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1167 Dubiago

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1167 Dubiago
Discovery[1]
Discovered byE. F. Skvortsov
Discovery siteSimeiz Obs.
Discovery date3 August 1930
Designations
(1167) Dubiago
Named after
Alexander Dubyago
(also spelled:Dubiago)[2]
1930 PB · 1931 VJ1
1938 WW · 1950 QX
A924 RF
main-belt · (outer)[3]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc86.71 yr (31,671 days)
Aphelion3.6517AU
Perihelion3.1772 AU
3.4145 AU
Eccentricity0.0695
6.31yr (2,305 days)
314.09°
0° 9m 22.32s / day
Inclination5.7477°
223.39°
71.344°
Physical characteristics
Dimensions63.12±5.6 km(IRAS:17)[4]
75.79±0.90 km[5]
14.3h[6]
34.8374±0.0990 h[7]
0.036±0.001[5]
0.0509±0.010(IRAS:17)[4]
Tholen =D[1] · D[3]
B–V = 0.743[1]
U–B = 0.196[1]
9.51±0.29[8] · 9.513±0.001(R)[7] · 9.85[1][3][4][5]

1167 Dubiago, provisional designation1930 PB, is a darkasteroid from the outer region of theasteroid belt, approximately 63 kilometers in diameter. It was discovered on 3 August 1930, by Soviet astronomerEvgenii Skvortsov atSimeiz Observatory on the Crimean peninsula, and named after astronomerAlexander Dubyago.[9][2]

Classification and orbit

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Dubiago orbits the Sun in theouter main-belt at a distance of 3.2–3.7 AU once every 6 years and 4 months (2,305 days). Its orbit has aneccentricity of 0.07 and aninclination of 6° with respect to theecliptic.[1] In 1924, it was first identified asA924 RF at the discovering observatory. The body'sobservation arc begins atYerkes Observatory about two months after its official discovery at Simeiz.[9]

Physical characteristics

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In theTholen classification,Dubiago is aD-type asteroid, a group of 46 known bodies, mostly beingJupiter trojans andcentaurs such as10199 Chariklo and624 Hektor.[10] It is thought that the Martian moonPhobos has a similar composition, and that theTagish Lake meteorite origins from a D-type asteroid.

Lightcurves

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In March 1990, a rotationallightcurve ofDubiago was obtained using theNordic Optical Telescope at theLa Palma site on the Canary Islands. Lightcurve analysis gave arotation period of 14.3 hours with a brightness variation of 0.23magnitude (U=2).[6] A second lightcurve was obtained in the R-band at thePalomar Transient Factory in October 2013, giving an alternative period solution of 34.8374 hours with an amplitude of 0.21 magnitude (U=2).[7]

Diameter and albedo

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According to the surveys carried out by the Infrared Astronomical SatelliteIRAS and the JapaneseAkari satellite,Dubiago measures 63.12 and 75.79 kilometers in diameter, and its surface has analbedo of 0.051 and 0.036, respectively.[4][5] TheCollaborative Asteroid Lightcurve Link adopts the results obtained by IRAS with anabsolute magnitude of 9.85.[3]

Naming

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Thisminor planet was named in honor ofAlexander Dubyago (1903–1959), a renowned astronomer of the Soviet Union. The lunar craterDubyago is also named in his and his father's honour.[2] The approved naming was suggested by the RussianInstitute of Theoretical Astronomy (ITA) and the officialnaming citation was published by theMinor Planet Center on 1 June 1967 (M.P.C. 2740).[11]

References

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  1. ^abcdefg"JPL Small-Body Database Browser: 1167 Dubiago (1930 PB)" (2017-07-05 last obs.).Jet Propulsion Laboratory. Retrieved26 July 2017.
  2. ^abcSchmadel, Lutz D. (2007). "(1167) Dubiago".Dictionary of Minor Planet Names – (1167) Dubiago.Springer Berlin Heidelberg. p. 98.doi:10.1007/978-3-540-29925-7_1168.ISBN 978-3-540-00238-3.
  3. ^abcd"LCDB Data for (1167) Dubiago". Asteroid Lightcurve Database (LCDB). Retrieved1 February 2017.
  4. ^abcdTedesco, E. F.; Noah, P. V.; Noah, M.; Price, S. D. (October 2004)."IRAS Minor Planet Survey V6.0".NASA Planetary Data System – IRAS-A-FPA-3-RDR-IMPS-V6.0.Bibcode:2004PDSS...12.....T. Retrieved17 October 2019.
  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. ^abDahlgren, M.; Lagerkvist, C.-I.; Fitzsimmons, A.; Williams, I. P. (May 1991)."Differential CCD photometry of Dubiago, Chiron and Hektor".Monthly Notices of the Royal Astronomical Society.250:115–118.Bibcode:1991MNRAS.250..115D.doi:10.1093/mnras/250.1.115.ISSN 0035-8711. Retrieved1 February 2017.
  7. ^abcWaszczak, Adam; Chang, Chan-Kao; Ofek, Eran O.; Laher, Russ; Masci, Frank; Levitan, David; et al. (September 2015)."Asteroid Light Curves from the Palomar Transient Factory Survey: Rotation Periods and Phase Functions from Sparse Photometry".The Astronomical Journal.150 (3): 35.arXiv:1504.04041.Bibcode:2015AJ....150...75W.doi:10.1088/0004-6256/150/3/75. Retrieved1 February 2017.
  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. Retrieved1 February 2017.
  9. ^ab"1167 Dubiago (1930 PB)".Minor Planet Center. Retrieved1 February 2017.
  10. ^"JPL Small-Body Database Search: list of D-type minor planets (Tholen/SMASSII)". Jet Propulsion Laboratory. Retrieved5 November 2015.
  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]
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