Collisions of small ice particles under microgravity conditions
C. R. Hill, D. Hei{\ss}elmann, J. Blum, H. J. Fraser

TL;DR
This study investigates low-velocity collisions of small ice particles under microgravity to understand their behavior in protoplanetary disks, revealing bouncing, fragmentation, and energy transfer characteristics relevant to planet formation.
Contribution
It provides experimental data on ice particle collisions at low velocities and temperatures, highlighting the effects of surface roughness and energy dissipation mechanisms.
Findings
Majority of collisions resulted in bouncing
Coefficients of restitution ranged from 0.08 to 0.65
Up to 17% of energy converted to rotation
Abstract
Planetisimals are thought to be formed from the solid material of a protoplanetary disk by a process of dust aggregation. It is not known how growth proceeds to kilometre sizes, but it has been proposed that water ice beyond the snowline might affect this process. To better understand collisional processes in protoplanetary disks leading to planet formation, the individual low velocity collisions of small ice particles were investigated. The particles were collided under microgravity conditions on a parabolic flight campaign using a purpose-built, cryogenically cooled experimental setup. The setup was capable of colliding pairs of small ice particles (between 4.7 and 10.8 mm in diameter) together at relative collision velocities of between 0.27 and 0.51 m s ^-1 at temperatures between 131 and 160 K. Two types of ice particle were used: ice spheres and irregularly shaped ice fragments.…
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