A&A 384, 937-953 (2002)
DOI: 10.1051/0004-6361:20020046
M. R. Zapatero Osorio1,2,3 - V. J. S. Béjar 4 - Ya. Pavlenko5 - R. Rebolo4,6 - C. Allende Prieto7 - E. L. Martín8 - R. J. García López4,9
1 - Division of Geological and Planetary Sciences, MS 150-21,
California Institute of Technology, Pasadena, CA 91125, USA
2 -
Mount Wilson Observatory, 740 Holladay Road, Pasadena, CA 91106, USA
3 -
Currently at: LAEFF-INTA, ESA Satellite Tracking Station, PO 50727,
28080 Madrid, Spain
4 -
Instituto de Astrofísica de Canarias, 38200 La Laguna, Tenerife,
Spain
5 -
Main Astronomical Observatory of Academy of Sciences of Ukraine,
Golosiiv woods, Kyiv-127, 03680, Ukraine
6 -
Consejo Superior de Investigaciones Científicas, Madrid, Spain
7 -
McDonald Observatory and Department of Astronomy, University of
Texas, Austin, TX 78712-1083, USA
8 -
Institute for Astronomy, Univ. of Hawaii at Manoa, Honolulu,
HI 96822, USA
9 - Departamento de Astrofísica, Universidad de La Laguna,
38206 La Laguna, Tenerife, Spain
Received 24 August 2001 / Accepted 2 January 2002
Abstract
We present intermediate- and low-resolution optical spectra
around H
and Li I
6708Å for a sample of
25 low mass stars and 2 brown dwarfs with confirmed membership in
the pre-main sequence stellar
Orionis cluster. Our
observations are intended to investigate the age of the cluster. The
spectral types derived for our target sample are found to be in the
range K6-M8.5, which corresponds to a mass interval of roughly
1.2-0.02
on the basis of state-of-the-art evolutionary
models. Radial velocities (except for one object) are found to be
consistent with membership in the Orion complex. All cluster members
show considerable H
emission and the Li I resonance
doublet in absorption, which is typical of very young ages. We find
that our pseudo-equivalent widths of H
and Li I
(measured relative to the observed local pseudo-continuum formed by
molecular absorptions) appear rather dispersed (and intense in the
case of H
)
for objects cooler than M3.5 spectral class,
occurring at the approximate mass where low mass stars are expected
to become fully convective. The least massive brown dwarf in our
sample, SOri45 (M8.5,
0.02
), displays
variable H
emission and a radial velocity that differs from
the cluster mean velocity. Tentative detection of forbidden lines in
emission indicates that this brown dwarf may be accreting mass from
a surrounding disk. We also present recent computations of Li
I
6708Å curves of growth for low gravities and for
the temperature interval (about 4000-2600K) of our sample. The
comparison of our observations to these computations allows us to
infer that no lithium depletion has yet taken place in
Orionis, and that the observed pseudo-equivalent widths
are consistent with a cluster initial lithium abundance close to the
cosmic value. Hence, the upper limit to the
Orionis
cluster age can be set at 8Myr, with a most likely value around
2-4Myr.
Key words: circumstellar matter - stars: abundances -
stars: late-type - stars: low mass, brown
dwarfs - stars: pre-main sequence - open clusters and
associations:
Orionis
Lithium absorption features in optical spectra can be used as a tracer
of the stellar internal structure. In addition, lithium is valuable to
assess the age of stars in clusters. Dating young clusters and field
objects based on lithium analysis is a procedure nearly independent of
distance and reddening, in marked contrast to the isochrone-fitting
technique. Moreover, lithium isochrones do not significantly depend on
metallicity (D'Antona 2000), rendering the lithium dating
technique very powerful. Pre-main sequence stars with large convective
regions burn lithium efficiently on short time scales (see
Pinsonneault 1997 for a review) as soon as the temperature at
the base of the convective zone becomes hot enough to undergo the
nuclear reaction 7Li+p
4He+
.
Stars
smaller than the Sun require only about 10-15Myr to deplete this
element by one order of magnitude, and all M-type stars are observed
to have destroyed their lithium at ages around 20-40Myr (e.g.,
Pinsonneault et al. 1990; D'Antona & Mazzitelli
1994, 1997; Baraffe et al.
1998). Furthermore, lithium detections in fully convective
objects near and below the substellar limit have been successfully
used to constrain the ages of clusters like the Pleiades (Basri et al. 1996;
Martín et al. 1998;
Stauffer et al. 1998),
Persei
(Stauffer et al. 1999), and IC2391 (Barrado y
Navascués et al. 1999). Lithium dating, which is
fundamentally a nuclear age calibrator, can be considered reliable
even though some uncertainties (rotation, activity, mixing processes)
may affect theoretical calculations.
Recently, various groups have investigated the stellar and substellar
populations around the bright, massive and multiple O9.5V-type star
Orionis, which gives its name to the association (Walter et al. 1994; Wolk 1996; Walter et al.
