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3281 Maupertuis

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3281 Maupertuis
Shape model ofMaupertuis from itslightcurve
Discovery [1]
Discovered byY. Väisälä
Discovery siteTurku Obs.
Discovery date24 February 1938
Designations
(3281) Maupertuis
Named after
Pierre Louis Maupertuis[1]
(French mathematician)
1938 DZ · 1961 TP
1970 AP · 1979 TV
main-belt[1][2] · (inner)
Vesta[3] · Flora[4]
Orbital characteristics[2]
Epoch 23 March 2018 (JD 2458200.5)
Uncertainty parameter 0
Observation arc86.03yr (31,422 d)
Aphelion2.5798AU
Perihelion2.1203 AU
2.3501 AU
Eccentricity0.0978
3.60 yr (1,316 d)
20.991°
0° 16m 24.96s / day
Inclination5.9904°
348.46°
240.52°
Physical characteristics
5.482±0.043 km[5]
5.680±0.031 km[6]
7.14 km(calculated)[4]
6.7295±0.0001 h[7][a]
6.72984±0.00001 h[8]
0.24(assumed)[4]
0.4611±0.0450[6]
0.489±0.020[5]
S(assumed)[4]
V(possibly)
12.7[6]
12.9[2][4]
13.11±0.45[9]

3281 Maupertuis (prov. designation:1938 DZ) is a brightVesta asteroid from the inner regions of theasteroid belt. It was discovered on 24 February 1938, by Finnish astronomerYrjö Väisälä at theTurku Observatory in southwest Finland.[1] The likely elongatedV-type asteroid has arotation period of 6.7 hours and measures approximately 5.5 kilometers (3.4 miles) in diameter.[4] It was named after Frenchgeodesist and mathematicianPierre Louis Maupertuis.[1]

Orbit and classification

[edit]

Maupertuis is a member of theVesta family (401),[3] a giantasteroid family of typically brightV-type asteroids. Vestian asteroids have a composition akin to cumulateeucrites (HED meteorites) and are thought to have originated deep within4 Vesta's crust, possibly from theRheasilvia crater, a largeimpact crater on its southern hemisphere near the South pole, formed as a result of a sub-catastrophic collision. Vesta is the main belt'ssecond-largest andsecond-most-massive body afterCeres.[10][11] Based on osculating Keplerianorbital elements, the asteroid has also been classified as a member of theFlora family (402), a giantasteroid family and the largest family of stony asteroids in the main-belt.[4]

It orbits the Sun in theinner asteroid belt at a distance of 2.1–2.6 AU once every 3 years and 7 months (1,316 days;semi-major axis of 2.35 AU). Its orbit has aneccentricity of 0.10 and aninclination of 6° with respect to theecliptic.[2] The body'sobservation arc begins with aprecovery taken at theLowell Observatory in March 1931, or nearly 7 years prior to its official discovery observation at Turku.[1]

Naming

[edit]

Thisminor planet was named after Frenchgeodesist and mathematicianPierre Louis Maupertuis (1698–1759), who was a member of theFrench Academy of Sciences and chief of theFrench Geodesic Mission to the Tornio river valley in Lapland, Finland, to conducted thedegree measurement of the meridian (1736–1737), which determined that the Earth is oblate rather than prolate(seespheroid), as proposed by his rivalJacques Cassini.[1] Thenaming was published by theMinor Planet Center on 27 June 1991 (M.P.C. 18451).[12] The lunar craterMaupertuis was also named in his honor.

Physical characteristics

[edit]

Maupertuis is an assumed stonyS-type asteroid.[4] Based on its high albedo(see below), and its membership to the Vesta family, it is possibly aV-type asteroid.

