A&A 492, L43-L47 (2008)
DOI: 10.1051/0004-6361:200811126
LETTER TO THE EDITOR
K. Werner1 - T. Rauch1 - J. W. Kruk2
1 - Institut für Astronomie und Astrophysik, Kepler Center for Astro and Particle Physics, Eberhard-Karls-Universität, Sand 1, 72076 Tübingen, Germany
2 - Department of Physics and Astronomy, Johns Hopkins University, Baltimore, MD 21218, USA
Received 10 October 2008 / Accepted 6 November 2008
Abstract
For the first time, we have identified photospheric emission
lines in the far-UV spectrum of a white dwarf. They were discovered in
the Far Ultraviolet Spectroscopic Explorer spectrum of the hot
(
200 000 K) DO white dwarf KPD 0005+5106 and they stem
from extremely highly ionized calcium (Ca X
1137, 1159 Å). Their photospheric origin is
confirmed by non-LTE line-formation calculations. This is the highest
ionisation stage of any element ever observed in a stellar
photosphere. Calcium has never been detected before in any hot white
dwarf or central star of planetary nebula. The calcium abundance
determination for KPD 0005+5106 (1-10 times solar) is difficult, because the
line strengths are rather sensitive to current uncertainties in the
knowledge of effective temperature and surface gravity. We discuss
the possibility that the calcium abundance is much lower than expected
from diffusion/levitation equilibrium theory. The same emission
lines are exhibited by the [WCE]-type central star NGC 2371. Another
Ca X line pair (
1461, 1504 Å) is probably
present in a Hubble Space Telescope spectrum of the PG 1159-type
central star NGC 246.
Key words: stars: abundances - stars: atmospheres - stars: evolution - stars: AGB and post-AGB - stars: white dwarfs
Observations of hot (pre-) white dwarfs with the Far Ultraviolet Spectroscopic Explorer (FUSE) have revealed a large number of chemical elements that were never detected before in these objects. Their abundances can be used either to probe interior processes in previous stellar evolution phases or to test predictions from theories for element diffusion and radiative levitation.
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Figure 1:
The two Ca X emission lines discovered in KPD 0005+5106 (thin graphs). Overplotted is the spectrum from a model with
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We have recently identified Ne VIII lines in the hottest
(
150 000 K) non-DA (pre-) white dwarfs,
i.e. objects of spectral type PG 1159, DO, and [WCE] (Werner et al. 2007). The discovery of these lines in the hottest known DO white dwarf
KPD 0005+5106 was particularly surprising, because this proves that its
effective temperature must be much higher than previously thought
(200 000 K instead of 120 000 K).
KPD 0005+5106 was frequently observed by FUSE as a calibration target over its entire lifetime. We have co-added all available spectra and obtained datasets with very high S/N ratio. A careful inspection of spectra taken with different detectors revealed the presence of two hitherto unidentified emission lines. While there is still a large number of unidentified absorption lines present in FUSE spectra of hot white dwarfs (WDs), the discovery of emission features is unique and was completely unexpected. In this Letter we identify them as Ca X lines and present results of non-LTE modeling in order to confirm their photospheric origin and to perform an abundance determination.
We present observations and line identifications in Sect. 2 and describe the modeling in Sect. 3. The results from line-profile fits are presented in Sect. 4. We conclude with Sect. 5.
The FUSE instrument consists of four independent co-aligned
telescopes and spectrographs; two with Al+LiF optical coatings and two
with SiC coatings. Taken together, the four channels span the
wavelength range 904-1187 Å with a typical resolving power of
R 20 000. Further information on the FUSE mission
and instrument can be found in Moos et al. (2000) and Sahnow et al. (2000). KPD 0005+5106 was observed as a wavelength calibration object throughout
the FUSE mission (observations M1070201-M1070234), in each of
the spectrograph apertures (LWRS, MDRS, HIRS), and once under program
P1040101 in LWRS. All observations were obtained in TTAG mode, except
for three early HIST mode observations; the latter were excluded as they
have different residual distortions in the wavelength scale. All
exposures were processed with the final version, v 3.2.2, of CalFUSE
(Dixon et al. 2007). Spectra for each channel were shifted to place
absorption lines from low-ionization interstellar gas at a heliocentric
velocity of -15 km s-1 (Werner et al. 1996), and
combined. Variations in losses due to event bursts and channel
misalignments caused the net exposure times to vary: HIRS times varied
from 7.0 ks in SiC2a to 17.9 ks in LiF2b; MDRS times varied from
11.6 ks in SiC1a to 18.6 ks in LiF2b; LWRS times varied from 28.5 ks
in LiF1b to 33.6 ks in LiF2b. The net signal ranges from 700 counts per
0.013 Å pixel in the HIRS spectra to 1200 c/pix in MDRS and as much
as 2700 c/pix in LWRS. The Ca X emission features are seen
clearly in each of the six available spectra (LiF1b and LiF2a in each of
HIRS, MDRS, LWRS). These six spectra were then resampled onto a common
wavelength scale and combined to produce a single spectrum with an
effective exposure time of 122.2 ks.
