.7 micrometers. Attempts to fit the observed colors (ratios of fluxes at different wavelengths) using a single grain composition failed. However, fits to the data were achieved for all three nights using a mixture of approximately 1 micrometer olivine grains and approximately 7 micrometers organic grains. The resulting olivine mass fraction was between 8% and 16% of the total dust mass-loss rate. We also estimate the radius of the nucleus to be r = 2.1 +/- 0.4 km.
Sarmecanic
J
J
Center for Astrophysics and Space Sciences, University of California, San Diego, La Jolla 92093-0424, USA.
Fomenkova
M
M
Jones
B
B
Lavezzi
T
T
D001256:Astronomy / Q000379:methods; D019443:Cosmic Dust / Q000032:analysis*; D005118:Extraterrestrial Environment; D058085:Iron Compounds; D017616:Magnesium Compounds; D019110:Meteoroids; D012542:Scattering, Radiation; D017640:Silicates; D013055:Spectrophotometry, Infrared
D019443:Cosmic Dust; D058085:Iron Compounds; D017616:Magnesium Compounds; D017640:Silicates; C034475:olivine