A&A 394, L43-L46 (2002)
DOI: 10.1051/0004-6361:20021377
B. König 1 - K. Fuhrmann1 - R. Neuhäuser1 - D. Charbonneau2 - R. Jayawardhana3
1 - Max-Planck-Institut für extraterrestrische Physik,
Gießenbachstraße 1, 85748 Garching, Germany
2 -
California Institute of Technology, 105-24 (Astronomy)
1200 E. California Blvd., Pasadena, CA 91125, USA
3 -
Department of Astronomy, University of Michigan, Ann Arbor, MI
48109, USA
Received 28 August 2002 / Accepted 18 September 2002
Abstract
We present an H-band image of the companion of Orionis
taken with the Keck adaptive optic system and NIRC 2 camera equipped
with a 300 mas-diameter coronographic mask. The direct detection of
this companion star enables us to calculate dynamical masses using only
Kepler's laws (
,
), and to study stellar evolutionary models
at a wide spread of masses. The application of Baraffe et al. (1998)
pre-main-sequence models implies an age of 70-130 Myrs. This is in
conflict to the age of the primary, a confirmed member of the Ursa Major
Cluster with a canonical age of 300 Myrs. As a consequence, either the
models at low masses underestimate the age or the Ursa Major Cluster is
considerably younger than assumed.
Figure 1: The H-band image of Ori behind the coronograph in the center and the companion to the left. Note the diffraction ring around the companion. | |
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The G-type star Ori and its companion form a binary with a very small mass ratio. A direct detection of the secondary would be significant as it would allow the masses to be determined without astrophysical assumption. The derived mass and observed luminosity allow the age to be inferred from comparison to pre-main-sequence evolutionary tracks, which in turn enables a calibration of other alternate estimators.
We observed Ori on Feb. 28, 2002, using the Keck 2 telescope equipped with the NIRC2 camera and the adaptive optic system (Wizinowich et al. 2000), an H-band filter and a 300 mas diameter coronograph. The coronograph is semi-transparent with a throughput slightly below half a percent as determined by us (different from what is given in the manual, but confirmed by the Keck staff), so the position of the star behind it can be measured precisely. The total integration time was 0.18 s. The FWHM of the companion is 50 mas.
We performed the data reduction, using the reduction software MIDAS (1991) provided by ESO. We divided the image by a normalized master sky-flat. We subtracted the background of Ori B depending on the distance from Ori A: Ori B is located in the PSF wing of the component A which causes the main contribution to the background emission. To obtain a background subtracted instrumental magnitude of B we subtract an azimuthal averaged background (a one pixel wide annulus around A excluding B) for each pixel used.
We determined the magnitude of the companion as well as that of two stars used as photometric standards: the UKIRT faint standard FS 11, mag (Hawarden et al. 2001) and TWA-5B, mag (Lowrance et al. 1999). The standards were observed in the same night, and analyzed with the same procedure. We used 121 different aperture sizes starting with the brightest central pixel and calculating a background subtracted peak-to-peak flux ratio and then consecutively adding the next brightest pixel until we end up with a pixel aperture box. For aperture sizes from 1 to 50 pixels, the resulting instrumental magnitude did not change significantly, so we use this value. By comparing the background subtracted instrumental magnitude of the companion to the background subtracted instrumental magnitudes obtained for TWA-5 B and FS 11, we measure the apparent H-band magnitude for the Ori companion of mag, taking into account also the slightly different FWHM and Strehl ratios. With the Hipparcos parallax for Ori of mas, we obtain mag for the B-component.
Figure 2: A spectrum of Ori A compared to the moon (=reflected sun light) in the range of H at 6563 Å. Note the considerable rotational velocity of Ori A, km s-1, and the slightly filled-in line core of H. | |
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Figure 3: Same as Fig. 2, but for the range of lithium at 6707.8 Å and calcium at 6717.8 Å. | |
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The basic stellar parameters of Ori A are derived from a model atmosphere analysis of high resolution, high S/N échelle spectra (Figs. 2 and 3) obtained in January 2000 at the Calar Alto Observatory, Spain, 2.2 m telescope with FOCES (Pfeiffer et al. 1998). The fairly high projected rotational velocity km s-1, the strong lithium feature at 6707 (Fig. 3), the "dipper-star-like'' kinematics ( U/V/W=24/7/0 km s-1), and the filled-in line cores of H (Fig. 2) and the Ca II infrared triplet all consistently confirm that Ori must belong to the Ursa Major Cluster. As in Fuhrmann et al. (1997) we deduce the effective temperature of the primary, K, from the Balmer line wings and the surface gravity, , from the iron ionization equilibrium and the wings of the Mg Ib lines. We find the metallicity to be slightly below the solar value ( ), again very typical for the mean abundance of Ursa Major Cluster stars of (Boesgaard & Friel 1990). With a bolometric magnitude , and and [Fe/H] as derived above, we find the mass to be (implied from the tracks given in Fuhrmann et al. 1997), i.e. slightly above solar and with an uncertainty of about . The secondary - being more than five magnitudes (extrapolating the measured H-band magnitude) fainter in the visible - does not have an impact on our spectra.