The UV spectrum of NGC 246, taken with the Space Telescope Imaging Spectrograph (STIS) with grating E140H aboard the Hubble Space Telescope (HST) was retrieved from the MAST archive.
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Figure 2: Grotrian diagram of our Ca X model ion. Lines discussed in the text are caused by transitions between n=4sublevels. The 4p-4d transition causes the observed UV emission lines. |
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In the FUSE spectrum of KPD 0005+5106 we detected two emission lines,
located at photospheric rest wavelengths
1136.5,
1159.2 Å (Fig. 1, radial velocity +35 km s-1;
Werner et al. 1996). We identify these lines as due the
4p 2S - 4d 2P
transition in the Ca X ion
(Fig. 2). Compared to the Ritz wavelengths in the
NIST
database, both observed lines are located at wavelengths shorter by
0.3 Å. Their NIST
-values are
and 0.46,
respectively. The third line component of this transition is located at
1161.4 Å according to NIST, so that in reality we expect
it to be found at
1161.1 Å. Its gf-value, however, is
much smaller (
)
explaining the fact that we
cannot detect it in the observation. (This is confirmed by our
line-formation calculations.)
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Figure 3: The two Ca X emission lines discovered in KPD 0005+5106 (top spectra) are also seen in the [WCE] central star NGC 2371. The model profiles are the same as in Fig. 1. No attempt is made to fit the possibly wind-contaminated [WCE] profiles. For clarity, the FUSE spectra were smoothed with Gaussians ( FWHM 0.05 and 0.1 Å, respectively). The model spectra (thick lines) were convolved with 0.1 Å Gaussians. |
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We searched for the two Ca X lines in other hot DO white dwarfs
and PG 1159 stars, but to no avail. As we will demonstrate below
(Sect. 4), this is a consequence of the extremely high
of KPD 0005+5106 combined with a relatively low surface gravity. However,
these lines are seen in the very hot, early-type Wolf-Rayet
central star NGC 2371 (Fig. 3). For this object we did
not attempt to fit these lines with our (static) model atmospheres,
because the profiles might be affected by the stellar wind.
In the course of our model calculations we found that further
Ca X lines might be detectable in other wavelength regions. The
4s-4p transition gives rise to a line doublet at
1461.8, 1503.8 Å. Our models predict only marginal
emission features for KPD 0005+5106, which cannot be detected in archival spectra
taken with the Faint Object Spectrograph aboard HST and
high-resolution spectra from the International Ultraviolet
Explorer. However, for NGC 246 our models predict absorption lines
that are possibly present in a HST/STIS spectrum
(Fig. 4). The positions of the tentatively identified
absorption features in NGC 246 differ from the NIST wavelengths by -0.7 and -0.2 Å, respectively.
From NIST level energies one expects the two strongest lines of yet
another transition of Ca X (4d-4f) to be located in the optical
UV at
3478, 3492 Å, respectively. A high-resolution
spectrum of NGC 246 taken with ESO's Very Large Telescope and the
UVES spectrograph as part of the SPY survey (Napiwotzki et al. 2003)
reveals no line features there. Our model for NGC 246 predicts
absorption lines with a depth of only 5% relative to the continuum. The
relatively fast rotation (v sin i = 70 km s-1) smears the
line features considerably, and they remain hidden in the noise.
Similar weak absorption profiles for these lines are predicted for KPD 0005+5106,
but no appropriate observations are available.
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Figure 4:
HST/STIS spectrum of the PG 1159-type
central star NGC 246 and computed profiles for the 4s-4p doublet
of Ca X. Their shape reflects the stellar rotation of
v sin i = 70 km s-1. The observation was smoothed with a Gaussian
with
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We have designed a calcium model atom for NLTE line-formation
calculations. These were performed using and keeping fixed the physical
structure (temperature, densities) of line-blanketed NLTE model
atmospheres which are described in detail in Werner et al. (2004). In
short, they are plane-parallel and in hydrostatic and radiative
equilibrium. The models are composed of He, C, O, and Ne. For KPD 0005+5106, we
assumed helium-dominated atmospheres with admixtures of
C = 0.003, O = 0.0006, Ne = 0.01 (mass fractions). The high neon abundance was derived
from Ne VIII lines (Werner et al. 2007). The C and O abundances
are uncertain, because they were derived in earlier work that assumed
that KPD 0005+5106 is relatively cool (
= 120 000 K; Werner et al. 1996). We verified that varying the C and O abundances within reasonable
limits does not change the Ca X lines significantly. A series of
models with various
and
values was computed to study the
dependency of the Ca X lines on these parameters (see
Sect. 4). For NGC 246 we adopted
= 150 000 K,
= 5.7, and the composition He/C/O/Ne = 0.62/0.30/0.06/0.02 (Werner
et al. 2007).
