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Formation of intermediate-mass planets via magnetically controlled disk fragmentation
by
Helled, Ravit
, Deng, Hongping
, Mayer, Lucio
in
639/33/34/4122
/ 639/33/445/862
/ Astronomy
/ Astrophysics and Cosmology
/ Jupiter
/ Letter
/ Magnetic fields
/ Physics
/ Physics and Astronomy
/ Planets
2021
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Formation of intermediate-mass planets via magnetically controlled disk fragmentation
by
Helled, Ravit
, Deng, Hongping
, Mayer, Lucio
in
639/33/34/4122
/ 639/33/445/862
/ Astronomy
/ Astrophysics and Cosmology
/ Jupiter
/ Letter
/ Magnetic fields
/ Physics
/ Physics and Astronomy
/ Planets
2021
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Formation of intermediate-mass planets via magnetically controlled disk fragmentation
Journal Article
Formation of intermediate-mass planets via magnetically controlled disk fragmentation
2021
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Overview
Intermediate-mass planets, from super-Earth to Neptune-sized bodies, are the most common types of planet in the Galaxy
1
. The prevailing theory of planet formation—core accretion
2
—predicts the existence of substantially fewer intermediate-mass giant planets than have been observed
3
,
4
. The competing mechanism for planet formation—disk instability—can produce massive gas giant planets on wide orbits, such as HR 8799
5
, by direct fragmentation of the protoplanetary disk
6
. Previously, fragmentation in magnetized protoplanetary disks has been considered only when the magneto-rotational instability is the driving mechanism for magnetic field growth
7
. However, this instability is naturally superseded by the spiral-driven dynamo when more realistic, non-ideal magneto-hydrodynamic conditions are considered
8
,
9
. Here, we report on magneto-hydrodynamic simulations of disk fragmentation in the presence of a spiral-driven dynamo. Fragmentation leads to the formation of long-lived bound protoplanets with masses that are at least one order of magnitude smaller than in conventional disk instability models
10
,
11
. These light clumps survive shear and do not grow further owing to the shielding effect of the magnetic field, whereby magnetic pressure stifles the local inflow of matter. The outcome is a population of gaseous-rich planets with intermediate masses, while gas giants are found to be rarer, in qualitative agreement with the observed mass distribution of exoplanets.
The formation mechanism of the most common type of planet in the Galaxy, those with masses between those of the Earth and Neptune, is far from clear. However, simulations of disk fragmentation presented here, which incorporate a spiral-driven dynamo, produce protoplanets of the right mass and longevity.
Publisher
Nature Publishing Group UK,Nature Publishing Group
Subject
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