9 Metis

Last updated

9 Metis
9 Metis VLT (2021), deconvolved.pdf
Discovery
Discovered by A. Graham
Discovery date25 April 1848
Designations
(9) Metis
Pronunciation /ˈmtɪs/ [1]
Named after
Mētis
1974 QU2
Main belt
Adjectives Metidian /mɛˈtɪdiən/
Symbol Metis symbol (bold).svg (historical)
Orbital characteristics [2]
Epoch 13 September 2023
(JD  2453300.5)
Aphelion 2.68  AU (401 million  km)
Perihelion 2.093 AU (313.1 million km)
2.387 AU (357.1 million km)
Eccentricity 0.1231
3.69 yr (1346.74 d)
345.43°
Inclination 5.577°
68.87°
6 November 2023
5.75°
Earth  MOID 1.1 AU (160 million km)
Proper orbital elements [3]
2.3864354  AU
Proper eccentricity
0.1271833
Proper inclination
4.6853629°
Proper mean motion
97.638314  deg  / yr
3.68708 yr
(1346.705 d)
Precession of perihelion
38.754973  arcsec  / yr
Precession of the ascending node
−41.998090  arcsec  / yr
Physical characteristics
Dimensionsc/a = 0.61±0.05 [4]
(222×182×130) ±12 km [5]
Mean diameter
173±2 km [4]
190±? km (Dunham) [2]
Mass (8.0±1.9)×1018 kg [4]
(11.3±2.2)×1018 kg [lower-alpha 1] [5]
Mean density
2.94±0.70 g/cm3 [4]
4.12±1.17 g/cm3 [5]
0.2116 d (5.079 h) [2]
0.18 [4]
0.118 [2]
Temperature max: 282 K (+9 °C) [6]
S [7]
8.1 [8] to 11.83
6.28 [2]
0.23" to 0.071"

    Metis (minor planet designation: 9 Metis) is one of the larger main-belt asteroids. It is composed of silicates and metallic nickel-iron, and may be the core remnant of a large asteroid that was destroyed by an ancient collision. [9] Metis is estimated to contain just under half a percent of the total mass of the asteroid belt. [10]

    Contents

    Metis passed within 0.034AU, or 5,000,000 kilometres (3,100,000 mi), of Vesta on 19 August 2004. [11]

    Discovery and naming

    The first 10 asteroids profiled against Earth's Moon. 9 Metis is second from right. Moon and Asteroids 1 to 10.svg
    The first 10 asteroids profiled against Earth's Moon. 9 Metis is second from right.

    Metis was discovered by Andrew Graham on 25 April 1848, at Markree Observatory in Ireland; it was his only asteroid discovery. [12] It also has been the only asteroid to have been discovered as a result of observations from Ireland until 7 October 2008, when, 160 years later, Dave McDonald from observatory J65 discovered (281507) 2008 TM9. [13] Its name comes from the mythological Metis, a Titaness and Oceanid, daughter of Tethys and Oceanus. [14] The name Thetis was also considered and rejected (it would later devolve to 17 Thetis).

    The historical symbol for Metis was an eye with a star above it. It is in the pipeline for Unicode 17.0 as U+1CEC3 𜻃 ( Metis symbol (fixed width).svg ). [15] [16]

    Characteristics

    Lightcurve-based 3D-model of Metis 9Metis (Lightcurve Inversion).png
    Lightcurve-based 3D-model of Metis

    Metis' direction of rotation is unknown at present, due to ambiguous data. Lightcurve analysis indicates that the Metidian pole points towards either ecliptic coordinates (β, λ) = (23°, 181°) or (9°, 359°) with a 10° uncertainty. [17] The equivalent equatorial coordinates are (α, δ) = (12.7 h, 21°) or (23.7 h, 8°). This gives an axial tilt of 72° or 76°, respectively.[ citation needed ]

    Hubble Space Telescope images [18] [19] and lightcurve analyses [17] are in agreement that Metis has an irregular elongated shape with one pointed and one broad end. [17] [19] Radar observations suggest the presence of a significant flat area, [20] in agreement with the shape model from lightcurves.

    The Metidian surface composition has been estimated as 30–40% metal-bearing olivine and 60–70% Ni-Fe metal. [9]

    Light curve data on Metis led to an assumption that it could have a satellite. However, subsequent observations failed to confirm this. [21] [22] Later searches with the Hubble Space Telescope in 1993 found no satellites. [19]

    Family relationships

    Metis was once considered to be a member of an asteroid family known as the Metis family, [23] but more recent searches for prominent families did not recognize any such group, nor is a clump evident in the vicinity of Metis by visual inspection of proper orbital element diagrams.