Rotation period and poles

[edit]

In March 2010, a rotationallightcurve ofMaupertuis was obtained fromphotometric observations by French amateur astronomerRené Roy. Lightcurve analysis gave a well-definedrotation period of 6.7295 hours with an exceptionally high brightness amplitude of 1.22magnitude (U=3), indicative of a strongly elongated shape.[7][a]

In March 2016, a second period was published based on data from the Lowell Photometric Database. Using lightcurve inversion and convex shape models, as well as distributed computing power and the help of individual volunteers, a sidereal period of6.25033±0.00001 hours was derived from the database's sparse-in-time photometry data. Twospin axes at (62.0°, −66.0°) and (231.0°, −74.0°) inecliptic coordinates (λ, β) were also determined.[8]

Diameter and albedo

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According to the survey carried out by theNEOWISE mission of NASA'sWide-field Infrared Survey Explorer,Maupertuis measures between 5.482 and 5.680 kilometers in diameter and its surface has analbedo between 0.4611 and 0.489.[5][6] TheCollaborative Asteroid Lightcurve Link assumes it to be a Florian asteroid and uses a lower albedo of 0.24 – derived from8 Flora, the family'sparent body – and consequently calculates a somewhat larger diameter of 7.14 kilometers based on anabsolute magnitude of 12.9.[4]

Notes

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  1. ^abPolar luster diagram of (3281) Maupertuis (diagramme polaire de l'éclat). Summary figures for at theAsteroids and comets rotation curves, CdR, Raoul Behrend, Geneva Observatory.

References

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  1. ^abcdefg"3281 Maupertuis (1938 DZ)".Minor Planet Center. Retrieved14 May 2018.
  2. ^abcd"JPL Small-Body Database Browser: 3281 Maupertuis (1938 DZ)" (2017-03-31 last obs.).Jet Propulsion Laboratory. Retrieved14 May 2018.
  3. ^ab"Asteroid 3281 Maupertuis – Nesvorny HCM Asteroid Families V3.0".Small Bodies Data Ferret. Retrieved26 October 2019.
  4. ^abcdefghi"LCDB Data for (3281) Maupertuis". Asteroid Lightcurve Database (LCDB). Retrieved14 May 2018.
  5. ^abcMasiero, Joseph R.; Grav, T.; Mainzer, A. K.; Nugent, C. R.; Bauer, J. M.; Stevenson, R.; et al. (August 2014). "Main-belt Asteroids with WISE/NEOWISE: Near-infrared Albedos".The Astrophysical Journal.791 (2): 11.arXiv:1406.6645.Bibcode:2014ApJ...791..121M.doi:10.1088/0004-637X/791/2/121.S2CID 119293330.
  6. ^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.S2CID 35447010. (catalog)
  7. ^abBehrend, Raoul."Asteroids and comets rotation curves – (3281) Maupertuis". Geneva Observatory. Retrieved14 May 2018.
  8. ^abDurech, J.; Hanus, J.; Oszkiewicz, D.; Vanco, R. (March 2016). "Asteroid models from the Lowell photometric database".Astronomy and Astrophysics.587: 6.arXiv:1601.02909.Bibcode:2016A&A...587A..48D.doi:10.1051/0004-6361/201527573.S2CID 118427201.
  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.S2CID 53493339.
  10. ^Nesvorný, D.; Broz, M.; Carruba, V. (December 2014). "Identification and Dynamical Properties of Asteroid Families".Asteroids IV. pp. 297–321.arXiv:1502.01628.Bibcode:2015aste.book..297N.doi:10.2458/azu_uapress_9780816532131-ch016.ISBN 9780816532131.S2CID 119280014.
  11. ^Kelley, Michael S.; Vilas, Faith; Gaffey, Michael J.; Abell, Paul A. (September 2003)."Quantified mineralogical evidence for a common origin of 1929 Kollaa with 4 Vesta and the HED meteorites".Icarus.165 (1):215–218.Bibcode:2003Icar..165..215K.doi:10.1016/S0019-1035(03)00149-0.
  12. ^"MPC/MPO/MPS Archive".Minor Planet Center. Retrieved14 May 2018.

External links

[edit]
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