The formation of Encke meteoroids and dust trail
William T. Reach, Mark V. Sykes, David Lien, John K. Davies

TL;DR
This study used infrared observations to analyze the dust environment of comet 2P/Encke, revealing large particles in the coma and trail, anisotropic emission patterns, and a high dust-to-gas ratio, with implications for spacecraft safety and comet longevity.
Contribution
First infrared imaging of Encke's dust trail and coma, revealing large particles, emission anisotropy, and high dust-to-gas ratio, advancing understanding of dust formation and evolution.
Findings
Large particles (>mm) dominate the coma.
Dust trail composed of ~5 cm particles from previous apparitions.
High dust-to-gas mass ratio of 10-30.
Abstract
We observed comet 2P/Encke with the Infrared Space Observatory ISOCAM on July 14, 1997 from a particularly favorable viewing geometry above the comet's orbital plane and at a distance of 0.25 AU. A structured coma was observed, along with a long, straight dust trail. For the first time, we are able to observe the path of particles as they evolve from the nucleus to the trail. The particles that produce the infrared coma are large, with a radiation to gravitational force ratio beta<0.001 (corresponding to >mm-sized particles). The dust trail follows the orbit of the comet across our image, with a central core that is 20,000 km wide, composed of particles with beta<1e-5 (size cm) from previous apparitions. The abundant large particles near the comet pose a significant hazard to spacecraft. There is no evidence of a classical cometary dust tail due to small particles with…
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Taxonomy
TopicsAstro and Planetary Science · Planetary Science and Exploration · Stellar, planetary, and galactic studies
