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Title: Insufficient Energy From MgO Exsolution to Power Early Geodynamo

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2017GL075283· OSTI ID:1423342
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [3]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [4]; ORCiD logo [1]
  1. Carnegie Inst. of Washington, Washington, DC (United States)
  2. Carnegie Inst. of Washington, Washington, DC (United States); Smithsonian Inst., Washington, DC (United States). National Museum of Natural History
  3. Yale Univ., New Haven, CT (United States)
  4. Univ. of Chicago, IL (United States). Center for Advanced Radiation Sources (CARS)

The origin of Earth's ancient magnetic field is an outstanding problem. It has recently been proposed that exsolution of MgO from the core may provide sufficient energy to drive an early geodynamo. Here, in this work, we present new experiments on Mg partitioning between iron-rich liquids and silicate/oxide melts. Our results indicate that Mg partitioning depends strongly on the oxygen content in the iron-rich liquid, in contrast to previous findings that it depends only on temperature. Consequently, MgO exsolution during core cooling is drastically reduced and insufficient to drive an early geodynamo alone. Using the new experimental data, our thermal model predicts inner core nucleation at ~850 Ma and a nearly constant paleointensity.

Research Organization:
Argonne National Laboratory (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
Sponsoring Organization:
Carnegie Fellowship; National Science Foundation (NSF); USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences, and Biosciences Division
Grant/Contract Number:
EAR-1447311; EAR-1321956; EAR-1551348; EAR-1128799; FG02-94ER14466; AC02-06CH11357; AC02‐06CH11357
OSTI ID:
1423342
Alternate ID(s):
OSTI ID: 1410579
Journal Information:
Geophysical Research Letters, Vol. 44, Issue 22; ISSN 0094-8276
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
ENGLISH
Citation Metrics:
Cited by: 24 works
Citation information provided by
Web of Science

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Cited By (5)

Ab Initio Molecular Dynamics Investigation of Molten Fe–Si–O in Earth's Core journal June 2019
Heat Flow in Earth's Core From Invariant Electrical Resistivity of Fe‐Si on the Melting Boundary to 9 GPa: Do Light Elements Matter? journal June 2019
Rotating double-diffusive convection in stably stratified planetary cores journal August 2019
FeO Content of Earth’s Liquid Core journal October 2019
Fe Melting Transition: Electrical Resistivity, Thermal Conductivity, and Heat Flow at the Inner Core Boundaries of Mercury and Ganymede journal July 2019