An alternative formation scenario for uranium-rich giants: engulfing an Earth-like planet

Author:

Xie Dian12ORCID,Zhu Chunhua1,Guo Sufen1,Liu Helei1ORCID,Lü Guoliang2ORCID

Affiliation:

1. School of Physical Science and Technology, Xinjiang University , Urumqi 830017, China

2. Xinjiang Astronomical Observatory, Chinese Academy of Sciences , 150 Science 1-Street, Xinjiang, Urumqi 830011, China

Abstract

ABSTRACT The actinides, such as the uranium (U) element, are typically synthesized through the rapid neutron-capture process (r-process), which can occur in core-collapse supernovae or double neutron star mergers. There exist nine r-process giant stars exhibiting conspicuous U abundances, commonly referred to as U-rich giants. However, the origins of these U-rich giants remain ambiguous. We propose an alternative formation scenario for these U-rich giants whereby a red giant (RG) engulfs an Earth-like planet. To approximate the process of an RG engulfing an Earth-like planet, we employ an accretion model wherein the RG assimilates materials from said planet. Our findings demonstrate that this engulfment event can considerably enhance the presence of heavy elements originating from Earth-like planets on the surfaces of very metal-poor stars (Z = 0.00001), while its impact on solar-metallicity stars is comparatively modest. Importantly, the structural and evolutionary properties of both very metal-poor and solar-metallicity stars remain largely unaffected. Notably, our engulfment model effectively accounts for the observed U abundances in known U-rich giants. Furthermore, the evolutionary trajectories of U abundances on the surfaces of RGs subsequent to the engulfment of Earth-like planets encompass all known U-rich giants. Therefore, it is plausible that U-rich giants are formed when an RG engulfs an Earth-like planet.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Xinjiang

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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