One year of AU Mic with HARPS – I. Measuring the masses of the two transiting planets

Author:

Zicher Norbert1ORCID,Barragán Oscar1,Klein Baptiste1ORCID,Aigrain Suzanne1,Owen James E2ORCID,Gandolfi Davide3ORCID,Lagrange Anne-Marie4,Serrano Luisa Maria3ORCID,Kaye Laurel1,Nielsen Louise Dyregaard15ORCID,Rajpaul Vinesh Maguire6ORCID,Grandjean Antoine4,Goffo Elisa37,Nicholson Belinda18

Affiliation:

1. Sub-department of Astrophysics, Department of Physics, University of Oxford, Oxford OX1 3RH, UK

2. Astrophysics Group, Blackett Laboratory, Imperial College London, London SW7 2AZ, UK

3. Dipartimento di Fisica, Università degli Studi di Torino, Via Pietro Giuria 1, I-10125 Torino, Italy

4. Université Grenoble Alpes, CNRS, IPAG, F-38000 Grenoble, France

5. Geneva Observatory, University of Geneva, Chemin des Mailettes 51, CH-1290 Versoix, Switzerland

6. Astrophysics Group, Cavendish Laboratory, University of Cambridge, J. J. Thomson Avenue, Cambridge CB3 0HE, UK

7. Thüringer Landessternwarte Tautenburg, Sternwarte 5, D-07778 Tautenburg, Germany

8. Centre for Astrophysics, University of Southern Queensland, QLD 4350 Toowoomba, Australia

Abstract

ABSTRACT The system of two transiting Neptune-sized planets around the bright, young M-dwarf AU Mic provides a unique opportunity to test models of planet formation, early evolution, and star–planet interaction. However, the intense magnetic activity of the host star makes measuring the masses of the planets via the radial velocity (RV) method very challenging. We report on a 1-yr, intensive monitoring campaign of the system using 91 observations with the HARPS spectrograph, allowing for detailed modelling of the ∼600 ${\rm m\, s^{-1}}$ peak-to-peak activity-induced RV variations. We used a multidimensional Gaussian Process framework to model these and the planetary signals simultaneously. We detect the latter with semi-amplitudes of Kb = 5.8 ± 2.5 ${\rm m\, s^{-1}}$ and Kc = 8.5 ± 2.5 ${\rm m\, s^{-1}}$, respectively. The resulting mass estimates, Mb = 11.7 ± 5.0 M⊕ and Mc = 22.2 ± 6.7 M⊕, suggest that planet b might be less dense, and planet c considerably denser than previously thought. These results are in tension with the current standard models of core-accretion. They suggest that both planets accreted a H/He envelope that is smaller than expected, and the trend between the two planets’ envelope fractions is the opposite of what is predicted by theory.

Funder

European Southern Observatory

NASA

Science and Technology Facilities Council

European Research Council

Swiss National Science Foundation

BEIS

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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