Rates of protoplanetary accretion and differentiation set nitrogen budget of rocky planets
Autor: | Rajdeep Dasgupta, Alexandra Farnell, Damanveer S. Grewal, Taylor Hough |
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Rok vydání: | 2021 |
Předmět: |
Solar System
010504 meteorology & atmospheric sciences FOS: Physical sciences chemistry.chemical_element 010502 geochemistry & geophysics 01 natural sciences Article Physics::Geophysics Astrobiology Physics - Geophysics chemistry.chemical_compound Planet 0105 earth and related environmental sciences Earth and Planetary Astrophysics (astro-ph.EP) Nitrogen Silicate Accretion (astrophysics) Geophysics (physics.geo-ph) chemistry Magma General Earth and Planetary Sciences Terrestrial planet Environmental science Astrophysics::Earth and Planetary Astrophysics Protoplanet Astrophysics - Earth and Planetary Astrophysics |
Zdroj: | Nat Geosci |
ISSN: | 1752-0894 |
Popis: | The effect of protoplanetary differentiation on the fate of life essential volatiles like nitrogen and carbon and its subsequent effect on the dynamics of planetary growth is unknown. Because the dissolution of nitrogen in magma oceans depends on its partial pressure and oxygen fugacity, it is an ideal proxy to track volatile redistribution in protoplanets as a function of their sizes and growth zones. Using high pressure and high temperature experiments in graphite undersaturated conditions, here we show that the iron loving character of nitrogen is an order of magnitude higher than previous estimates across a wide range of oxygen fugacity. The experimental data combined with metal, silicate and atmosphere fractionation models suggest that asteroid sized protoplanets, and planetary embryos that grew from them, were nitrogen depleted. However, protoplanets that grew to planetary embryo size before undergoing differentiation had nitrogen rich cores and nitrogen poor silicate reservoirs. Bulk silicate reservoirs of large Earth like planets attained nitrogen from the cores of latter type of planetary embryos. Therefore, to satisfy the volatile budgets of Earth like planets during the main stage of their growth, the timescales of planetary embryo accretion had to be shorter than their differentiation timescales, that is, Moon to Mars sized planetary embryos grew rapidly within 1 to 2 million years of the Solar System formation. 44 pages, 6 figures, 9 extended data figures. Nat. Geosci. (2021) |
Databáze: | OpenAIRE |
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