Wednesday, 29 April 2015

Kuiper belt

                               The Kuiper belt , sometimes called the Edgeworth–Kuiper belt, is a region of the Solar System beyond the planets, extending from the orbit of Neptune (at 30 AU) to approximately 50 AU from the Sun. It is similar to the asteroid belt, but it is far larger—20 times as wide and 20 to 200 times as massive. Like the asteroid belt, it consists mainly of small bodies, or remnants from the Solar System's formation. Although many asteroids are composed primarily of rock and metal, most Kuiper belt objects are composed largely of frozen volatiles (termed "ices"), such as methaneammonia and water. The Kuiper belt is home to three officially recognized dwarf planetsPlutoHaumea, and Makemake. Some of the Solar System's moons, such as Neptune's Triton Andand Saturn's Phoebe, are also believed to have originated in the region.
The Kuiper belt was named after Dutch-American astronomer Gerard Kuiper, though his role in hypothesising it has been heavily contested. Since it was discovered in 1992, the number of known Kuiper belt objects (KBOs) has increased to over a thousand, and more than 100,000 KBOs over 100 km (62 mi) in diameter are believed to exist. The Kuiper belt was initially thought to be the main repository for periodic comets, those with orbits lasting less than 200 years. However, studies since the mid-1990s have shown that the belt is dynamically stable, and that comets' true place of origin is the scattered disc, a dynamically active zone created by the outward motion of Neptune 4.5 billion years ago; scattered disc objects such as Eris have extremely eccentric orbits that take them as far as 100 AU from the Sun.
Known objects in the Kuiper belt beyond the orbit of Neptune (scale in AUepoch as of January 2015).
      Sun
      Jupiter trojans
      Giant planets: J · S · U · N
      Kuiper belt
      Scattered disc
      Neptune trojans
  The first astronomer to suggest the existence of a trans-Neptunian population was Frederick C. Leonard. Soon after Pluto's discovery by Clyde Tombaugh in 1930, Leonard pondered whether it was "not likely that in Pluto there has come to light the first of a series of ultra-Neptunian bodies, the remaining members of which still await discovery but which are destined eventually to be detected". That same year, astronomer Armin O. Leuschner suggested that Pluto "may be one of many long-period planetary objects yet to be discovered."

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