Open Access
Fig. 7

Scaling of the Q factor as a function of mantle viscosity η, tidal frequency χ, Andrade α parameter, and iron content, δFe, relative to reference values (ηref = 5 × 1022 Pa s, χref = 2π∕1day), for four planet masses (1, 2, 5 and 10 M⊕).
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