1998; Béjar et al. 1999;
Zapatero Osorio et al. 1999, 2000; Béjar et al. 2001). These authors have adopted a cluster age
between 1Myr and 7Myr (Blaauw 1964; Warren & Hesser
1978; Brown et al. 1994). This is
the age interval estimated for the O9.5V-type star based on its
physical properties, evolutionary stage (still burning hydrogen on the
main sequence) and membership in the Orion OB1b subgroup (Blaauw
1991). Other properties of the
Orionis cluster,
e.g., distance (352pc) and reddening (
mag), are
discussed in Béjar et al. (2001). Here we examine low
mass stars and brown dwarfs with confirmed membership to determine the
most likely age of the cluster. We report on observations of
intermediate- and low-resolution optical spectroscopy in
Sects. 3 and 4. A discussion and main
conclusions are given in Sects. 5
and 6, respectively.
| Object | I | Obs. date | Observ. | Disp. | Wl. range | Exp. time | |
| (
|
(mag) | (UT) | (Å/pix) | (Å) | (s) | ||
| 4771-1075 | 05 39 05.3 -2 32 30 | 12.66 | 20 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 700 |
| 4771-1097 | 05 38 35.7 -2 30 43 | 12.43 | 20 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 800 |
| r053907-0228 | 05 39 07.6 -2 28 23 | 14.33 | 20 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 2 |
| SOriJ053958.1-022619 | 05 39 58.1 -2 26 19 | 14.19 | 21 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 2 |
| SOriJ053920.5-022737 | 05 39 20.5 -2 27 37 | 13.51 | 21 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 2 |
|
r053833-0236 |
05 38 33.9 -2 36 38 | 13.71 | 21 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 2 |
| 22 Nov. 1998 | CAHA | 2.41 | 6194-10000 | 650 | |||
| 26 Jan. 1999 | ORM | 0.84 | 6034-6840 | 1200 | |||
| SOriJ053949.3-022346 | 05 39 49.3 -2 23 46 | 15.14 | 21 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 1800 |
|
4771-1051 |
05 38 44.1 -2 40 20 | 12.33 | 21 Nov. 1998 | CAHA | 0.55 | 6220-7297 | 900, 535 |
| 26 Jan. 1999 | ORM | 0.84 | 6034-6840 | 1200 | |||
| SOriJ053715.1-024202 | 05 37 15.1 -2 42 02 | 15.07 | 21 Nov. 1998 | CAHA | 2.41 | 6194-10000 | 600 |
| SOriJ053951.6-022248 | 05 39 51.6 -2 22 48 | 14.59 | 22 Nov. 1998 | CAHA | 2.41 | 6194-10000 | 2 |
| SOri45 | 05 38 25.5 -2 48 36 | 19.59 | 21 Dec. 1998 | Keck | 0.85 | 6324-8025 | 3 |
| SOri27 | 05 38 17.3 -2 40 24 | 17.07 | 21 Dec. 1998 | Keck | 0.85 | 6324-8025 | 2 |
| r053820-0237 |
05 38 20.3 -2 37 47 | 12.83 | 25 Jan. 1999 | ORM | 0.84 | 6034-6993 | 2 |
| r053831-0235 |
05 38 31.4 -2 35 15 | 13.52 | 25 Jan. 1999 | ORM | 0.84 | 6034-6840 | 600, 1800 |
| 4771-899 |
05 38 47.9 -2 27 14 | 12.08 | 25 Jan. 1999 | ORM | 0.84 | 6034-6840 | 300 |
| SOriJ053847.5-022711 | 05 38 47.5 -2 27 11 | 14.46 | 26 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| SOriJ054005.1-023052 | 05 40 05.1 -2 30 52 | 15.90 | 26 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| SOriJ054001.8-022133 | 05 40 01.8 -2 21 33 | 14.32 | 26 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
|
r053838-0236 |
05 38 38.0 -2 36 38 | 12.37 | 27 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| 4771-41 | 05 38 27.1 -2 45 10 | 12.82 | 27 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| 4771-1038 |
05 39 11.5 -2 36 03 | 12.78 | 28 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| r053840-0230 |
05 38 40.2 -2 30 19 | 12.80 | 28 Jan. 1999 | ORM | 0.84 | 6034-6840 | 2 |
| r053820-0234 | 05 38 20.4 -2 34 09 | 14.58 | 29 Jan. 1999 | ORM | 0.84 | 6034-6840 | 900, 1800 |
|
r053849-0238 |
05 38 49.0 -2 38 21 | 12.88 | 03 Dec. 1999 | McDonald | 0.70 | 6150-6850 | 5 |
| r053923-0233 |
05 39 22.7 -2 33 33 | 14.16 | 03 Dec. 1999 | McDonald | 0.70 | 6150-6850 | 8 |
| SOriJ053827.4-023504 | 05 38 27.4 -2 35 04 | 14.50 | 05 Dec. 1999 | McDonald | 0.70 | 6150-6850 | 12 |
| SOriJ053914.5-022834 | 05 39 14.5 -2 28 34 | 14.75 | 06 Dec. 1999 | McDonald | 0.70 | 6150-6850 | 2 |
| SOriJ053820.1-023802 | 05 38 20.1 -2 38 02 | 14.41 | 06 Dec. 1999 | McDonald | 0.70 | 6150-6850 | 10 |
| Run | Observ. | Teles. | Spectrograph | Grating | Detector | Spatial res. | Slit width |
| 20 Nov. 1998 | CAHA | 3.5-m | TWIN | T06 | SITe
|
0.56
|
1.2
|
| 21 Nov. 1998 | CAHA | 3.5-m | TWIN | T11 | SITe
|
0.56
|
1.2
|
| 20 Dec. 1998 | Keck | Keck II | LRIS | 900/5500 |
|
0.22
|
1.0
|
| 25-28 Jan. 1999 | ORM | INT | IDS | R1200Y | Tektronix
|
0.70
|
1.7
|
| 03-06 Dec. 1999 | McDonald | 2.1-m | ES2 | #25 | Craf/Cassini
|
2.72
|
2.1
|
Our list of 28 targets (
,
![]()
4200-2400K) comprises
Orionis solar-mass
and low mass stars, and brown dwarfs selected from different surveys
(see Table 1). All have been identified as genuine cluster
members using various techniques. Stars labelled with "4771'' and
"r'' were first identified by Wolk (1996). VRIJHKphotometry, spectroscopy, and strong X-ray detections (in many cases)
are available. Wolk (1996) provided equivalent widths of the
Li I resonance doublet for a few of these stars. However, his
spectroscopic data of relatively faint sources have poor
signal-to-noise (S/N) ratios, which severely affects the measurements.
