Issue |
A&A
Volume 514, May 2010
|
|
---|---|---|
Article Number | A92 | |
Number of page(s) | 11 | |
Section | Stellar atmospheres | |
DOI | https://doi.org/10.1051/0004-6361/200912227 | |
Published online | 27 May 2010 |
The solar photospheric abundance of carbon
Analysis of atomic carbon lines with the CO5BOLD solar model
E. Caffau1 - H.-G. Ludwig2,1,3 - P. Bonifacio2,1,4 - R. Faraggiana5 - M. Steffen6 - B. Freytag7 - I. Kamp8 - T. R. Ayres9
1 - GEPI, Observatoire de Paris, CNRS, Université Paris Diderot, 92195
Meudon Cedex, France
2 -
CIFIST Marie Curie Excellence Team
3 -
Zentrum für Astronomie der Universität Heidelberg, Landessternwarte, Königstuhl 12, 69117 Heidelberg, Germany
4 -
Istituto Nazionale di Astrofisica,
Osservatorio Astronomico di Trieste, via G.B. Tiepolo 11,
34143 Trieste, Italy
5 -
Università degli Studi di Trieste,
via G.B. Tiepolo 11, 34143 Trieste, Italy
6 -
Astrophysikalisches Institut Potsdam, An der Sternwarte 16, 14482 Potsdam, Germany
7 -
CRAL,UMR 5574: CNRS, Université de Lyon,
École Normale Supérieure de Lyon,
46 allée d'Italie, 69364 Lyon Cedex 7, France
8 -
Kapteyn Astronomical Institute, Postbus 800, 9700 AV Groningen, The Netherlands
9 -
Center for Astrophysics and Space Astronomy, University of Colorado
389 UCB (CASA), Boulder, CO 80309-0389, USA
Received 29 March 2009 / Accepted 9 February 2010
Abstract
Context. The analysis of the solar spectra using
hydrodynamical simulations, with a specific selection of lines, atomic
data, and method for computing deviations from local thermodynamical
equilibrium, has led to a downward revision of the solar
metallicity, Z. We are using the latest simulations
computed with the CO5BOLD code to reassess the solar chemical
composition. Our previous analyses of the key elements, oxygen and
nitrogen, have not confirmed any extreme downward revision of Z, as derived in other works based on hydrodynamical models.
Aims. We determine the solar photospheric carbon abundance with
a radiation-hydrodynamical CO5BOLD model and compute the departures
from local thermodynamical equilibrium by using the Kiel code.
Methods. We measured equivalent widths of atomic C I
lines on high-resolution, high signal-to-noise ratio solar atlases of
disc-centre intensity and integrated disc flux. These equivalent widths
were analysed with our latest solar 3D hydrodynamical simulation
computed with CO5BOLD. Deviations from local thermodynamic equilibrium
we computed in 1D with the Kiel code, using the average temperature
structure of the hydrodynamical simulation as a background model.
Results. Our recommended value for the solar carbon abundance relies on 98 independent measurements of observed lines and is A(C
.
The quoted error is the sum of statistical and systematic errors.
Combined with our recent results for the solar oxygen and nitrogen
abundances, this implies a solar metallicity of Z=0.0154 and
Z/X=0.0211.
Conclusions. Our analysis implies a solar carbon abundance that
is about 0.1 dex higher than what was found in previous analyses
based on different 3D hydrodynamical computations. The difference is
partly driven by our equivalent width measurements (we measure, on
average, larger equivalent widths than the other work based on a 3D
model), in part because of the different properties of the
hydrodynamical simulations and the spectrum synthesis code. The solar
metallicity we obtain from the CO5BOLD analyses is in slightly better
agreement with the constraints of helioseismology than the previous 3D
abundance results.
Key words: Sun: abundances - stars: abundances - hydrodynamics - line: formation
1 Introduction
The importance of an accurate knowledge of the solar abundances can hardly be overstated since they serve as the reference for all other celestial objects. The good performance of the new-generation instruments allows accurate stellar abundances to be derived and therefore the requested accuracy of the reference solar abundances is increased. This can, at least partly, explain the current revival in spectroscopic solar abundance studies. The very large gap in resolution between solar and stellar spectra, which existed until a few decades ago, is diminishing rapidly. The majority of recent solar abundance determinations relies on observational data that are almost 30 years old, both for the disc-centre intensity and for the integrated disc flux (Jungfraujoch grating spectra and Kitt Peak Fourier Transform Spectra, respectively).
For a long time, solar abundances
were considered as well established, and only
minor refinements were suggested
by each new study, usually driven by improved
atomic or molecular data.
By using atomic or molecular lines, or both, the many analyses
of the photospheric solar carbon made in 1980-2000,
were converging toward the value of
A(C
(Grevesse & Sauval 1998),
which was slightly lowering
the previous values by including the appropriate NLTE
corrections.