    However, a spectroscopic analysis found strong spectral similarities between Metis and 113 Amalthea, and it is suggested that these asteroids may be remnants of a very old (at least ~1 Ga) dynamical family whose smaller members have been pulverised by collisions or perturbed away from the vicinity. The putative parent body is estimated to have been 300 to 600 km in diameter (Vesta-sized) and differentiated. [9] Metis would be the relatively intact core remnant (though smaller than 16 Psyche), and Amalthea a fragment of the mantle, with 90% of the original body unaccounted for. [9] Coincidentally, both Metis and Amalthea have namesakes among Jupiter's inner moons.

    Occultations

    In 1984 an occultation of a star produced seven chords that Kristensen used to derive an ellipsoidal profile of 210×170 km. [24] On 6 August 1989, Metis occulted a magnitude 8.7 star producing five chords suggesting a diameter of 173.5 km. [24] Observations of an occultation on 11 February 2006, produced only two chords indicating a minimum diameter 156 km. [25] All three of these occultations fit the ellipsoid 222×182×130 km suggested by Baer. [10]

    On 7 March 2014, Metis occulted the star HIP 78193 (magnitude 7.9) over parts of Europe and the Middle East. [26] [27]

    See also

    Notes

    1. 5.7 ± 1.1) × 10−12M

    Related Research Articles

    <span class="mw-page-title-main">3 Juno</span> Asteroid in the asteroid belt

    3 Juno is a large asteroid in the asteroid belt. Juno was the third asteroid discovered, in 1804, by German astronomer Karl Harding. It is one of the twenty largest asteroids and one of the two largest stony (S-type) asteroids, along with 15 Eunomia. It is estimated to contain 1% of the total mass of the asteroid belt.

    <span class="mw-page-title-main">6 Hebe</span> Large main-belt asteroid

    Hebe is a large main-belt asteroid, containing around 0.5% of the mass of the belt. However, due to its apparently high bulk density, Hebe does not rank among the top twenty asteroids by volume. This high bulk density suggests an extremely solid body that has not been impacted by collisions, which is not typical of asteroids of its size – they tend to be loosely-bound rubble piles.

    <span class="mw-page-title-main">7 Iris</span> Large main-belt asteroid

    Iris is a large main-belt asteroid and possible remnant planetesimal orbiting the Sun between Mars and Jupiter. It is the fourth-brightest object in the asteroid belt. 7 Iris is classified as an S-type asteroid, meaning that it has a stony composition.

    <span class="mw-page-title-main">8 Flora</span> Large main-belt asteroid

    Flora is a large, bright main-belt asteroid. It is the innermost large asteroid: no asteroid closer to the Sun has a diameter above 25 kilometres, and not until 20-km 149 Medusa was discovered was an asteroid known to orbit at a closer mean distance. It is the seventh-brightest asteroid with a mean opposition magnitude of +8.7. Flora can reach a magnitude of +8.1 at a favorable opposition near perihelion, such as occurred in November 2020 when it was 0.88 AU from Earth.

    <span class="mw-page-title-main">11 Parthenope</span> Main-belt asteroid

    Parthenope is a large, bright main-belt asteroid.

    <span class="mw-page-title-main">13 Egeria</span> Main-belt asteroid

    Egeria is a large main-belt G-type asteroid. It was discovered by Annibale de Gasparis on November 2, 1850. Egeria was named by Urbain Le Verrier, whose computations led to the discovery of Neptune, after the mythological nymph Egeria of Aricia, Italy, the wife of Numa Pompilius, second king of Rome.

    <span class="mw-page-title-main">14 Irene</span> Main-belt asteroid

    Irene is a large main-belt asteroid, discovered by the English astronomer John Russell Hind on May 19, 1851. It is orbiting the Sun at a distance of 2.585 AU with a period of 4.16 yr and an eccentricity of 0.168. The orbital plane is tilted at an angle of 9.1° to the plane of the ecliptic.

    <span class="mw-page-title-main">15 Eunomia</span> Main-belt asteroid

    Eunomia is a very large asteroid in the middle asteroid belt. It is the largest of the stony (S-type) asteroids, with 3 Juno as a close second. It is quite a massive asteroid, in 6th to 8th place. It is the largest Eunomian asteroid, and is estimated to contain 1% of the mass of the asteroid belt.

