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1957 Angara

From Wikipedia, the free encyclopedia
Main-belt asteroid

1957 Angara
Modelled shape ofAngara from itslightcurve
Discovery[1]
Discovered byL. Chernykh
Discovery siteCrimean Astrophysical Obs.
Discovery date1 April 1970
Designations
(1957) Angara
Named after
Angara River
(Siberian river)[2]
1970 GF · 1962 WG1
1969 AA
main-belt · Eos[3]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc60.58 yr (22,126 days)
Aphelion3.1828AU
Perihelion2.8338 AU
3.0083 AU
Eccentricity0.0580
5.22yr (1,906 days)
345.36°
0° 11m 20.04s / day
Inclination11.191°
50.702°
209.03°
Physical characteristics
Dimensions17.907±0.108 km[4]
18.189±0.229 km[5]
18.38 km(derived)[3]
21.44±0.70 km[6]
30.41±0.58 km[7]
3.67 h[8]
0.055±0.006[7]
0.111±0.008[6]
0.14(assumed)[3]
0.1438±0.0310[5]
S[3][8]
B–V = 0.900[1]
U–B = 0.380[1]
11.16±0.34[9] · 11.36[1][6][7] · 11.43[3][5][8]

1957 Angara (prov. designation:1970 GF) is a stonyEos asteroid from the outer regions of theasteroid belt, approximately 18 kilometers (11 miles) in diameter. It was discovered on 1 April 1970, by Soviet astronomerLyudmila Chernykh at theCrimean Astrophysical Observatory in Nauchnyj, and named after the SiberianAngara River.[2][10]

Classification and orbit

[edit]

Angara is a member of theEos family, well known for mostly being of asilicaceous composition. It orbits the Sun in theouter main-belt at a distance of 2.8–3.2 AU once every 5 years and 3 months (1,906 days). Its orbit has aneccentricity of 0.06 and aninclination of 11° with respect to theecliptic.[1] A firstprecovery was taken atGoethe Link Observatory in 1956, extending the body'sobservation arc by 14 years prior to its official discovery observation at Nauchnyj.[10]

Naming

[edit]

Thisminor planet was named for the over 1000-mile long SiberianAngara River that drainsLake Baikal.[2] The officialnaming citation was published by theMinor Planet Center on 30 June 1977 (M.P.C. 4190).[11]

Physical characteristics

[edit]

In December 1983, a rotationallightcurve ofAngara was obtained from photometric observations by American astronomerRichard Binzel. Lightcurve analysis gave a well-definerotation period of 3.67 hours with a brightness amplitude of 0.52magnitude, indicative of a non-spheroidal shape (U=3).[8] Binzel also classified the body as a stonyS-type asteroid.[8]

According to the surveys carried out by the JapaneseAkari satellite and NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission,Angara measures between 17.907 and 30.41 kilometers in diameter and its surface has analbedo between 0.055 and 0.1438.[4][5][6][7] TheCollaborative Asteroid Lightcurve Link assumes a standard albedo for stony Eoan asteroids of 0.14 – taken from the family's largest member and namesake,221 Eos – and derives a diameter of 18.38 kilometers with anabsolute magnitude of 11.43.[3]

References

[edit]
  1. ^abcdef"JPL Small-Body Database Browser: 1957 Angara (1970 GF)" (2017-06-02 last obs.).Jet Propulsion Laboratory. Retrieved2 July 2017.
  2. ^abcSchmadel, Lutz D. (2007). "(1957) Angara".Dictionary of Minor Planet Names.Springer Berlin Heidelberg. p. 157.doi:10.1007/978-3-540-29925-7_1958.ISBN 978-3-540-00238-3.
  3. ^abcdef"LCDB Data for (1957) Angara". Asteroid Lightcurve Database (LCDB). Retrieved4 April 2017.
  4. ^abMasiero, Joseph R.; Mainzer, A. K.; Grav, T.; Bauer, J. M.; Cutri, R. M.; Dailey, J.; et al. (November 2011)."Main Belt Asteroids with WISE/NEOWISE. I. Preliminary Albedos and Diameters".The Astrophysical Journal.741 (2): 20.arXiv:1109.4096.Bibcode:2011ApJ...741...68M.doi:10.1088/0004-637X/741/2/68. Retrieved4 April 2017.
  5. ^abcdMainzer, A.; Grav, T.; Masiero, J.; Hand, E.; Bauer, J.; Tholen, D.; et al. (November 2011). "NEOWISE Studies of Spectrophotometrically Classified Asteroids: Preliminary Results".The Astrophysical Journal.741 (2): 25.arXiv:1109.6407.Bibcode:2011ApJ...741...90M.doi:10.1088/0004-637X/741/2/90.
  6. ^abcdUsui, Fumihiko; Kuroda, Daisuke; Müller, Thomas G.; Hasegawa, Sunao; Ishiguro, Masateru; Ootsubo, Takafumi; et al. (October 2011)."Asteroid Catalog Using Akari: AKARI/IRC Mid-Infrared Asteroid Survey".Publications of the Astronomical Society of Japan.63 (5):1117–1138.Bibcode:2011PASJ...63.1117U.doi:10.1093/pasj/63.5.1117. (online,AcuA catalog p. 153)
  7. ^abcdMasiero, Joseph R.; Mainzer, A. K.; Grav, T.; Bauer, J. M.; Cutri, R. M.; Nugent, C.; et al. (November 2012)."Preliminary Analysis of WISE/NEOWISE 3-Band Cryogenic and Post-cryogenic Observations of Main Belt Asteroids".The Astrophysical Journal Letters.759 (1): 5.arXiv:1209.5794.Bibcode:2012ApJ...759L...8M.doi:10.1088/2041-8205/759/1/L8. Retrieved4 April 2017.
  8. ^abcdeBinzel, R. P. (October 1987)."A photoelectric survey of 130 asteroids".Icarus.72 (1):135–208.Bibcode:1987Icar...72..135B.doi:10.1016/0019-1035(87)90125-4.ISSN 0019-1035. Retrieved4 April 2017.
  9. ^Veres, Peter; Jedicke, Robert; Fitzsimmons, Alan; Denneau, Larry; Granvik, Mikael; Bolin, Bryce; et al. (November 2015)."Absolute magnitudes and slope parameters for 250,000 asteroids observed by Pan-STARRS PS1 - Preliminary results".Icarus.261:34–47.arXiv:1506.00762.Bibcode:2015Icar..261...34V.doi:10.1016/j.icarus.2015.08.007. Retrieved4 April 2017.
  10. ^ab"1957 Angara (1970 GF)".Minor Planet Center. Retrieved4 April 2017.
  11. ^Schmadel, Lutz D. (2009). "Appendix – Publication Dates of the MPCs".Dictionary of Minor Planet Names – Addendum to Fifth Edition (2006–2008). Springer Berlin Heidelberg. p. 221.doi:10.1007/978-3-642-01965-4.ISBN 978-3-642-01964-7.

External links

[edit]
Minor planets
Asteroid
Distant minor planet
Comets
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Authority control databasesEdit this at Wikidata
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