22 Kalliope

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22 Kalliope   
Discovery
Discovered by: John Russell Hind
Discovery date: November 16, 1852
Alternative names: none
Minor planet category: Main belt
Orbital characteristics
Epoch November 12, 2005 (JD 2453686.5)
Aphelion distance: 479.931 Gm (3.208 AU)
Perihelion distance: 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)
Avg. orbital speed: 17.42 km/s
Mean anomaly: 303.545°
Inclination: 13.710°
Longitude of ascending node: 66.240°
Argument of perihelion: 356.172°
Physical characteristics
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 (IPA: [kʰəˈlaɪʊpi]) 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.

Contents

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. 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 also independently detected the moon 3 days later. [6]

Stationary,
retrograde
Opposition Distance to
Earth (AU)
Maximum
brightness (mag)
Stationary,
prograde
Conjunction
to Sun
13 January 2005 19 July 2005 1.89334 10.6 30 August 2005 26 October 2005
19 April 2006 2 November 2006 1.65462 9.9 19 December 2006 4 February 2007
14 August 2007 8 February 2008 2.07558 10.9 26 March 2008 25 May 2008
7 November 2008 16 April 2009 2.17696 10.8 10 June 2009 4 August 2009
16 January 2010 23 July 2010 1.87442 10.6 4 September 2010 30 October 2010
24 April 2011 8 November 2011 1.66633 10.0 24 December 2011 8 February 2012
18 August 2012 10 February 2013 2.08827 10.9 30 March 2013 29 May 2013
10 November 2013 20 April 2014 2.17218 10.9 13 June 2014 7 August 2014
20 January 2015 28 July 2015 1.85526 10.5 8 September 2015 4 November 2015
28 April 2016 12 November 2016 1.67969 10.0 27 December 2016 13 February 2017
22 August 2017 13 February 2018 2.10024 10.9 3 April 2018 2 June 2018
13 November 2018 24 April 2019 2.16665 10.9 16 June 2019 10 August 2019
23 January 2020 31 July 2020 1.83594 10.5 12 September 2020 7 November 2020

  1. ^ a b Supplemental IRAS Minor Planet Survey
  2. ^ a b M. Kaasalainen et al (2002). "Models of Twenty Asteroids from Photometric Data". Icarus 159: 369. 
  3. ^ a b c F. Marchis et al (2003). "A three-dimensional solution for the orbit of the asteroidal satellite of 22 Kalliope". Icarus 165: 112. 
  4. ^ a b J.L. Margot & M.E. Brown (2003). "A Low-Density M-type Asteroid in the Main Belt". Science 300: 1939. 
  5. ^ a b PDS lightcurve data
  6. ^ a b synthesis of several observations including recent ones with the VLT 8m telescope.
  7. ^ A.S. Rivkin et al (2000). "The nature of M-class asteroids from 3-micron observations". Icarus 145: 351. 
  8. ^ D.F. Lupishko et al (1982). "UBV photometry of the M-type asteroids 16 Psyche and 22 Kalliope". Solar System Research 16: 75. 


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