Investigating the Bouncing Barrier with Collision Simulations of Compressed Dust Aggregates
arXiv:2502.03107 · doi:10.3847/1538-4357/adbf04
Abstract
The collision outcomes of dust aggregates in protoplanetary disks dictate how planetesimals form. Experimental and numerical studies have suggested that bouncing collisions occurring at low impact velocities may limit aggregate growth in the disks, but the conditions under which bouncing occurs have yet to be fully understood. In this study, we perform a suite of collision simulations of moderately compact dust aggregates with various impact velocities, aggregate radii, and filling factors ranging between 0.4 and 0.5. Unlike previous simulations, we generate compact aggregates by compressing more porous ones, mimicking the natural processes through which compact aggregates form. We find that the compressed aggregates bounce above a threshold mass, which decreases with impact velocity. The threshold mass scales with impact velocity as the power, consistent with the findings of previous experiments. We also find that the threshold aggregate mass for bouncing depends strongly on filling factor, likely reflecting the strong filling-factor dependence of the compressive strength of compressed aggregates. Our energy analysis reveals that nearly 90\% of the initial impact energy is dissipated during the initial compression phase, and over 70\% of the remaining energy is dissipated during the subsequent stretching phase, regardless of whether the collision results in sticking or bouncing. Our results indicate that dust aggregates with a filling factor of 0.4 cease to grow beyond 100 as a result of the bouncing barrier.
16 pages, 15 figures; accepted for publication in ApJ
References in corpus (19)
- Closed-form expressions for particle relative velocities induced by turbulence
- Dust coagulation in protoplanetary disks: porosity matters
- Contacts of Water Ice in Protoplanetary Disks - Laboratory Experiments
- ALMA Reveals Transition of Polarization Pattern with Wavelength in HL Tau's Disk
- The Physics of Protoplanetesimal Dust Agglomerates. IV. Towards a Dynamical Collision Model
- The Physics of Protoplanetesimal Dust Agglomerates II. Low Velocity Collision Properties
- Leaky dust traps: How fragmentation impacts dust filtering by planets
- Effect of dust size and structure on scattered light images of protoplanetary discs
- Tensile Strength of Porous Dust Aggregates
- Porous Dust Particles in Protoplanetary Disks: Application to the HL Tau Disk
- Rapid formation of Gas Giant Planets via Collisional Coagulation from Dust Grains to Planetary Cores
- Support for fragile porous dust in a gravitationally self-regulated disk around IM Lup
- Collisional properties of cm-sized high-porosity ice and dust aggregates and their applications to early planet formation
- Impact of Differential Dust Settling on the SED and Polarization: Application to the Inner Region of the HL Tau Disk
- Size Dependence of the Bouncing Barrier in Protoplanetary Dust Growth
- Collisions between sintered icy aggregates
- Coagulation Instability in Protoplanetary Disks: A Novel Mechanism Connecting Collisional Growth and Hydrodynamical Clumping of Dust Particles
- Collisional Growth and Fragmentation of Dust Aggregates. II. Mass Distribution of Icy Fragments
- Formulating Compressive Strength of Dust Aggregates from Low to High Volume Filling Factors with Numerical Simulations
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