We decided to re-observe them to improve the quality of the spectra.
SOri targets (IAU nomenclature) have been selected from the RIJsurvey of Béjar (2001). They nicely fit in the cluster
optical-infrared sequence. Albeit we lack previous spectroscopic data
for them, the spectra presented here confirm them as very active,
young sources, and therefore, they have to be cluster members. The two
brown dwarfs in our sample, SOri27 and 45, have been taken from
Béjar et al. (1999), where they are discussed at length.
Names, coordinates and I magnitudes of our sample are provided in
Table 1. Their location in the optical color-magnitude diagram
is illustrated in Fig. 1, where RI photometry has been taken
from Wolk (1996), Béjar et al. (1999) and Béjar
(2001). Overplotted are the solar metallicity, and
"no-dust'' 3Myr and 5Myr isochrones of D'Antona & Mazzitelli
(1997) and Baraffe et al. (1998),
respectively. Masses as predicted by the models are indicated in the
figure. Comparisons with other tracks are provided in Béjar et al.
(1999). Our targets have masses ranging from
1.2
down to roughly 0.02
.
![]() |
Figure 1:
Optical color-magnitude diagram of our
|
| Open with DEXTER | |
![]() |
Figure 2: CAHA spectra. Data have been normalized to the counts at around 7050Å and shifted by 1 in the upper panel and by 1.5 in the lower panel for clarity. |
| Open with DEXTER | |
![]() |
Figure 3: ORM spectra. Data have been normalized to the counts at around 6535Å and shifted by 1 for clarity. |
| Open with DEXTER | |
![]() |
Figure 4:
Keck spectra of two brown
dwarfs in the |
| Open with DEXTER | |
![]() |
Figure 5: McDonald spectra. Data have been normalized to the counts at around 6540Å and shifted by 1 for clarity. |
| Open with DEXTER | |
Raw images were reduced with standard procedures including bias
subtraction and flat-fielding within NOAO IRAF
. We extracted object and sky spectra using the optimal
extraction algorithm available in the APEXTRACT package. A full
wavelength solution from calibration lamps taken immediately after
each target was applied to the spectra. The rms of the fourth-order
polynomial fit to the wavelength calibration is typically 5-10% the
nominal dispersion. To complete the data reduction, we corrected the
extracted spectra for instrumental response using data of
spectrophotometric standard stars (HD19445, Feige34, G191B2B,
BD+262606) obtained on the same nights and with the same
instrumental configurations. These stars have fluxes available in the
IRAF environment (Massey et al. 1988).
The resulting spectra are depicted in
Figs. 2-5. They are ordered by increasingly
late spectral type and shifted by a constant for clarity. The region
around the Li I
6708Å line is amplified in
Figs. 6-9. In Fig. 7 we have
included the spectrum of the field M6-type spectroscopic standard star
Gl406 for a better comparison.
![]() |
Figure 6:
Region around the Li I
|
| Open with DEXTER | |
![]() |
Figure 7:
Region around the
Li I |
| Open with DEXTER | |
![]() |
Figure 8:
Region around the
Li I |
| Open with DEXTER | |
![]() |
Figure 9:
Region around
the Li I |
| Open with DEXTER | |
| Objecta | I | R-I | Sp.T.b | MJDc | pEWd (H |
pEWe (Li I) | log
|
vr | Template |
| (-51000) | (Å) | (Å) | (kms-1) | ||||||
| 4771-1075 | 12.66 | 0.87 | K7.0 | 137.9536 |
|
-
|
4771-1051 | ||
| 4771-1097 | 12.43 | 0.79 | K6.0 | 137.9686 |
|
-
|
4771-1051 | ||
| r053907-0228 | 14.33 | 1.41 | M3.0 | 137.9881 |
|
-
|
4771-1051 | ||
| J053958.1-022619 | 14.19 | 1.41 | M3.0 | 138.0676 |
|
-
|
4771-1051 | ||
| J053920.5-022737 | 13.51 | 1.34 | M2.0 | 138.1046 |
|
-
|
4771-1051 | ||
| r053833-0236 | 13.71 | 1.54 | M4.0 | 138.1237 |
|
|
-
|
4771-1051 | |
| M3.0 | 139.1788 |
|
-
|
- | |||||
| M3.5 | 204.0726 |
|
-
|
4771-1051 | |||||
| J053949.3-022346 | 15.14 | 1.80 | M4.0 | 138.1696 |
|
|
-
|
4771-1051 | |
| 4771-1051 | 12.33 | 0.79 | K7.5 | 138.2073 |
|
-
|
Gl14 | ||
| K8.0 | 204.0912 |
|
-
|
- | |||||
| J053715.1-024202 | 15.07 | 1.63 | M4.0 | 138.9739 |
|
-
|
r053833-0236 | ||
| J053951.6-022248 | 14.59 | 1.91 | M5.5 | 139.0881 |
|
|
-
|
r053833-0236 | |
| SOri45 | 19.59 | 2.88 | M8.5 | 168.4644 |
|
|
-
|
- |
vB10 |
| SOri27 | 17.07 | 2.13 | M6.5 | 168.5276 |
|
-
|
vB10 | ||
| r053820-0237 | 12.83 | 0.94 | M5.0 | 203.8482 |
|
|
-
|
4771-1051 | |
| r053831-0235 | 13.52 | 1.09 | M0.0 | 203.8849 |
|
-
|
4771-1051 | ||
| 4771-899 | 12.08 | 0.82 | K7.0 | 203.9329 |
|
-
|
4771-1051 | ||
| J053847.5-022711 | 14.46 | 1.74 | M5.0 | 203.9476 |
|
-
|
4771-1051 | ||
| J054005.1-023052 | 15.90 | 1.80 | M5.0 | 204.0101 |
|
|
-
|
4771-1051 | |
| J054001.8-022133 | 14.32 | 1.52 | M4.0 | 204.0382 |
|
|
-
|
4771-1051 | |
| r053838-0236 | 12.37 | 0.86 | K8.0 | 205.9079 |
|
-
|
4771-1051 | ||
| 4771-41 | 12.82 | 0.82 | K7.0 | 205.9222 |
|
|
-
|
4771-1051 | |
| 4771-1038 | 12.78 | 0.90 | K8.0 | 206.0002 |
|
-
|
4771-1051 | ||
| r053840-0230 | 12.80 | 0.94 | M0.0 | 206.0299 |
|
-
|
4771-1051 | ||
| r053820-0234 | 14.58 | 1.59 | M4.0 | 207.0720 |
|
|
-
|
4771-1051 | |
| r053849-0238 | 12.88 | 1.00 | M0.5 | 515.2615 |
|
