A. Kanaan1 - A. Nitta2 - D. E. Winget3 - S. O. Kepler4 - M. H. Montgomery5,3 - T. S. Metcalfe6,3 - H. Oliveira1 - L. Fraga1 - A. F. M. da Costa4 - J. E. S. Costa4 - B. G. Castanheira4 - O. Giovannini7 - R. E. Nather3 - A. Mukadam3 - S. D. Kawaler8 - M. S. O'Brien8 - M. D. Reed8,9 - S. J. Kleinman2 - J. L. Provencal10 - T. K. Watson11 - D. Kilkenny12 - D. J. Sullivan13 - T. Sullivan13 - B. Shobbrook14 - X. J. Jiang15 - B. N. Ashoka16 - S. Seetha16 - E. Leibowitz17 - P. Ibbetson17 - H. Mendelson17 - E. G. Meistas18 - R. Kalytis18 - D. Alisauskas19 - D. O'Donoghue12 - D. Buckley12 - P. Martinez12 - F. van Wyk12 - R. Stobie12 - F. Marang12 - L. van Zyl12 - W. Ogloza20 - J. Krzesinski20 - S. Zola20,21 - P. Moskalik22 - M. Breger23 - A. Stankov23 - R. Silvotti24 - A. Piccioni25 - G. Vauclair26 - N. Dolez26 - M. Chevreton27 - J. Deetjen28 - S. Dreizler28,29 - S. Schuh28,29 - J. M. Gonzalez Perez30 - R. Østensen31 - A. Ulla32 - M. Manteiga32 - O. Suarez32 - M. R. Burleigh33 - M. A. Barstow33
1 - Departamento de Física Universidade Federal de Santa
Catarina, CP 476, 88040-900 Florianópolis, SC, Brazil
2 - Apache Point Observatory, 2001 Apache Point Road, PO
Box 59, Sunspot, NM 88349, USA
3 - Department of Astronomy, 1 University Station Stop C1400,
University of Texas, Austin, TX 78712, USA
4 - Instituto de Física, Universidade Federal de Rio
Grande do Sul, CP 10501, 91501-970 Porto Alegre, RS, Brazil
5 - Institute of Astronomy, University of Cambridge,
Madingley Road, Cambridge CB3 0HA, UK
6 - Harvard-Smithsonian Center for Astrophysics, USA
7 - Departamento de Fisica e Quimica, UCS, Brazil
8 - Dept. of Physics & Astronomy, Iowa State University, USA
9 - Astronomy Dept., Southwest Missouri State University, USA
10 - Dept. of Physics & Astronomy, University of Delaware, USA
11 - Southwestern University, Georgetown, TX, USA
12 - South African Astronomical Observatory, South Africa
13 - Victoria University of Wellington, New Zealand
14 - Chatterton Astronomy Dept., University of Sydney, Australia
15 - Astronomical Observatory, Academy of Sciences, PR China
16 - Indian Space Research Organization, India
17 - Wise Observatory, Tel-Aviv University, Israel
18 - Institute of Theoretical Physics & Astronomy, Lithuania
19 - Vilnius University, Lithuania
20 - Mt. Suhora Observatory, Cracow Pedagogical University, Poland
21 - Astronomical Observatory, Jagiellonia University, Poland
22 - Copernicus Astronomical Center, Poland
23 - Institut für Astronomie, Universität Wien, Austria
24 - INAF - Osservatorio Astronomico di Capodimonte, Italy
25 - Dipartimento di Astronomia, Università di Bologna, Italy
26 - Université Paul Sabatier, Observatoire
Midi-Pyrénées, France
27 - Observatoire de Paris-Meudon, France
28 - Institut für Astronomie und Astrophysik, Germany
29 - Universitätssternwarte Göttingen, Germany
30 - University of Tromsø, Norway
31 - Isaac Newton Group, Spain
32 - Departamento de Física Aplicada, Universidad de Vigo,
Spain
33 - Dept. of Physics & Astronomy, University of Leicester, UK
Received 20 April 2004 / Accepted 31 October 2004
Abstract
BPM 37093 is the only hydrogen-atmosphere white dwarf currently
known which has sufficient mass (1.1
)
to theoretically
crystallize while still inside the ZZ Ceti instability strip (
K). As a consequence, this star represents our first
opportunity to test crystallization theory directly. If the core is
substantially crystallized, then the inner boundary for each pulsation
mode will be located at the top of the solid core rather than at the
center of the star, affecting mainly the average period spacing. This is
distinct from the "mode trapping'' caused by the stratified surface
layers, which modifies the pulsation periods more selectively. In this
paper we report on Whole Earth Telescope observations of BPM 37093
obtained in 1998 and 1999. Based on a simple analysis of the average
period spacing we conclude that a large fraction of the total stellar mass
is likely to be crystallized.
