Experimental Study on Bouncing Barriers in Protoplanetary Disks
arXiv:1401.4280 · doi:10.1088/0004-637X/783/2/111
Abstract
For dust aggregates in protoplanetary discs a transition between sticking and bouncing in individual collisions at mm to cm size has been observed in the past. This lead to the notion of a bouncing barrier for which growth gets stalled. Here, we present long term laboratory experiments on the outcome of repeated aggregate collisions at the bouncing barrier. About 100 SiO dust aggregates of 1 mm in size were observed interacting with each other. Collisions occured within a velocity range from below mm/s up to cm/s. Aggregates continuously interacted with each other over a period of 900 s. During this time more than collisions occured. Nearly 2000 collisions were analyzed in detail. No temporal stable net growth of larger aggregates was observed even though sticking collision occur. Larger ensembles of aggregates sticking together are formed but were disassembled again during the further collisional evolution. The concept of a bouncing barrier supports the formation of planetesimals by seeded collisional growth as well as by gravitational instability favouring a significant total mass being limited to certain size ranges. Within our parameter set the experiments confirm that bouncing barriers are one possible and likely evolutionary limit of a self consistent particle growth.
References in corpus (7)
- Towards planetesimals: dense chondrule clumps in the protoplanetary nebula
- Planetesimal formation around the snow line in MRI-driven turbulent protoplanetary disks
- High Velocity Dust Collisions: Forming Planetesimals in a Fragmentation Cascade with Final Accretion
- Microgravity experiments on the collisional behavior of Saturnian ring particles
- Collisions between equal sized ice grain agglomerates
- Preplanetary scavengers: Growing tall in dust collisions
- Crossing barriers in planetesimal formation: The growth of mm-dust aggregates with large constituent grains
Cited by in corpus (35)
- Evidence of fast pebble growth near condensation fronts in the HL Tau protoplanetary disk
- Close-in planetesimal formation by pile-up of drifting pebbles
- Contacts of Water Ice in Protoplanetary Disks - Laboratory Experiments
- Can dust coagulation trigger streaming instability?
- Collisions of CO Ice Grains in Planet Formation
- Understanding planet formation using microgravity experiments
- Failed Growth at the Bouncing Barrier in Planetesimal Formation
- From Pebbles and Planetesimals to Planets and Dust: the Protoplanetary Disk--Debris Disk Connection
- Seeding the Formation of Mercurys: An Iron-sensitive Bouncing Barrier in Disk Magnetic Fields
- Is There a Temperature Limit in Planet Formation at 1000 K?
- Size Dependence of the Bouncing Barrier in Protoplanetary Dust Growth
- Composition and Size Dependent Sorting in Preplanetary Growth: Seeding the Formation of Mercury-like Planets
- Growing into and out of the bouncing barrier in planetesimal formation
- Are Pebble Pile Planetesimals Doomed?
- Mechanical equilibrium of aggregates of dielectric spheres
- Growth of Aggregates with Liquid-Like Ice-Shells in Protoplanetary Discs
- Observation of bottom-up formation for charged grain aggregates related to pre-planetary evolution beyond the bouncing barrier
- ARISE: A granular matter experiment on the International Space Station
- Primordial Dusty Rings and Episodic Outbursts in Protoplanetary Discs
- The growth of super-large pre-planetary pebbles to an impact erosion limit
- Dense Particle Clouds in Laboratory Experiments in Context of Drafting and Streaming Instability
- Collisions of solid ice in planetesimal formation
- Free Collisions in a Microgravity Many-Particle Experiment. IV. - Three-Dimensional Analysis of Collision Properties
- Electrostatic Repulsion of Dust from Planetary Surfaces
- Onset of planet formation in the warm inner disk -- Colliding dust aggregates at high temperatures
- The Curie line in protoplanetary disks and the formation of Mercury-like planets
- Experimental study of clusters in dense granular gas and implications for the particle stopping time in protoplanetary disks
- Forbidden planetesimals
- Selective Aggregation Experiments on Planetesimal Formation and Mercury-Like Planets
- The motion of chondrules and other particles in a protoplanetary disc with temperature fluctuations
- On the origin of transition disk cavities: Pebble-accreting protoplanets vs Super-Jupiters
- Ionizing Protoplanetary Disks in Pebble Collisions
- Gas Phase Ions in Protoplanetary Disks from Collisions of Solids
- Clusters of tribocharged dust aggregates as pebbles in protoplanetary disks
- The Dissolution of Planetesimals in Electrostatic Fields