-
|
Gl873, Gl182 | ||
| r053923-0233 | 14.16 | 1.23 | M2.0 | 515.3933 |
|
-
|
Gl873, Gl182 | ||
| J053827.4-023504 | 14.50 | 1.33 | M3.5 | 517.4297 |
|
|
-
|
Gl873, Gl182 | |
| J053914.5-022834 | 14.75 | 1.48 | M3.5 | 518.2596 | -- | Gl873, Gl182 | |||
| J053820.1-023802 | 14.41 | 1.60 | M4.0 | 518.3899 |
|
-
|
Gl873, Gl182 |
| a Note the drop of "SOri'' for some objects. b Uncertainty of half a subclass. c Modified Julian date at the beginning of the exposure. d In emission. Whenever more than one spectrum available, the pEW has been measured over the combined data. e In absorption. Whenever more than one spectrum available, the pEW has been measured over the combined data. |
We note that our spectral classification relies on field dwarf objects
with high gravities. The gravity of
Orionis cluster members
is expected to be around logg=4.0 (CGS units) according to the
evolutionary models of Baraffe et al. (1998) and
D'Antona & Mazzitelli (1994). Older K-type stellar
counterparts in the field (
5Gyr) display similar gravities,
but early-M and late-M stars have values 0.5dex and 1.0dex larger,
respectively. Cool giants are characterized by very low gravities
(logg=1.5-2, Bonnell & Tell 1993; van Belle
1999). Therefore, it is reasonable to base the spectral
classification of young late-type objects on a scheme intermediate
between that of dwarfs and that of giants. Luhman (1999)
successfully applied this exercise to members of the young cluster
IC348, inferring that the spectral classification of objects like
those of
Orionis can be obtained from dwarfs with an
accuracy up to half a subclass. We have confirmed this by comparing
the optical spectrum of our M8.5 brown dwarf with brown dwarfs of
identical types in
Oph and IC348 (Luhman et al.
1997; Luhman 1999). The three spectra overlap
very nicely. We are confident that the spectral types given in
Table 3 are reliable within the quoted uncertainty.
![]() |
Figure 10:
I magnitude against spectral
type for |
| Open with DEXTER | |
Since the spectral classification reflects effective temperatures,
cluster members should lie along a defined sequence in magnitude
vs. spectral type diagrams. The
Orionis spectroscopic
sequence is depicted in Fig. 10, where we have combined data
presented here with data taken from Béjar et al. (1999),
Barrado y Navascués et al. (2001a) and Martín et
al. (2001). We note that the figure covers a wide range
of masses: stars, brown dwarfs and planetary-mass objects.
Free-floating low mass stars and isolated planetary-mass objects in
the
Orionis cluster have luminosities in the I-band that
differ by about 3 orders of magnitude. Because substellar objects
contract and fade very rapidly, such a difference becomes incredibly
large at older ages, e.g., 8 orders of magnitude at 100Myr (Chabrier
et al. 2000).
Radial velocities, their uncertainties and the templates used are
provided in Table 3. We took special care in cross-correlating
spectral windows (e.g. 6100-6800Å, 8400-8800Å) that are
not affected by telluric absorptions and that contain many
photospheric lines. In addition, we considered only parts of the
spectra free of emission lines. The error bars in the table point to a
possible 1/4 pixel uncertainty in the Fourier cross-correlation
technique (Martín et al. 1999; Lane et al.
2001). We have checked this by cross-correlating the McDonald
spectra against two reference stars. The spectrum of SOri45 is
rather noisy, and the quoted error bar comes from the dispersion
observed after cross-correlating different spectral regions. The
majority of our radial velocities are obtained to an accuracy of the
order of 10kms-1. After discarding the largest and smallest
radial velocity values from Table 3 (i.e., r053820-0237 and
SOri45, respectively), the mean heliocentric radial velocity of
our
Orionis sample is
=37.3kms-1 with a
standard deviation of 5.8kms-1. This is comparable to the
systemic radial velocity of the cluster's central star, which has been
determined to be in the range 27-38kms-1 (Bohannan &
Garmany 1978; Garmany et al. 1980; Morrell
& Levato 1991). Additionally, these velocities (except
for one, see Sect. 5) are consistent with our sample
belonging to the Orion OB association (Alcalá et al.
2000), and their distribution is significantly different
from that of field stars.
We derived H
pseudo-equivalent widths via direct integration
of the line profile with the task SPLOT in IRAF. We note
that given the cool nature of our sample, equivalent widths in the
optical are generally measured relative to the observed local
pseudo-continuum formed by (mainly TiO) molecular absorptions
(Pavlenko 1997). We will refer to these equivalent widths as
"pseudo-equivalent widths'' (pEWs).
Because of the resolution of our observations, broad H
lines
appear blended with other nearby spectral features. The results of our
measurements, given in Table 3, have been extracted by adopting
the base of the line as the continuum. The error bars were obtained
after integrating over the reasonable range of possible continua.
