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2531 Cambridge

From Wikipedia, the free encyclopedia
Main-belt asteroid

2531 Cambridge
Discovery[1]
Discovered byE. Bowell
Discovery siteAnderson Mesa Stn.
Discovery date11 June 1980
Designations
(2531) Cambridge
Named after
Cambridge (UK) andCambridge, MA (USA)[2]
1980 LD · 1931 AP
1942 EQ · 1952 BG
1963 FK · 1963 HD
1971 VY · 1974 KH
A916 FE
main-belt · (outer)
Eos[3][4]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc86.40 yr (31,557 days)
Aphelion3.1787AU
Perihelion2.8383 AU
3.0085 AU
Eccentricity0.0566
5.22yr (1,906 days)
199.25°
0° 11m 20.04s / day
Inclination11.032°
104.36°
32.390°
Physical characteristics
19.15±1.9 km[5]
19.15 km(derived)[3]
22.349±0.196 km[6]
22.911±0.130 km[7]
23.44±0.95 km[8]
8.80±0.01h[9]
12.200±0.0032 h[10]
0.147±0.014[8]
0.1491±0.0193[7]
0.166±0.026[6]
0.2102(derived)[3]
0.2104±0.050[5]
S(assumed)[3]
10.712±0.001(R)[1][3][5][7][8][10]

2531 Cambridge, provisional designation1980 LD, is a stony Eoanasteroid from the outer regions of theasteroid belt, approximately 20 kilometers in diameter. It was discovered on 11 June 1980, by American astronomerEdward Bowell at Lowell'sAnderson Mesa Station in Arizona, United States. The asteroid was named for the "centers of learning in England and in Massachusetts".[2]

Classification and orbit

[edit]

Cambridge is a member of theEos family (606),[3][4] the largestasteroid family in theouter main belt consisting of nearly 10,000 known asteroids.[11]: 23  It orbits the Sun 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]

It was first identified asA916 FESimeiz Observatory in 1916. The body'sobservation arc begins with aprecovery taken atLowell Observatory in 1931, or 49 years prior to its official discovery observation at Anderson Mesa.[2]

Physical characteristics

[edit]

Cambridge is an assumed stonyS-type asteroid,[3] in line with the overallspectral type for members of the Eos family.[11]: 23 

Rotation period

[edit]

In February 2004, a rotationallightcurve ofCambridge was obtained from photometric observations by French amateur astronomerRené Roy. Lightcurve analysis gave arotation period of 8.80 hours with a brightness variation of 0.21magnitude (U=2-).[9] In October 2010, observations at thePalomar Transient Factory, California, gave a longer period of 12.200 hours with an amplitude of 0.20 magnitude (U=2).[10]

Diameter and albedo

[edit]

According to the surveys carried out by the Infrared Astronomical SatelliteIRAS, the JapaneseAkari satellite, and NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission,Cambridge measures between 19.15 and 23.44 kilometers in diameter and its surface has analbedo between 0.147 and 0.2104.[5][6][7][8]

TheCollaborative Asteroid Lightcurve Link derives an albedo of 0.2102 and a diameter of 19.15 kilometers with anabsolute magnitude of 10.9, identical with the results obtained by IRAS.[3][5]

Naming

[edit]

Thisminor planet was named after theUniversity of Cambridge in England and the universities in the city ofCambridge, Massachusetts (United States), where theMinor Planet Center (MPC) is located at the Smithsonian Astrophysical Observatory.[2] The approved naming citation was published by the MPC on 8 April 1982 (M.P.C. 6834).[12]

References

[edit]
  1. ^abcd"JPL Small-Body Database Browser: 2531 Cambridge (1980 LD)" (2017-06-05 last obs.).Jet Propulsion Laboratory. Retrieved18 June 2017.
  2. ^abcd"2531 Cambridge (1980 LD)".Minor Planet Center. Retrieved18 June 2017.
  3. ^abcdefgh"LCDB Data for (2531) Cambridge". Asteroid Lightcurve Database (LCDB). Retrieved18 June 2017.
  4. ^ab"Asteroid 2531 Cambridge – Nesvorny HCM Asteroid Families V3.0".Small Bodies Data Ferret. Retrieved26 October 2019.
  5. ^abcdeTedesco, E. F.; Noah, P. V.; Noah, M.; Price, S. D. (October 2004)."IRAS Minor Planet Survey V6.0".NASA Planetary Data System.12: IRAS-A-FPA-3-RDR-IMPS-V6.0.Bibcode:2004PDSS...12.....T. Retrieved22 October 2019.
  6. ^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.
  7. ^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.
  8. ^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)
  9. ^abBehrend, Raoul."Asteroids and comets rotation curves – (2531) Cambridge".Geneva Observatory. Retrieved18 June 2017.
  10. ^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.
  11. ^abNesvorný, 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.
  12. ^"MPC/MPO/MPS Archive".Minor Planet Center. Retrieved18 June 2017.

External links

[edit]
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