Key words: stars: evolution - stars: individual: BPM 37093 - stars: interiors - stars: oscillations - white dwarfs
Since 1960 most astronomers have agreed that cool white dwarfs must eventually crystallize (Kirzhnitz 1960; Salpeter 1961; Abrikosov 1960). The process theoretically begins when the electrostatic interaction between the ions becomes much larger than the thermal energy. This effect is based on such well known physics that it has become widely accepted without ever having been tested empirically.
BPM 37093 is a ZZ Ceti star (Kanaan et al. 1992) with an unusually high mass
(1.10 ,
Bergeron et al. 2004). White dwarfs this massive are subject to
much higher pressures and densities in their cores, and we expect a
1.0
white dwarf to begin crystallizing at temperatures within or
above the ZZ Ceti instability strip (Wood 1992; Winget et al. 1997). Our goal in
observing BPM 37093 with the Whole Earth Telescope (WET, Nather et al. 1990)
was to obtain seismological data to determine whether or not the stellar
interior is crystallized. The fundamental objective was simply to detect
as many independent pulsation modes as possible, and then to compare the
observed frequencies with those calculated from white dwarf models that
have been artificially crystallized to various degrees.
For years we have faced a troubling ambiguity between the effects of the
crystallized mass fraction (
), the hydrogen layer mass
(
), and the stellar mass (M*) and effective temperature (
). Changes to these four characteristics of white dwarf models can
all modify the average spacing between the calculated pulsation periods
(see Montgomery & Winget 1999, Eq. (7)). Fortunately, the latter two quantities can be
constrained by fitting model atmospheres to spectroscopic observations,
but the others can only be determined through asteroseismology. Recent
improvements in our theoretical description of the composition transition
zones between the stratified surface layers in our models
(Córsico et al. 2002; Althaus et al. 2003) have helped to reduce the degeneracy between
and
.
However, the huge number of possible parameter combinations,
and the need for an efficient method of exploring them, remained serious
obstacles to progress until recently (Metcalfe & Charbonneau 2003; Metcalfe et al. 2004).
Like the cool DAV G 29-38 (Kleinman et al. 1998), BPM 37093 exhibits irregular
modulations in the amplitudes of its pulsation modes. On one occasion all of the modes vanished below the detection threshold of 1 mma
(Kanaan et al. 1998). However, the modes that disappeared were observed to
reappear later with the same pulsation frequencies. This gives us
confidence that we can learn more about this star by using the full set of
frequencies that have been observed over time - a concept known as
"time-ensemble'' asteroseismology, pioneered by Kleinman et al. (1998). In this
paper we report WET observations obtained in 1998 and 1999, and we use the
identified pulsation periods to define a range for the average period
spacing. This allows us to constrain
and
by following
the analysis of Montgomery & Winget (1999) with an updated prescription for the envelope
composition transition zones.
In 1996 and 1997, observations of BPM 37093 were obtained from the 0.9 m
telescope at CTIO and the 1.6 m telescope at Observatório Pico dos Dias
(OPD, Brazil) respectively. The two initial goals of these observations
were: 1) to identify as many pulsation modes as possible, to help
constrain asteroseismological model fitting, and 2) to find stable
pulsation modes suitable for measuring the rate of period change
(), as has been done for other white dwarfs
(Costa et al. 1999; Mukadam et al. 2003; Kepler et al. 2000a). Further analysis (see Sect. 3)
revealed that no modes were stable enough to use for
measurements.
