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Discovery
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| Discovered by | John Russell Hind |
| Discovery date | November 16, 1852 |
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Designations
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| Alternative names | none |
| Minor planet category |
Main belt |
| Epoch November 12, 2005 (JD 2453686.5) | |
| Aphelion | 479.931 Gm (3.208 AU) |
| Perihelion | 390.433 Gm (2.610 AU) |
| Semi-major axis | 435.182 Gm (2.909 AU) |
| Eccentricity | 0.103 |
| Orbital period | 1812.245 d (4.96 a) |
| Average orbital speed | 17.42 km/s |
| Mean anomaly | 303.545° |
| Inclination | 13.710° |
| Longitude of ascending node | 66.240° |
| Argument of perihelion | 356.172° |
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Physical characteristics
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| Dimensions | 215×180×150 km [1][2] |
| Mass | 6.3 ± 0.5 ×1018 kg [3][4] |
| Mean density | 2.03 ± 0.16 g/cm³ [3] |
| Equatorial surface gravity | 0.038 m/s² |
| Escape velocity | 0.09 km/s |
| Rotation period | 0.1728 d (4.148 h) [5] |
| Albedo | 0.142 [1] |
| Temperature | ~161 K max: 240 K (-32 °C) |
| Spectral type | M [5] |
| Absolute magnitude | 6.45 |
22 Kalliope (pronounced /kəˈlaɪəpi/, Greek: Καλλιόπη) is a large main belt asteroid of the M-type, discovered by J. R. Hind on November 16, 1852. It is named after Calliope, the Greek Muse of epic poetry.
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Kalliope is somewhat elongated, approximately 180 km in diameter, and slightly asymmetric, as evidenced by resolved images taken with the VLT at the European Southern Observatory [6].
While its spectrum is an M-type, Kalliope does not appear to be metallic, similarly to other M-types such as 21 Lutetia, for example. Firstly, its density, which is known with confidence from its satellite's orbit, is far too low to agree with any plausible metallic substance, even a rubble pile. It would have to be 70% porous, which is inconsistent with packing considerations. Furthermore, spectroscopic studies have shown evidence of hydrated minerals [7] and silicates [8], which indicate rather a stony surface composition. Kalliope also has a low radar albedo [4], which is again inconsistent with a metallic surface.
Lightcurve analysis indicates that Kalliope's pole most likely points towards ecliptic coordinates (β, λ) = (-23°, 20°) with a 10° uncertainty [2][3], which gives Kalliope an axial tilt of 103°. Kalliope's rotation is then slightly retrograde.
Kalliope has one known natural satellite, Linus, or (22) Kalliope I Linus. It is quite large being 30-40 km in diameter, and would be a sizeable asteroid by itself. It orbits about 1065 km from Kalliope, equivalent to about 12 Kalliope radii. Linus was discovered on August 29, 2001 by Jean-Luc Margot and Michael E. Brown, while another team lead by William Merline also independently detected the moon 3 days later. [6]
On November 7 2006, the first stellar occultation by the satellite of an asteroid (Linus) was successfully observed by a group of Japanese observers [9]according to a prediction that was made just one day before by Berthier et al. [10] based on more than 5 years of regular observations of Kalliope binary system using adaptive optics systems on ground-based telescopes. The observed chords of Linus give a unique opportunity to estimate the size of the moonlet which was estimated to 20-28 km.
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