Numerical Simulations of Highly Porous Dust Aggregates in the Low-Velocity Collision Regime
arXiv:1001.1617 · doi:10.1051/0004-6361/200913596
Abstract
A highly favoured mechanism of planetesimal formation is collisional growth. Single dust grains, which follow gas flows in the protoplanetary disc, hit each other, stick due to van der Waals forces and form fluffy aggregates up to centimetre size. The mechanism of further growth is unclear since the outcome of aggregate collisions in the relevant velocity and size regime cannot be investigated in the laboratory under protoplanetary disc conditions. Realistic statistics of the result of dust aggregate collisions beyond decimetre size is missing for a deeper understanding of planetary growth. Joining experimental and numerical efforts we want to calibrate and validate a computer program that is capable of a correct simulation of the macroscopic behaviour of highly porous dust aggregates. After testing its numerical limitations thoroughly we will check the program especially for a realistic reproduction of various benchmark experiments. We adopt the smooth particle hydrodynamics (SPH) numerical scheme with extensions for the simulation of solid bodies and a modified version of the Sirono porosity model. Experimentally measured macroscopic material properties of silica dust are implemented. We calibrate and test for the compressive strength relation and the bulk modulus. SPH has already proven to be a suitable tool to simulate collisions at rather high velocities. In this work we demonstrate that its area of application can not only be extended to low-velocity experiments and collisions. It can also be used to simulate the behaviour of highly porous objects in this velocity regime to a very high accuracy.The result of the calibration process in this work is an SPH code that can be utilised to investigate the collisional outcome of porous dust in the low-velocity regime.
accepted by Astronomy & Astrophysics
References in corpus (11)
- Coagulation, fragmentation and radial motion of solid particles 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
- Dust coagulation in protoplanetary disks: porosity matters
- Numerical simulations of impacts involving porous bodies: I. Implementing sub-resolution porosity in a 3D SPH Hydrocode
- High Velocity Dust Collisions: Forming Planetesimals in a Fragmentation Cascade with Final Accretion
- A representative particle approach to coagulation and fragmentation of dust aggregates and fluid droplets
- The Physics of Protoplanetesimal Dust Agglomerates. IV. Towards a Dynamical Collision Model
- Collisional evolution of dust aggregates. From compaction to catastrophic destruction
- Collisions between equal sized ice grain agglomerates
- Numerical determination of the material properties of porous dust cakes
Cited by in corpus (17)
- The outcome of protoplanetary dust growth: pebbles, boulders, or planetesimals? I. Mapping the zoo of laboratory collision experiments
- Planetesimal formation by sweep-up: How the bouncing barrier can be beneficial to growth
- Static compression of porous dust aggregates
- Free Collisions in a Microgravity Many-Particle Experiment III: The Collision Behavior of sub-Millimeter-Sized Dust Aggregates
- Bouncing Behavior of Microscopic Dust Aggregates
- Dust growth in protoplanetary disks - a comprehensive experimental/theoretical approach
- The Physics of Protoplanetesimal Dust Agglomerates. V. Multiple Impacts of Dusty Agglomerates at Velocities Above the Fragmentation Threshold
- Growth and fragmentation of centimetre-sized dust aggregates: the dependence on aggregate size and porosity
- Experiments on centimeter-sized dust aggregates and their implications for planetesimal formation
- Collisions of inhomogeneous pre-planetesimals
- Compression Behaviour of Porous Dust Agglomerates
- A dearth of small particles in debris disks: An energy-constrained smallest fragment size
- An Analytical Theory for the Growth from Planetesimals to Planets by Polydisperse Pebble Accretion
- Tensile & shear strength of porous dust agglomerates
- The four-populations model: a new classification scheme for pre-planetesimal collisions
- Formulating Compressive Strength of Dust Aggregates from Low to High Volume Filling Factors with Numerical Simulations
- On the elastoplastic behavior in collisional compression of spherical dust aggregates