Figure 4: Baraffe et al. (1998) isochrones for solar metallicity in a mass-luminosity plot compared to the position of Ori B. The error-bars for the mass are derived by the spectroscopy (solid) and for the dynamical mass (dots). The age for Ori B ranges from 70-130 Myrs using the dynamical mass. | |
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Figure 5: Baraffe et al. (1998) tracks for solar metallicity. The horizontal line in the first plot gives for the companion star with the top shaded area indication the error for and the temperature range. In panel a), the bottom shaded area is the age range determined for the Ursa Major cluster using different methods. With a mass of the companion appears younger compared to the age range of the Ursa Major cluster. In the other two panels the same tracks plotted are for the primary, indicating the position of the primary by the shaded area. In panel a) and b) the model parameters are , Y=0.275 and . For c) the parameters have been adjusted to fit the sun to , Y=0.282 and . | |
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The mass of the companion to Ori has been determined precisely to
(Han & Gatewood 2002). The
main uncertainty is
.
This leads to a
spectroscopic (
)
and dynamic mass (
), which are both in good agreement.
The position of the Ori B in the mass-luminosity plot
(Figs. 4 and 5a) compared to the isochrones
provided by Baraffe et al. (1998) indicates that the star lies about
mag above the main sequence.
Figures 5b and 5c show H-R diagrams for the primary star
including the tracks of Baraffe et al. (1998). Figure 5b
shows models for
,
Y=0.275, and the mixing length of
.
Baraffe et al. (1998) acknowledge that these models do not
reproduce the sun at present age. Those tracks and isochrones also do not
reproduce Ori A.
Figure 5c shows the same as Fig. 5b
except that the parameters
,
Y=0.282, and the mixing length of
were adjusted to fit the sun. With these
parameters the present sun could be reproduced and for Ori A they
also seem to work. The MH predicted by Baraffe et al. (1998) is a bit
lower than the measured MH value for Ori A. This could be
because Ori A is slightly iron underabundant (
)
and the tracks were calculated for solar abundance. No tracks
for masses of 0.15-0.175
are available for the model with the
parameter set to fit the sun.
The age prediction by the pre-main-sequence models can be directly compared to other age determinations for the Ursa Major Cluster. While the canonical value for the age of the Ursa Major Cluster is 300 Myrs (cf. e.g. Soderblom & Mayor 1993, and references therein) derived by comparing the members of the Ursa Major Cluster nucleus stars in a color-magnitude diagram to theoretical isochrones computed by VandenBerg (1985), more recent observations of Sirius' white dwarf companion led Holberg et al. (1998) to suggest an age of 160 Myrs with reference to the cooling tracks of Wood (1992). Since Sirius B is also well-known as a fairly massive degenerate white dwarf with a mass of (Holberg et al. 1998), the initial-final mass relation suggests a progenitor of about 6-7 which means that we can expect another 60-70 Myr for the pre-white-dwarf evolution. Hence, an age only somewhat above 200 Myrs may be more in line with this nearby open cluster. More recent white dwarf cooling models of Salaris et al. (2000) (models with a pure hydrogen atmosphere) suggest the age of the white dwarf of 111 Myrs derived from the V-magnitude and the temperature published by Holberg et al. (1998). Assuming the lifetime of the progenitor of the white dwarf of 46 Myrs this leads to an age of the UMa cluster of 157 Myrs.
The comparison of the age using Baraffe et al. (1998) (70-130 Myrs) to the ages of the Ursa Major Cluster (200-300 Myrs) indicate that either: (i) the Ursa Major Cluster has a larger than expected age spread, (ii) there are problems with the models at a solar and/or at mass, (iii) the canonical age for the Ursa Major Cluster is too high (300 Myrs), or (iv) Ori is not a member of the Cluster. Considering possibility (i), we note that the age spread of 70-300 Myrs seems too large for a Cluster. As for the option (iv), Ori is a classical member of the Ursa Major Cluster, located near the cluster center. The spectrum of Ori A would support an age of 200 Myrs regarding the activity indicators, as would the cooling tracks for the Sirius B white dwarf.
Acknowledgements
This research has made use of the SIMBAD database, operated at CDS, Strasbourg, France. B.K. wants to thank F. Dufey for help with the algebra. R.N. wishes to acknowledge financial support from the Bundesministerium für Bildung und Forschung through the Deutsches Zentrum für Luft- und Raumfahrt e.V. (DLR) under grant number 50 OR 0003. R.J. wishes to acknowledge support from NASA grant NAG5-11905. Some of the Data presented herein were obtained at the W. M. Keck Observatory, which is operated as a scientific partnership among the California Institute of Technology, the University of California and the National Aeronautics and Space Administration. The Observatory was made possible by the generous financial support of the W. M. Keck Foundation. The authors wish to recognize and acknowledge the very significant cultural role and religious significance that the summit of Mauna Kea has always had within the indigenous Hawaiian community. We are most fortunate to have the opportunity to conduct observations from this mountain. The authors would like to thank Randy Campbell and David LeMignant for help during the observing nights. We thank the referee, G. Gatewood for the helpful comments.