# The splitting of double-component active asteroid P/2016 J1 (PANSTARRS)

**Authors:** Fernando Moreno, Francisco Pozuelos, Bojan Novakovic, Javier Licandro,, Antonio Cabrera-Lavers, Bryce Bolin, Robert Jedicke, Brett Gladman, Michele, Bannister, Stephen Gwyn, Peter Veres, Kenneth Chambers, Serge Chastel, Larry, Denneau, Heather Flewelling, Mark Huber, Eva Schunova-Lilly, Eugene Magnier,, Richard Wainscoat, Christopher Waters, Robert Weryk, Davide Farnocchia, Marco, Micheli

arXiv: 1702.03665 · 2017-03-08

## TL;DR

This study investigates the origin and activity of the double-component asteroid P/2016 J1, revealing a likely fragmentation event and ice sublimation as the cause of its dust activity through observational and modeling analyses.

## Contribution

It provides the first detailed analysis linking the asteroid's fragmentation event to its dust activity, emphasizing ice sublimation as the driving mechanism.

## Key findings

- Closest approach of components occurred ~2300 days ago, likely due to fragmentation.
- Both components became active simultaneously about 250 days before perihelion.
- Dust activity lasted 6 to 9 months, consistent with ice sublimation processes.

## Abstract

We present deep imaging observations, orbital dynamics, and dust tail model analyses of the double-component asteroid P/2016 J1 (J1-A and J1-B). The observations were acquired at the Gran Telescopio Canarias (GTC) and the Canada-France-Hawaii Telescope (CFHT) from mid March to late July, 2016. A statistical analysis of backward-in-time integrations of the orbits of a large sample of clone objects of P/2016 J1-A and J1-B shows that the minimum separation between them occurred most likely $\sim$2300 days prior to the current perihelion passage, i.e., during the previous orbit near perihelion. This closest approach was probably linked to a fragmentation event of their parent body. Monte Carlo dust tail models show that those two components became active simultaneously $\sim$250 days before the current perihelion, with comparable maximum loss rates of $\sim$0.7 kg s$^{-1}$ and $\sim$0.5 kg s$^{-1}$, and total ejected masses of 8$\times$10$^{6}$ kg and 6$\times$10$^{6}$ kg for fragments J1-A and J1-B, respectively. In consequence, the fragmentation event and the present dust activity are unrelated. The simultaneous activation times of the two components and the fact that the activity lasted 6 to 9 months or longer, strongly indicate ice sublimation as the most likely mechanism involved in the dust emission process.

## Full text

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## Figures

7 figures with captions in the complete paper: https://tomesphere.com/paper/1702.03665/full.md

## References

34 references — full list in the complete paper: https://tomesphere.com/paper/1702.03665/full.md

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Source: https://tomesphere.com/paper/1702.03665