Although this procedure does not give an absolute equivalent width,
i.e., measured with respect the real continuum, it is commonly used by
various authors, and allows us to compare our values with those
published in the literature. We note that all of our program objects
show H
in emission and that no significant H
variability is found in any of them, except for r053833-0236 and
SOri45. We also note that the H
emission of the fast
rotator 4771-1097 is not stronger than that of other similar-type
cluster members.
![]() |
Figure 11:
Pseudo-equivalent widths of H |
| Open with DEXTER | |
Figure 11 shows the distribution of H
pEWs as a function
of spectral type. Effective temperatures are given on the basis of the
temperature - spectral-type relationships by Leggett et al.
(1996), Jones et al. (1995) and Bessell
(1991). Masses as inferred from the 5Myr evolutionary
isochrone of Baraffe et al. (1998) are also indicated in
the figure. In general, there is a trend of increasing H
emission for cooler spectral classes, i.e., for lower masses. This
behavior has been observed in various young clusters, like the
Pleiades and Hyades (Stauffer et al. 1994), IC4665
(Prosser 1993),
Persei (Prosser
1994), and Praesepe (Barrado y Navascués et al. 1998). The relative increase of H
in
M-dwarfs may be (at least partially) explained by the drop of the flux
continuum and the larger TiO molecular absorptions in the optical as a
consequence of cooler
s. We note that, on average,
H
for a given spectral type is slightly larger in
Orionis than in other open clusters. This is very likely a
direct consequence of the marked youth of
Orionis.
![]() |
Figure 12:
Double-peak H |
| Open with DEXTER | |
In Fig. 11 H
emission appears very strong
(
Å) and dispersed for late spectral classes
(
M3.5), corresponding to masses below 0.25
at the
age of
Orionis. Various authors have found an apparent
"turnover'' in the distribution of H
emission in the Pleiades
(Stauffer et al. 1994; Hodgkin et al.
1995) and
Persei (Zapatero Osorio et al.
1996). Pleiades and
Per stars with spectral types
later than M3.5-M4 show a lower level of emission than stars with
warmer classes. The authors suggest that this turnover is due to the
transition from radiative to convective cores. By inspecting D'Antona
& Mazzitelli (1994) pre-main sequence evolutionary
models, we find that this transition takes place at masses
0.3-0.2
regardless of age. In
Orionis we do
not see a drop in the H
emission of fully convective objects,
but an enhacement. The source of such large emission clearly
diminishes by the age of the
Persei cluster (90Myr,
Stauffer et al. 1999). However, the emission level of
more massive stars remains with similar strengths.
![]() |
Figure 13:
Ratio of H |
| Open with DEXTER | |
Three stars in our sample, namely 4771-41 (K7),
SOriJ054001.8-022133 (M4) and 4771-899 (K7), show profiles of
H
emission similar to those of classical TTauri (CTT) stars,
i.e., double peak structure and very broad lines spanning over
300kms-1 from the line center. We illustrate in
Fig. 12 the region around H
for these objects. While
the emission intensity is rather large in 4771-41 and
SOriJ054001.8-022133 (pEWs above 45Å), it is moderate in
4771-899.
| [O I] | [N II] | He I | [S II] | ||||||
| Object | MJDa | H |
|||||||
| (-51000) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | |
| r053833-0236 | 138.1237 |
|
|
|
|
|
|
|
|
| 138.1433 |
|
|
|
|
|
|
|
|
|
| J053949.3-022346 | 138.1696 |
|
|
|
|
||||
| SOri45b | 168.4644 | - |
|
|
|||||
| J054001.8-022133 | 204.0382 |
|
|
|
|
|
|
||
| 204.0531 |
|
|
|
|
|
||||
| 4771-41 | 205.9222 |
|
blended |
|
|
|
|
|
|
| 205.9366 |
|
|
|
|
|
|
|||
| r053840-0230 | 206.0299 |
|
|
|
|||||
| 206.0582 |
|
|
|
|
|
||||
| r053849-0238 | 515.2615 |
|
|
||||||
| J053827.4-023504 | 517.4297 |
|
|
|
|||||
| a Modified Julian date at the beginning of the exposure.
b Measures over the combined spectrum. Individual H |
We have calculated the H
luminosity (
)
for
our sample as in Herbst & Miller (1989) and Hodgkin et al. (1995). The ratio of
to bolometric
luminosity (
)
is independent of the
surface area and represents the fraction of the total energy output in
H
.
To derive
we have used bolometric corrections
provided by Monet et al. (1992) and Kenyon & Hartmann
(1995). The logarithmic values of
are listed in Table 3; uncertainties take into
account errors in photometry and in H
pEWs. Figure 13
shows the distribution of log(
)
with
spectral type. For comparison purposes, we have also included the
Pleiades mean values (Hodgkin et al. 1995). In the
Pleiades, the
ratio clearly increases to
a maximum at around the M3 spectral type and then turns over. This is
not observed in the
Orionis cluster, where cooler objects
present larger H
output fluxes than the older Pleiades
spectral counterparts. Discarding
Orionis members with
dex, cluster data
appear to display a flat distribution from late K to late M (i.e., no
dependence on color and mass) at around log(
)=-3.61dex, with a standard deviation of 0.18dex.
Some of our program targets display, however, other permitted
(He I
6678Å) and forbidden ([O I]
6300Å, [N II]
6548,
6583Å,
[S II]
6716,
6731Å) emission lines. We
have measured their pEWs; values are given in Table 4
as a function of Julian date. We note that some contamination from
terrestrial night-sky emission lines may be expected in the
measurements of the faintest sources. The objects of
Table 4 are plotted with different symbols in various
figures of this paper, except for r053833-0236 (for this star we have
used the "quiet'' ORM data). The majority of the targets from Wolk
(1996) are, in addition, classified as strong X-ray emitters
by this author. In contrast to the younger CTT stars, WTT objects are
not accreting mass from disks. However, the presence of He I
and [O I], [N II], [S II] emission lines is
related to jets and outflows, which are typical of CTT stars and
accretion processes (Edwards et al. 1987; Hartigan et al. 1995).
