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(6178) 1986 DA

From Wikipedia, the free encyclopedia
Asteroid

(6178) 1986 DA
Discovery[1]
Discovered byM. Kizawa
Discovery siteShizuoka Obs.
Discovery date16 February 1986
Designations
(6178) 1986 DA
1986 DA
Amor · NEO[2]
Orbital characteristics[1]
Epoch 4 September 2017 (JD 2458000.5)
Uncertainty parameter 0
Observation arc38.03 yr (13,890 days)
Aphelion4.4648AU
Perihelion1.1805 AU
2.8226 AU
Eccentricity0.5818
4.74yr (1,732 days)
233.20°
0° 12m 28.08s / day
Inclination4.3056°
64.643°
127.36°
Earth MOID0.1922 AU · 74.9LD
Jupiter MOID0.5212 AU
Physical characteristics
2.3 km(dated)[1]
3.149 km[3]
3.15 km(taken)[4]
3.199±0.207 km[5]
3.50h[6][a]
3.51 h[7]
0.0778[3]
0.15[1]
0.161±0.034[5]
M[4][8]
B–V = 0.677[1]
U–B = 0.267[1]
15.1[1][5] · 15.40±0.1(R)[a] · 15.9±0.112[3][4] · 16.11[7]

(6178) 1986 DA is a metallicasteroid, classified asnear-Earth object of theAmor group, approximately 3 kilometers in diameter. It was discovered on 16 February 1986, by Japanese astronomerMinoru Kizawa at Shizuoka Observatory, Japan.[2]

1986 DA was the first near Earth asteroid thought to be of metallic composition, with high radar brightness; with that it was predicted to have 100 thousand tons of platinum group metals including gold and suggested as a resource for future space colonists.[9]

Orbit and classification

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As an eccentric Amor asteroid has an Earthminimum orbit intersection distance of 0.1922 AU (28,800,000 km) and approaches the orbit of Earth from the outside but does not cross it. It crosses however the orbit of Mars and can be classified as aMars-crosser and also approaches the orbit of Jupiter within 0.5 AU.[1] The asteroid orbits the Sun at a distance of 1.2–4.5 AU once every 4 years and 9 months (1,732 days). Its orbit has aneccentricity of 0.58 and aninclination of 4° with respect to theecliptic.[1] The firstprecovery was taken atSiding Spring Observatory in 1977, extending the asteroid'sobservation arc by 9 years prior to its discovery.[2]

Physical characteristics

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The metallicM-type asteroid is notable for being significantly moreradar-reflective than otherasteroids. Radar measurements suggest it is composed ofnickel andiron and that it was derived from the center of a much larger object that experienced melting and differentiation. The observed radaralbedo was 0.58 and the optical albedo was 0.14.[8]

Rotation and shape

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It was most probably formed from a larger body through a catastrophic collision with another object. Radar measurements of this body indicate that the surface is relatively smooth on scales of less than a meter, but it is highly irregular on scales of 10–100 meters.[citation needed] Severallightcurve analysis gave it a concurringrotation period of 3.50 to 3.51 hours with a relatively high brightness amplitude between 0.03 and 0.48 inmagnitude, indicating an irregular shape (U=3/3/n.a.).[6][7][a]

Diameter and albedo

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According to the survey carried out by NASA'sWide-field Infrared Survey Explorer with its subsequentNEOWISE mission, the asteroid has an albedo of 0.08 and 0.16, and a diameter of 3.1 to 3.2 kilometers, respectively.[3][5] TheCollaborative Asteroid Lightcurve Link selects 3.15 kilometers as best result, while the first estimate from 1994 gave a diameter of 2.3 kilometers.[1]

Mining considerations

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The asteroid achieved its most notable recognition when scientists revealed that it contained over "10,000 tons of gold and 100,000 tons ofplatinum", or an approximate value at the time of its discovery of "$90 billion for the gold and a cool trillion dollars for the platinum, plus loose change for the asteroid's 10 billion tons of iron and a billion tons of nickel."[10] In 2024 the estimated value of 100,000 tons of platinum was worth approximately 3.4 trillion US dollars. Thedelta-v for a spacecraft rendezvous with this asteroid fromlow Earth orbit is 7.1 km/s.[11]

Notes

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  1. ^abcPravec (1999) web: rotation period3.50 hours with a brightness amplitude of0.3 mag. H = 15.4. No LCDB quality code assigned. No lightcurve published (note: "N"). Summary figures atCollaborative Asteroid Lightcurve Link (CALL) for (6178) andPravec, P.; Wolf, M.; Sarounova, L. (1999)

See also

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References

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  1. ^abcdefghij"JPL Small-Body Database Browser: 6178 (1986 DA)" (2015-07-28 last obs.).Jet Propulsion Laboratory. Retrieved26 May 2017.
  2. ^abc"6178 (1986 DA)".Minor Planet Center. Retrieved26 May 2016.
  3. ^abcdPravec, 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.
  4. ^abc"LCDB Data for (6178)". Asteroid Lightcurve Database (LCDB). Retrieved26 May 2016.
  5. ^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 118700974.
  6. ^abZeigler, K. W. (March 1990). "Photoelectric Photometry of Asteroids 81 Terpsichore, 381 Myrrha, and 1986 DA".The Minor Planet Bulletin.17: 1.Bibcode:1990MPBu...17....1Z.
  7. ^abcWisniewski, W. Z. (June 1987). "Photometry of six radar target asteroids".Icarus.70 (3):566–572.Bibcode:1987Icar...70..566W.doi:10.1016/0019-1035(87)90096-0.ISSN 0019-1035.
  8. ^abOstro, S. J.; Rosema, K. D.; Campbell, D. B.; Chandler, J. F.; Hine, A. A.; Hudson, R. S. (June 1991). "Asteroid 1986 DA - Radar evidence for a metallic composition".Science.252 (5011): 1399–1404.NASA–supportedresearch.(SciHomepage).Bibcode:1991Sci...252.1399O.doi:10.1126/science.252.5011.1399.hdl:2060/19920003664.ISSN 0036-8075.PMID 17772910.S2CID 2510757.
  9. ^"Near-Earth Metal Asteroid Discovered".NASA/JPL. Retrieved30 October 2018.
  10. ^Ostro, Steven J.; Campbell, D. B.; Chandler, J. F.; Hine, A. A.; Hudson, R. S.; Rosema, K. D.; et al. (October 1991). "Asteroid 1986 DA: Radar evidence for a metallic composition".In NASA.252 (5011):1399–1704.Bibcode:1991plas.rept..174O.doi:10.1126/science.252.5011.1399.hdl:2060/19920003664.PMID 17772910.S2CID 2510757.
  11. ^"Delta-v for spacecraft rendezvous with all known near-Earth asteroids". NASA. 1 June 2006. Archived fromthe original on 3 June 2001. Retrieved8 June 2006.

External links

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