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PROCYON

From Wikipedia, the free encyclopedia
Japanese space probe (2014–2015)

PROCYON
Mission typeAsteroid flyby, technology demonstration
OperatorUniversity of Tokyo /JAXA
COSPAR ID2014-076DEdit this at Wikidata
SATCATno.40322Edit this on Wikidata
WebsitePROCYON on University of Tokyo site
Spacecraft properties
Launch massTotal: 67 kg (148 lb)
Dry mass64.5 kg (142 lb)
Dimensions0.55 × 0.55 × 0.67 m (1.8 × 1.8 × 2.2 ft)
Power25
Start of mission
Launch date3 December 2014, 04:22 UTC (2014-12-03UTC04:22Z)
RocketH-IIA 202
Launch siteLA-Y,Tanegashima Space Center
End of mission
Last contact3 December 2015 (2015-12-04)
Flyby ofEarth
Closest approach3 December 2015
Flyby of(185851) 2000 DP107
Closest approachIntended: 2016

PROCYON (Proximate Object Close flyby with Optical Navigation) was an asteroid flybyspace probe that was launched together withHayabusa2 on 3 December 2014 13:22:04 (JST). It was developed byUniversity of Tokyo andJAXA.It was a small (70 kg, approx. 60 cm cube), low cost (¥500 million) spacecraft.[1]

It was intended to flyby the asteroid(185851) 2000 DP107 in 2016,[2] but the plan was abandoned due to the malfunction of theion thruster.[1]

Mission overview

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PROCYON was launched as secondary payload together with theHayabusa2 asteroid landing probe. After separation from the carrier rocket, PROCYON was left on aheliocentric orbit. On 22 February 2015, the ion engine was started, with the intention of adjusting the orbit so that an Earth flyby in December 2015 would direct the probe towards asteroid2000 DP107.[3] Initial results were favourable - the engine delivered 330 μN of thrust rather than the designed 250 μN - but the engine failed on 10 March and could not be restarted; PROCYON flew past Earth on 3 December 2015, but was unable to make a controlled orbit change. Shortly after the Earth flyby, contact with the spacecraft was lost.[4]

The 70 kg spacecraft had aspecific impulse of 1000 seconds, for adelta-v budget of about 500 m/s; the intention was to use 20% of thexenon propellant for the initial orbit correction, and the rest of the propellant between the Earth flyby and the asteroid flyby to ensure a controlled flyby distance of 30 km.[5]

A novel subsystem tested by PROCYON involved feeding both the main ion engine and the eight attitude controlcold-gas thrusters from the same tank (containing 2.5 kg of xenon at launch)

Instruments

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  • Small telescope for near-asteroid navigation and data acquisition.
  • Lyman-alpha imaging camera to observegeocorona[6]

Science results

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PROCYON observed theLyman-alpha emission of comet67P/Churyumov–Gerasimenko to determine its overall coma structure.[7] PROCYON captured the first complete image of thegeocorona, confirming for the first time that it has north–south symmetry.[8]

See also

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References

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  1. ^abプロキオン:小惑星への接近観測断念.Mainichi Shimbun. 8 May 2015. Archived fromthe original on 18 May 2015. Retrieved8 May 2015.
  2. ^超小型探査機「PROCYON」 二重小惑星を目指して航行中 [Very Small Probe PROCYON Cruising Toward a Binary Asteroid].Space Elevator News. 7 April 2015. Archived fromthe original on 16 March 2017. Retrieved7 April 2015.
  3. ^"Low-thrust trajectory design and operations of PROCYON, the first deep-space micro spacecraft"(PDF).
  4. ^"On the situation of ultra small deep space explorer "PROCYON (Proquion)"".ISAS (Institute of Space and Astronautical Science). Retrieved23 March 2018.
  5. ^"50kg- class Deep Space Exploration Technology Demonstration Micro-spacecraft PROCYON". digitalcommons.edu.
  6. ^PROCYON development team.超小型深宇宙探査機 PROCYON(プロキオン)(PDF) (in Japanese). Archived fromthe original(PDF) on 24 September 2015. Retrieved14 May 2015.
  7. ^"Micro spacecraft investigates cometary water mystery". National Astronomical Observatory of Japan. 24 January 2017. Retrieved26 January 2017.
  8. ^Kameda, S.; Ikezawa, S.; Sato, M.; Kuwabara, M.; Osada, N.; Murakami, G.; Yoshioka, K.; Yoshikawa, I.; Taguchi, M.; Funase, R.; Sugita, S.; Miyoshi, Y.; Fujimoto, M. (9 November 2017)."Ecliptic North-South Symmetry of Hydrogen Geocorona".Geophysical Research Letters.44 (23): 11,706–11, 712.Bibcode:2017GeoRL..4411706K.doi:10.1002/2017GL075915.

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