These lines are generally
detected in objects with strong H
emissions
(
Å, see Fig. 11). The coexistence of
Orionis members with properties of WTT and CTT stars is
indeed indicative of ages of a few Myr. It may also indicate that
small objects are accreting for longer periods than are more massive
stars (Hillenbrand et al. 1998; Haisch et al.
2001), provided that their strong H
emissions are
due to disk accretion.
The star r053833-0236 shows strong H
emission and noticeable
forbidden lines of [O I], [N II] and [S II] in
two consecutive CAHA spectra (Fig. 2, upper panel). However,
its H
intensity clearly decreased, and no other emission lines
were present in data collected on the following night
(Fig. 2, lower panel) or with the INT (Fig. 3). The
sources of this episodic flarelike event are not continuous in
r053833-0236, probably indicating inhomogeneus mass infall onto the
star surface.
The case of the brown dwarf SOri45 (
0.02
)
is
particularly interesting and noteworthy. Albeit the detection of
[N II] and [S II] emission lines is affected by large
uncertainties because of the modest quality of the Keck spectrum, this
finding is very encouraging. It suggests that substellar objects, even
those with very low masses, can sustain surrounding disks from which
matter is accreted. Muzerolle et al. (2000) has
recently reported on the evidence for disk accretion in a TTauri
object at the substellar limit. The presence of disks around brown
dwarfs in the Trapezium cluster (
1Myr) has been proved by
Muench et al. (2001). The emission lines observed in
SOri45 indicate that "substellar'' disks can last up to ages like
those of the
Orionis cluster. It is also feasible that the
probable binary nature of SOri45 (see Sect. 5)
triggers the formation of these emission lines. Nevertheless, further
spectroscopic data will be very valuable to confirm the presence of
forbidden emission lines in SOri45. The rapid H
variability of this brown dwarf is also remarkable.
We have computed theoretical optical spectra in the wavelength range
6680-6735Å around the Li I
6708Å resonance
doublet for gravity logg=4.0 (CGS units) and for
=4000-2600K by running the WITA6 code described in
Pavlenko (2000). This code is designed to opperate in the
framework of classical approximations: local thermodynamic equilibrium
(LTE), a plane-parallel geometry, neither sources nor drops of energy.
The synthetical spectra have been obtained using the atmospheric
structure of the NextGen models published in Hauschildt et al. (1999). We have adopted a microturbulent velocity
value of
=2kms-1, solar elemental abundances (Anders
& Grevesse 1989), except for lithium, and solar isotopic
ratios for titanium and oxygen atoms. The ionization-dissociation
equilibria were solved for about 100 different species, where
constants of chemical equilibrium were taken from Tsuji
(1973) and Gurvitch et al. (1979). For the
particular case of the TiO molecule, we have adopted a dissociation
potential of D0=7.9 eV and the molecular line list of Plez
(1998). The atomic line parameters have been taken from the
VALD database (Piskunov et al. 1995), and the procedure
for computing damping constants is discussed in Pavlenko et al.
(1995) and Pavlenko (2001).
Synthetic spectra were originally obtained with a step of 0.03Å in
wavelength, and were later convolved with appropiate Gaussians to
match a resolution of 1.68Å, which corresponds to the majority of
our data. We have produced a grid of theoretical spectra for nine
different abundances of lithium [logN(Li)=1.0, 1.3, ..., 3.1,
3.4, referred to the usual scale of logN(H)=12] and seven
values of
(4000, 3600, 2400, 3200, 3000, 2800 and
2600K), covering the spectral sequence of our program targets.
Determinations of the meteoritic lithium abundance (Nichiporuk &
Moore 1974; Grevesse & Sauval 1998) lie
between logN(Li)=3.1 and 3.4. Extensive lithium studies
performed in solar metallicity, intermediate-age clusters like the
Pleiades (Soderblom et al. 1993),
Per
(Balachandran et al. 1996), Blanco 1
(Jeffries & James 1999), NGC2516 (Jeffries et al. 1998),
and IC2602 and IC2391 (Randich et al. 2001), as well as in the Taurus star-forming region
(Martín et al. 1994) show that non-depleted stars
preserve an amount of lithium compatible with a logarithmic abundance
between 2.9dex and 3.2dex. We will adopt the mean value of
logN0(Li)=3.1 as the cosmic "initial'' lithium abundance.
![]() |
Figure 14:
The upper panel shows theoretical
spectra computed for
|
| Open with DEXTER | |
|
|
logN(Li) | |||||
| (K) | 1.0 | 1.6 | 1.9 | 2.5 | 3.1 | 3.4 |
| 2600 | .357 | .444 | .479 | .552 | .617/.644 |
.656/.694 |
| 2800 | .346 | .440 | .475 | .551 | .623/.675 |
.669/.728 |
| 3000 | .312 | .404 | .441 | .522 | .596/.666 |
.652/.741 |
| 3200 | .296 | .386 | .423 | .504 | .578/.639 |
.637/.729 |
| 3400 | .266 | .350 | .385 | .456 | .544/.634 |
.604/.720 |
| 3600 | .262 | .337 | .373 | .442 | .536/.566 |
.609/.665 |
| 4000 | .189 | .281 | .319 | .403 | .507/.537 |
.588/.620 |
Figure 14 depicts some of our theoretical spectra for
different values of lithium abundance and surface temperature. The
observed spectrum of SOri27 is compared to a few computations in
Fig. 15. Optical spectra at these cool temperatures are
clearly dominated by molecular absorptions of TiO. Only the core of
the lithium line is observable, since the doublet wings are completely
engulfed by TiO lines (Pavlenko 1997). We have obtained the
theoretical Li I
6708Å pEWs via direct integration
of the line profile over the spectral interval 6703.0-6710.8Å.
