Hayabusa2 (はやぶさ2) is a mission to survey a near-Earth asteroid and collect a surface sample for return to Earth in 2021. The spacecraft arrived at asteroid 162173 Ryugu (just ‘Ryugu’ for short) on 27 June 2018. Asteroids like Ryugu are time capsules that can teach us more about the origin and evolution of the solar system. Learning about them also helps efforts to defend Earth from potential asteroid impacts.
Hayabusa2 completed 2 successful touchdowns and sample collections in 2019. The second touchdown collected material excavated from an artificial crater created using explosives and a copper projectile. The spacecraft also carried 4 deployable surface landers — 3 of which have been successfully dropped on the surface — and 5 target markers containing names collected by The Planetary Society and JAXA.
This short clip shows Hayabusa 2's second touchdown, which occurred on 11 July 2019 at 01:06 UTC, as seen from the spacecraft's small monitor camera (CAM-H). The sequence plays at roughly 10 times normal speed. See the full video here.
The Planetary Society and the Japan Aerospace Exploration Agency invited people worldwide to submit their names for a round-trip ride to asteroid Bennu. Search for your certificate here.
Hayabusa2 is a follow-on mission to JAXA’s successful Hayabusa, which visited S-type asteroid (25143) Itokawa and returned a sample on 13 June 2010. Hayabusa’s samples proved that S-type asteroids (the most common in the near-Earth asteroid population) are the parents of ordinary chondrite meteorites.
Hayabusa2’s goal is to sample a member of different near-Earth asteroid population, a C-type asteroid. The mission has four science objectives (Watanabe et al. 2017):
Find out how dynamic the early solar system was by studying how different kinds of materials (rocky matter, organic matter, ices, etc.) are distributed and layered on Ryugu
Study the chemical reactions among minerals, ices, and organic material that happened during solar system formation by searching for organic materials in returned samples, and finding out which kinds of minerals coexist with them
Do radioisotope age dating on the returned samples to find out when the asteroid’s materials formed and when significant heating happened in the past
Map Ryugu’s surface and tell its geologic story, especially its impact history
Used to create an artificial crater on Ryugu’s surface, uncovering materials not currently exposed to space. Consists of a small deployable box of explosives and a lump of copper (used to differentiate the impactor from native Ryugu materials). Hayabusa2 will release the explosive box, fire its reaction control thrusters, and hide behind Ryugu while the box explodes and shoots the copper lump into the surface at about 2 kilometers per second, creating a crater a few meters in diameter. Principal investigator: Masahiko Arakawa. Saiki et al. (2017) | Yoshikawa et al. (2014) | Tsuda et al. (2013) | July 2018 fact sheet
Deployable Camera 3 (DCAM3)
After deploying SCI, several tens of minutes before the explosion, Hayabusa2 will release this instrument, a cylinder 78 mm in diameter and 80 mm tall. It contains two cameras to capture the explosion and crater formation: a low-resolution analog imager that will transmit to Hayabusa2 in real-time (DCAM3-A, color, viewing angle 71º x 53º, 720 x 526 pixels, resolution 10 m/pixel) and one high-resolution digital imager that will send data to Hayabusa2 after the crater impact (DCAM-3-D, monochrome, viewing angle 74º x 74º, 2000 x 2000 pixels, resolution 1m/pixel). The system is IKAROS heritage. A separate component on the spacecraft will receive the DCAM3 images and also has a small camera head (DCAM3-CAM-H) that can take images of the Hayabusa2 sampler horn. Sawada et al. (2017) | Ogawa et al. (2017) | Ishibashi et al. (2017)
Other instruments and technologies
Hayabusa2’s sample system is similar to that of Hayabusa, with minor improvements. The system consists of a one-meter-long sample horn, a sample catcher, a sample container, and an Earth re-entry capsule.
When Hayabusa2’s sample horn touches the surface, it fires a tantalum projectile into the surface within the sample horn, kicking up surface material. The use of tantalum allows sample material to be distinguished easily from impactor material. The material floats up the horn, through a 90-degree turn, and into a sample catcher. Just 1 second after touchdown, the spacecraft fires its thrusters for ascent to avoid tipping over. The sample horn also contains a catch at the bottom opening to allow small pieces of gravel to stay in the horn. When Hayabusa2 decelerates, any caught gravel pieces can tumble up the horn into the sample catcher. The catcher itself has 3 collection compartments.
Hayabusa2 carries three drum-shaped rovers designed to hop across Ryugu. MINERVA-II-1 consists of two rovers: Rover-1A and Rover-1B. Both were successfully deployed on 21 September 2018. MINERVA-II-2 is a third, larger rover that isn’t believed to be working properly, but may be deployed anyway. Principal investigator: Hirohide Demura.
Hayabusa2's first touchdown and sample collection site (Tamatebako) is located on Ryugu's equator, roughly between Kintaro crater to the west and Brabo crater to the east. It was chosen for safety reasons, because it had no rocks larger than 60 centimeters.
The second touchdown and sample collection site (Uchide-no-kozuchi) is also on the equator, east of Brabo crater and just west of Kolobok crater. It was chosen due to its proximity to the artificial crater created during the SCI experiment. The SCI site was a relatively hazard-free spot geologically similar to the first touchdown site, allowing for an above-and-beneath-the-surface comparison.
Ryugu surface map
Ryugu's surface with labeled major features and locations, as of August 2019.
11 July 2019: Hayabusa2 successfully completes second Ryugu touchdown
5 April 2019: SCI experiment creates artificial crater on surface