EPSC Abstracts
Vol. 19, EPSC2026-20, 2026, updated on 02 Jul 2026
https://doi.org/10.5194/epsc2026-20
Europlanet Science Congress 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 07 Sep, 18:00–19:30 (CEST), Display time Monday, 07 Sep, 08:30–19:30| Foyer 3, F3.55
Migration of dust particles ejected from the Earth and Mars
Sergei Ipatov
Sergei Ipatov
  • Vernadsky Institute of Geochemistry and Analytical Chemistry of RAS, Moscow, Russia (siipatov@hotmail.com)

Introduction. Сollisions of large bodies with planets (mainly during planet formation) could produce ejection of bodies and dust particles. The probabilities of collisions of bodies ejected from the Earth with planets and the Moon were studied by Ipatov (2024a, 2025a). Ipatov (2024b-c, 2025b-c, 2926) presented shorter information about probabilities of collisions of bodies ejected from all terrestrial planets and the Moon with planets. Migration of dust particles was shortly discussed in (Ipatov, 2025c). Below I study the migration of dust ejected from the Earth and Mars. In each calculation variant (“run”), the motion of 250 ejected dust particles was studied for the fixed values of an ejection angle iej, a velocity vej of ejection, and one of three points of ejection. In different variants, iej equaled to 45o, or 15o, or 90o, and vej varied from 11.3 to 20 km/s for the Earth and from 5.05 to 20 km/s for Mars. For points W and B, the particles started from the forward point on the planet's surface in the direction of the planet's motion and from the back point on the opposite side of the planet, respectively. The starting point F is located most far from the Sun. The gravitational influence of the Sun and all planets, radiation pressure, the Poynting-Robertson effect and the solar wind were taken into account. The evolution of orbits was studied during the dynamical lifetime Tend of all particles (until all particles left the Solar System or collided with the Sun or planets). Calculations were carried out for the ratio β of radiation pressure force to gravitational force equaled to 0.0004, 0.004, 0.04 and 0.4 (corresponding to silicate particle diameters of about 1 mm, 100, 10 and 1 micron).

Ejection from the Earth. At β=0.0004 the values of Tend (for a run with 250 particles) were typically between 0.5 and 10 Myr, but could exceed 100 Myr. For 8500 considered 1-mm particles, there were 35 collisions with Mercury, 43 with Venus and 40 with the Earth. For iej=45o the fraction pej of ejected particles was 0 for all ejections from point B and for ejection at small vej from other points. At vej=20 km/s and iej=45opej reached 0.3 for point F and 1 for point W.

At β=0.004 the values of Tend were between 0.006 and 10 Myr. For 8500 considered 100-micron particles, there were 2 collisions with Mercury, 7 with Venus, and 6 with the Earth. Most of particles collided with the Sun. Ejection of particles was in 7 among 34 runs. All particles were ejected from point W at vej=20 km/s and iej=45o. For ejection from point F at vej=20 km/s and iej=45o, pej equaled to 0.27.

At β=0.04 the values of Tend were between 0.003 and 5 Myr. Among 7750 considered 10-micron particles, there was only one collision with planets. The fraction of ejected particles was 0 in all calculations for ejection from point B and also for ejection from point W at iej=89o. For ejection from point W at iej=45o, pej varied from 0 at vej=11.5 km/s to 1 at vej=20 km/s. For ejection from point F at iej=45o, pej varied from 0 at vej=11.3 km/s to 0.3 at vej=20 km/s.

At β=0.4, Tend was less than 0.4 Myr. For 8500 considered micron particles, there were no their collisions with planets. In most calculations at β=0.4, about a half of particles collided with the Sun, and other particles were ejected from the Solar System. For ejection from point W at vej≥14 km/s and iej≥45o, all micron particles were ejected into hyperbolic orbits.

The estimated (based on arrays of orbital elements of migrating particles) ratio of probabilities of collisions of particles with the Earth and the Moon was between 20 and 65 (more often between 25 and 35).

Ejection from Mars. For each β, 4000 particles were considered at iej=45o and different vej and ejection points. At β=0.0004, for 4000 particles there were 15 collisions with Mercury, 20 with Venus, 18 with Earth, and 4 with Mars. For considered series of calculations, Tend was between 0.0005 and 7 Myr. Tend equaled to 0.0005 Myr for ejection from point W at vej=20 km/s. The fraction of bodies collided with the Sun and the fraction pej of ejected particles varied from 0 to 1. At β=0.004, there were 5 collisions with Mercury, 4 with Venus, and 4 with Earth. Depending on vej and an ejection point, pej and the fraction of bodies collided with the Sun varied from 0 to 1, and 0.0005≤Tend≤5 Myr. At β=0.04, the values of pej were between 0 and 1, 0.0005≤Tend≤1.3 Myr, and there were no collisions of particles with planets. At β=0.4, there were no collisions of particles with planets, and in different runs pej varied from 0.5 to 1 (other particles collided with the Sun). The values of Tend were between 0.0004 and 0.45 Myr. For a few series of runs, the estimated ratio of probabilities of collisions with the Earth and the Moon was between 21 and 23 at β=0.4, between 30 and 50 at β=0.04, between 15 and 40 at β=0.004, and between 15 and 35 at β=0.0004.

Acknowledgements: The studies of delivery of material to the Moon were supported by the Russian Science Foundation, project 25-17-00051. Other studies were carried out under government-financed research project for the Vernadsky Institute.

References: Ipatov S.I. (2024a) Solar System Research 58:94-111. https://doi.org/10.1134/S0038094624010040, http://arxiv.org/abs/2405.19797. Ipatov S.I. (2024b) Solar System Research 58. Suppl. 1. P. S50-S63. https://doi.org/10.1134/S0038094623600105. http://arxiv.org/abs/2411.05436. Ipatov S.I. (2024c) Modern astronomy: from the Early Universe to exoplanets and black holes. P. 904-909. https://doi.org/10.26119/VAK2024.143. https://arxiv.org/abs/2501.00134. Ipatov S.I. (2025a) Icarus 425, id. 116341 (24 p.). https://doi.org/10.1016/j.icarus.2024.116341, http://arxiv.org/abs/2411.04218. Ipatov S.I. (2025b) Moscow University Physics Bulletin, V. 80. Suppl. 1. P. S423-S427. https://doi.org/10.3103/S0027134925701279, https://www.researchgate.net/publication/403719268. Ipatov S.I. (2025c) Formation and evolution of planetary systems (in Russian). ISBN 978-5-6055159-1-3. Moscow. Onebook.ru. 132 p. DOI: 10.17513/np.649. https://dx.doi.org/10.17513/np.649. Ipatov S.I. (2026) Proc. of IAU, V. 20, Symposium S393. P. 9-13. DOI: https://doi.org/10.1017/S1743921324001911.

How to cite: Ipatov, S.: Migration of dust particles ejected from the Earth and Mars, Europlanet Science Congress 2026, The Hague, The Netherlands, 7–11 Sep 2026, EPSC2026-20, https://doi.org/10.5194/epsc2026-20, 2026.