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Was the moon magnetized by impact plasmas?

Oran R., B. P. Weiss, Y. Shprits, K. Miljkovic, G. T{‘o}th, (2020), Was the moon magnetized by impact plasmas?, Science Advances, 6, doi:10.1126/sciadv.abb1475

Abstract

The crusts of the Moon, Mercury, and many meteorite parent bodies are magnetized. Although the magnetizing field is commonly attributed to that of an ancient core dynamo, a longstanding hypothesized alternative is amplification of the interplanetary magnetic field and induced crustal field by plasmas generated by meteoroid impacts. Here, we use magnetohydrodynamic and impact simulations and analytic relationships to demonstrate that although impact plasmas can transiently enhance the field inside the Moon, the resulting fields are at least three orders of magnitude too weak to explain lunar crustal magnetic anomalies. This leaves a core dynamo as the only plausible source of most magnetization on the Moon.

Authors (sorted by name)

Miljkovic Oran Shprits Toth Weiss

Journal / Conference

Science Advances

Bibtex

@article {10.1126/sciadv.abb1475,
	author = {Oran, Rona and Weiss, Benjamin P. and Shprits, Yuri and Miljkovic, Katarina and T{'o}th, G{'a}bor},
	title = {Was the moon magnetized by impact plasmas?},
	volume = {6},
	number = {40},
	elocation-id = {eabb1475},
	year = {2020},
	doi = {10.1126/sciadv.abb1475},
	publisher = {American Association for the Advancement of Science},
	abstract = {The crusts of the Moon, Mercury, and many meteorite parent bodies are magnetized. Although the magnetizing field is commonly attributed to that of an ancient core dynamo, a longstanding hypothesized alternative is amplification of the interplanetary magnetic field and induced crustal field by plasmas generated by meteoroid impacts. Here, we use magnetohydrodynamic and impact simulations and analytic relationships to demonstrate that although impact plasmas can transiently enhance the field inside the Moon, the resulting fields are at least three orders of magnitude too weak to explain lunar crustal magnetic anomalies. This leaves a core dynamo as the only plausible source of most magnetization on the Moon.},
	URL = {https://advances.sciencemag.org/content/6/40/eabb1475},
	eprint = {https://advances.sciencemag.org/content/6/40/eabb1475.full.pdf},
	journal = {Science Advances}
}