Observation of bottom-up formation for charged grain aggregates related to pre-planetary evolution beyond the bouncing barrier
arXiv:2106.01081 · doi:10.1051/0004-6361/202039430
Abstract
Context. Particles in protoplanetary disks go through a number of phases that are dominated by collisions. In each of these events, grains exchange electrical charge via triboelectric effects. This enhances the stability of particle aggregates. Aim. Dielectric grains are easily charged by collisions. Here, we investigate whether a charge is capable of inducing an aggregation of particles and we consider how collision properties, such as ticking velocities and collisional cross-sections, are altered. Methods. We explored aggregation in microgravity experiments based on the observation of the motion of submillimeter (submm) grains following many collisions. In the process, grains attract each other, collide, stick, and ultimately form small aggregates. Results. We observed a bottom-up formation of irregular aggregates from submm grains. While some of the observed trajectories during the approach of grains reflect the presence of a pure Coulomb potential, the motion is not always in agreement with pure Kepler motion. Higher-order potentials of multipole charge distributions stand as a plausible explanation for this behavior. An immediate consequence of charging is that the particles continue to stick to each other at velocities of while surface forces of neutral grains are only expected to allow sticking below . No bouncing collision was observed among hundreds of collisions in the given parameter range. Applied to early phases of planet formation, the forming aggregates are therefore the first steps in a new growth phase beyond the traditional bouncing barrier in planet formation.
References in corpus (38)
- Rapid planetesimal formation in turbulent circumstellar discs
- Streaming Instabilities in Protoplanetary Disks
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? II. Introducing the bouncing barrier
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? I. Mapping the zoo of laboratory collision experiments
- Observations of Protoplanetary Disk Structures
- Concentrating small particles in protoplanetary disks through the streaming instability
- Electric charging of dust aggregates and its effect on dust coagulation in protoplanetary disks
- Planetesimal formation by sweep-up: How the bouncing barrier can be beneficial to growth
- Exclusion of Cosmic Rays in Protoplanetary Disks: Stellar and Magnetic Effects
- Dust release and tensile strength of the non-volatile layer of cometary nuclei
- Free Collisions in a Microgravity Many-Particle Experiment. I. Dust Aggregate Sticking at Low Velocities
- Size-dependent same-material tribocharging in insulating grains
- Why do Particle Clouds Generate Electric Charges?
- Resonant Drag Instabilities in protoplanetary disks: the streaming instability and new, faster-growing instabilities
- Electrostatic Barrier against Dust Growth in Protoplanetary Disks. I. Classifying the Evolution of Size Distribution
- Protoplanetary Disk Rings as Sites for Planetesimal Formation
- Free Collisions in a Microgravity Many-Particle Experiment III: The Collision Behavior of sub-Millimeter-Sized Dust Aggregates
- Turbulence in weakly-ionized proto-planetary disks
- Electrostatic Barrier against Dust Growth in Protoplanetary Disks. II. Measuring the Size of the "Frozen" Zone
- Dust-Pileup at the Dead-Zone Inner Edge and Implications for the Disk Shadow
- Preplanetary scavengers: Growing tall in dust collisions
- Experimental Study on Bouncing Barriers in Protoplanetary Disks
- Failed Growth at the Bouncing Barrier in Planetesimal Formation
- Ionization and Dust Charging in Protoplanetary Disks
- Is There a Temperature Limit in Planet Formation at 1000 K?
- Quantitatively consistent, scale-spanning model for same-material tribocharging
- Dust-Dust Collisional Charging and Lightning in Protoplanetary Discs
- Harvesting the decay energy of Al to drive lightning discharge in protoplanetary discs
- Growing into and out of the bouncing barrier in planetesimal formation
- Cosmic Dust Aggregation with Stochastic Charging
- A Smoking Gun for Planetesimal Formation: Charge Driven Growth into a New Size Range
- Mechanical equilibrium of aggregates of dielectric spheres
- A Possible Mechanism for Overcoming the Electrostatic Barrier Against Dust Growth in Protoplanetary disks
- Grain charging in protoplanetary discs
- Drifting inwards in protoplanetary discs I Sticking of chondritic dust at increasing temperatures
- Collisions of solid ice in planetesimal formation
- Cosmic radiation does not prevent collisional charging in (Pre)-Planetary Atmospheres
- Development of a Method for the Observation of Lightning in Protoplanetary Disks Using Ion Lines
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- Aggregation of Sub-mm Particles in Strong Electric Fields under Microgravity Conditions
- The growth of super-large pre-planetary pebbles to an impact erosion limit
- Violation of triboelectric charge conservation on colliding particles
- Electrostatic Repulsion of Dust from Planetary Surfaces
- Positive Feedback: How a Synergy Between the Streaming Instability and Dust Coagulation Forms Planetesimals
- Forbidden planetesimals
- Ionizing Protoplanetary Disks in Pebble Collisions
- Clusters of tribocharged dust aggregates as pebbles in protoplanetary disks
- The Dissolution of Planetesimals in Electrostatic Fields
- Collisional Charging in the Low Pressure Range of Protoplanetary Disks
- Positive Feedback II: How Dust Coagulation inside Vortices Can Form Planetesimals at Low Metallicity