After these two attempts to obtain single-site data on BPM 37093, it
became clear that we would be unable to resolve the pulsation spectrum of
this star from a single observatory. By 1997 we had already accumulated
more than 100 h of photometry on BPM 37093, which led to the
identification of only 4 pulsation modes with highly variable amplitudes
(Kanaan et al. 1998).
BPM 37093 was chosen as the southern primary target for a Whole Earth Telescope campaign (XCOV 16) in 1998, and again in 1999 (XCOV 17) to coincide with simultaneous observations using the Hubble Space Telescope (HST). A journal of observations for the data obtained for these two campaigns is shown in Tables 1 and 2. Overall, we obtained more than 142 h of data in April-May 1998 with a duty cycle of 50% during the central 10 days, and an impressive 180 hours in April 1999 with a better duty cycle of 65% during the central 10 days. The latter observations included almost complete coverage during the two scheduled HST visits near the middle of the campaign, and preliminary results were reported by Nitta et al. (2000).
Table 1: Journal of observations in 1998 (XCOV 16).
Table 2: Journal of observations in 1999 (XCOV 17).
The primary goal of the HST observations was to use the limb darkening
method devised by Robinson et al. (1995) to provide an independent determination of
the spherical degree ()
for each pulsation mode. Unfortunately, this
method could be applied only to the modes with the highest amplitudes, and
the observations were not sensitive enough to distinguish between
and
.
In this paper we infer
based only on the average
period spacing between modes.
One of the initial goals of our observations was to identify pulsation
modes stable enough to measure the rate of period change (). As a
white dwarf star cools over time, the slow change in the thermal structure
should lead to a detectable increase in the pulsation periods. We expect
that the periods in a crystallizing star should change more slowly than in
other ZZ Ceti stars because the associated release of latent heat causes
the temperature to drop more slowly than in a non-crystallizing star.
However, the observations from CTIO in 1996 made it clear that measurements would not be possible for BPM 37093. In Fig. 1
we show the evolution of daily Fourier Transforms (FTs), night by night
during the 10 night run. On the tenth night, the pulsations vanished below
the detection threshold. Comparing the other panels of Fig. 1, it
is also clear that the amplitudes of the detected modes are highly
variable. Kanaan et al. (1998) demonstrated that these amplitude changes must be
intrinsic to the star, rather than due to the beating of closely spaced
modes, since there was no correlation between the changes in amplitude
and phase. Such intrinsic behavior has been reported for other ZZ Ceti
stars on a timescale of months (Kleinman et al. 1998), but not from night to night
as observed in BPM 37093. These short-timescale variations will lead
us to derive average amplitudes from the FTs of long data sets,
but will still allow us to identify the pulsation modes which have the
highest amplitudes and the longest lifetimes.
The FTs of the two WET campaigns on BPM 37093 are shown in
Fig. 2. In each panel we have marked all of the peaks that exceed
4 times the observational noise level. During XCOV 16 we detected many
more modes than were evident in the 1996 observations - of the 8
frequencies detected, only 2 coincide with those seen previously.
Comparing this with XCOV 17, it seems clear that the detection of more
independent modes in XCOV 16 can be attributed to the star itself, rather
than to differences in our detection threshold. During the second WET
campaign on BPM 37093 we detected 7 frequencies, of which 4 coincide with
others seen previously. Only the 512 s and 661 s modes are unique to the
data obtained for XCOV 17. The full list of frequencies detected in these
two WET campaigns is shown in Table 3, along with the mode
identifications of Metcalfe et al. (2004) for those modes found in the preliminary
analysis of Kanaan et al. (2000).
