Collisions between equal sized ice grain agglomerates
C. Sch\"afer, R. Speith, W. Kley (University of T\"ubingen)

TL;DR
This study uses numerical simulations to explore how equal-sized porous ice agglomerates collide at low velocities, shedding light on conditions that could lead to planetesimal formation in protoplanetary disks.
Contribution
It introduces a detailed numerical approach to analyze collisional outcomes of porous ice agglomerates, considering material strength and porosity effects, which was previously unexplored.
Findings
Low velocity impacts may allow growth of protoplanetesimals.
Collisions with larger impact parameters tend to induce rotation.
Most collisions do not result in sticking for typical material strengths.
Abstract
Following the recent insight in the material structure of comets, protoplanetesimals are assumed to have low densities and to be highly porous agglomerates. It is still unclear if planetesimals can be formed from these objects by collisional growth. Therefore, it is important to study numerically the collisional outcome from low velocity impacts of equal sized porous agglomerates which are too large to be examined in a laboratory experiment. We use the Lagrangian particle method Smooth Particle Hydrodynamics to solve the equations that describe the dynamics of elastic and plastic bodies. Additionally, to account for the influence of porosity, we follow a previous developed equation of state and certain relations between the material strength and the relative density. Collisional growth seems possible for rather low collision velocities and particular material strengths. The remnants of…
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