However, Allende Prieto et al. (2002) have announced a large
downward revision of the C abundance from the analysis
of the forbidden [CI] 872.7 nm line (A(C
).
A subsequent paper by Asplund et al. (2005a) also obtained a similar
downward revision of the carbon abundance when using permitted
atomic and molecular lines.
The new abundances of C, as well as those of other elements, conflict with some solar properties; for instance, solar models (Yang & Bi 2007) and helioseimology (Delahaye & Pinsonneault 2006; Basu & Antia 2008; Chaplin & Basu 2008) cannot be reconciled with the recent revision of solar abundances by Asplund et al. (2005b). Solar abundances of the light elements, which have the highest cosmic abundance, are particularly important for understanding stellar and galactic composition. Besides being the main contributors to the solar metallicity Z, the CNO abundances are useful for studying the depletion in the interstellar gas (ISM). For example, the comparison of the C/O ratio in the ISM with that in the solar photosphere tells us how much C has been locked into dust. Also studying the diffusion effects in the corona and solar wind requires using photospheric solar abundances as a reference. Because it is a highly volatile element, carbon has partly escaped carbonaceous chondrites, so that the solar system abundance of C mainly relies on the analysis of the photospheric spectrum.
The solar spectrum is rich in atomic C lines, as well
as in lines of C-bearing molecules. Because of its high first
ionisation potential (11.26 eV), the measurable lines
of carbon in the Sun are only those of C I.
Several tens of C I
lines are present in the visual and near IR spectrum, but only a few are suitable
for abundance analysis. The chosen lines should be weak, unblended, with
accurately known transition probabilities and, ideally, formed in LTE.
Strong lines, with large equivalent width (EW hereafter,
pm) should be
rejected because the collisional damping constants are uncertain.
Only one forbidden line, at 872.7126 nm, has been detected in the
solar spectrum.
Molecular lines are highly temperature sensitive and require very accurate analysis of the photospheric thermal structure as the one made by Ayres et al. (2006) for the infrared CO features. Holweger (2001) prefers to consider only atomic lines, while Grevesse et al. (1987) derive the carbon abundance from the vibration-rotation and pure rotation lines of the CO and CN diatomic molecules.
In the present paper we analyse only C I atomic transitions to derive the solar photospheric carbon abundance.
2 Selection of lines
As a starting point, we looked at a sample obtained by combining the C I lines chosen by Grevesse et al. (1991), Bièmont et al. (1993), Takeda (1994), and Asplund et al. (2005a) (see Table 1). We examined these lines, comparing the available solar atlases among them and to synthetic profiles. We excluded from our analysis those lines that we judged too heavily blended (e.g. the line at 477.0 nm) compared to the synthetic spectra or the lines for which the disagreement among observed spectra was unexplained and too large (e.g. the line at 1180.1 nm). Furthermore, we eliminated the lines whenever we suspected a significant contamination from telluric absorption, based on the comparison of the observed atlases and synthetic spectra, and also on the inspection of spectra of rapidly rotating stars, indicating the presence of telluric lines (e.g. the line at 1602.1 nm). The excluded lines are flagged by ``3'' in the columns ``Quality'' of Table 1. The final list of our sample of lines, labelled as Quality ``1'' or ``2'' in Table 1, is given in Table 3. We labelled as ``1'' those lines that are not blended, or the blends are negligible in comparison to the C I line, or we think we are able to model the blends. We labelled as ``2'' the lines we are less confident in. These lines show differences among the observed spectra (e.g. the line at 711.1 nm) or we can hardly reproduce their shape with a synthetic profile (e.g. the line at 1734.6 nm) or we are not confident of being able to take the telluric absorptions into account (e.g. the line at 1778.9 nm). The final selection consists of 45 individual lines for which we have 98 EW measurements. The subsample of good data, labelled ``Quality = 1'', contains 25 lines, 66 measured EWs.
Table 1: Lines considered for the abundance determination.
For the abundance determination, one could rely on line-profile fitting or on EW measurements. The line-profile fitting procedure has many advantages because not only the strength of the line is taken into account, but also the line shape. When the synthetic line profile provides a faithful reproduction of the line shape, we consider this procedure superior. We stress here that by ``line-profile'' fitting we mean fitting with a synthetic profile, computed by using all the known lines in the range. But ``fitting'' with a synthetic profile consisting of a single line is conceptually identical to measuring the EW by fitting with a Gaussian or Voigt profile, although it has the advantage of correctly treating the line asymmetry, which is, however, in general irrelevant for abundance work. If poorly known blends interfere, the EW measurement procedure with deblending (see below) is the more reliable option. The present analysis is based on EW measurements. We prefer this approach because of the following problems with the available C I lines.
- A large fraction of the lines are blended and the atomic data of the contaminants are not well known, so that, when included in the 3D synthetic spectra, the comparison with the observed spectra is not reliable. Measurement of the EW, on the other hand, can be reliable, since the extra absorption can be modelled by a suitable Gaussian or Voigt profile.