![]() |
Figure 1: Nightly FTs of BPM 37093 during ten nights of observations from CTIO in 1996. The amplitudes are highly variable on short timescales. All of the modes vanish below the detection threshold on the final night. |
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We can understand the erratic behavior of BPM 37093 by considering previous observations of other ZZ Ceti pulsators. Kleinman et al. (1998) documented very similar results for the star G 29-38, and proposed that each set of observations can provide a subset of the full spectrum of normal modes. The fundamental idea behind this hypothesis is that the underlying structure of the star does not change on the timescales of the observed amplitude variations. Instead, something in the excitation mechanism must select certain modes and exclude others in a manner that varies over time. Setting aside the question of what specifically causes these amplitude modulations, we only need to assume that the observed frequencies are, in each case, normal modes of oscillation that can be described by spherical harmonics. Such an assumption rests on a firm body of evidence (Kepler et al. 2000b; Robinson et al. 1982; Clemens et al. 2000), and is also supported by the fact that modes which disappear below the detection threshold are observed to reappear later with the same frequencies.
We adopt for our analysis the full set of frequencies that have been
observed in BPM 37093 over time, giving preference to the WET campaigns for
their superior frequency precision. For the isolated frequencies we assume
that each mode has an azimuthal order m=0 (see Metcalfe 2003), and for
the modes consisting of two closely-spaced frequencies we use the average of
the two. For modes that were observed in both campaigns, we use the
frequency from the observation with the highest amplitude. This leads to a
total of 7 independent modes that have been identified as
by
Metcalfe et al. (2004). The average period spacing between consecutive radial
overtones for these 7 modes is
s. This implies that the
identification should be correct for the majority of the modes,
since an
identification would yield a much larger period spacing
(
s, Montgomery & Winget 1999).
Table 3: Frequencies detected from two WET campaigns.
![]() |
Figure 2: Fourier Transforms and window functions at the same scale for the Whole Earth Telescope observations of the ZZ Ceti star BPM 37093 obtained during a) the XCOV 16 campaign in 1998, and b) the XCOV 17 campaign in 1999. |
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To get beyond the degeneracy, we need to use the individual
pulsation periods in addition to
.
Fundamentally, this is
possible because variations to
change the individual periods
through "mode trapping'', while variations to
affect mainly
the average period spacing. If BPM 37093 is partially crystallized, the
inner boundary for each pulsation mode will be located at the top of the
solid core rather than at the center of the star. This reduces the size of
the resonant cavity, increasing the average period spacing and modifying
the periods of all of the modes. By contrast, the hydrogen layer
produces a sharp chemical gradient somewhere near the surface. Any
individual mode whose eigenfunction is large in this region can interact
with the chemical gradient and become "trapped'' - its period will be
shifted more than the periods of other modes. Clearly, each mode will be
modified in a different manner through this interaction.
Montgomery & Winget (1999) understood that the signatures of
and
are
in principle distinct. However, by focusing only on the average period
spacing they were unable to place strong constraints on either
or
.
Our present models are somewhat improved: Montgomery & Winget
used hydrogen profiles that were derived assuming diffusive equilibrium in
the trace element approximation. This produced unrealistically sharp
chemical gradients at the base of the hydrogen layer, leading to stronger
mode trapping in their models. This was demonstrated by Córsico et al. (2002), who
compared models that assumed diffusive equilibrium in the trace element
approximation with models that computed the abundance profiles based on
time-dependent diffusion calculations. In a recent extension of this work
to massive ZZ Ceti stars, Althaus et al. (2003) described an improved method of
calculating diffusive equilibrium profiles that compare favorably with the
fully time-dependent results (see their Fig. 18). We have incorporated
this method of computing the hydrogen abundance profiles into the code
used by Montgomery & Winget (1999). However, since the sharpness of the hydrogen
transition zone should mainly affect the mode trapping properties of the
models, we expect that our new average period spacings will differ only
slightly from those computed by Montgomery & Winget (1999).
As a simple illustration of the potential of our observations, we
calculated
for a small grid with various combinations of
and
.
We fixed the mass, temperature, and helium layer
thickness to the values used for Fig. 10b of Montgomery & Winget (1999), but we assumed a
uniform O core. We show this grid of models in Fig. 3 with the
shaded 1
range of the average period spacing from the WET
observations of BPM 37093. As expected, the average period spacing of the
0% crystallized model is virtually identical to that found by
Montgomery & Winget (1999). However, due to the different assumed C/O profiles, the
crystallized curves have shifted with respect to the results of
Montgomery & Winget (1999).