Many of the lithium LTE curves of growth employed in this work are
presented in Table 5. Various authors (e.g., Magazzù et al. 1992; Martín et al.
1994; Pavlenko et al. 1995; Pavlenko
1998) have shown that the differences between LTE and non-LTE
calculations for cool temperatures are negligible compared to
uncertainties of pEW,
and gravity. Similarly, the
effects of chromospheric activity on the line formation are found to
be of secondary importance (Pavlenko et al. 1995; Houdebine
& Doyle 1995; Pavlenko 1998) and have not been
included in our calculations. The Li I resonance doublet
appears to have very light dependence on the temperature structure of
the outer layers (see also Stuik et al. 1997). We
find a rather poor agreement between the predicted Li I pEWs of
Table 5 and those provided in Pavlenko & Magazzù
(1996). These authors' values are considerably larger because
they measured theoretical equivalent widths (note the drop of
"pseudo'') relative to the computed "real'' continuum, while we have
determined pEWs relative to the computed pseudo-continuum formed by
molecular absorptions.
![]() |
Figure 15:
Synthetic spectra
(
|
| Open with DEXTER | |
![]() |
Figure 16:
Pseudo-equivalent widths of Li I
|
| Open with DEXTER | |
Li I pEWs are plotted against spectral type in
Fig. 16. SOriJ053914.5-022834 is excluded from the
diagram. Overplotted onto the data are the theoretical pEWs for
logg=4.0 and two different lithium abundances:
logN0(Li)=3.1 ("initial'') and logN(Li)=1.9 (about
one order of magnitude of destruction). We have also included in the
figure the "initial'' curve of growth for a slightly larger gravity,
.
The trend of the observations is nicely reproduced
by the logN0(Li) curves, implying that lithium is still
preserved at the age of the
Orionis cluster. We will discuss
this issue further in Sect. 5.2. We note the differences due
to gravity in the Li I curves of growth. Although these
differences are rather small (
Å) for
![]()
3700K, they become twice as large for cooler
temperatures. Given the error bars of the observed Li I pEWs,
we cannot easily discriminate between gravities.
The scatter of the Li I pEWs is considerable for spectral types
cooler than M3.5 (Fig. 16). The problem of the lithium
star-to-star dispersion occurring at
![]()
5300K has
been widely discussed in the literature (e.g., Soderblom et al.
1993; Pallavicini et al. 1993; Russell
1996; Randich et al. 1998; Barrado y
Navascués et al. 2001b). Nevertheless, this phenomenon
still remains obscure and proves challenging to explain theoretically.
The dispersion could be ascribed to a variability in the Li I
line as a consequence of stellar activity, different mixing processes,
presence or absence of circumstellar disks, binarity, or different
rotation rates from star to star. Recently, Fernández & Miranda
(1998) have found that the Li I
6708Å line in the WTT star V410Tau varies according to
its rotational period. From Figs. 11 and 16 we observe
that the region of the largest lithium scatter coincides with that of
the strongest H
emissions. This might indicate that some hot
continuum is "veiling'' the optical spectra (Joy 1945; Basri
& Batalha 1990; Basri et al.
1991), thereby affecting our pEW measurements. We note,
however, that if any "veiling'' exists around H
and Li
I in our spectra, it has to be small compared with that of many
other CTT stars, because there is no clear correlation between strong
H
emission and low values of Li I pEWs (except for
SOriJ053951.6-022248). There are other possible explanations for
the significant Li I pEW scatter, such as different gravities
(objects with low Li I pEWs might have lower gravities, and
therefore, younger ages), and contamination by lithium-depleted
interlopers.
![]() |
Figure 17: Radial velocities against I magnitudes. SOri45 is not included in the figure (see text). |
| Open with DEXTER | |
Only the brown dwarf SOri45 clearly shows a rather discrepant
radial velocity, which differs by more than 2.5
with respect
to the cluster mean velocity. With a mass estimated at around
0.02
(Béjar et al. 1999), SOri45 is the
smallest object in our sample. It might belong to another kinematical
group of young stars, like the Taurus star-forming region or the Gould
Belt. On the basis of its multi-wavelength photometry and
spectroscopy, SOri45 is probably not a member of Taurus. The
distance modulus to Taurus is 5.76 (Wichmann et al.
1998), which would make SOri45 incredibly
overluminous by 2.2mag in the HR diagram. Guillout et al.
(1998) and Alcalá et al. (2000) have shown
that the distribution of candidate members of the Gould Belt for the
particular direction towards Orion lies at 200-300pc from the Sun
and well to the southwest of the Orion A cloud. This is relatively far
away from
Orionis (>55pc). SOri45 fits the
photometric and spectroscopic sequences of the
Orionis
cluster very nicely (Béjar et al. 1999,
2001), supporting its location in the Orion complex.
Furthermore, this brown dwarf displays strong H
emission and
lithium in its atmosphere, which is typical of ages much younger than
that of the Gould Belt (30-80Myr, Alcalá et al.
2000; Moreno et al. 1999), and it
does not show a radial velocity consistent with membership in either
Taurus or the Gould Belt. Alternatively, SOri45 might be a runaway
object of the
Orionis cluster resulting from encounters with
other cluster members; it may have been dynamically ejected from the
multiple system where it originated (Kroupa 1998; Portegies
Zwart et al. 1999; Reipurth & Clarke 2001;
Boss 2001), or SOri45 might be a brown dwarf close
binary. So far none of these hypotheses can be discarded. Further
radial velocity measurements are needed to assess the possible binary
nature. If SOri45 is proved to be a spectroscopic binary, the
dynamical masses of the components will be valuable for testing
theoretical evolutionary tracks at very young ages and substellar
masses.
