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4082 Swann

From Wikipedia, the free encyclopedia
Asteroid within the Asteroid Belt

4082 Swann
Discovery[1]
Discovered byC. Shoemaker
Discovery sitePalomar Obs.
Discovery date27 September 1984
Designations
(4082) Swann
Named after
Gordon Swann
(American geologist)[2]
1984 SW3 · 1947 UF
1969 PE
main-belt · (inner)[3]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc69.54 yr (25,399 days)
Aphelion3.0076AU
Perihelion1.7721 AU
2.3899 AU
Eccentricity0.2585
3.69yr (1,349 days)
317.29°
0° 16m 0.48s / day
Inclination9.5978°
294.36°
100.28°
Physical characteristics
Dimensions5.85 km(derived)[3]
9.535±0.066 km[4]
11.06±0.29 km[5]
4.03632±0.00009h[a]
4.1±0.1 h[6]
0.029±0.012[4]
0.101±0.006[5]
0.20(assumed)[3]
SMASS = Ch[1] · C[3]
12.90[5] · 13.08±0.2(R)[a] · 13.4[1] · 13.46±0.206[3][7] · 13.58±0.27[8] · 14.55[4]

4082 Swann, provisional designation1984 SW3, is a carbonaceousasteroid from the inner regions of theasteroid belt, approximately 10 kilometers in diameter.

The asteroid was discovered on 27 September 1984, by American astronomerCarolyn Shoemaker atPalomar Observatory in California, United States, and later named for American geologistGordon Swann.[2][9]

Orbit and classification

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Swann orbits the Sun in theinner main-belt at a distance of 1.8–3.0 AU once every 3 years and 8 months (1,349 days). Its orbit has aneccentricity of 0.26 and aninclination of 10° with respect to theecliptic.[1] First identified as1947UF at the FinnishTurku Observatory in 1947,Swann'sobservation arc was extended by 37 years prior to its official discovery observation at Palomar.[9]

Physical characteristics

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TheC-type asteroid is classified as a Ch-subtype in theSMASS taxonomy.[1]

Diameter and albedo

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According to the surveys carried out by the JapaneseAkari satellite and NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission,Swann measures 9.5 and 11.1 kilometers in diameter and its surface has analbedo of 0.029 and 0.101, respectively.[4][5] TheCollaborative Asteroid Lightcurve Link, however, assumes a standard albedo for stony asteroids of 0.20 and derives a much smaller diameter of 5.85 kilometers, based on an absolutemagnitude of 13.46.[3]

Rotation period

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In July 2006, a rotationallightcurve ofSwann was obtained from photometric observations byPetr Pravec at theOndřejov Observatory in the Czech Republic. It gave arotation period of4.03632±0.00009 hours with a brightness variation of 0.67 magnitude (U=3).[a] A second lightcurve obtained by Jean-Gabriel Bosch in September 2006, gave a period of4.1±0.1 hours and an amplitude of 0.35 magnitude (U=2).[6]

Naming

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Thisminor planet was named after American geologistGordon A. Swann (born 1931). He served as the principal investigator of the "Apollo Lunar Geologic Experiment" conducted at the lunar landing sites ofApollo 14 andApollo 15.[2] The official naming citation was published by theMinor Planet Center on 12 December 1989 (M.P.C. 15576).[10]

Notes

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  1. ^abcPravec (2006) web: rotation period of4.03632±0.00009 hours with a brightness amplitude of0.67 mag. Summary figures for (4082) Swann atCollaborative Asteroid Lightcurve Link (CALL) andPravec, P.; Wolf, M.; Sarounova, L. (2006)

References

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  1. ^abcdef"JPL Small-Body Database Browser: 4082 Swann (1984 SW3)" (5 May 2017 last obs.).Jet Propulsion Laboratory. Retrieved19 June 2017.
  2. ^abcSchmadel, Lutz D. (2007). "(4082) Swann".Dictionary of Minor Planet Names – (4082) Swann.Springer Berlin Heidelberg. p. 348.doi:10.1007/978-3-540-29925-7_4060.ISBN 978-3-540-00238-3.
  3. ^abcdef"LCDB Data for (4082) Swann". Asteroid Lightcurve Database (LCDB). Retrieved30 October 2016.
  4. ^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. Retrieved30 October 2016.
  5. ^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)
  6. ^abBehrend, Raoul."Asteroids and comets rotation curves – (4082) Swann".Geneva Observatory. Retrieved30 October 2016.
  7. ^Pravec, Petr; Harris, Alan W.; Kusnirák, Peter; Galád, Adrián; Hornoch, Kamil (September 2012)."Absolute magnitudes of asteroids and a revision of asteroid albedo estimates from WISE thermal observations".Icarus.221 (1):365–387.Bibcode:2012Icar..221..365P.doi:10.1016/j.icarus.2012.07.026. Retrieved17 December 2015.
  8. ^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. Retrieved30 October 2016.
  9. ^ab"4082 Swann (1984 SW3)". Minor Planet Center. Retrieved30 October 2016.
  10. ^"MPC/MPO/MPS Archive". Minor Planet Center. Retrieved30 October 2016.

External links

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