- Some of the lines are contaminated by telluric absorption; also in this case, the contaminating telluric absorption can be modelled as above providing a reliable measure of the EW.
- The continuum placement is problematic for some lines, because of neighbouring lines whose atomic data are often poorly known. The EW measurement with splot, on the other hand, is designed to handle such situations.
- NLTE effects, not taken into account in the 3D synthetic profile, can change the shape of the line.
For measuring the EW we used the IRAF(Tody 1993) task
splot. In the case of blended lines,
we used the deblending option of splot,
which permits fitting the spectral profile with a number of
Gaussian and/or Voigt functions. In this way any known line in a range
can be simulated with a theoretical profile.
Generally for weak lines we used a Gaussian profile
to fit the observed profile, while we used a Voigt function for strong lines.
For unblended lines we also used direct integration.
We are aware that the observed profile is asymmetric,
while both Gaussian and Voigt functions are symmetric.
Several experiments convinced us that the use of a Voigt profile to measure the EW of an asymmetric
3D profile provides a measurement of the EW which differs from the real one by less than 1%.
This error is surely negligible when compared to the uncertainty
of the EW measurement due to the continuum placement, which in the
case of a typical observed spectrum can reach 5%.
For the majority of the lines, the EWs we obtain are close to the values of Bièmont et al. (1993), but not for all. We could compare only the Delbouille disc-centre spectrum, which is the observed data considered in Bièmont et al. (1993). In principle, strong lines should be rejected because of uncertain values of NLTE corrections and line broadening parameters that become important. We keep these strong lines anyway in the sample, because they do not disagree with the other lines, and there is no evident trend for the abundance as a function of the EW.
When available, we used
from NIST (Wiese et al. 1996), as retrieved
from the ASD database (Ralchenko 2005).
The values are given in Table 3.
All
-values used in Bièmont et al. (1993), except the one of the
801.8 nm line, are very close to the values of NIST.
For our sample of C I, lines the NIST database relies on four sources
(Luo & Pradhan 1989; Weiss 1996; Nussbaumer & Storey 1984; Hibbert et al. 1993), the main one being
Hibbert et al. (1993), which covers all the lines.
For the Van der Waals broadening constants, we proceeded as in Caffau et al. (2008). When available (for 35 lines of our sample), we relied on Barklem et al. (1998) values. For the remaining lines, we used the WIDTH approximation, implemented in the Kurucz routine WIDTH (see Ryan 1998). If we remove the lines without Van der Waals broadening constants from Barklem et al. (1998), the derived carbon abundance is less than 0.03 dex higher than when considering the complete sample of lines. Therefore we decided to keep all the lines we selected for the abundance determination.
3 Equivalent widths in the literature
Reliable observed EWs are those measured by Grevesse et al. (1991) and by Bièmont et al. (1993) on the disc-centre Jungfraujoch Atlas. The values used by Stürenburg & Holweger (1990) are taken from the EW measurements by Baschek & Holweger (1967), which were based on old atlases, and the ones in Asplund et al. (2005a) are the EWs of the synthetic best-fit profile. Only two lines have been considered in all four analyses, and they are presented in Table 2.
Table 2: Comparison of the disc-centre EW of two C I lines determined by different authors.
For the line at 960.3036 nm, we find a significantly larger EW than the three other authors, whose results agree closely. On the other hand, our EW for the line at 2102.3151 nm is very similar to those by Grevesse et al. (1991) and Bièmont et al. (1993), while the theoretical EW derived by Asplund et al. (2005a) from their 3D model by using their best-fit abundance is much lower (see Table 2), even though the measured EWs should be corrected for blending.
We note that Bièmont et al. (1993) gave a low weight to both of these lines, presumably because they are affected by telluric absorption and other blends, making reliable EWs difficult to measure. Nevertheless, Table 2 demonstrates once again that EWmeasurements differ considerably from author to author and are a major source of uncertainty.
All the investigations of the solar carbon abundance cited above rely on a single solar atlas. In fact, as already mentioned in Caffau et al. (2008), the available solar atlases do not always agree. This could be due to telluric absorption, to variability in solar spectrum, or to systematic effects related to the different observations. The present analysis is based on four different solar spectra so should yield more reliable abundances.
Table 3: Line parameters, 3D and 1D carbon abundance (LTE), and 1D NLTE corrections for our sample of selected C I lines.
4 Observed spectra
![]() |
Figure 1: Comparison of the observed disc-centre solar spectrum (dashed lines, DI for the two reddest lines and NI for the others) with the corresponding 3D synthetic profiles (solid lines) for a selection of clean C I lines. |
Open with DEXTER |
5 Model atmospheres
We used the same radiation-hydrodynamical model,
computed with the CO5BOLD code (Freytag et al. 2002; Wedemeyer et al. 2004; Freytag et al. 2003)
used in our previous solar abundance analyses.
