Analytic expressions for geometric cross-sections of fractal dust aggregates
arXiv:2104.06804 · doi:10.1093/mnras/stab1069
Abstract
In protoplanetary discs and planetary atmospheres, dust grains coagulate to form fractal dust aggregates. The geometric cross-section of these aggregates is a crucial parameter characterizing aerodynamical friction, collision rates, and opacities. However, numerical measurements of the cross-section are often time-consuming as aggregates exhibit complex shapes. In this study, we derive a novel analytic expression for geometric cross-sections of fractal aggregates. If an aggregate consists of monomers of radius , its geometric cross-section is expressed as \begin{equation} \frac{G}{NπR_0^2}=\frac{A}{1+(N-1)\tildeσ}, \nonumber \end{equation} where is an overlapping efficiency, and is a numerical factor connecting the analytic expression to the small non-fractal cluster limit. The overlapping efficiency depends on the fractal dimension, fractal prefactor, and of the aggregate, and its analytic expression is derived as well. The analytic expressions successfully reproduce numerically measured cross-sections of aggregates. We also find that our expressions are compatible with the mean-field light scattering theory of aggregates in the geometrical optics limit. The analytic expressions greatly simplify an otherwise tedious calculation and will be useful in model calculations of fractal grain growth in protoplanetary discs and planetary atmospheres.
arXiv comment12 pages, 8 figures, 1 table; Accepted for publication in MNRAS
References in corpus (17)
- Rapid Coagulation of Porous Dust Aggregates Outside the Snow Line: A Pathway to Successful Icy Planetesimal Formation
- Dust coagulation and fragmentation in molecular clouds. I. How collisions between dust aggregates alter the dust size distribution
- Fluffy dust forms icy planetesimals by static compression
- Dust coagulation in protoplanetary disks: porosity matters
- Numerical Modeling of the Coagulation and Porosity Evolution of Dust Aggregates
- Aggregate dust particles at comet 67P/Churyumov-Gerasimenko
- Erosion and the limits to planetesimal growth
- Light scattering by fractal dust aggregates: I. Angular dependence of scattering
- Collisional evolution of dust aggregates. From compaction to catastrophic destruction
- A panoptic model for planetesimal formation and pebble delivery
- Geometrical Cross Sections of Dust Aggregates and a Compression Model for Aggregate Collisions
- Unveiling Dust Aggregate Structure in Protoplanetary Disks by Millimeter-wave Scattering Polarization
- The influence of grain rotation on the structure of dust aggregates
- Effect of dust size and structure on scattered light images of protoplanetary discs
- Light Scattering by Fractal Dust Aggregates. II. Opacity and Asymmetry Parameter
- Clouds of Fluffy Aggregates: How They Form in Exoplanetary Atmospheres and Influence Transmission Spectra
- Scattering polarization of 3-m water-ice feature by large icy grains
Cited by in corpus (8)
- Fractal aggregates of sub-micron-sized grains in the young planet-forming disk around IM Lup
- Collisional evolution of dust and water ice in protoplanetary discs during and after an accretion outburst
- Aerosols are not Spherical Cows: Using Discrete Dipole Approximation to Model the Properties of Fractal Particles
- Observed polarized scattered light phase functions of planet-forming disks
- The water-ice feature in near-infrared disk-scattered light around HD 142527: Micron-sized icy grains lifted up to the disk surface?
- Root mean squares of distance and geodesic between two constituent particles within fractal aggregates prepared by BCCA, DLA, and GSAW procedures
- Grain Growth in Escaping Atmospheres: Implications for the Radius Inflation of Super-Puffs
- The Influence of the Fractal Dimension on Dust Evolution in Protoplanetary Disks