Formation of intermediate-mass planets via magnetically-controlled disk fragmentation
Hongping Deng (Cambridge), Lucio Mayer (UZH), Ravit Helled (UZH)

TL;DR
This study uses MHD simulations to show that magnetic fields in protoplanetary disks can lead to the formation of intermediate-mass planets through fragmentation, aligning with observed exoplanet distributions.
Contribution
It introduces a new model of disk fragmentation driven by spiral dynamo magnetic fields, producing lighter protoplanets than traditional models.
Findings
Formation of long-lived, intermediate-mass protoplanets.
Magnetic pressure prevents further growth of these protoplanets.
Results align with observed exoplanet mass distribution.
Abstract
Intermediate mass planets, from Super-Earth to Neptune-sized bodies, are the most common type of planets in the galaxy. The prevailing theory of planet formation, core-accretion, predicts significantly fewer intermediate-mass giant planets than observed. The competing mechanism for planet formation, disk instability, can produce massive gas giant planets on wide-orbits, such as HR8799, by direct fragmentation of the protoplanetary disk. Previously, fragmentation in magnetized protoplanetary disks has only been considered when the magneto-rotational instability is the driving mechanism for magnetic field growth. Yet, this instability is naturally superseded by the spiral-driven dynamo when more realistic, non-ideal MHD conditions are considered. Here we report on MHD simulations of disk fragmentation in the presence of a spiral-driven dynamo. Fragmentation leads to the formation of…
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