Details of the model can be found in Caffau & Ludwig (2007); Caffau et al. (2008).
The same holds for the employed 1D models.
As a reference model we used a plane parallel 1D model
(
with mixing-length parameter of 1.0) that shares the
micro-physics and radiation transfer scheme with CO5BOLD.
We also used a 1D model obtained by temporal and horizontal
averaging of the 3D hydrodynamic structure on surfaces of
equal optical depth (
), as well as the Holweger-Müller
semi-empirical model (Holweger 1967; Holweger & Müller 1974).
When necessary, this was put on a column mass scale,
assuming the same abundances and opacities as in the CO5BOLD model.
For the spectrum synthesis based on the 1D models, we adopted a
microturbulence of 1.0 km s-1, both for disc-centre (intensity)
and integrated disc (flux) spectra.
![]() |
Figure 2: As Fig. 1, but showing the HM synthetic profile (solid lines) superimposed on the observed solar spectrum (dashed lines). To be consistent with Fig. 1, the synthetic profile is computed with Linfor3D, ignoring any blending lines. |
Open with DEXTER |
6 Results
6.1 The [CI] line at 872.7 nm
There is only one observable forbidden [CI] line, located at 872.7126 nm (2p2 1D2 - 2p2 1S0), with a lower level excitation potential of 1.264 eV. This line is important, because it is weak and therefore insensitive to the assumption about the damping constant and, according to Stürenburg & Holweger (1990), not affected by NLTE.
We measured the EW on the two disc-centre and two integrated disc solar spectra.
The result is EW(DI)=0.511 pm, EW(NI)=0.509 pm, EW(NF)=0.517 pm,
EW(KF)=0.508 pm.
We subtracted the contribution of the Fe I blending line
(72.7132 nm,
= -3.93,
eV, EW(Int)=
0.040 pm, EW(Flux)=0.045 pm) according to the 3D computation.
The [CI] line is formed in LTE, so that the LTE abundance derived from
the four observed solar atlases should closely agree. While the two
disc-centre and the two integrated disc spectra are in very good agreement
with each other, we find a difference in the carbon abundance
of 0.04 dex between disc-centre and integrated disc spectra.
This effect could be attributed to NLTE effects on the
blending iron line, which can be different for disc-centre and integrated disc
spectra.
6.2 Permitted lines
The abundances derived from all the lines of our sample
are assembled in Table 3. Atomic data
for each line, the measured EWs, and the derived LTE abundances
using the 3D,
,
and
models are provided in the table.
The total 3D correction, defined as 3D-
is positive for all
the lines, except for the 477.5907 nm line.
The so-called granulation correction, quantified by the difference
3D-
measures the effect of the horizontal temperature fluctuations.
It is never very large and may be in the same direction
as the total 3D correction, or in the opposite direction, depending on
the line.
All our permitted C I lines originate in highly excited lower levels
(
eV).
The 3D-
corrections for the weaker lines (EW <4.0 pm)
in the optical and near infra-red range (450 nm
20 nm)
are small and mostly negative (3D-
<0.01).
We can compare these 3D-
corrections to the value
defined in Steffen & Holweger (2002).
The hydro-simulation they consider is a 2D model, while the 1D model is
the temporal and horizontal average over surfaces of equal optical depth
of their 2D model, meaning that it is similar to our
model.
The C I lines investigated in Steffen & Holweger (2002)
have
nm and
pm.
For
eV,
is indeed slightly negative,
(see their Table 1 and their Fig. 5) in qualitative agreement with
the results found for comparable C I lines in the present study.
Both 3D corrections (3D-
and 3D-
)
increase with EW,
possibly indicating an inadequate choice of the microturbulence
parameter for the 1D models. We cannot discern any trend with
the excitation energy or the wavelength.
We do not yet have the capability of computing
the deviations from local thermodynamic equilibrium (NLTE effects)
in the 3D spectrum synthesis,
and, to our knowledge, such calculations have not yet been performed elsewhere.
As a first approximation, we have therefore computed 1D NLTE corrections
using the
model as a background model.
For each line we computed NLTE corrections with the
Kiel code (Steenbock & Holweger 1984) and the model-atom of Stürenburg & Holweger (1990).
The line blanketing is treated with an opacity distribution function
as provided by Castelli & Kurucz (2003), assuming solar metallicity and a microturbulence
of 2
.
We considered three possible choices for the parameter
quantifying the thermalizing effect of collisions with neutral hydrogen
according to the generalised Drawin approximation (Drawin 1969)
as proposed by Steenbock & Holweger (1984):
- 1.
- classical scaling (
),
- 2.
- no effect of collisions with neutral H (
),
- 3.
- intermediate collisional efficiency (
).
As explained above, we rely on EW measurements for the carbon abundance
determination, because a considerable fraction of the lines is blended,
and NLTE effects are non-negligible. Nevertheless, it is useful to compare
the observed spectrum with the 3D synthetic profiles for some of the cleanest
lines. A few examples are shown in Fig. 1.
