Composition and Size Dependent Sorting in Preplanetary Growth: Seeding the Formation of Mercury-like Planets
arXiv:2006.13692 · doi:10.3847/PSJ/ab93c4
Abstract
In an earlier work, we found that large metallic iron fractions in dust aggregates and strong magnetic fields boost preplanetary growth. This sets an initial bias for the formation of Mercury-like planets in the inner part of protoplanetary disks. We extended these experiments here by adding pure quartz aggregates to the iron-rich aggregates. Magnetic boost still leads to the formation of larger clusters of aggregates. These clusters now include silicate aggregates, which can also be connecting bridges between chains. However, at least a certain fraction of iron-rich aggregates are needed to trigger magnetic boost. Without a magnetic field, the sticking properties of the aggregates and their constituents determine the composition of clusters of a given size. This introduces a new fractionation and sorting mechanism by cluster formation at the bouncing barrier.
References in corpus (15)
- The stickiness of micrometer-sized water-ice particles
- Magnetic fields in protoplanetary disks
- Can dust coagulation trigger streaming instability?
- Sticking Properties of Silicates in Planetesimal Formation Revisited
- Fossil magnetic field of accretion disks of young stars
- K2-66b and K2-106b: Two extremely hot sub-Neptune-size planets with high densities
- Magnetic fields in protoplanetary disks: from MHD simulations to ALMA observations
- Failed Growth at the Bouncing Barrier in Planetesimal Formation
- Seeding the Formation of Mercurys: An Iron-sensitive Bouncing Barrier in Disk Magnetic Fields
- A challenge for Martian lightning: Limits of collisional charging at low pressure
- Magnetic fields in circumstellar disks: The potential of Zeeman observations
- Meteorite cloudy zone formation as a quantitative indicator of paleomagnetic field intensities and cooling rates on planetesimals
- Rocky Planetesimal Formation Aided by Organics
- Explaining Mercury's Density through Magnetic Erosion
- ARISE: A granular matter experiment on the International Space Station