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Updated: Oct 16, 2025

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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
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Paleomagnetic evidence for a disk substructure in the early solar system
Cauê S Borlina1, Benjamin P Weiss1, James F J Bryson2
1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA.
Science Advances
|October 15, 2021
Summary
Paleomagnetic study of meteorites reveals a strong magnetic field in the early solar nebula, suggesting disk substructures and significant mass loss in the outer solar system.
Area of Science:
- Planetary Science
- Astrophysics
- Geophysics
Background:
- Substructures are hypothesized to be common in protoplanetary disks and the early solar nebula.
- Meteorite studies offer insights into conditions of the early solar system.
Purpose of the Study:
- To investigate the existence and nature of disk substructures in the solar nebula.
- To determine the paleomagnetic field strength in the outer solar nebula.
Main Methods:
- Paleomagnetic measurements of chondrules from CO carbonaceous chondrites.
- Analysis of magnetic field intensity and comparison between inner and outer solar system meteorite data.
Main Results:
- Evidence for a strong magnetic field (101 ± 48 μT) in the outer solar nebula (3-7 AU).
- A significant mismatch (5-150x) in nebular accretion between inner and outer solar system reservoirs.
- Indication of substantial disk mass loss, potentially driven by a magnetized disk wind.
Conclusions:
- The findings support the presence of disk substructures in the solar nebula.
- A magnetized disk wind is a plausible mechanism for mass loss and accretion mismatch.
- This research provides crucial data on the early solar system's magnetic environment and evolution.
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