Cometary masses derived from non-gravitational forces
Andrea Sosa, Julio A. Fernandez

TL;DR
This study estimates the masses and densities of ten periodic comets using non-gravitational forces and gas production data, revealing very low densities consistent with porous structures and highlighting the method's utility for statistical analysis.
Contribution
It applies a simplified non-gravitational force model to derive cometary masses and densities, providing a statistical perspective on their physical properties.
Findings
Densities range from 0.3 to 400 x 10^12 kg in mass.
Average density is approximately 0.4 g/cm^3.
Comet densities are lower than those of near-Earth asteroids.
Abstract
We compute masses and densities for ten periodic comets with known sizes: 1P/Halley, 2P/Encke, 6P/d'Arrest, 9P/Tempel 1, 10P/Tempel 2, 19P/Borrelly, 22P/Kopff, 46P/Wirtanen, 67P/Churyumov-Gerasimenko and 81P/Wild 2. The method follows the one developed by Rickman and colleagues (Rickman 1986, 1989; Rickman et al. 1987), which is based on the gas production curve and on the change in the orbital period due to the non-gravitational force. The gas production curve is inferred from the visual lightcurve. We found that the computed masses cover more than three orders of magnitude: ~(0.3 - 400)*10^12 kg. The computed densities are in all cases very low (<= 0.8 g cm^-3), with an average value of 0.4 g cm^-3, in agreement with previous results and models of the cometary nucleus depicting it as a very porous object. The computed comet densities turn out to be the lowest among the different…
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Taxonomy
TopicsAstro and Planetary Science · Astronomical Observations and Instrumentation · Stellar, planetary, and galactic studies
