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The Role of Ferromagnetic Iron in Planetesimal Formation

Subject Area Astrophysics and Astronomy
Term from 2016 to 2020
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 320743803
 
Final Report Year 2020

Final Report Abstract

Planetary bodies in the solar system show an iron gradient with iron-rich bodies being closer to the sun. An extreme is Mercury with an iron core well beyond the average planetary core size. There are also a couple of extrasolar planets found which are iron-rich. Hubbard (2014) suggested magnetic erosion as a model to explain selective growth of iron-rich matter. In the magnetic fields of a protoplanetary disk, ferromagnetic material would be harder to fragment and easier to reassemble. We verified this idea in laboratory experiments. While we found that this mechanism does not work at the high energies, we found a magnetic boost in growth at the bouncing barrier, where collisions usually no longer lead to sticking and growth but where particles bounce off each other. The size of particles is increased for (metallic) iron-rich matter in magnetic fields. This magnetic boost sets a bias in particle growth. If this is inherited to later evolutionary phases, this indeed offers a way to explain the formation of iron-rich planets and an iron gradient in planetary systems.

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