The agreement is encouraging, but the abundance needed to achieve the best (visual)
agreement between 3D-synthetic and observed line profile is not always identical
to the abundance obtained from matching the EWs.
This can stem from remaining blends not included in the 3D-synthetic profile, NLTE
effects that can change the shape of the line profile, or the adopted damping constants.
Comparison of Figs. 1 and 2 shows that the
3D synthetic profiles generally can reproduce the observed profiles of the selected clean
C I lines somewhat better than the 1D synthetic profiles calculated from the HM model with a microturbulence of 1.0
.
6.3 The solar carbon abundance
The final carbon abundance depends only weakly
on the assumption made about .
By applying the NLTE corrections to the 3D LTE results and computing
the average of the abundances of Table 3, we obtain
![]() |
(1) |
For reference, the results for the HM model are
![]() |
(2) |
The results from CO5BOLD and HM models are in very good agreement. The carbon abundances from the various lines as a function of wavelength are shown in Fig. 3 for the CO5BOLD model and in Fig. 4 for the HM model.
![]() |
Figure 3:
The carbon abundance as a function of wavelength of the individual
C I lines compiled in Table 3, as obtained from the 3D solar
model for different assumptions about the 1D NLTE corrections, which are
all based on the
|
Open with DEXTER |
![]() |
Figure 4: As Fig. 3, but showing the carbon abundances obtained from the HM model. |
Open with DEXTER |
Our favoured value is A(C
,
obtained by applying the NLTE correction, with
,
to the 3D-LTE abundance.
If we restrict the abundance determination to the lines labelled as
``Quality=1'' in Table 1, the result is
A(C
.
The carbon abundance from the subsample is very close to the one
obtained from the complete sample, only 0.008 dex smaller,
while the line-to-line scatter is much reduced.
Nevertheless, we prefer the result from the complete sample,
since we are aware that the selection of ``good'' lines is somehow
subjective, and hardly changes the mean carbon abundance.
7 Discussion
If we consider the EWs of 55 lines in Bièmont et al. (1993), based on Delbouille disc-centre
spectra, together with the
-values used in that work, we find
A(C
from our 3D model. If we instead use the updated
-values
from the NIST database, we obtain A(C
.
This value can be compared to our LTE result, based on the 40 lines in common
with Bièmont et al. (1993) and measured in the same solar atlas,
of A(C
obtained with the 3D model,
and of A(C
obtained with the HM model.
The LTE abundance based on our complete sample of 98 lines is
A(C
from the 3D model and A(C
from the HM model.
Our abundance is slightly higher than the one of Bièmont et al. (1993) because of
the line selection and differences in the EWs for some lines, but the overall agreement
is very satisfactory.
The 3D-NLTE abundances are obtained by applying the 1D-NLTE corrections with
to the individual 3D-LTE abundances.
All 98 3D-NLTE abundances lie within 3
of the mean value,
A(C
.
When keeping only abundances within 2
of the mean value,
94 values meet the cutoff, and the average becomes A(C
;
within 1
,
70 values still survive, and A(C
.
As expected,
the standard deviation becomes smaller, but the average almost remains the same.
![]() |
Figure 5:
The carbon abundances as a function of EW for the 3D model.
The two numbers in the lower part of the plots indicate the slope of the
best-fit linear relation and its 1 |
Open with DEXTER |
![]() |
Figure 6: The carbon abundances as a function of EW for the HM model. |
Open with DEXTER |
We find no obvious trend in the abundance with the lower level energy, neither for the LTE nor for the NLTE results. However, this is not surprising since all carbon lines of our sample originate in similar high excitation levels, since the range in energy is little more than 2 eV.
There is, however, a clear trend for the 3D-LTE abundances to increase with
EW (see Fig. 5). The trend is reduced or even reversed
after application of the NLTE corrections, depending on the choice of
.
As illustrated in Fig. 5, there is a slight
negative trend of the 3D-NLTE abundance with EW for
,
and a
slightly positive one for
.
The trend vanishes for a value
of
somewhere in the range [0,1/3].
The corresponding results obtained using the HM model are shown in Fig. 6.
This behaviour is similar to what is found with the 3D model, but the slope of
the A(C)-EW relations is systematically reduced (more negative) in all cases.
The results from the HM model suggest that the slope vanished for
close to 1. The correlation A(C)
persists even if we only
consider weak lines, indicating that the slope is in fact caused by NLTE effects.
Without available experimental data on cross sections for collisions with neutral hydrogen,
one might be tempted to fix the value of
empirically by requiring a
vanishing slope in the A(C)-EW plane. Our 3D results would then suggest that
.
However, we prefer to delay this conclusion until a
complete 3D-NLTE computation becomes available.
In the meantime, since obliged to take a decision, we adopt the intermediate
value of
,
which is the favourite value of the Holweger school.