The Ca model atom considers the ionization stages VIII-XII, represented by 1, 15, 25, 4, 1 NLTE levels, respectively,
plus a number of LTE levels. In the ions Ca IX-XI we
include 23, 126, and 2 line transitions, respectively. Atomic data were taken
from the NIST, Opacity (Seaton et al. 1994), and IRON (Hummer et al. 1993)
Projects databases (TIPTOPbase). Fine-structure splitting is
accounted for in the final formal solution for the synthetic
line-profile computation, distributing the level populations among
sublevels assuming LTE. For all lines we assumed quadratic Stark
broadening for the profile calculation.
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Figure 5:
Ionization fraction of calcium as a function of atmospheric
depth in the model with
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Particularly for the Ca X
1137, 1159 Å lines
the values of the oscillator strengths differ between the OP and NIST
databases. We use the OP values for our NLTE level population
iterations, because they are complete, in contrast to the NIST
database. For the final line-profile calculation we prefer the NIST
values, which are higher than the OP values by
25%. The
differences do not affect our conclusions.
Photoionization cross-sections are taken from the Opacity Project
database when available or, otherwise, computed in a hydrogen-like
approximation. Electron collisional rates were calculated with the usual
approximation formulae. The Ca model atoms that were used for this
analysis have been developed in the framework of the German
Astrophysical Virtual Observatory
(GAVO) project and are provided
within the Tübingen Model-Atom Database
TMAD
.
Figure 1 shows a fit to the Ca X emission lines in
KPD 0005+5106 with a model
= 200 000 K,
= 6.2, and a solar
Ca abundance (
,
mass fraction; Asplund et al. 2005). In Fig. 5 we show the ionization structure of
Ca throughout this model atmosphere. Within the entire line-forming region
Ca XI is dominant, followed by Ca X.
In order to achieve
the observed emission strength in a model with this temperature and
Ca abundance, the surface gravity must be that low (
= 6.2). This is
0.3 dex lower than what is preferred from the He II line spectrum
(Werner et al. 2007). We will show, however, that the fit to the
Ca X lines can be achieved with more than one parameter set.
The occurrence of this line emission can be understood when the non-LTE
departure coefficients
for the
populations ni of the involved atomic levels and the line source
function Sl are inspected (Fig. 6). The line source
function is determined by the ratio of the departure coefficients of the
lower and upper levels (i,j) and can be written as
,
where
is the Planck function. An overpopulation of the upper
level relative to the lower (i.e.
)
may lead to line
emission. In fact, this condition is fulfilled in the line-forming
region (Fig. 6), although both levels are underpopulated
(i.e. bi<1).
We have computed a small grid of models with different
and
(representing the uncertainties with which these parameters are
known) and Ca abundances. The results are presented in
Fig. 7. Generally, high
and low
is
necessary in order to bring this line into emission (left and right
upper panels). If
decreases (and/or
increases), the lines
first turn from emission into weak absorption features and then
disappear at about 140 000 K. This explains why other DOs do not
exhibit these lines: they are significantly cooler and have higher
gravities compared to KPD 0005+5106.
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Figure 6:
Left: departure coefficients ![]() ![]() ![]() ![]() ![]() |
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The sensitivity of these emission lines to the calcium abundance is
complicated and depends on
and
of the
atmosphere (Fig. 7, left and right lower
panels). Increasing the Ca abundance over the solar value can strongly
increase the emission height (model
= 200 000 K
= 6) or
decrease it (model
= 200 000 K
= 6.5). For KPD 0005+5106 we
achieved a good fit at
= 200 000 K,
= 6.2, and solar
Ca abundance. As mentioned, however, our previous analysis favors a gravity
higher by 0.3 dex. Increasing the gravity to
= 6.5 makes the
emission weaker, but this can be compensated by simultaneously
increasing the Ca abundance to 3 times the solar value and
to
220 000 K. A much higher abundance, as predicted by diffusion theory,
can be excluded. We have calculated models with 70 times solar
Ca abundance. The emission line peak heights hardly change in the
= 200 000 K,
= 6.2 model when Ca is increased from solar
to 70 times solar; however, detailed inspection of the relative strength
of both lines shows that it is not in agreement with the observation. In
the observation as well as in the
solar Ca abundance models
the 1159 Å emission is stronger than the 1137 Å emission, as can
be expected from the gf-value ratio. In the 70 times solar models the
emission strength ratio is reversed, in contrast to the observation.
