Fine-grained rim formation -- high speed, kinetic dust aggregation in the early Solar System
Kurt Liffman

TL;DR
This paper proposes a high-speed dust collision model called kinetic dust aggregation to explain the formation of fine-grained rims on meteorite components, addressing limitations of previous gentle adhesion models.
Contribution
It introduces a novel high-speed impact model for FGR formation that accounts for observed properties like low porosity and the linear rim thickness relationship.
Findings
KDA naturally explains rim thickness linearity with a non-zero intercept.
The model accounts for low porosity and microchondrule formation.
It suggests a possible link to dust aggregation in protostellar disks.
Abstract
Type 3 chondritic meteorites often contain chondrules and refractory inclusions that are coated with accretionary, fine-grained rims (FGRs). FGRs are of low porosity, were subject to centrally directed pressure, may contain high temperature products like microchondrules and there is a linear relationship between the rim thickness and the radius of the enclosed object. FGRs are thought to have formed by the gentle adhesion of dust onto the central object with the subsequent compression of this fluffy rim within the parent body. However, this model does not explain the low porosity, micro-chondrules and centralized pressure. This model also has difficulties explaining the linear relationship between rim thickness and object size including the existence of a non-zero constant in that linear relationship. We propose that FGRs formed by the relatively high-speed interaction between dust and…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
