Asteroid sharing Earth’s orbit discovered – could it help future space missions?

Asteroid sharing Earth’s orbit discovered – could it help future space missions?

Where 2020 XL5 would appear in the dawn sky if we could see it with the naked eye from Chile. NOIRLab/NSF/AURA/J. da Silva, CC BY-NC-SA

Research has shown that the Earth trails an asteroid barely a kilometre across in its orbit about the Sun – only the second such body to have ever been spotted. It goes round the Sun on average two months ahead of the Earth, dancing around in front like an excited herald of our coming.

This object, known as 2020 XL₅, was first spotted in December 2020 using Pan-STARRS telescopes on the summit of Haleakala on the Hawaiian island of Maui. But determination of its orbit required follow-up observations using the 4.1-metre SOAR (Southern Astrophysical Research) telescope in Chile.

Image plotting 500 years of 2020 XL5 orbits.
500 years of 2020 XL5 orbits plotted, relative to Earth.
By Phoenix7777 – Own workData source: HORIZONS System, JPL, NASA CC BY-SA 4.0

Based on this data, a team led by planetary scientist Toni Santana-Ros of the University of Alicante in Spain has now announced that 2020 XL₅ is trapped for at least the next several thousand years in an orbit about one of the Sun-Earth “Lagrange points”. These are where the gravitational forces of the Earth and the Sun balance to create stable locations. It means the object keeps pace with the Earth as it goes round the Sun.

Lagrange points exist around other planets too, they are equilibrium points for any objects with small mass under the influence of any two much more massive bodies. There are three such points on the Sun-Earth line (L1, L2 and L3, see image below), first discovered mathematically by the Swiss mathematician Leonhard Euler. Spacecraft, such as James Webb Space Telecope (at L2) and DSCOVR (at L1), can be maintained there with only a small expenditure of fuel.

Lagrange points in relaton to Earth's orbit
The Lagrange points associated with Earth’s orbit (sizes and distances not to scale).
NOIRLab/NSF/AURA/J. da Silva

Two other points, L4 and L5, were discovered in 1772 by Euler’s student Joseph-Louis Lagrange. Here, a small-mass object making an equilateral triangle with Sun and Earth is in a stable equilibrium. These points are 60 degrees ahead of and 60 degrees behind the Earth, and because 60 degrees (see image above) is one-sixth of the Earth’s orbit this amounts to two months separation.

If a small-mass object is perturbed so as to move away from L4 or L5, the combined gravity of the Sun and Earth draws it back – bending its path into a stable orbit around the Lagrange point that looks kidney bean shaped relative to Earth.

XL5, but no fireball

2020 XL₅ is being called a Trojan companion to the Earth by analogy with Jupiter’s Trojan asteroids. Jupiter shares its orbit with nearly ten thousand known asteroids, half of them ahead of Jupiter, and half behind. The first of those, discovered in 1906, was named Achilles after a central character at the siege of Troy in Homer’s Iliad.

A convention developed to name each one after a hero from the same story. Only those trailing Jupiter (clustered at the Sun-Jupiter L5 position) are given Trojan names, such as Hektor, whereas those ahead of Jupiter (at L4) are give Greek names, such as Achilles. Collectively, whether at L4 or L5 they are all referred to as Trojans.

Image showing asteroid positions, with Jupiter's Trojans in green
Asteroid positions, with Jupiter’s Trojans in green.
Mdf at English Wikipedia, Public domain, via Wikimedia Commons

Small numbers of Trojan asteroids have now been discovered associated with Neptune (23), Uranus (1) and Mars (9). But 2020 XL₅ is only the second Trojan companion of Earth to have been found. The first, 2010 TK₇, was discovered in 2010. That’s only about 300 metres across, so 2020 XL₅ considerably outmasses it at about 1.2km across.

There are probably many more Earth Trojans, but they are hard to discover from Earth because they can only ever be seen fairly low in the pre-dawn sky if at L4 like both 2010 TK₇ and 2020 XL₅, or just after sunset if at L5 (where none have yet been found). Their orbits are not stable over millions of years, so they can’t be remnants that have been there ever since Earth’s formation but must have drifted into place later.

However, the SOAR observations were able to show that 2020 XL₅ appears to be a carbon-rich asteroid (called C-type). So it is a sample of what the Solar System was built from, and it would be instructive to study Earth’s Trojan companions in more detail as examples of unaltered material.

But could we mine them or use them in other ways? Santana-Ros notes that 2020 XL₅ has an orbit that bobs above and below Earth’s orbital plane. This means that to manoeuvre a spacecraft into a rendezvous (to orbit or land on it) would require considerable velocity change. That would probably need too much fuel to be practical. The same applies to 2010 TK₇.

However, the study points out that if other Earth Trojans are found in orbits that are less tilted, these might make handy bases as staging posts for exploration of the Solar System. They’d be much easier to take off from than from the Earth or Moon because their gravity is so slight. They could even be a source of resources that we could mine.

The Conversation

David Rothery is Professor of Planetary Geosciences at the Open University. He is co-leader of the European Space Agency's Mercury Surface and Composition Working Group, and a Co-Investigator on MIXS (Mercury Imaging X-ray Spectrometer) that is now on its way to Mercury on board the European Space Agency's Mercury orbiter BepiColombo. He has received funding from the UK Space Agency and the Science & Technology Facilities Council for work related to Mercury and BepiColombo, and from the European Commission under its Horizon 2020 programme for work on planetary geological mapping (776276 Planmap). He is author of Planet Mercury – from Pale Pink Dot to Dynamic World (Springer, 2015), Moons: A Very Short Introduction (Oxford University Press, 2015) and Planets: A Very Short Introduction (Oxford University Press, 2010). He is Educator on the Open University's free learning Badged Open Course (BOC) on Moons and its equivalent FutureLearn Moons MOOC, and chair of the Open University's level 2 course on Planetary Science and the Search for Life.