Our carbon abundances are larger than
those derived by Allende Prieto et al. (2002) and
Asplund et al. (2005a). The difference is
striking if we consider the [CI] line.
While the measured EWs are similar,
we adopt an EW that is about
12% smaller than that of Asplund et al. (2005a),
owing to the correction for the blending
Fe I line.
In spite of this, our derived A(C) is 0.11 dex higher
than that of Asplund et al. (2005a).
This must be ascribed to the difference between
the CO5BOLD solar model + Linfor3D and the hydrodynamical
simulation and spectral-synthesis code employed by Asplund et al. (2005a).
The difference between the models (see Fig. 1 in Caffau et al. 2008)
affects both the mean
temperature structure and the temperature
fluctuations in the region where the [CI] line is formed.
Figure 7 shows that the main contribution to the [CI]
line absorption comes from the layers between
,
to -2where the differences between the two hydrodynamical simulations are largest.
Since the mean temperature gradient is steeper in the 3D model of
Asplund et al. (2005a), a lower carbon abundance is needed to reproduce the
observed EW, in qualitative agreement with the results
mentioned above.
The same behaviour has been noticed for the [OI] line at 636.3 nm line
(see Caffau et al. 2008 and Asplund et al. 2004).
![]() |
Figure 7:
3D and
|
Open with DEXTER |
The situation is similar
if we compare the average carbon abundance.
From the permitted C I lines, Asplund et al. (2005a)
derive
.
This value must be compared with our value of
,
which corresponds to
,
and is consistent with the
assumption of Asplund et al. (2005a). Part of the difference stems
from our EWs, which are generally close to those of Bièmont et al. (1993),
hence larger than those of Asplund et al. (2005a). Part of the
difference is, however, due to the different hydrodynamical
model and/or the different spectrum synthesis code.
In Table 4 the carbon abundance determinations in the past thirty
years are listed. The difference of 0.28 dex from the highest to the lowest
values cannot be explained by NLTE effects, which, according to our analysis,
are about -0.05 dex on average for
.
The average of the values in the table is 8.51 with a standard deviation
of 0.09.
Table 4: Solar abundance of C in the literature.
8 Conclusions
Our recommended value for the solar carbon abundance
is A(C
,
corresponding
to a weak efficiency of the collisions with
neutral hydrogen atoms (
),
the favourite value of the Holweger school.
The quoted error is the linear sum
of a statistical error, 0.02 dex, and
a systematic error, 0.04 dex, caused by the
uncertainty in the treatment of the hydrogen
collisions in the NLTE computation.
The statistical error was estimated by dividing
the line-to-line scatter, 0.11 dex, by
the square root of the 45 independent lines
used in the analysis.
The value
was also
adopted in our investigations of the solar abundances
of oxygen (Caffau et al. 2008) and nitrogen
(Caffau et al. 2009b). It is not obvious
why the same value of
should
apply to different atoms, or even to
different lines of the same atom.
It is comforting that the difference between
the extreme assumptions about the efficiency of
the H collisions (
or 1)
only amounts to 0.08 dex.
Our preferred value for the solar carbon abundance is very close to the recommendation of Grevesse & Sauval (1998). If we take this carbon abundance, together with A(N)=7.86 from Caffau et al. (2009b), A(O)=8.76 from Caffau et al. (2008), and A(Ne)=8.02 (see Caffau et al. 2009b for an explanation of this choice), we obtain a solar metallicity of Z=0.0154and Z/X = 0.0211. This value is higher than the metallicity recommended by Asplund et al. (2005b) and Grevesse et al. (2007), Z=0.0122, and goes in the direction of reconciling the spectroscopic abundances with the constraints from helioseismology.
That different 3D hydrodynamical simulations provide significantly different results (of the order of 0.1 dex) underlines the need for further development and validation of the hydrodynamical models. Recently, Asplund et al. (2009) have presented results based on a new generation 3D model, which is much closer to the CO5BOLD model than the one used by Asplund et al. (2005a) and which has lead to an upward revision of his carbon, oxygen, and iron abundances. It is likely that any residual difference between this new result and the present analysis can be ascribed to the line selection and to the different treatment of hydrogen collisions in the NLTE computations, although details on the analysis of Asplund et al. (2009) are not yet available. The excellent agreement of our CO5BOLD solar model with the observed centre-to-limb variation, shown in Ludwig et al. (2009), provides strong support for the thermal structure of the model and for the abundances deduced by its application (Caffau et al. 2009a).
AcknowledgementsE.C., H.G.L., and P.B. acknowledge financial support from EU contract MEXT-CT-2004-014265 (CIFIST).
