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(10302) 1989 ML

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(10302) 1989 ML
1989 ML photographed by the Canada–France–Hawaii Telescope in December 2015
Discovery[1]
Discovered byE. F. Helin, J. Alu
Discovery sitePalomar Observatory, United States
Discovery date29 June 1989
Designations
MPO 244277, 1992 WA
Orbital characteristics[2]
Epoch 24 October 2005 (JD 2453667.5)
Uncertainty parameter 0
Observation arc12250 days (33.54 yr)
Aphelion1.4472 AU (216.50 Gm)
Perihelion1.0985 AU (164.33 Gm)
1.2728 AU (190.41 Gm)
Eccentricity0.1370
1.436 yr (524.518 d)
26.28 km/s
125.941°
0° 41m 11.911s / day
Inclination4.379°
104.409°
183.283°
Earth MOID0.08233 AU
Physical characteristics
Dimensions0.276±0.037 km[3]
19.228 h (0.8012 d)[4]
0.37±0.15[3]
X-type[5]: 142 
E-type[3]
19.45 (JPL)[2]

(10302) 1989 ML is an unnamed near-Earth asteroid. It is relatively small, estimated to be around 300 metres (980 ft) in diameter. An Amor asteroid, it orbits between Earth and Mars. It is an X-type asteroid, so its precise surface composition is yet unknown, though telescopic observations indicate it may be relatively enriched in iron. It was discovered by Eleanor F. Helin and Jeff T. Alu at Palomar Observatory on 29 June 1989. 1989 ML was the former backup target for Japan's Hayabusa mission, but launch delays meant that the rendezvous had to be cancelled.

Orbit

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A diagram of 1989 ML's orbit, with the orbits of the inner planets shown.

1989 ML is classified as a near-Earth object (NEO) and an Amor asteroid,[1] meaning that its orbit never crosses the Earth's.[6]: 489  It has a semi-major axis of 1.273 astronomical units (AU), completing an orbit around the Sun every 1.436 years (524.518 days). It has a moderately elliptical orbit with an orbital eccentricity of 0.137, with its distance from the Sun varying from 1.0985 AU to 1.273 AU. 1989 ML has a relatively low orbital inclination of 4.379° with respect to the ecliptic plane.[2] Its proximity to Earth means that 1989 ML's orbit is strongly perturbed and chaotic; the Lyapunov time of its orbit is roughly 1,000 years.[7]

Physical characteristics

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In 2007, a team of astronomers led by Michael Mueller used observations from the Spitzer Space Telescope to estimate 1989 ML's physical properties. Adopting an absolute magnitude value of 19.5±0.3, Mueller et al. derived a diameter of 0.246 ± 0.037 kilometres (0.153 ± 0.023 mi).[3] Analysis of 1989 ML's lightcurve, or fluctuations in its observed brightness, indicate that it rotates once every 19.228 hours and has a tumbling rotation.[4] The high amplitude of its lightcurve implies that it may be very elongated, with its longest axis being at least 2.2 times longer than its intermediate axis.[8]

Spectrum and surface

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Spectroscopic observations conducted by Palomar Observatory in 1999 revealed that 1989 ML has a relatively flat (or neutral) spectrum. As a result, a definitive interpretation of its surface composition could not be made, though its spectrum was noted to resemble dark, impact-shocked chondrites.[5]: 144  Due to its neutral spectrum, 1989 ML was classified as an Xc-type asteroid under the Bus classification scheme, suggesting that it belongs to the E-type, M-type, or P-type classifications under the Tholen classification scheme.[3][9]: 31  These asteroid types are spectrally degenerate, meaning that they can only be distinguished from each other by albedo.[10] E-type asteroids have relatively high geometric albedos of 0.3–0.6; M-type asteroids have moderate albedos of 0.1–0.2; and P-type asteroids have dark albedos below 0.1, appearing to be rich in organic compounds.[3]

Mueller et al. estimated 1989 ML's geometric albedo to be 0.37±0.15, suggesting an E-type classification and ruling out a P-type classification. 1989 ML's optical and near-infrared colors were additionally compared to other asteroids, demonstrating that they differed from the color data of M-type and P-type asteroids. They also differed from the colors of the E-type asteroids 64 Angelina and 3103 Eger, but agreed with the color of 44 Nysa, another E-type asteroid. Nysa-type spectra are consistent with silicate mineralogy enriched in iron, whilst Angelina-type spectra are consistent with silicates containing sulfides, indicating that 1989 ML is relatively enriched in iron.[3]