From Fig. 10 we observe that r053820-0237 (M5) appears remarkably overluminous with respect to the cluster photometric sequence. In addition, its radial velocity is the largest amongst our measurements. These two properties suggest that this star is an equal mass binary.
![]() |
Figure 18: Surface curves for lithium depletions by factors of 3 (logN(Li)=2.5, upper panel) and 10 (logN(Li)=2.0, lower panel) as a function of age and mass. Models are taken from D'Antona & Mazzitelli (1994, dashed line), D'Antona & Mazzitelli (1997, dotted line), Pinsonneault et al. (1990, solid line) and Baraffe et al. (1998, dash-dotted line). |
| Open with DEXTER | |
According to various evolutionary models available in the literature,
very low mass stars (M
0.3
)
burn lithium very
efficiently by one order of magnitude at ages older than 15Myr
(D'Antona & Mazzitelli 1994, 1997;
Pinsonneault et al. 1990; Baraffe et al.
1998). Stars with masses in the interval
0.5-0.8
do it in a shorter time scale. This is
summarized in Fig. 18, which shows surface curves for a given
lithium abundance as a function of age and stellar mass. The age of
the
Orionis cluster will be constrained by late-K and
early-M stars. More massive members (M
0.9
)
need longer times to deplete some lithium, so they are not useful for
our purposes.
Lithium depletion by a factor of 10 will impose a rather conservative
upper limit on the age of the cluster. From Fig. 18 we infer
that this upper limit is around 10Myr (based on Baraffe et al.
1998 and Pinsonneault et al. 1990 models),
because this is the time required by 0.6-0.8
-stars to
consume their lithium from initial abundance down to
logN(Li)=2.0. Models by D'Antona & Mazzitelli
(1994, 1997) predict values that are twice as
young, i.e., around 5Myr. However, since no lithium depletion is
apparent in any cluster member, it seems reasonable to establish
shorter upper limits. If we adopt the surface curve corresponding to a
factor of 3 lithium depletion, the plausible oldest age of the
Orionis cluster is 8Myr (as given by Baraffe et al.
1998 and Pinsonneault et al. 1990 models). We
have also inspected the lithium depletion tracks provided by Proffitt
& Michaud (1989) and Soderblom et al.
(1998) obtaining very similar values. Our result fully
agrees with the maximum age expected for the central, most massive
cluster star to blow up as a supernova (Meynet et al.
1994).
Orionis low mass stars span an age range
similar to that of the early-type members, i.e., the low and high mass
populations are essentially coeval. Similar upper limits are found for
other associations in Orion, like the star-forming region around the
Orionis star (7-8Myr, Mathieu et al.
2001), and Orion WTT stars (Alcalá et al. 1998). We could adopt as the mean cluster age
the oldest isochrone for which lithium is still preserved within
0.2dex across the entire mass range. This occurs at roughly
2-4Myr considering all models, a result in full consistency with
previous analysis of theoretical isochrone fitting to the observed
photometry (Béjar et al. 1999).
An additional constraint to the age of the cluster comes from the
ratio of CTT stars to WTT stars. Based on strong H
emission
and the presence of forbidden emission lines, this ratio turns out to
be in the range 30-40% in
Orionis. Follow-up observations
of our targets (mid-infrared, radio) are, however, desirable to
confirm the presence of circumstellar disks. The ratio obtained in
Orionis is slightly smaller than that of younger regions,
like the area around the Orion Molecular Cloud (ratio
40%,
1-3Myr, Rebull et al. 2000), and considerably larger
than the one of older clusters and associations, like the Sco-Cen OB
association (ratio of 11%), whose population of CTT stars, WTT stars
and post-TTauri stars has been investigated by Martín
(1998). This author defines post -TTauri stars as young,
late-type stars that are burning lithium and display moderate
H
emission. The average age of the whole Sco-Cen OB
association is in the range 5-15Myr, as determined by de Geus et al. (1989). We do not find evidence for the
existence of post-TTauri stars in
Orionis, and hence, this
cluster is essentially younger than the Sco-Cen OB association.
We note the intriguing case of the coolest object in our sample,
SOri45, an M8.5-type brown dwarf with a mass estimated at
0.02
(Béjar et al. 1999). It has a very
intense, variable H
emission and lithium in absorption. Our
tentative detection of forbidden emission lines of [N II] and
[S II] suggests that SOri45 may have a cool, surrounding
disk from which it is accreting. This brown dwarf also displays a
radial velocity that deviates significantly from the cluster mean
velocity.
We have also presented very recent computations of Li I
6708Å curves of growth for low gravities (
and 4.5), cool temperatures (
=4000-2600K), and
lithium abundances in the interval logN(Li)=1.0-3.4. The
distribution of our observed Li I pEWs appears to be well
reproduced by the theoretical pEWs computed for the cosmic lithium
abundance of logN0(Li)=3.1. This leads us to conclude that
lithium has not yet been depleted in the
Orionis cluster.
Therefore, after comparison to various lithium depletion curves
available in the literature, we impose an upper limit to the cluster
age of 8Myr, while the most likely age is in the interval 2-4Myr.
Acknowledgements
We are grateful to I. Baraffe and colleagues for making electronic files of their evolutionary models available to us, and to Louise Good for correcting the English language used in the manuscript. We also thank the staff at McDonald Observatory, especially David Doss, for their helpful assistance. This research has made use of the SIMBAD database, operated at CDS, Strasbourg, France. Partial financial support was provided by the Spanish DGES PB98-0531-C02-02. YP acknowledges partial financial support from Small Research Grant of American Astronomical Society. CAP acknowledges partial financial support from NSF (AST-0086321).