3494 Purple Mountain

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3494 Purple Mountain
Discovery  [1]
Discovered by Purple Mountain Obs.
Discovery site Purple Mountain Obs.
Discovery date7 December 1980
Designations
(3494) Purple Mountain
Named after
 Purple Mountain Observatory   [1]
(Discovering observatory)
1980 XW ·1962 WV1
1969 UD ·1972 OA
main-belt   [1] [2]  ·(inner)
Vesta   [3] [4]  · Flora   [5]
Orbital characteristics   [2]
Epoch 23 March 2018 (JD 2458200.5)
Uncertainty parameter 0
Observation arc 66.38 yr (24,247 d)
Aphelion 2.6571 AU
Perihelion 2.0419 AU
2.3495 AU
Eccentricity 0.1309
3.60 yr (1,315 d)
237.24°
0° 16m 25.32s / day
Inclination 5.8320°
234.42°
72.646°
Physical characteristics
6.507±0.091  km [6] [7]
7.82 km (calculated) [5]
2.928±0.001  h (1⁄2-p.) [8]
5.857±0.001 h [9]
0.24(assumed) [5]
0.347±0.035 [6] [7]
V (SMASS-I Xu) [3]  · V   [4]
S (assumed) [5]
S/SV (SDSS-MOC) [10]
12.7 [2] [5] [7]

    3494 Purple Mountain, provisional designation 1980 XW, is a bright Vestian asteroid and a formerly lost minor planet from the inner regions of the asteroid belt, approximately 6.5 kilometers (4 miles) in diameter. First observed in 1962, it was officially discovered on 7 December 1980, by Chinese astronomers at the Purple Mountain Observatory in Nanking, China, and later named in honor of the discovering observatory. [1] The V-type asteroid has a rotation period of 5.9 hours. [5]

    Contents

    Orbit and classification

    Purple Mountain is a core member of the Vesta family ( 401 ), [3] a giant asteroid family of typically bright V-type asteroids. Vestian asteroids have a composition akin to cumulate eucrites (HED meteorites) and are thought to have originated deep within 4 Vesta's crust, possibly from the Rheasilvia crater, a large impact crater on its southern hemisphere near the South pole, formed as a result of a subcatastrophic collision. Vesta is the main belt's second-largest and second-most-massive body after Ceres. [11] [4] Based on osculating Keplerian orbital elements, the asteroid has also been classified as a member of the Flora family ( 402 ), a giant asteroid family and the largest family of stony asteroids in the main-belt. [5]

    Purple Mountain orbits the Sun in the inner asteroid belt at a distance of 2.0–2.7  AU once every 3 years and 7 months (1,315 days; semi-major axis of 2.35 AU). Its orbit has an eccentricity of 0.13 and an inclination of 6° with respect to the ecliptic. [2] The body's observation arc begins with a precovery taken at Palomar Observatory in December 1951, or 29 years prior to its official discovery observation. [1]

    Lost asteroid

    Purple Mountain has been a lost minor planet. In November 1962, Purple Mountain was observed as 1962 WV1 at Goethe Link Observatory. A total of three additional observations were taken at Crimea–Nauchnij in 1969 and 1972, when it was designated as 1969 UD and 1972 OA, respectively, but was subsequently lost with no follow-up observations until its official discovery at Nanking in 1980. [1]

    Physical characteristics

    Based on the Moving Object Catalog (MOC) of the Sloan Digital Sky Survey, Purple Mountain is a common, stony S-type asteroid, with a sequential best-type taxonomy of SV. [10] The Collaborative Asteroid Lightcurve Link (CALL) also assumes it to be a stony S-type. [5]

    In the SMASS-I classification by Xu, the asteroid is a V-type. This agrees with its measured high albedo (see below) often seen among the core members of the Vesta family. [11] : 23  In 2013, a spectroscopic analysis showed it to have a composition very similar to the cumulate eucrite meteorites, which also suggests that the basaltic asteroid has originated from the crust of 4 Vesta. [4]

    Rotation period

    In June 2015, a rotational lightcurve of Purple Mountain was obtained from photometric observations by astronomers at Texas A&M University, using the SARA-telescopes of the Southeastern Association for Research and Astronomy consortium. The 0.9-meter SARA-North telescope is located at Kitt Peak National Observatory, Arizona, while the 0.6-meter SARA-South telescope is hosted at the Cerro Tololo Inter-American Observatory in Chile. Lightcurve analysis gave a rotation period of 5.857 hours with a brightness variation of 0.32 magnitude ( U=3- ). [9] One month later, in July 2015, another period of 2.928 hours and an amplitude of 0.40 magnitude was measured at MIT's George R. Wallace Jr. Observatory ( U=2 ). [8] The results are in good agreement, apart from the fact that the latter is an alternative, monomodal solution with half the period of the former. CALL adopts the longer, bimodal period solution as the better result in its Lightcurve Data Base, due to the lightcurve's distinct amplitude and the small phase angle of the first observation. [5]