Concerning PG 1159 stars, the behaviour of these Ca lines is rather
similar and therefore not shown in detail here. There are seven objects
that are hot enough and for which FUSE spectroscopy is
available. These are the low-gravity central stars of planetary nebulae
K1-16, Longmore 4, RX J2117.1+3412, NGC 246 (
= 140 000-170 000 K,
5.5-6), the higher-gravity objects PG 1520+525 and
PG 1144+005 (
= 150 000 K,
= 6.5-7), as well as the
peculiar H1504+65 (
= 200 000 K,
= 8). Model calculations were
performed for all of these objects with solar Ca abundance (diffusion is
not at work in these objects' atmospheres; see Unglaub & Bues
2000). They exhibit the Ca X
1137, 1159 Å lines as weak absorption features with a maximum depth of 5% of the
continuum flux. Such weak lines cannot be detected in the available
FUSE spectra.
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Figure 7:
Profile shapes of the Ca X
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We have discovered Ca X emission lines in far-UV spectra of the
DO white dwarf KPD 0005+5106. This is the first detection of photospheric
emission lines in this spectral range of any hot (pre-) white
dwarf. Provencal et al. (2005) discovered low-ionisation emission lines
in HST/STIS UV spectra of two relatively cool
(
12 500 K) He-rich white dwarfs (spectral type DQ). It
was shown, however, that they are chromospheric in origin. The
Ca X lines are the highest ionisation stage of any element
identified in any stellar photosphere. Our discovery also represents the
first identification of calcium in hot (pre-) WDs.
The Ca abundance in KPD 0005+5106 is in the range 1-10 times
solar. A more precise determination from the emission lines is not
possible. A comparison of this result with predictions from radiative
levitation/gravitational diffusion equilibrium theory is difficult
because
and
of KPD 0005+5106 are outside of the range considered
by Chayer et al. (1995, their Fig. 20). For the closest parameters
(
= 130 000 K,
=7) a huge overabundance is predicted
(2500 times solar). Our estimate for
is smaller (6.2-6.5) which would
result in an even higher overabundance. On the other hand it is
impossible to make a solid estimate for the effect of the higher
(200 000-220 000 K) on the behaviour of the Ca equilibrium
abundance, because the dominant ionisation stage in KPD 0005+5106 is
Ca XI, while it is Ca VIII in the hottest Chayer et al. model (
= 130 000 K,
=7.5). Looking at the behaviour of
other elements (S, Ar), namely how their equilibrium abundance changes
when their (respective isoelectronic) ionisation stages increase (with
increasing
), it is suggestive that the Ca abundance at
=200 000 K is lower than at 130 000 K, but not by orders of
magnitude. Although detailed calculations are required for a definitive
statement, we conclude that the atmosphere of KPD 0005+5106 is probably not in
levitation/diffusion equilibrium. This is confirmed by the
diffusion/mass-loss calculations of Unglaub & Bues (2000) which suggest
that KPD 0005+5106 has yet to cross the wind-limit on its evolutionary track,
meaning that mass-loss is large enough to prevent both gravitational
settling and the accumulation of radiatively supported heavy
elements. In this case, KPD 0005+5106 is not a descendant of the PG 1159
stars. An evolutionary link to the He-dominated central stars of
spectral type O(He) and to the RCrB stars has been suggested (Werner
et al. 2008).
If unaffected by diffusion processes, then the photospheric composition of KPD 0005+5106 is the consequence of previous evolutionary phases. In contrast, the presence of Ca in the atmospheres of cooler white dwarfs (spectral types DAZ and DBZ, with low-ionisation optical Ca absorption lines) requires on-going accretion of circumstellar matter, because gravitational settling rapidly removes heavy elements from the photosphere (e.g. Koester & Wilken 2006).
The non-detection of the Ca X
1137, 1159 Å lines in the hottest PG 1159 stars is explained by undetectably weak
absorption line features in the models. Another Ca X line pair
(
1462, 1504 Å) is possibly present in absorption in
NGC 246 and suggests a roughly solar Ca abundance. The only other object
in which we discovered the Ca X
1137, 1159 Å emission lines is the [WCE]-type central star NGC 2371. This
corroborates the extraordinarily high effective temperature of this
object.
Acknowledgements
T.R. is supported by the German Astrophysical Virtual Observatory (GAVO) project of the German Federal Ministry of Education and Research under grant 05 AC6VTB. J.W.K. is supported by the FUSE project, funded by NASA contract NAS5-32985. Some of the data presented in this paper were obtained from the Multimission Archive at the Space Telescope Science Institute (MAST).