References
- Allende Prieto, C., Lambert, D. L., & Asplund, M. 2002, ApJ, 573, L137 [NASA ADS] [CrossRef] [Google Scholar]
- Anders, E., & Grevesse, N. 1989, Geochim. Cosmochim. Acta, 53, 197 [Google Scholar]
- Asplund, M., Grevesse, N., Sauval, A. J., Allende Prieto, C., & Kiselman, D. 2004, A&A, 417, 751 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Asplund, M., Grevesse, N., Sauval, A. J., Allende Prieto, C., & Blomme, R. 2005a, A&A, 431, 693 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Asplund, M., Grevesse, N., & Sauval, A. J. 2005b, Cosmic Abundances as Records of Stellar Evolution and Nucleosynthesis, ASP Conf. Ser., 336, 25 [Google Scholar]
- Asplund, M., Grevesse, N., Sauval, A. J., & Scott, P. 2009, ARA&A, 47, 481 [NASA ADS] [CrossRef] [Google Scholar]
- Ayres, T. R., Plymate, C., & Keller, C. U. 2006, ApJS, 165, 618 [NASA ADS] [CrossRef] [Google Scholar]
- Barklem, P. S., Anstee, S. D., & O'Mara, B. J. 1998, PASA, 15, 336 [NASA ADS] [CrossRef] [Google Scholar]
- Baschek, B., & Holweger, H. 1967, ZAp, 67, 143 [NASA ADS] [Google Scholar]
- Basu, S., & Antia, H. M. 2008, Phys. Rep., 457, 217 [NASA ADS] [CrossRef] [Google Scholar]
- Bièmont, E., Hibbert, A., Godefroid, M., & Vaeck, N. 1993, ApJ, 412, 431 [NASA ADS] [CrossRef] [Google Scholar]
- Caffau, E., & Ludwig, H.-G. 2007, A&A, 467, L11 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Caffau, E., Ludwig, H.-G., Steffen, M., et al. 2008, A&A, 488, 1031 [CrossRef] [EDP Sciences] [Google Scholar]
- Caffau, E., Ludwig, H.-G., Steffen, M. 2009a, MmSAI, 80, 3 [Google Scholar]
- Caffau, E., Maiorca, E., Bonifacio, P., et al. 2009b, A&A, 498, 877 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Castelli, F., & Kurucz, R. L. 2003, in Modelling of Stellar Atmospheres, ed. N. Piskunov et al., Poster A20, IAU Symp., 210 [arXiv:astro-ph/0405087] [Google Scholar]
- Chaplin, W. J., & Basu, S. 2008, Sol. Phys., 251, 53 [NASA ADS] [CrossRef] [Google Scholar]
- Delahaye, F., & Pinsonneault, M. H. 2006, ApJ, 649, 529 [NASA ADS] [CrossRef] [Google Scholar]
- Delbouille, L., Roland, G., & Neven, L. 1973, Liège: Université de Liège, Institut d'Astrophysique, 1973 [Google Scholar]
- Delbouille, L., Roland, G., & Brault, T. 1981, Photometric atlas of the solar spectrum from 1850 to 10 000 cm-1, http://bass2000.obspm.fr/solar_spect.php [Google Scholar]
- Drawin, H. W., 1969, Z. Phys., 225, 483 [Google Scholar]
- Farmer, C. B., Norton, R. H., & Geller, M. 1989, NASA Ref. Publ., 1224 [Google Scholar]
- Farmer, C. B. 1994, Infrared Sol. Phys., 154, 511 [Google Scholar]
- Freytag, B., Steffen, M., & Dorch, B. 2002, Astron. Nachr., 323, 213 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Freytag, B., Steffen, M., Wedemeyer-Böhm, S., & Ludwig, H.-G. 2003, CO5BOLD User Manual, http://www.astro.uu.se/ bf/co5bold_main.html [Google Scholar]
- Grevesse, N., Sauval, A. J., Farmer, C. B., & Norton, R. H. 1987, Liege International Astrophysical Colloquia, 27, 111 [NASA ADS] [Google Scholar]
- Grevesse, N., Lambert, D. L., Sauval, A. J., et al. 1991, A&A, 242, 488 [NASA ADS] [Google Scholar]
- Grevesse, N., Sauval, A. J., & Blomme, R. 1994, Infrared Sol. Phys., 154, 539 [NASA ADS] [Google Scholar]
- Grevesse, N., & Sauval, A. J. 1998, Space Sci. Rev., 85, 161 [NASA ADS] [CrossRef] [Google Scholar]
- Grevesse, N., Sauval, A., & Murdin, P. 2000, Encyclopedia of Astronomy and Astrophysics [Google Scholar]
- Grevesse, N., Asplund, M., & Sauval, A. J. 2007, Space Sci. Rev., 130, 105 [Google Scholar]
- Hibbert, A., Biemont, E., Godefroid, M., & Vaeck, N. 1993, A&AS, 99, 179 [Google Scholar]
- Holweger, H. 1967, ZAp, 65, 365 [NASA ADS] [Google Scholar]
- Holweger, H. 2001, Joint SOHO/ACE workshop Solar and Galactic Composition, AIP Conf. Proc., 598, 23 [Google Scholar]
- Holweger, H., & Müller, E. A. 1974, Sol. Phys., 39, 19 [NASA ADS] [CrossRef] [Google Scholar]
- Kurucz, R. L. 2005a, Mem. Soc. Astron. Ital. Suppl., 8, 189 [Google Scholar]
