A&A 392, 501-503 (2002)
DOI: 10.1051/0004-6361:20021059
Research Note
U. Giveon1 - C. Morisset2 - A. Sternberg1
1 - School of Physics and Astronomy and the Wise Observatory,
The Beverly and Raymond Sackler Faculty of Exact Sciences,
Tel Aviv University, Tel Aviv 69978, Israel
2 -
Institut d'Astrophysique de Marseille, CNRS & Univ. de Provence, BP 8,
13376 Marseille Cedex 12, France
Received 7 May 2002 / Accepted 16 July 2002
Abstract
Two independent groups
(Giveon et al. 2002; Martín-Hernández et al. 2002)
have recently investigated the Galactic metallicty gradient as
probed by ISO observations of mid-infrared emission-lines from HII regions.
We show that the different gradients inferred by the two groups are due to
differing source selection and differing extinction corrections. We show that
both data sets in fact provide consistent results if identical assumptions are
made in the analysis. We present a consistent set of gradients in which we
account for extinction and variation in electron temperature across the
Galactic disk.
Key words: Galaxy: abundances - ISM: HII regions
In two recent studies Giveon et al. (2002) and Martín-Hernández et al. (2002) analyzed mid-infrared fine-structure emission lines, as observed by the Infrared Space Observatory (ISO), to study the excitation and metallicity of HII regions across the Galactic disk. Discrepancies appear to be present between the gradients published in these two papers. In this note we re-analyze the reduced data compiled by Giveon et al. and Martin-Hernandez et al. and we demonstrate that similar results are obtained if the same source samples are chosen, and no assumptions are made for the extinction correction. We then apply extinction and electron temperature corrections to both data sets and infer consistent Galactic abundance gradients from the two independent ISO studies.
Giveon et al. (2002) presented a sample of 112
Galactic H II regions, observed by ISO-SWS, spanning galactocentric radii
<18 kpc. Most of their sources show
prominent [Ar II]6.99 m, [Ar III]8.99
m, [Ne II]12.8
m, [Ne III]15.6
m, [S III]18.7
m and
[S III]33.5
m fine-structure lines and
also the hydrogen recombination lines Br
and Br
at 4.05 and 2.60
m.
Only 48 sources have both argon or neon lines and a physical Brackett ratio.
For case-B recombination, the Br
/Br
ratio ranges from 1.7 to 1.9 for
temperatures
K. Since extinction should only increase
the ratio, five sources with Brackett ratios
<1.68 were excluded from the analysis.
The Brackett line ratios, an assumed gas temperature of 104 K,
and the Draine (1989)
mid-infrared extinction curve (see below)
were used to de-redden the fine-structure lines
intensities.
A similar analysis was performed by Martín-Hernández et al. (2002), who used the ISO-SWS & LWS spectral catalog of 34 compact H II regions (Peeters et al. 2002). The line intensities in their paper were not corrected for dust extinction due to the small number of sources for which the Brackett recombination lines were observed. However, corrections due to possible electron temperature variations across the disk were applied. In contrast, Giveon et al. did not apply such corrections to their data. Martín-Hernández et al. also published gradients of S/H and N/O. Here we discuss only the common results as analyzed by Martín-Hernández et al. Giveon et al., and show results for Ar/H, Ne/H, and S/H.
The results published in Giveon et al. and Martín-Hernández et al. are
listed in the first row of each panel in Table 1.
