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Precise radial velocities of giant stars. XII. Evidence against the proposed planet Aldebaran b

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 نشر من قبل Katja Reichert
 تاريخ النشر 2019
  مجال البحث فيزياء
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Radial-velocity variations of the K giant star Aldebaran ($alpha$ Tau) were first reported in the early 1990s. After subsequent analyses, the radial-velocity variability with a period of $sim 629,mathrm{d}$ has recently been interpreted as caused by a planet of several Jovian masses. We want to further investigate the hypothesis of an extrasolar planet around Aldebaran. We combine 165 new radial-velocity measurements from Lick Observatory with seven already published data sets comprising 373 radial-velocity measurements. We perform statistical analyses and investigate whether a Keplerian model properly fits the radial velocities. We also perform a dynamical stability analysis for a possible two-planet solution. As best Keplerian fit to the combined radial-velocity data we obtain an orbit for the hypothetical planet with a smaller period ($P=607,mathrm{d}$) and a larger eccentricity ($e=0.33 pm 0.04$) than the previously proposed one. However, the residual scatter around that fit is still large, with a standard deviation of $117,mathrm{ms}^{-1}$. In 2006/2007, the statistical power of the $sim 620,mathrm{d}$ period showed a temporary but significant decrease. Plotting the growth of power in reverse chronological order reveals that a period around $620,mathrm{d}$ is clearly present in the newest data but not in the data taken before $sim$ 2006. Furthermore, an apparent phase shift between radial-velocity data and orbital solution is observable at certain times. A two-planet Keplerian fit matches the data considerably better than a single-planet solution, but poses severe dynamical stability issues. The radial-velocity data from Lick Observatory do not further support but in fact weaken the hypothesis of a substellar companion around Aldebaran. Oscillatory convective modes might be a plausible alternative explanation of the observed radial-velocity variations.



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