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Fig. 1

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Temporal evolution of the semi-major axis a for a class of tidal models with k2/Q ∝ χα and with different values of the parameter α. The abscissa represents time in years, the vertical axis measures the deviation of the semi-major axis from its initial value a0. Our plots serve to compare realistic rheologies (α = 0.2,0.3,0.4) with less physical ones – those with α = 0 (Kaula 1964) and α = −1 (Singer 1968; Mignard 1979).

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