![]() |
Figure 3:
The average period spacing of a small grid of models with various
combinations of ![]() ![]() ![]() |
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Unfortunately, the degeneracy between
and
is still
present, but we have not yet used the hidden third dimension of the grid:
at each point we have also computed the root-mean-square differences
between the observed and calculated periods (
), to exploit
the information contained in the individual modes. Although the
observed range of
can accommodate values of
between -5 (
)
and -8 (uncrystallized), not all
hydrogen layer masses are equally successful at reproducing the individual
modes. The model with
and
% has
s, which is substantially better than anything else
in this small grid (the next best model has
s).
A theoretical model with this same set of structural parameters is
expected to be between 66-92% crystallized for a C/O mixture, or
even more crystallized if the core is composed of an O/Ne mixture
(see Córsico et al. 2004, for some recent calculations).
Of course, the individual modes also contain information about the mass, temperature, helium layer, and core composition. If we have fixed these parameters incorrectly, it is likely that we have found a locally optimal match to the observed periods rather than the global solution. Montgomery & Winget (1999) recognized this difficulty, and discussed the need for an automated procedure to search this enormous parameter-space. Such a procedure, based on a parallel genetic algorithm, has recently been developed (Metcalfe & Charbonneau 2003) and applied to this problem. The initial results from this large-scale exploration of the models have been published separately by Metcalfe et al. (2004), who present a more detailed discussion of the initial model fitting results.
The Whole Earth Telescope has once again deciphered the complex pulsation spectrum of an astrophysically interesting white dwarf star. BPM 37093 is the only known ZZ Ceti star massive enough to allow a seismological test of crystallization theory, and previous attempts to understand it from single site observations were not successful. The superior frequency precision and extended coverage of two WET campaigns finally allowed us to document a series of 9 independent pulsation modes in this star. While it is always useful to search for additional frequencies to help constrain the model fitting, the observational requirements of this project have now largely been satisfied.
The limiting factor in our ability to test crystallization theory through
asteroseismology of BPM 37093 is now computational. The initial study of
Metcalfe et al. (2004) was limited to several fixed masses and core compositions,
but all of their optimal models suggested that a large fraction of
the core is crystallized - a result that is qualitatively supported by our
simple analysis of the average period spacing. We have only fit
to the nearest 0.1 M*, but Montgomery & Winget (1999) showed that the pulsations
are sensitive to changes of 0.01 M* in this parameter. As computers get
faster, we should be able to extend the genetic algorithm based model
fitting method to treat
,
M* and the composition of the
liquid portion of the core as fully adjustable parameters. In the
meantime, we should apply the same fitting procedure to lower mass ZZ Ceti
stars that are not expected to be crystallized, as a check of the method.
The Sloan Digital Sky Survey (SDSS) has recently discovered several new ZZ Ceti stars that may also be massive enough to test crystallization theory (Mukadam et al. 2004). All of the new pulsators in the SDSS sample are significantly fainter than the previously known white dwarfs, so larger telescopes will probably be required to resolve their pulsation spectra. Several current and planned space missions (MOST, Walker et al. 2003; COROT, Baglin et al. 2002) promise to revolutionize the field of asteroseismology in the coming decade. However, none of them is likely to contribute to our understanding of pulsating white dwarfs stars, which are too faint to be observed by these satellites. The Whole Earth Telescope remains the instrument of choice for these fainter targets. The availability of larger ground-based telescopes may allow the WET concept to be extended to 2 m and 4 m class instruments. With a growingharvest of new objects from SDSS, the future looks bright for white dwarf asteroseismology.
Acknowledgements
This work was partially supported by NASA, NSF, Brazilian institutions FAPERGS, CNPq, CAPES, and FINEP, and by the Smithsonian Institution through a CfA Postdoctoral Fellowship. PM is partially supported by Polish KBN grants 5 P03D 012 20 and 5 P03D 030 20.