# The footprint of cometary dust analogs: I. Laboratory experiments of low-velocity impacts and comparison with Rosetta data

## TL;DR

This study conducts laboratory impact experiments with cometary dust analogs to understand the collision outcomes and compares the results with data from the Rosetta spacecraft, revealing how impact velocity influences dust particle fragmentation and deposition.

## Contribution

It provides new experimental insights into dust impact processes and links laboratory results with spacecraft observations, enhancing understanding of cometary dust evolution.

## Key findings

- Impact velocity determines whether dust sticks, bounces, or fragments.
- Particles larger than 80 μm tend to fragment at impact velocities above 2 m/s.
- Deposits from experiments resemble those observed by the Rosetta spacecraft.

## Abstract

Cometary dust provides a unique window on dust growth mechanisms during the onset of planet formation. Measurements by the Rosetta spacecraft show that the dust in the coma of comet 67P/Churyumov-Gerasimenko has a granular structure at size scales from sub-um up to several hundreds of um, indicating hierarchical growth took place across these size scales. However, these dust particles may have been modified during their collection by the spacecraft instruments. Here we present the results of laboratory experiments that simulate the impact of dust on the collection surfaces of COSIMA and MIDAS, instruments onboard the Rosetta spacecraft. We map the size and structure of the footprints left by the dust particles as a function of their initial size (up to several hundred um) and velocity (up to 6 m/s). We find that in most collisions, only part of the dust particle is left on the target; velocity is the main driver of the appearance of these deposits. A boundary between sticking/bouncing and fragmentation as an outcome of the particle-target collision is found at v ~ 2 m/s. For velocities below this value, particles either stick and leave a single deposit on the target plate, or bounce, leaving a shallow footprint of monomers. At velocities > 2 m/s and sizes > 80 um, particles fragment upon collision, transferring up to 50 per cent of their mass in a rubble-pile-like deposit on the target plate. The amount of mass transferred increases with the impact velocity. The morphologies of the deposits are qualitatively similar to those found by the COSIMA instrument.