    <span class="mw-page-title-main">17 Thetis</span> Main-belt asteroid

    Thetis, minor planet designation 17 Thetis, is a stony asteroid from the inner regions of the asteroid belt, approximately 90 kilometers in diameter. It was discovered on 17 April 1852, by German astronomer Robert Luther at Bilk Observatory in Düsseldorf, Germany who deferred to Friedrich Wilhelm August Argelander the naming his first asteroid discovery after Thetis from Greek mythology. Its historical symbol was a dolphin and a star; it is in the pipeline for Unicode 17.0 as U+1CECA 𜻊.

    <span class="mw-page-title-main">18 Melpomene</span> Main-belt asteroid

    Melpomene is a large, bright main-belt asteroid that was discovered by J. R. Hind on 24 June 1852, and named after Melpomenē, the Muse of tragedy in Greek mythology. Its historical symbol was a dagger over a star; it is in the pipeline for Unicode 17.0 as U+1CECB 𜻋.

    <span class="mw-page-title-main">19 Fortuna</span> Main-belt asteroid

    Fortuna is one of the largest main-belt asteroids. It has a composition similar to 1 Ceres: a darkly colored surface that is heavily space-weathered with the composition of primitive organic compounds, including tholins.

    <span class="mw-page-title-main">29 Amphitrite</span> Main-belt asteroid

    Amphitrite is one of the largest S-type asteroids, approximately 200 kilometers in diameter, and probably fifth largest after Eunomia, Juno, Iris and Herculina.

    <span class="mw-page-title-main">41 Daphne</span> Main-belt asteroid

    Daphne is a large asteroid from the asteroid belt. It is a dark-surfaced body 174 km in diameter is probably composed of primitive carbonaceous chondrites. The spectra of the asteroid displays evidence of aqueous alteration. It was discovered by H. Goldschmidt on May 22, 1856, and named after Daphne, the nymph in Greek mythology who was turned into a laurel tree. Incorrect orbital calculations initially resulted in 56 Melete being mistaken for a second sighting of Daphne. Daphne was not sighted again until August 31, 1862.

    <span class="mw-page-title-main">88 Thisbe</span> Main-belt asteroid

    Thisbe, minor planet designation 88 Thisbe, is the 13th largest main-belt asteroid. It was discovered by C. H. F. Peters on June 15, 1866, and named after Thisbe, heroine of a Roman fable. This asteroid is orbiting the Sun at a distance of 2.768 AU with a period of 4.60 years and an orbital eccentricity (ovalness) of 0.165. The orbital plane is inclined at an angle of 5.219° to the ecliptic.

    <span class="mw-page-title-main">95 Arethusa</span> Main-belt asteroid

    Arethusa is a large main-belt asteroid. It was discovered by German astronomer Robert Luther on 23 November 1867, and named after one of the various Arethusas in Greek mythology. Arethusa has been observed occulting a star three times: first on 2 February 1998, and twice in January 2003.

    <span class="mw-page-title-main">113 Amalthea</span> Main-belt asteroid

    113 Amalthea is a stony Florian asteroid and binary system from the inner regions of the asteroid belt, approximately 50 kilometers in diameter. It was discovered on 12 March 1871, by German astronomer Robert Luther at the Bilk Observatory in Düsseldorf, Germany. The elongated S-type asteroid has a rotation period of 9.95 hours. It was named after Amalthea from Greek mythology. A purported satellite of Amalthea was announced in July 2017, but was later found to be a software error in July 2021.

    <span class="mw-page-title-main">230 Athamantis</span> Main-belt asteroid

    Athamantis is a fairly large main-belt asteroid that was discovered by the German-Austrian astronomer K. de Ball on September 3, 1882, in Bothkamp. It was his only asteroid discovery. The asteroid was named after Athamantis, daughter of Athamas the mythical Greek king of Orchomenus.

    <span class="mw-page-title-main">247 Eukrate</span> Main-belt asteroid

    Eukrate is a rather large main-belt asteroid. It is dark and probably a primitive carbonaceous body. The asteroid was discovered by Robert Luther on March 14, 1885, in Düsseldorf. It was named after Eucrate, a Nereid in Greek mythology.

    914 Palisana, provisional designation 1919 FN, is a Phocaean asteroid from the inner regions of the asteroid belt, approximately 77 kilometers in diameter. It was discovered by German astronomer Max Wolf at Heidelberg Observatory on 4 July 1919.

    <span class="mw-page-title-main">174567 Varda</span> Trans-Neptunian object

    174567 Varda (provisional designation 2003 MW12) is a binary trans-Neptunian planetoid of the resonant hot classical population of the Kuiper belt, located in the outermost region of the Solar System. Its moon, Ilmarë, was discovered in 2009.

