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Umbriel (moon) - Simple English Wikipedia, the free encyclopedia

Umbriel (moon)

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Umbriel
Discovery
Discovered by William Lassell
Discovered in October 24, 1851
Orbital characteristics
Semi-major axis 266,000 km
Eccentricity 0.0039
Periastron (Periuranion) 265,000 km
Apastron (Apuranion) 267,000 km
Orbital circumference 1,671,000 km
Orbital period 4.144 d
Mean orbital speed 4.668 km/s
Minimum orbital speed 4.650 km/s
Maximum orbital speed 4.686 km/s
Inclination 0.205° (to Uranus' equator)
Is a moon of Uranus
Physical characteristics[1]
Mean diameter 1169.4 km (0.092 Earths)
Surface area 4,296,000 km2 (0.008 Earths)
Volume 837,300,000 km3 (0.0008 Earths)
Mass 1.2±0.1×1021 kg (0.0002 Earths)
Mean density 1.40±0.16 g/cm3
Surface gravity 0.23 m/s2 (0.023 g)
Escape velocity 0.52 km/s
Rotation period synchronous
Axial tilt zero
Rotation velocity 36.94 km/h (at the equator)
Albedo 0.21 ± 0.02[1]
Apparent magnitude 14.81[2]
Angular size 0.093" (max)
Surface temp.
min mean max
 ? K ~61 K  ? K
Atmospheric pressure 0 kPa

Umbriel is a moon of Uranus found on October 24, 1851 by William Lassell. It was found at the same time as Ariel.

Contents

[change] Name

The name "Umbriel" and the names of all four moons of Uranus then known were suggested by John Herschel in 1852 at the request of Lassell.[3] Lassell had earlier supported Herschel's 1847 naming scheme for the seven then-known moons of Saturn and had named his newly-found eighth moon Hyperion in accordance with Herschel's naming scheme in 1848. Umbriel is the 'dusky melancholy sprite' in Alexander Pope's The Rape of the Lock, and the name suggests the Latin umbra, shadow. The adjectival form of the name is Umbrielian.

It is also designated Uranus II.

[change] Physical characteristics

So far the only close-up images of Umbriel are from the Voyager 2 probe, which made observations of the moon during its Uranus flyby in January, 1986. During the flyby the southern hemisphere of the moon was pointed towards the Sun so only it was studied.

Umbriel's surface is the darkest of the Uranian moons, and reflects only about half as much light as Ariel, Uranus' brightest moon. It has far more and bigger craters than do Ariel and Titania and is also the least geologically active.[4] It is mostly made of water ice, with the balance made up of silicate rock, and other ices such as methane. Methane can break down and form reddish-black organic compounds such as tholins when bombarded by high-energy particles.[5] Near-IR spectra of Ariel and Umbriel clearly show that water ice dominates the spectra of these objects.[6]

[change] Other websites

[change] References

  1. 1.0 1.1 Yeomans, Donald K. (2006-Jul-13). Planetary Satellite Physical Parameters. JPL Solar System Dynamics. Retrieved on 12 June 2005.
  2. Classic Satellites of the Solar System. Observatorio ARVAL. Retrieved on 28 September 2007.
  3. http://adsabs.harvard.edu//full/seri/AN.../0034//0000169.000.html Adsabs.harvard.edu Retrieved on 06-01-07
  4. Arnett, William A. (2006 Aug 25). Umbriel. The Nine Planets. Retrieved on 9 November 2007.
  5. Overbye, Roger (April 1986). Voyager was on target again; in the latest unmanned triumph, Voyager 2 surveyed Uranus and sent back a real bull's-eye. Discover. Retrieved on 9 November 2007.
  6. Dumas, Christophe, Bradford A. Smith, and Richard J. Terrile (2003). "Hubble Space Telescope NICMOS Multiband Photometry of Proteus and Puck". The Astronomical Journal 126 (2003): 1080–1085. DOI:10.1086/375909.


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