Issue |
A&A
Volume 614, June 2018
|
|
---|---|---|
Article Number | A97 | |
Number of page(s) | 5 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/201832806 | |
Published online | 20 June 2018 |
Comparison of the orbital properties of Jupiter Trojan asteroids and Trojan dust
Astronomy Research Unit, University of Oulu,
90014
Oulu,
Finland
e-mail: xiaodong.liu@oulu.fi
Received:
10
February
2018
Accepted:
7
March
2018
In a previous paper we simulated the orbital evolution of dust particles from the Jupiter Trojan asteroids ejected by the impacts of interplanetary particles, and evaluated their overall configuration in the form of dust arcs. Here we compare the orbital properties of these Trojan dust particles and the Trojan asteroids. Both Trojan asteroids and most of the dust particles are trapped in the Jupiter 1:1 resonance. However, for dust particles, this resonance is modified because of the presence of solar radiation pressure, which reduces the peak value of the semi-major axis distribution. We find also that some particles can be trapped in the Saturn 1:1 resonance and higher order resonances with Jupiter. The distributions of the eccentricity, the longitude of pericenter, and the inclination for Trojans and the dust are compared. For the Trojan asteroids, the peak in the longitude of pericenter distribution is about 60 degrees larger than the longitude of pericenter of Jupiter; in contrast, for Trojan dust this difference is smaller than 60 degrees, and it decreases with decreasing grain size. For the Trojan asteroids and most of the Trojan dust, the Tisserand parameter is distributed in the range of two to three.
Key words: meteorites, meteors, meteoroids / planets and satellites: rings / minor planets, asteroids: general / zodiacal dust / celestial mechanics / solar wind
© ESO 2018
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