Collisional evolution of dust aggregates. From compaction to catastrophic destruction
arXiv:0909.3168 · doi:10.1051/0004-6361/200810682
Abstract
The coagulation of dust aggregates occurs in various astrophysical environments. Each one is characterized by different conditions that influence the growth, e.g. relative velocities, composition, and size of the smallest constituents (monomers). Here we study the microphysics of collisions of dust aggregates in a four-dimensional parameter space. The parameters are the collision energy, the initial compactness of agglomerates, the mass ratio of collision partners, and the impact parameter. For this purpose we employ a state of the art molecular dynamics type of model that has been extensively and successfully tested against laboratory experiments. It simulates the motion of individual monomers interacting dynamically via van der Waals surface forces. The structure of aggregates is quantified by the filling factor that provides information about the internal structure, the packing density of monomers, and the projected surface area of aggregates. Our results show the importance of the impact parameter that causes formation of elongated particles, due to tensile forces acting in offset collisions. We also describe in detail the internal structure of the resulting aggregates. Our findings are summarized in the form of a simple collision recipe. The recipe specifies the outcome of a collision, averaged over the impact parameter. It is provided in tabular form for a range of physical parameters such as impact energy and pre-collision filling factor. The dependence on the mass ratio of impactor and target is taken into account by providing both a local and a global branch of the recipe.
18 pages, 17 figures, Astronomy and Astrophysics in press
References in corpus (6)
- Dust coagulation in protoplanetary disks: porosity matters
- Planetesimal formation around the snow line in MRI-driven turbulent protoplanetary disks
- Dust Coagulation and Settling in Layered Protoplanetary Disks
- The Physics of Protoplanetesimal Dust Agglomerates II. Low Velocity Collision Properties
- Collisions between equal sized ice grain agglomerates
- Numerical determination of the material properties of porous dust cakes
Cited by in corpus (43)
- Gas- and dust evolution in protoplanetary disks
- Fluffy dust forms icy planetesimals by static compression
- Dust size distributions in coagulation/fragmentation equilibrium: Numerical solutions and analytical fits
- Planetesimal formation by sweep-up: How the bouncing barrier can be beneficial to growth
- Dust evolution in protoplanetary discs and the formation of planetesimals. What have we learned from laboratory experiments?
- Can grain growth explain transition disks?
- Dust Density Distribution and Imaging Analysis of Different Ice Lines in Protoplanetary Disks
- Dust growth and evolution in protoplanetary disks
- Direct imaging of the water snow line at the time of planet formation using two ALMA continuum bands
- Erosion and the limits to planetesimal growth
- Light scattering by fractal dust aggregates: I. Angular dependence of scattering
- Electrostatic Barrier against Dust Growth in Protoplanetary Disks. I. Classifying the Evolution of Size Distribution
- Static compression of porous dust aggregates
- Geometrical Cross Sections of Dust Aggregates and a Compression Model for Aggregate Collisions
- Electrostatic Barrier against Dust Growth in Protoplanetary Disks. II. Measuring the Size of the "Frozen" Zone
- Hints on the origins of particle traps in protoplanetary disks given by the relation
- Charging of Aggregate Grains in Astrophysical Environments
- Bouncing Behavior of Microscopic Dust Aggregates
- Unveiling Dust Aggregate Structure in Protoplanetary Disks by Millimeter-wave Scattering Polarization
- Preplanetary scavengers: Growing tall in dust collisions
- Condition for the formation of micron-sized dust grains in dense molecular cloud cores
- Clouds of Fluffy Aggregates: How They Form in Exoplanetary Atmospheres and Influence Transmission Spectra
- From grains to pebbles: the influence of size distribution and chemical composition on dust emission properties
- Macroscopic Dust in Protoplanetary Disks - From Growth to Destruction
- Compression Behaviour of Porous Dust Agglomerates
- Formation of Comets
- Numerical Simulations of Highly Porous Dust Aggregates in the Low-Velocity Collision Regime
- Ice aggregate contacts at the nm-scale
- Cosmic Dust Aggregation with Stochastic Charging
- Linking planetesimal and dust content in protoplanetary disks via a local toy model
- Analytic expressions for geometric cross-sections of fractal dust aggregates
- Fragmentation with Discontinuous Galerkin schemes: Non-linear fragmentation
- Collisional Growth and Fragmentation of Dust Aggregates. II. Mass Distribution of Icy Fragments
- Discrete stochastic charging of aggregate grains
- Dust Coagulation Regulated by Turbulent Clustering in Protoplanetary Disks
- Formulating Compressive Strength of Dust Aggregates from Low to High Volume Filling Factors with Numerical Simulations
- Impacts of viscous dissipation on collisional growth and fragmentation of dust aggregates
- Ejection of Chondrules from Fluffy Matrices
- Selective Aggregation Experiments on Planetesimal Formation and Mercury-Like Planets
- On the elastoplastic behavior in collisional compression of spherical dust aggregates
- Last giant impact on the Neptunian system. Constraints on oligarchic masses in the trans-Saturnian region
- Gas permeability and mechanical properties of dust grain aggregates at hyper- and zero-gravity
- A Pathway for Collisional Planetesimal Growth in the Ice-Dominant Regions of Protoplanetary Disks