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- W4283708708 abstract "Abstract Though ferric iron indisputably exists on the highly reduced Moon, its formation mechanism and evolution have yet to be disclosed. Here we show that micrometeorite impact-induced ferrous disproportionation could produce a large amount of ferric iron (average Fe 3+ /∑Fe > 0.4) in agglutinate melts returned by Chang’e-5 mission. The disproportionation reaction synchronously generated nanophase metallic iron (npFe 0 ), a dominant formation pathway of npFe 0 within the lunar agglutinate glass. The discovery of the disproportionation reaction in the agglutinates suggests that much more Fe 3+ could be ubiquitously present on the Moon than previously thought, and its abundance is progressively increasing with micrometeoroid impacts." @default.
- W4283708708 created "2022-06-30" @default.
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- W4283708708 date "2022-06-28" @default.
- W4283708708 modified "2023-10-17" @default.
- W4283708708 title "Ubiquitous and Increasing Ferric Iron on Lunar Surface Revealed by Chang’E-5 Samples" @default.
- W4283708708 doi "https://doi.org/10.21203/rs.3.rs-1691132/v1" @default.
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