3200 Phaethon Explained

Minorplanet:yes
Background:
  1. FFC2E0
3200 Phaethon
Discovered:October 11, 1983
Named After:Phaëthon
Mpc Name:(3200) Phaethon
Adjective:Phaethonian
Alt Names:1983 TB
Epoch:April 27, 2019 (JD 2458000.5)
Uncertainty:0
Observation Arc:12941days
Aphelion:2.4028AU
Perihelion:0.13998sigfig=3NaNsigfig=3
Time Periastron:May 15, 2022[1]
Semimajor:1.2714sigfig=3NaNsigfig=3
Eccentricity:0.88990
Period:523.6days
Avg Speed:19.9km/s
Inclination:22.260°
Asc Node:265.22°
Mean Anomaly:313.94°
Mean Motion:day
Arg Peri:322.19°
Moid:0.01955sigfig=3NaNsigfig=3
Jupiter Moid:2.7375sigfig=3NaNsigfig=3
Tisserand:4.510
Dimensions: × [2]
Mean Diameter:3.6miles
Rotation:3.604hours
Spectral Type:F-type asteroid
Abs Magnitude:14.6
Magnitude:10.7 (December 14, 2017)

3200 Phaethon (; previously sometimes spelled Phaeton), provisionally designated, is an active Apollo asteroid with an orbit that brings it closer to the Sun than any other named asteroid (though there are numerous unnamed asteroids with smaller perihelia, such as). For this reason, it was named after the Greek myth of Phaëthon, son of the sun god Helios. It is 3.6miles in diameter and is the parent body of the Geminids meteor shower of mid-December. With an observation arc of 35+ years, it has a very well determined orbit. The 2017 Earth approach distance of about 10 million km was known with an accuracy of ±700 m.

Discovery

Phaethon was the first asteroid to be discovered using images from a spacecraft. Simon F. Green and John K. Davies discovered it in images from October 11, 1983, while searching Infrared Astronomical Satellite (IRAS) data for moving objects. It was formally announced on October 14 in IAUC 3878 along with optical confirmation by Charles T. Kowal, who reported it to be asteroidal in appearance. Its provisional designation was, and it later received the numerical designation and name in 1985.

Orbital characteristics

Phaethon is categorized as an Apollo asteroid, as its orbital semi-major axis is greater than that of the Earth's at 1.27AU. It is also suspected to be a member of the Pallas family of asteroids.

Its most remarkable distinction is that it approaches the Sun closer than any other named asteroid: its perihelion is only 0.14sigfig=3NaNsigfig=3 - less than half of Mercury's perihelial distance. It is a Mercury-, Venus-, Earth-, and Mars-crosser as a result of its high orbital eccentricity. The surface temperature at perihelion could reach around 1025K.

Phaethon is a possible candidate for detecting general relativistic and/or solar oblateness effects in its orbital motion due to the frequent close approaches to the Sun. The Apollo asteroids (155140) 2005 UD and (225416) 1999 YC share similar orbits with Phaethon, suggesting a possible common breakup origin.[3]

Potentially hazardous asteroid

Phaethon is categorized as a potentially hazardous asteroid (PHA), but that does not mean there is a near-term threat of an impact. It is a potentially hazardous asteroid merely as a result of its size (absolute magnitude) and Earth minimum orbit intersection distance). The Earth minimum orbit intersection distance (E-MOID) is, which is defined by the shortest distance between the orbit of Phaethon and the orbit of Earth. With a 30+ year observation arc, the orbit of Phaethon is very well understood with very small uncertainties. Close approaches of Phaethon are well constrained for the next 400 years.

Physical characteristics

Phaethon is an asteroid with fairly unusual characteristics in that its orbit more closely resembles that of a comet than an asteroid; it has been referred to as a "rock comet". In studies performed by NASA's STEREO spacecraft in 2009 and 2012, rapid brightening and dust tail have been observed.[4] [5] It is possible that the Sun's heat is causing fractures similar to mudcracks in a dry lake bed. This occurs because Phaethon's orbit takes it closer to the Sun than any other named asteroid (0.14 AU at perihelion) causing extreme heating and enough solar radiation pressure to push any separated pieces off the asteroid's surface. Since its discovery, several other objects were found exhibiting mixed cometary and asteroidal features, such as 133P/Elst–Pizarro, leading to a new class of objects dubbed "active asteroids".[6]

In 2018, observations revealed that Phaethon was blue in color. This is extremely rare, as most asteroids tend to be grey or red.[7] [8] In 2020, polarimetric study revealed Phaethon has a surface with steep slopes covered by a mix of regolith with larger pebbles.[9] Phaethon's composition fits the notion of its cometary origin; it is classified as a F-type asteroid because it is composed of dark material or a B-type asteroid because of its blue color. In 2022 it was shown [10] how Phaethon's blue color and its rock-comet-like emission activity can be explained by the effects of the intense solar heating at perihelion causing sublimation of any darkish-red refractory organic, nano-phase iron (nFe0), and pyroxene materials on its surface.

