Europium as a lodestar: diagnosis of radiogenic heat production in terrestrial exoplanets
arXiv:2010.04632 · doi:10.1051/0004-6361/202038386
Abstract
Long-lived radioactive nuclides, such as K, Th, U and U, contribute to persistent heat production in the mantle of terrestrial-type planets. As refractory elements, the concentrations of Th and U in a terrestrial exoplanet are implicitly reflected in the photospheric abundances in the stellar host. However, a robust determination of these stellar abundances is difficult in practice owing to the general paucity and weakness of the relevant spectral features. We draw attention to the refractory, process element europium, which may be used as a convenient and practical proxy for the population analysis of radiogenic heating in exoplanetary systems. As a case study, we present a determination of Eu abundances in the photospheres of Cen A and B. We find that europium is depleted with respect to iron by 0.1 dex and to silicon by 0.15 dex compared to solar in both binary components. To first order, the measured Eu abundances can be converted to the abundances of Th, U and U with observational constraints while the abundance of K is approximated independently with a Galactic chemical evolution model. We find that the radiogenic heat budget in an -Cen-Earth is TW upon its formation and TW at the present day, respectively % and % lower than that in the Hadean and modern Earth. As a consequence, mantle convection in an -Cen-Earth is expected to be overall weaker than that of the Earth (assuming other conditions are the same) and thus such a planet would be less geologically active, suppressing its long-term potential to recycle its crust and volatiles. With Eu abundances being available for a large sample of Sun-like stars, the proposed approach can extend our ability to make predictions about the nature of other rocky worlds.
Accepted for publication in Astronomy & Astrophysics. 11 pages, 4 figures, and 4 tables
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