    References

    1. Noah Webster (1884) A Practical Dictionary of the English Language
    2. 1 2 3 4 5 "JPL Small-Body Database Browser: 9 Metis" (last observation: 2023-08-13). Retrieved 18 September 2023.
    3. "AstDyS-2 Metis Synthetic Proper Orbital Elements". Department of Mathematics, University of Pisa, Italy. Retrieved 1 October 2011.
    4. 1 2 3 4 5 P. Vernazza et al. (2021) VLT/SPHERE imaging survey of the largest main-belt asteroids: Final results and synthesis. Astronomy & Astrophysics 54, A56
    5. 1 2 3 James Baer, Steven Chesley & Robert Matson (2011) "Astrometric masses of 26 asteroids and observations on asteroid porosity." The Astronomical Journal, Volume 141, Number 5
    6. L. F. Lim et al., Thermal infrared (8–13 μm) spectra of 29 asteroids: the Cornell Mid-Infrared Asteroid Spectroscopy (MIDAS) Survey, Icarus Vol. 173, p. 385 (2005).
    7. asteroid lightcurve data file (March 2001)
    8. Donald H. Menzel & Jay M. Pasachoff (1983). A Field Guide to the Stars and Planets (2nd ed.). Boston, MA: Houghton Mifflin. pp.  391. ISBN   0-395-34835-8.
    9. 1 2 3 4 Kelley, Michael S; Michael J. Gaffey (2000). "9 Metis and 113 Amalthea: A Genetic Asteroid Pair". Icarus. 144 (1): 27–38. Bibcode:2000Icar..144...27K. doi:10.1006/icar.1999.6266.
    10. 1 2 Jim Baer (2010). "Recent Asteroid Mass Determinations". Personal Website. Archived from the original on 2 July 2013. Retrieved 13 February 2011.
    11. "JPL Close-Approach Data: 9 Metis". 15 March 2009. Retrieved 6 May 2009.
    12. Graham, A.; New Planet, Monthly Notices of the Royal Astronomical Society, Vol. 8, No. 6 (dated 14 April 1848!), p. 146 (signed 29 April 1848; the discovery was first announced on 27 April)
    13. "Amateur Astronomer Becomes Second Ever to Discover Asteroid from Ireland, After 160 Years". International Year of Astronomy in Ireland. 10 October 2008. Archived from the original on 21 July 2011. Retrieved 2 March 2009.
    14. Graham, A.; Metis, Monthly Notices of the Royal Astronomical Society, Vol. 8, No. 7 (dated 12 May 1848), pp. 147–150
    15. Bala, Gavin Jared; Miller, Kirk (18 September 2023). "Unicode request for historical asteroid symbols" (PDF). unicode.org. Unicode. Retrieved 26 September 2023.
    16. Unicode. "Proposed New Characters: The Pipeline". unicode.org. The Unicode Consortium. Retrieved 6 November 2023.
    17. 1 2 3 J. Torppa et al., Shapes and rotational properties of thirty asteroids from photometric data, Icarus Vol. 164, p. 346 (2003).
    18. A. D. Storrs et al., A closer look at main-belt asteroids 1: WF/PC images, Icarus Vol. 173, p. 409 (2005).
    19. 1 2 3 Hubble Space Telescope observations Archived 30 October 2008 at the Wayback Machine
    20. D. L. Mitchell et al., Radar Observations of Asteroids 7 Iris, 9 Metis, 12 Victoria, 216 Kleopatra, and 654 Zelinda, Icarus Vol. 118, p. 105 (1995).
    21. research at IMCCE Archived 12 June 2002 at the Wayback Machine (in French)
    22. "other" reports of asteroid companions
    23. J. G. Williams, Asteroid Families – An Initial Search, Icarus Vol. 96, p. 251 (1992).
    24. 1 2 Kissling, W.M; Blow, G. L.; Allen, W. H.; Priestley, J.; Riley, P.; Daalder, P.; George, M. (1991). "The Diameter of 9 Metis from the Occultation of SAO:190531". Proceedings of the Astronomical Society of Australia. 9 (1): 150–152. Bibcode:1991PASA....9..150K. doi:10.1017/S1323358000025352. S2CID   117689158.
    25. "Occultation of TYC 0862-00695-1 by (9) Metis 2006 February 11". Royal Astronomical Society of New Zealand. Archived from the original on 27 August 2008. Retrieved 6 December 2008. (Chords) Archived 24 July 2011 at the Wayback Machine
    26. Asteroid Occulations Archived 6 March 2014 at the Wayback Machine
    27. Map Archived 6 March 2014 at the Wayback Machine