NEON | ||||
Martín-Hernández Catalog | Giveon Catalog | |||
ASSUMPTIONS |
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1. Published (20021) |
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2. Sub-catalog, not corrected |
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3. Full catalog, not corrected |
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4. Full catalog, att. corrected |
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5. Full catalog, att. & temp. corrected |
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ARGON | ||||
Martín-Hernández Catalog | Giveon Catalog | |||
ASSUMPTIONS |
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1. Published (20021) |
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2. Sub-catalog, not corrected |
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3. Full catalog, not corrected |
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4. Full catalog, att. corrected |
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5. Full catalog, att. & temp. corrected |
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SULFUR | ||||
Martín-Hernández Catalog | Giveon Catalog | |||
ASSUMPTIONS |
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3. Full catalog, not corrected |
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4. Full catalog, att. corrected |
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5. Full catalog, att. & temp. corrected |
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If only the common sources for the two samples, and no extinction corrections are applied, the two data-sets give comparable metallicity gradients. There are 22 sources in Giveon et al. which are common with Martín-Hernández et al. We exclude the most distant source (WB89 380; IRAS 01045+6506) in the samples, since the assumed distance to this source differs between the two studies. For the 21 common sources we obtain the coefficients listed in the second row of Table 1. The results derived from the common sources are in reasonable agreement. The small discrepancies may be due to differing (<5%) inferred line fluxes in the independent data reduction and small differences (<10%) in the assumed galactocentric positions of the sources.
We now consider the gradients resulting from the full samples of Giveon et al. (2002) and Martín-Hernández et al. (2002), with corrections due to extinction and electron temperature dependence of the line emissivities.
We first take the entire samples and compute the abundance gradients
with no corrections applied.
An electron temperature of 104 K is assumed.
The resulting gradients are given in the third row of Table 1.
The upper limits were included in these fits.
We show the total gradients for the uncorrected data in Fig. 1.
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Figure 1: Argon, neon, and sulfur abundances vs. galactocentric radius for the full catalogs of Martín-Hernández et al. and Giveon et al. (raw data). Solid lines are fits to the data, whose values are given in the third row of Table 1. In these plots no extinction or electron temperature corrections have been applied. The vertical lines are representative error bars. |
Open with DEXTER |
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Figure 2: Argon, neon, and sulfur abundances vs. galactocentric radius for the full catalogs of Martín-Hernández et al. and Giveon et al. attenuation and temperature corrected. Solid lines are fits to the data, whose values are given in the fifth row of Table 1. |
Open with DEXTER |
Next, we apply extinction corrections to the full catalogs.
Both Giveon et al. (2002)
and Martín-Hernández et al. (2002)
employed the mid-infrared Draine (1989) extinction curve in their
analysis. For short wavelengths (
m) both groups
assumed
.
However, for long wavelengths (
m)
Giveon et al. adopted the Draine mid-IR extinction curve
assuming a "strong''
9.7
m silicate absorption normalization,
A9.7/E(J-K)=0.7,
whereas Martín-Hernández et al. assumed a "weak''
normalization
A9.7/E(J-K)=0.3. Here we adopt an
intermediate value,
A9.7/E(J-K)=0.5, for both
catalogs. The associated values of
for
the various emission lines are listed in Table 2.
The resulting gradients for the
attenuation-corrected full catalogs are given in the fourth row of Table
1.
Line | Br![]() |
Br![]() |
[ArII] | [ArIII] | [SIV] | [NeII] | [NeIII] | [SIII] |
Wavelength(![]() |
2.60 | 4.05 | 7.0 | 9.0 | 10.5 | 12.8 | 15.5 | 18.7 |
A![]() |
0.72 | 0.33 | 0.13 | 0.64 | 0.70 | 0.28 | 0.22 | 0.32 |
We note that the attenuation-corrected argon
and sulfur gradients are much
flatter than the uncorrected ones, while the neon
gradients are only slightly affected. This is mainly due to the large
extinction of [Ar III]8.99 m and [S III]18.7
m. These lines coincide
with the silicate absorption features at 9.7 and 18
m
(Draine 1989).
Next, we apply an electron temperature correction to the data. The temperature
correction accounts for possible variation in the H II region temperatures
across the disk.
Following Martín-Hernández et al. we assume that
the electron temperature varies as
We conclude that the Galactic metallicity gradients, as expressed by the argon, neon, and sulfur abundances gradients, of Giveon et al. (2002) and Martín-Hernández et al. (2002) are consistent within the error bars. This conclusion applies both to the raw data and the fully corrected data.
Acknowledgements
The ISO spectrometer data center at MPE is supported by DLR under grants 50 QI 8610 8 and 50 QI 9402 3. Our research is supported by the German-Israeli Foundation (grant I-0551-186.07/97). We thank the referee for useful comments.