- Lambert, D. L. 1978, MNRAS, 182, 249 [NASA ADS] [CrossRef] [Google Scholar]
- Ludwig, H.-G., Caffau, E., Bonifacio, P., et al. 2009, in ed. K. Cunha, M. Spite, & B. Barbuy, IAU Symp., 265 [Google Scholar]
- Luo, D., & Pradhan, A. K. 1989, J. Phys. B Atomic Mol. Phys., 22, 3377 [NASA ADS] [CrossRef] [Google Scholar]
- Neckel, H., & Labs, D. 1984, Sol. Phys., 90, 205 [NASA ADS] [CrossRef] [Google Scholar]
- Neckel, H. 1999, Sol. Phys., 184, 421 [NASA ADS] [CrossRef] [Google Scholar]
- Nussbaumer, H., & Storey, P. J. 1984, A&A, 140, 383 [NASA ADS] [Google Scholar]
- Pinsonneault, M. H., & Delahaye, F. 2009, ApJ, 704, 1174 [NASA ADS] [CrossRef] [Google Scholar]
- Ralchenko, Y. 2005, Mem. Soc. Astron. Ital. Supp., 8, 96 [Google Scholar]
- Ryan, S. G. 1998, A&A, 331, 1051 [NASA ADS] [Google Scholar]
- Scott, P. C., Asplund, M., Grevesse, N., & Sauval, A. J. 2006, A&A, 456, 675 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Steenbock, W., & Holweger, H. 1984, A&A, 130, 319 [NASA ADS] [Google Scholar]
- Steffen, M., & Holweger, H. 2002, A&A, 387, 258 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Stürenburg, S., & Holweger, H. 1990, A&A, 237, 125 [NASA ADS] [Google Scholar]
- Takeda, Y. 1994, PASJ, 46, 53 [NASA ADS] [Google Scholar]
- Tody, D. 1993, Astronomical Data Analysis Software and Systems II, 52, 173 [NASA ADS] [Google Scholar]
- Wedemeyer, S., Freytag, B., Steffen, M., Ludwig, H.-G., & Holweger, H. 2004, A&A, 414, 1121 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
- Weiss, A. W. 1996, priv. comm. NIST [Google Scholar]
- Wiese, W. L., Fuhr, J. R., & Deters, T. M. 1996, Atomic transition probabilities of carbon, nitrogen, and oxygen: a critical data compilation, ed. W. L. Wiese, J. R. Fuhr, & T. M. Deters (Washington, DC: American Chemical Society), for the National Institute of Standards and Technology (NIST), QC 453, 53 [Google Scholar]
- Yang, W. M., & Bi, S. L. 2007, ApJ, 658, L67 [NASA ADS] [CrossRef] [Google Scholar]
Footnotes
- ... IRAF
- IRAF is distributed by the National Optical Astronomy Observatories, which are operated by the Association of Universities for Research in Astronomy, Inc., under cooperative agreement with the National Science Foundation.
All Tables
Table 1: Lines considered for the abundance determination.
Table 2: Comparison of the disc-centre EW of two C I lines determined by different authors.
Table 3: Line parameters, 3D and 1D carbon abundance (LTE), and 1D NLTE corrections for our sample of selected C I lines.
Table 4: Solar abundance of C in the literature.
All Figures
![]() |
Figure 1: Comparison of the observed disc-centre solar spectrum (dashed lines, DI for the two reddest lines and NI for the others) with the corresponding 3D synthetic profiles (solid lines) for a selection of clean C I lines. |
Open with DEXTER | |
In the text |
![]() |
Figure 2: As Fig. 1, but showing the HM synthetic profile (solid lines) superimposed on the observed solar spectrum (dashed lines). To be consistent with Fig. 1, the synthetic profile is computed with Linfor3D, ignoring any blending lines. |
Open with DEXTER | |
In the text |
![]() |
Figure 3:
The carbon abundance as a function of wavelength of the individual
C I lines compiled in Table 3, as obtained from the 3D solar
model for different assumptions about the 1D NLTE corrections, which are
all based on the
|
Open with DEXTER | |
In the text |
![]() |
Figure 4: As Fig. 3, but showing the carbon abundances obtained from the HM model. |
Open with DEXTER | |
In the text |
![]() |
Figure 5:
The carbon abundances as a function of EW for the 3D model.
The two numbers in the lower part of the plots indicate the slope of the
best-fit linear relation and its 1 |
Open with DEXTER | |
In the text |
![]() |
Figure 6: The carbon abundances as a function of EW for the HM model. |
Open with DEXTER | |
In the text |
![]() |
Figure 7:
3D and
|
Open with DEXTER | |
In the text |
Copyright ESO 2010
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.