Exploration

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1989 ML is an attractive target for spacecraft exploration due to its relative accessibility from Earth. It was considered as a backup target of JAXA's sample-return mission Hayabusa (then MUSES-C), with the primary target being 4660 Nereus. However, both targets had to be given up due to launch delays.[5]: 140, 143  Hayabusa would instead go on to rendezvous with 25143 Itokawa in 2005.[11] 1989 ML was also considered by the European Space Agency as a candidate target for the Don Quijote mission concept to study the effects of impacting a spacecraft into an asteroid; however, they too changed to other targets.[12]

See also

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References

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  1. ^ a b "(10302) = 1989 ML = 1992 WA". Minor Planet Center. Retrieved 4 June 2015.
  2. ^ a b c "10302 (1989 ML)". JPL Small-Body Database. NASA/Jet Propulsion Laboratory. Retrieved 31 March 2025.
  3. ^ a b c d e f g Mueller, Michael; Harris, Alan W.; Fitzsimmons, Alan (April 2007). "Size, albedo, and taxonomic type of potential spacecraft target Asteroid (10302) 1989 ML" (PDF). Icarus. 187 (2): 611–615. Bibcode:2007Icar..187..611M. doi:10.1016/j.icarus.2007.01.002.
  4. ^ a b Warner, Brian D.; Stephens, Robert D. (October 2022). "Near-Earth Asteroid Lightcurve Analysis at the Center for Solar System Studies: 2022 March-June". Bulletin of the Minor Planets Section of the Association of Lunar and Planetary Observers. 49 (4): 274–279. Bibcode:2022MPBu...49..274W.
  5. ^ a b c Binzel, Richard P.; Harris, Alan W.; Bus, Schelte J.; Burbine, Thomas H. (June 2001). "Spectral Properties of Near-Earth Objects: Palomar and IRTF Results for 48 Objects Including Spacecraft Targets (9969) Braille and (10302) 1989 ML". Icarus. 151 (2): 139–149. Bibcode:2001Icar..151..139B. doi:10.1006/icar.2001.6613.
  6. ^ Fernández, Y. R.; Li, J. -Y.; Howell, E. S.; Woodney, L. M. (17 April 2015). "Asteroids and Comets". In Schubert, Gerald (ed.). Treatise on Geophysics (2nd ed.). Elsevier. pp. 487–528. ISBN 978-0-444-53803-1.
  7. ^ Yoshikawa, M.; Froeschlé, Ch.; Michel, P. (2000). "Orbital Evolution of Two Near-Earth Asteroids: Nereus and 1989 ML". Advances in Space Research. 25 (2): 273–276. Bibcode:2000AdSpR..25..273Y. doi:10.1016/S0273-1177(99)00937-0.
  8. ^ Abe, M.; Sato, I.; Araki, H. (2000). "Lightcurve and Color of Near-Earth-Asteroid 1989ML". Advances in Space Research. 25 (2): 269–272. Bibcode:2000AdSpR..25..269A. doi:10.1016/S0273-1177(99)00938-2.
  9. ^ DeMeo, F. E.; Alexander, C. M. O'D.; Walsh, K. J.; Chapman, C. R.; Binzel, R. P. (2015). "The Compositional Structure of the Asteroid Belt" (PDF). In Michel, Patrick; DeMeo, Francesca E.; Bottke, William F. (eds.). Asteroids IV. University of Arizona Press, Tucson. pp. 13–41. arXiv:1506.04805. Bibcode:2015aste.book...13D. doi:10.2458/azu_uapress_9780816532131-ch002. ISBN 978-0-816-53213-1.
  10. ^ Tholen, D.J.; Barucci, M.A. (1989). "Asteroid taxonomy". In Binzel, Richard P.; Gehrels, Tom; Matthews, Mildred Shapley (eds.). Asteroids II. University of Arizona Press. pp. 298–315. ISBN 0-8165-1123-3.
  11. ^ Fujiwara, A.; et al. (June 2006). "The Rubble-Pile Asteroid Itokawa as Observed by Hayabusa". Science. 312 (5778): 1330–1334. Bibcode:2006Sci...312.1330F. doi:10.1126/science.1125841. PMID 16741107.
  12. ^ "Sancho Study: Designing the Minimum Earth Escape Spacecraft". European Space Agency. 23 May 2012. Archived from the original on 17 October 2011. Retrieved 5 November 2009.
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