Analysis of a mid-infrared spectral emissivity spectrum from the Spitzer Space Telescope showed Phaethon to be linked to the rare Yamato-type (CY) carbonaceous chondrites.[11] Further analysis of this spectrum confirmed the presence of Mg-rich olivine, carbonates, and Fe-sulfides. These minerals decompose at the temperatures that Phaethon reaches at perihelion, resulting in outgassing, in a process called thermal decomposition. It is believed that this process leads to dust ejection and can explain the formation of the Geminid meteor stream.

Meteor shower

Shortly after its discovery, Fred Whipple observed that the "orbital elements of 1983 TB shown on IAUC 3879 are virtually coincident with the mean orbital elements of 19 Geminid meteors photographed with the super-Schmidt meteor cameras". In other words, Phaethon is the long-sought parent body of the Geminids meteor shower of mid-December.

Planned flyby

DESTINY+ (Demonstration and Experiment of Space Technology for INterplanetary voYage Phaethon fLyby dUSt science) is a planned mission to fly by 3200 Phaethon, as well as various minor bodies originating from it. The spacecraft is being developed by the Japanese space agency JAXA, and will demonstrate advanced technologies for future deep space exploration. DESTINY+ is planned to be launched no earlier than 2024.[12]

Close approaches

Phaethon approached to 0.120895abbr=onNaNabbr=on of Earth on December 10, 2007, and was detected by radar at Arecibo. When Phaethon came to perihelion in July 2009, it was found to be brighter than expected. During its approach, the STEREO-A spacecraft detected an unexpected brightening, roughly by a factor of two.

2010 approach

2017 approach

On December 16, 2017, at 23:00 UT, Phaethon passed 0.06893169AU from Earth (27 lunar distances). The Earth approach distance was known with a 3-sigma precision of ±700 m. This was the best opportunity to date for radar observations by Goldstone and Arecibo, with a resolution of 75m (246feet).

The asteroid was bright enough to see in small telescopes, peaking at magnitude 10.8 between December 13–15 while dimming slightly to magnitude 11 on December 16 at closest approach. Arecibo made observations of Phaethon from December 15–19.[13] It will not make an Earth approach closer than the 2017 passage until December 14, 2093, when it will pass 0.01981AU from Earth.

External links

Notes and References

  1. http://ssd.jpl.nasa.gov/horizons.cgi?find_body=1&body_group=sb&sstr=3200 JPL Horizons
  2. Web site: (3200) Phaethon 2021 Oct 3. Hayamizu Astro Laboratory. 3 October 2021. 14 February 2022.
  3. Cukier . W. Z. . Szalay . J. R. . June 1, 2023 . Formation, Structure, and Detectability of the Geminids Meteoroid Stream . The Planetary Science Journal . 4 . 6 . 109 . 10.3847/psj/acd538 . 2632-3338 . 2306.11151 . 2023PSJ.....4..109C . free .
  4. Recurrent Perihelion Activity in (3200) Phaethon. Jing. Li. David. Jewitt. 2013. Astronomical Journal. 145 . 6 . 154 . 10.1088/0004-6256/145/6/154. 1304.1430. 2013AJ....145..154L . 6242944 . 2022-01-22.
  5. Activity in Geminid Parent (3200) Phaethon. David. Jewitt. Jing. Li. 2010. Astronomical Journal. 140 . 5 . 1519–1527 . 10.1088/0004-6256/140/5/1519 . 1009.2710. 2010AJ....140.1519J . 6446528 . 2022-01-22.
  6. Book: The Active Asteroids. David. Jewitt. Henry. Hsieh. Jessica. Agarwal. 2015. Asteroids IV. 221–241. Michel. P. . others. 1 . University of Arizona. 10.2458/azu_uapress_9780816532131-ch012 . 1502.02361. 2015aste.book..221J . 9780816532131. 119209764. 2020-01-30.
  7. Web site: Rare blue asteroid sometimes behaves like a comet. Eleanor Imster. EarthSky. November 1, 2018. April 6, 2019.
  8. Web site: A look at 3200 Phaethon: A big, bizarre, blue asteroid we plan to visit. Eric Mack. CNET. October 23, 2018. April 6, 2019.
  9. 2001.00789. Golubeva. L. F.. Polarimetric properties of asteroid 3200 Phaethon. Shestopalov. D. I.. Kvaratskhelia. O. I.. astro-ph.EP. 2020.
  10. http://space.com/asteroid-phaethon-blue-because-of-sunlight How the bluest asteroid in the solar system got its color
  11. MacLennan . Eric . Granvik . Mikael . Thermal decomposition as the activity driver of near-Earth asteroid (3200) Phaethon . Nature Astronomy . 2 November 2023 . 10.1038/s41550-023-02091-w. 2207.08968 .
  12. Web site: 宇宙科学ミッション打上げ計画について. Kuninaka. Hitoshi. PDF. JAXA. 19 May 2020. 2020-09-28. ja.
  13. Web site: Arecibo Radar Returns with Asteroid Phaethon Images . NASA . D. C. . Agle . Dwayne . Brown . Suraiya . Farukhi . December 22, 2017 . January 8, 2018.