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5026 Martes

From Wikipedia, the free encyclopedia
Asteroid

5026 Martes
Shape model ofMartes from itslightcurve
Discovery[1]
Discovered byA. Mrkos
Discovery siteKleť Obs.
Discovery date22 August 1987
Designations
(5026) Martes
Pronunciation/ˈmɑːrtɪs/
Named after
pine marten
beech marten
(Mustelidae mammals)[2]
1987 QL1 · 1965 QE
1976 QL · 1980 VA2
main-belt · (inner)[3]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc63.37 yr (23,145 days)
Aphelion2.9540AU
Perihelion1.8020 AU
2.3780 AU
Eccentricity0.2422
3.67yr (1,339 days)
75.131°
0° 16m 7.68s / day
Inclination4.2831°
304.77°
17.652°
Physical characteristics
4.93 km(calculated)[3]
8.967±2.335 km[4]
4.423±0.0011 h[5]
4.424087±0.000002 h[6]
4.4243±0.005h[7]
0.066±0.072[4]
0.20(assumed)[3]
B–V =0.863±0.042[8]
V–R =0.440±0.047[8]
C[9] · S[3]
13.80[4] · 13.9[1][3] · 14.065±0.010(R)[5] · 14.17±0.36[9]

5026 Martes (prov. designation:1987 QL1) is a carbonaceousasteroid from theinner region of theasteroid belt, approximately 9 kilometers (6 miles) in diameter. It was discovered on 22 August 1987, by Czech astronomerAntonín Mrkos atKleť Observatory in the Czech Republic.[10] It is named after the two weasel-like animal species:pine marten andbeech marten.[2]

Orbit and classification

[edit]

Martes is the namesake member of a small asteroid family, named theMartes family.[citation needed] It orbits the Sun in theinner main-belt at a distance of 1.8–3.0 AU once every 3 years and 8 months (1,339 days). Its orbit has aneccentricity of 0.24 and aninclination of 4° with respect to theecliptic.[1]

A firstprecovery was taken atPalomar Observatory in 1953, extending the body'sobservation arc by 34 years prior to its official discovery observation at Klet.[10]

Naming

[edit]

Thisminor planet was named for the two species of the family Mustelidae, thepine marten andbeech marten. They also live in the forests near the discoveringKleť Observatory.[2] The official naming citation was published by theMinor Planet Center on 22 June 1999 (M.P.C. 34920).[11]

Physical characteristics

[edit]

Martes has been characterized as a carbonaceousC-type asteroid byPanSTARRS' photometric survey.[9]

Asteroid pair

[edit]

Martes forms an asteroid pair with2005 WW113, and was part of the 35 sample asteroid pairs inPetr Pravec's studyFormation of asteroid pairs by rotational fission, published in the journalNature.[7]

Lightcurves

[edit]

Between 2008 and 2010, several rotationallightcurves ofMartes were obtained from photometric observations. Lightcurve analysis gave a well-definedrotation period of 4.4243 hours with a brightness amplitude of 0.69magnitude (U=3-/3/2+/3/2).[3][7][6][5]

Diameter and albedo

[edit]

According to the survey carried out by NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission,Martes measures 8.967 kilometers in diameter and its surface has analbedo of 0.066, which is typical for carbonaceous asteroids.[4] TheCollaborative Asteroid Lightcurve Link, however, assumes a standard albedo for stony asteroids of 0.20 and consequently calculates a much smaller diameter of 4.93 kilometers, due to the higher albedo.[3]

References

[edit]
  1. ^abcd"JPL Small-Body Database Browser: 5026 Martes (1987 QL1)" (2016-08-27 last obs.).Jet Propulsion Laboratory. Retrieved20 June 2017.
  2. ^abcSchmadel, Lutz D. (2007). "(5026) Martes".Dictionary of Minor Planet Names.Springer Berlin Heidelberg. p. 432.doi:10.1007/978-3-540-29925-7_4893.ISBN 978-3-540-00238-3.
  3. ^abcdefg"LCDB Data for (5026) Martes". Asteroid Lightcurve Database (LCDB). Retrieved28 March 2017.
  4. ^abcdNugent, C. R.; Mainzer, A.; Masiero, J.; Bauer, J.; Cutri, R. M.; Grav, T.; et al. (December 2015)."NEOWISE Reactivation Mission Year One: Preliminary Asteroid Diameters and Albedos".The Astrophysical Journal.814 (2): 13.arXiv:1509.02522.Bibcode:2015ApJ...814..117N.doi:10.1088/0004-637X/814/2/117. Retrieved28 March 2017.
  5. ^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. Retrieved28 March 2017.
  6. ^abPolishook, D. (October 2014)."Spin axes and shape models of asteroid pairs: Fingerprints of YORP and a path to the density of rubble piles".Icarus.241:79–96.arXiv:1406.3359.Bibcode:2014Icar..241...79P.doi:10.1016/j.icarus.2014.06.018. Retrieved28 March 2017.
  7. ^abcPravec, P.; Vokrouhlický, D.; Polishook, D.; Scheeres, D. J.; Harris, A. W.; Galád, A.; et al. (August 2010)."Formation of asteroid pairs by rotational fission".Nature.466 (7310):1085–1088.arXiv:1009.2770.Bibcode:2010Natur.466.1085P.doi:10.1038/nature09315.PMID 20740010. Retrieved28 March 2017.
  8. ^abYe, Q.-z. (February 2011)."BVRI Photometry of 53 Unusual Asteroids".The Astronomical Journal.141 (2): 8.arXiv:1011.0133.Bibcode:2011AJ....141...32Y.doi:10.1088/0004-6256/141/2/32. Retrieved29 March 2017.
  9. ^abcVeres, 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. Retrieved28 March 2017.
  10. ^ab"5026 Martes (1987 QL1)".Minor Planet Center. Retrieved28 March 2017.
  11. ^"MPC/MPO/MPS Archive".Minor Planet Center. Retrieved28 March 2017.

External links

[edit]
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