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Revision as of 09:22, 3 August 2013 editDanielCarrera (talk | contribs)81 edits Rephrased a couple of sentences because Neptunes and mini-Neptunes are not made primarily of gas, but usually ices or liquids← Previous edit Revision as of 03:06, 4 August 2013 edit undoPlanetStar (talk | contribs)Autopatrolled, Extended confirmed users21,134 editsNo edit summaryNext edit →
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E.J.W. de Mooij (1), M. Brogi (1), R.J. de Kok (2), J. Koppenhoefer (3,4), S.V. Nefs (1), I.A.G. Snellen (1), J. Greiner (4), J. Hanse (1), R.C. Heinsbroek (1), C.H. Lee (3), P.P. van der Werf (1),</ref> An estimated dividing line between a rocky planet and a gaseous planet is around two Earth radii,<ref>, Daniel C. Fabrycky, Jack J. Lissauer, Darin Ragozzine, Jason F. Rowe, Eric Agol, Thomas Barclay, Natalie Batalha, William Borucki, David R. Ciardi, Eric B. Ford, John C. Geary, Matthew J. Holman, Jon M. Jenkins, Jie Li, Robert C. Morehead, Avi Shporer, Jeffrey C. Smith, Jason H. Steffen, Martin Still</ref><ref>, blogs.scientificamerican.com, 20 June 2012</ref> but for mass, it can vary widely for different planets depending on their compositions. The dividing mass can vary from as low as two Earth masses to as high as 20 Earth masses. E.J.W. de Mooij (1), M. Brogi (1), R.J. de Kok (2), J. Koppenhoefer (3,4), S.V. Nefs (1), I.A.G. Snellen (1), J. Greiner (4), J. Hanse (1), R.C. Heinsbroek (1), C.H. Lee (3), P.P. van der Werf (1),</ref> An estimated dividing line between a rocky planet and a gaseous planet is around two Earth radii,<ref>, Daniel C. Fabrycky, Jack J. Lissauer, Darin Ragozzine, Jason F. Rowe, Eric Agol, Thomas Barclay, Natalie Batalha, William Borucki, David R. Ciardi, Eric B. Ford, John C. Geary, Matthew J. Holman, Jon M. Jenkins, Jie Li, Robert C. Morehead, Avi Shporer, Jeffrey C. Smith, Jason H. Steffen, Martin Still</ref><ref>, blogs.scientificamerican.com, 20 June 2012</ref> but for mass, it can vary widely for different planets depending on their compositions. The dividing mass can vary from as low as two Earth masses to as high as 20 Earth masses.


Several ]s have been discovered that are possibly gas dwarfs, based on known masses and densities. For example, ]<ref name="galactica"/> has mass of 2.3 Earth masses, yet its density is the same as that of ], implying that this planet is a gas dwarf with a solid or liquid ocean surrounded by a hydrogen-helium atmosphere. Such planets should not orbit too close to the heat of their parent stars otherwise that thick atmosphere would be blown away by stellar winds. It is demonstrated in the Kepler-11 system that inner planets have higher densities than planets orbiting farther away. Several ]s have been discovered that are possibly gas dwarfs, based on known masses and densities. For example, ]<ref name="galactica"/> has mass of 2.3 Earth masses, yet its density is the same as that of ], implying that this planet is a gas dwarf with a liquid ocean surrounded by thick hydrogen-helium atmosphere and only a small rocky core. Such planets should not orbit too close to the heat of their parent stars otherwise that thick atmosphere would be blown away by stellar winds. It is demonstrated in the Kepler-11 system that inner planets have higher densities than planets orbiting farther away.


== See also == == See also ==

Revision as of 03:06, 4 August 2013

A mini-Neptune (sometimes known as a gas dwarf or transitional planet) is a planet smaller than Uranus and Neptune, up to 10 Earth masses. Those planets have thick hydrogen-helium atmospheres, probably with deep layers of ice, rock or liquid oceans (made of water, ammonia, a mixture of both, or heavier volatiles). Mini-Neptunes have small cores made of low-density volatiles. Theoretical studies of such planets are loosely based on knowledge about Uranus and Neptune. Without a thick atmosphere, it would be classified as an ocean planet instead. An estimated dividing line between a rocky planet and a gaseous planet is around two Earth radii, but for mass, it can vary widely for different planets depending on their compositions. The dividing mass can vary from as low as two Earth masses to as high as 20 Earth masses.

Several exoplanets have been discovered that are possibly gas dwarfs, based on known masses and densities. For example, Kepler-11f has mass of 2.3 Earth masses, yet its density is the same as that of Saturn, implying that this planet is a gas dwarf with a liquid ocean surrounded by thick hydrogen-helium atmosphere and only a small rocky core. Such planets should not orbit too close to the heat of their parent stars otherwise that thick atmosphere would be blown away by stellar winds. It is demonstrated in the Kepler-11 system that inner planets have higher densities than planets orbiting farther away.

See also

References

  1. ^ "Gas Dwarf". Orion's Arm. Encyclopedia Galactica.
  2. Optical to near-infrared transit observations of super-Earth GJ1214b: water-world or mini-Neptune?, E.J.W. de Mooij (1), M. Brogi (1), R.J. de Kok (2), J. Koppenhoefer (3,4), S.V. Nefs (1), I.A.G. Snellen (1), J. Greiner (4), J. Hanse (1), R.C. Heinsbroek (1), C.H. Lee (3), P.P. van der Werf (1),
  3. Architecture of Kepler's Multi-transiting Systems: II. New investigations with twice as many candidates, Daniel C. Fabrycky, Jack J. Lissauer, Darin Ragozzine, Jason F. Rowe, Eric Agol, Thomas Barclay, Natalie Batalha, William Borucki, David R. Ciardi, Eric B. Ford, John C. Geary, Matthew J. Holman, Jon M. Jenkins, Jie Li, Robert C. Morehead, Avi Shporer, Jeffrey C. Smith, Jason H. Steffen, Martin Still
  4. When Does an Exoplanet’s Surface Become Earth-Like?, blogs.scientificamerican.com, 20 June 2012

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