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 | ![]() |
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-
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4771-1051 |
4771-1097 | 12.43 | 0.79 | K6.0 | 137.9686 | ![]() |
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-
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4771-1051 |
r053907-0228 | 14.33 | 1.41 | M3.0 | 137.9881 | ![]() |
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-
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4771-1051 |
J053958.1-022619 | 14.19 | 1.41 | M3.0 | 138.0676 | ![]() |
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-
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4771-1051 |
J053920.5-022737 | 13.51 | 1.34 | M2.0 | 138.1046 | ![]() |
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-
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4771-1051 |
r053833-0236 | 13.71 | 1.54 | M4.0 | 138.1237 |
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-
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4771-1051 |
M3.0 | 139.1788 | ![]() |
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-
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- | |||
M3.5 | 204.0726 | ![]() |
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-
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4771-1051 | |||
J053949.3-022346 | 15.14 | 1.80 | M4.0 | 138.1696 |
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-
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4771-1051 |
4771-1051 | 12.33 | 0.79 | K7.5 | 138.2073 | ![]() |
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-
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Gl14 |
K8.0 | 204.0912 | ![]() |
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-
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- | |||
J053715.1-024202 | 15.07 | 1.63 | M4.0 | 138.9739 | ![]() |
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-
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r053833-0236 |
J053951.6-022248 | 14.59 | 1.91 | M5.5 | 139.0881 |
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-
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r053833-0236 |
SOri45 | 19.59 | 2.88 | M8.5 | 168.4644 |
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-
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-![]() |
vB10 |
SOri27 | 17.07 | 2.13 | M6.5 | 168.5276 | ![]() |
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-
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vB10 |
r053820-0237 | 12.83 | 0.94 | M5.0 | 203.8482 |
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-
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4771-1051 |
r053831-0235 | 13.52 | 1.09 | M0.0 | 203.8849 | ![]() |
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-
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4771-1051 |
4771-899 | 12.08 | 0.82 | K7.0 | 203.9329 | ![]() |
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-
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4771-1051 |
J053847.5-022711 | 14.46 | 1.74 | M5.0 | 203.9476 | ![]() |
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-
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4771-1051 |
J054005.1-023052 | 15.90 | 1.80 | M5.0 | 204.0101 |
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-
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4771-1051 |
J054001.8-022133 | 14.32 | 1.52 | M4.0 | 204.0382 |
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-
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4771-1051 |
r053838-0236 | 12.37 | 0.86 | K8.0 | 205.9079 | ![]() |
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-
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4771-1051 |
4771-41 | 12.82 | 0.82 | K7.0 | 205.9222 |
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-
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4771-1051 |
4771-1038 | 12.78 | 0.90 | K8.0 | 206.0002 | ![]() |
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-
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4771-1051 |
r053840-0230 | 12.80 | 0.94 | M0.0 | 206.0299 | ![]() |
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-
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4771-1051 |
r053820-0234 | 14.58 | 1.59 | M4.0 | 207.0720 |
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-
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4771-1051 |
r053849-0238 | 12.88 | 1.00 | M0.5 | 515.2615 | ![]() |
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-
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Gl873, Gl182 |
r053923-0233 | 14.16 | 1.23 | M2.0 | 515.3933 | ![]() |
![]() |
-
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Gl873, Gl182 |
J053827.4-023504 | 14.50 | 1.33 | M3.5 | 517.4297 |
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-
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Gl873, Gl182 |
J053914.5-022834 | 14.75 | 1.48 | M3.5 | 518.2596 | ![]() |
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-- | ![]() |
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 ![]() ![]() |
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![]() |
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![]() ![]() ![]() ![]() ![]() |
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![]() ![]() |
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 | ![]() |
![]() |
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H![]() |
![]() |
![]() |
![]() |
(-51000) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | (Å) | |
r053833-0236 | 138.1237 |
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138.1433 |
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|
J053949.3-022346 | 138.1696 |
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SOri45b | 168.4644 | - | ![]() |
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J054001.8-022133 | 204.0382 |
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204.0531 |
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|
4771-41 | 205.9222 |
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blended |
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205.9366 |
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|
r053840-0230 | 206.0299 | ![]() |
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206.0582 |
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|
r053849-0238 | 515.2615 |
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J053827.4-023504 | 517.4297 |
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![]() |
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.
![]() |
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 16:
Pseudo-equivalent widths of Li I
![]() |
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.
Copyright ESO 2002