Issue |
A&A
Volume 672, April 2023
|
|
---|---|---|
Article Number | A50 | |
Number of page(s) | 18 | |
Section | Numerical methods and codes | |
DOI | https://doi.org/10.1051/0004-6361/202243069 | |
Published online | 29 March 2023 |
A Monte Carlo code for the collisional evolution of porous aggregates (CPA)
1
CONICET and ITIC, Universidad Nacional de Cuyo,
Padre Contreras 1300,
Mendoza
5500,
Argentina
2
CONICET and Facultad de Ingeniería, Universidad de Mendoza,
Boulogne Sur Mer 683,
Mendoza
5500,
Argentina
3
Physics Department and Research Center OPTIMAS, University Kaiserslautern,
Erwin-Schrödinger-Straße,
67663
Kaiserslautern,
Germany
e-mail: urbassek@uni-kl.de
4
Centro de Nanotecnología Aplicada, Facultad de Ciencias, Universidad Mayor,
8580000
Huechuraba, Santiago,
Chile
Received:
9
January
2022
Accepted:
11
February
2023
Context. The collisional evolution of submillimeter-sized porous dust aggregates is important in many astrophysical fields.
Aims. We have developed a Monte Carlo code to study the processes of collision between mass-asymmetric, spherical, micron-sized porous silica aggregates that belong to a dust population.
Methods. The Collision of Porous Aggregates (CPA) code simulates collision chains in a population of dust aggregates that have different sizes, masses, and porosities. We start from an initial distribution of granular aggregate sizes and assume some collision velocity distribution. In particular, for this study we used a random size distribution and a Maxwell-Boltzmann velocity distribution. A set of successive random collisions between pairs of aggregates form a single collision chain. The mass ratio, filling factor, and impact velocity influence the outcome of the collision between two aggregates. We averaged hundreds of thousands of independent collision chains to obtain the final, average distributions of aggregates.
Results. We generated and studied four final distributions (F), for size (n), radius (R), porosity, and mass-porosity distributions, for a relatively low number of collisions. In general, there is a profuse generation of monomers and small clusters, with a distribution F (R) ∝ R−6 for small aggregates. Collisional growth of a few very large clusters is also observed. Collisions lead to a significant compaction of the dust population, as expected.
Conclusions. The CPA code models the collisional evolution of a dust population and incorporates some novel features, such as the inclusion of mass-asymmetric aggregates (covering a wide range of aggregate radii), inter-granular friction, and the influence of porosity.
Key words: planets and satellites: formation / protoplanetary disks / methods: numerical
© The Authors 2023
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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