    Diameter and albedo

    According to the survey carried out by the NEOWISE mission of NASA's Wide-field Infrared Survey Explorer, Purple Mountain measures 6.507 kilometers in diameter and its surface has an albedo of 0.347, [6] [7] while CALL assumes an albedo of 0.24 – derived from the body's classification into the Flora family – and consequently calculates a larger diameter of 7.82 kilometers based on an absolute magnitude of 12.7. [5]

    Naming

    This minor planet was named in honor of the Purple Mountain Observatory (PMO), an astronomical observatory located in Nanking (Nanjing), China. Built in 1934, the observatory is known for its astrometric observations and for its numerous discoveries of small Solar System bodies. It has played an important role in developing modern Chinese astronomy. [1] The official naming citation was published by the Minor Planet Center on 29 November 1993 ( M.P.C. 22829). [12]

    Related Research Articles

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    <span class="mw-page-title-main">3281 Maupertuis</span>

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    <span class="mw-page-title-main">2590 Mourão</span>

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    2011 Veteraniya, provisional designation 1970 QB1, is a stony Vestian asteroid from the inner regions of the asteroid belt, approximately 6 kilometers in diameter. It was discovered on 30 August 1970, by Soviet astronomer Tamara Smirnova at the Crimean Astrophysical Observatory, Nauchnyj, on the Crimean peninsula, and named for the Soviet veterans of the Second World War.

    3703 Volkonskaya, provisional designation 1978 PU3, is a Vestian asteroid and asynchronous binary system from the inner regions of the asteroid belt, approximately 4 kilometers (2.5 miles) in diameter. It was discovered on 9 August 1978, by Soviet astronomers Lyudmila Chernykh and Nikolai Chernykh at the Crimean Astrophysical Observatory in Nauchnij, on the Crimean peninsula. It was named by the discoverers after the Russian princess Mariya Volkonskaya. The V-type asteroid has a rotation period of 3.2 hours. The discovery of its 1.4-kilometer minor-planet moon was announced in December 2005.

    6181 Bobweber, provisional designation 1986 RW, is a stony asteroid from the inner regions of the asteroid belt, approximately 5 kilometers in diameter. It was discovered on 6 September 1986, by American astronomer Eleanor Helin at the U.S. Palomar Observatory in California, and named after astronomer Robert Weber.

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    References

    1. 1 2 3 4 5 6 7 "3494 Purple Mountain (1980 XW)". Minor Planet Center. Retrieved 15 May 2018.
    2. 1 2 3 4 "JPL Small-Body Database Browser: 3494 Purple Mountain (1980 XW)" (2018-04-20 last obs.). Jet Propulsion Laboratory . Retrieved 15 May 2018.
    3. 1 2 3 "Asteroid 3494 Purple Mountain – Nesvorny HCM Asteroid Families V3.0". Small Bodies Data Ferret. Retrieved 26 October 2019.
    4. 1 2 3 4 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.
    5. 1 2 3 4 5 6 7 8 9 10 "LCDB Data for (3494) Purple Mountain". Asteroid Lightcurve Database (LCDB). Retrieved 15 May 2018.
    6. 1 2 3 Masiero, Joseph R.; Mainzer, A. K.; Grav, T.; Bauer, J. M.; Cutri, R. M.; Dailey, J.; et al. (November 2011). "Main Belt Asteroids with WISE/NEOWISE. I. Preliminary Albedos and Diameters". The Astrophysical Journal. 741 (2): 20. arXiv: 1109.4096 . Bibcode:2011ApJ...741...68M. doi:10.1088/0004-637X/741/2/68. S2CID   118745497.
    7. 1 2 3 4 Mainzer, 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)
    8. 1 2 Kosiarek, M.; Nisley, I.; Patra, K.; Hatano, R.; Bates, H.; Chavez, E.; et al. (July 2017). "Rotation Period of Asteroid 3494 Purple Mountain". The Minor Planet Bulletin. 44 (3): 171–172. Bibcode:2017MPBu...44..171K. ISSN   1052-8091.
    9. 1 2 Cantu, Sarah A.; Kozdon, Janus; Montgomery, Kent; Lyons, Vanessa (July 2016). "Lightcurves and Rotational Periods of Three Main-belt Asteroids". The Minor Planet Bulletin. 43 (3): 210–212. Bibcode:2016MPBu...43..210C. ISSN   1052-8091.
    10. 1 2 Carvano, J. M.; Hasselmann, P. H.; Lazzaro, D.; Mothé-Diniz, T. (February 2010). "SDSS-based taxonomic classification and orbital distribution of main belt asteroids". Astronomy and Astrophysics. 510: 12. Bibcode:2010A&A...510A..43C. doi: 10.1051/0004-6361/200913322 . Retrieved 30 October 2019. (PDS data set)
    11. 1 2 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.
    12. ↑ "MPC/MPO/MPS Archive". Minor Planet Center. Retrieved 15 May 2018.
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