The primordial He budget of the Earth set by percolative core formation in planetesimals

Roth, A.S.G.; Liebske, C.; Maden, C.; Burton, K.W.; Schönbächler, M.; Busemann, H.

Abstract

The primordial He budget of the Earth’s interior is commonly thought to have been set by full liquid metal-silicate equilibration in a terrestrial magma ocean. However, incomplete metal-silicate equilibration during accretion will have a substantial effect on this budget. Here we present liquid-solid partitioning experiments indicating that He behaves as a moderately siderophile element during percolative core formation in planetesimals. Mass balance considerations show that even minor disequilibrium will allow the Earth’s early core to incorporate sufficient primordial He—and possibly other noble gases—to supply the lower mantle throughout Earth’s history. We conclude that the high 3He/4He ratios in basalts may well represent primarily the last vestiges of metal-silicate disequilibrium in a terrestrial magma ocean preserved from the time of Earth’s formation.

Citation

Roth, A., Liebske, C., Maden, C., Burton, K., Schönbächler, M., & Busemann, H. (2019). The primordial He budget of the Earth set by percolative core formation in planetesimals. Geochemical perspectives letters, 9, 26-31. https://doi.org/10.7185/geochemlet.1901

• Journal Article Type: Article
• Acceptance Date: Nov 19, 2018
• Online Publication Date: Jan 21, 2019
• Publication Date: 2019
• Deposit Date: May 29, 2019
• Publicly Available Date: May 29, 2019
• Journal: Geochemical Perspectives Letters
• Print ISSN: 2410-339X
• Electronic ISSN: 2410-3403
• Publisher: European Association of Geochemistry (EAG)
• Peer Reviewed: Peer Reviewed
• Volume: 9
• Pages: 26-31
• DOI: https://doi.org/10.7185/geochemlet.1901
• Public URL: https://durham-repository.worktribe.com/output/1300578