A&A 379, L35-L38 (2001)
DOI: 10.1051/0004-6361:20011304
V. Burwitz1 - V. E. Zavlin1 - R. Neuhäuser1 - P. Predehl1 - J. Trümper1 - A. C. Brinkman2
1 - Max-Planck-Institut für extraterrestrische Physik,
PO Box 1312, 85741 Garching, Germany
2 - Space Research Organization of the Netherlands,
Soorbonnelaan 2, 3584 CA Utrecht, The Netherlands
Received 1 August 2001 / Accepted 18 September 2001
Abstract
We present the Chandra LETGS X-ray spectrum of the
nearby (
pc) neutron star RXJ1856.5-3754.
Detailed spectral analysis of the combined X-ray and
optical data rules out the nonmagnetic neutron star
atmosphere models with
hydrogen, helium, iron and solar
compositions.
We
also conclude
that strongly magnetized atmosphere models
are unable to
represent the data.
The data can be explained with a two-component blackbody
model.
The harder component with temperature of
eV and a radius
km of the emitting region
well fits the X-ray data and can be interpreted as
radiation from a hot region on the
star's
surface.
Key words: stars: atmospheres - stars: individual: RX J1856.5-3754 - stars: neutron - X-rays: stars
It was suggested by Walter et al. (1996) and
supported by Neuhäuser et al. (1997) that
RXJ1856.5-3754 (or RXJ1856 for short) is an isolated
neutron star (NS).
It has a strong and non-variable X-ray flux
erg s-1 cm-2and a soft spectrum with a blackbody temperature
eV.
Thousands of such NSs were expected in RASS (e.g.,
Colpi et al. 1993; Madau & Blaes 1994),
moving fast through the interstellar medium.
Only a few such objects have been found, three of them show
pulsations on time-scale of seconds (Haberl et al. 1997,
1999; Hambaryan et al. 2001).
Neuhäuser & Trümper (1999) argued that the
number of isolated NSs expected in RASS was overestimated
mainly due to unrealistic velocity distributions.
Walter & Matthews (1997) and Neuhäuser et al. (1998) found an optical counterpart for
RXJ1856 with V26mag.
This and the large proper motion of
masyr-1(Walter 2001; Neuhäuser 2001)
are additional arguments that it is indeed an isolated NS.
Walter (2001) also detected parallactic motion,
determined the distance to the source
d=61+9-8pc
and suggested that RXJ1856 could be the remnant of the original
primary of the
Oph system.
This implies a NS age of
yr.
First spectral modelling of RXJ1856 based on its ROSAT
data was presented by Pavlov et al. (1996;
hereafter P96), who showed that the optical/UV flux
predicted by NS atmosphere models depends drastically on the
surface chemical composition.
More recently Pons et al. (2002; hereafter P02)
have analyzed combined optical and X-ray data and concluded
that it may have either a Fe or Si-ash atmosphere.
However, the inferred NS radius
km and mass
are not allowed for any plausible
equation of state of the NS inner matter.
RXJ1856 was observed with the Chandra Low Energy Transmission Grating Spectrometer (LETGS; Brinkman et al. 2000). First preliminary results were presented by Burwitz et al. (2001). Here we describe the LETGS data (Sect. 2), results of spectral (Sect. 3) and timing (Sect. 4) analysis and discuss implications on the nature of RXJ1856 (Sect. 5).
RXJ1856 was observed on March 10, 2000 with the standard
LETGS (LETG + HRC-S) configuration in a 56.1ks exposure.
The LETGS spectrum of RXJ1856 was extracted from the
level 1.5 event file.
The only pulse-height filtering applied to the data was the
removal of photons with a pulse-height amplitude equal to 255
as other pulse-height filters do not reduce the background level
evenly for all energies.
We used the extraction region recommended in the Chandra
Proposers' Observatory Guide [POG])
for extracting the source spectrum (see Fig. 1).
For the background, large regions above and below the
source extraction area are selected.
Towards longer wavelengths
Å the
background regions become wider in order to maintain the
constant ratio of areas between source and background spectral
bins (here the ratio is equal to 6).
The measured dispersed source count rate is
ks-1in the 0.15-0.82 keV range (where the source spectrum prevails
over the background).
The extracted source spectrum (binned in 686 spectral bins)
and the most up-to-date effective area tables for the 1st
order (status of October 31, 2000)
were used for spectral fits.
To search for spectral lines, we used the method applied by
Pavlov et al. (2001) to the dispersed LETGS data
on the Vela pulsar. We first binned the extracted source-plus-background and
background spectra in 0.02Å bins.
Then we grouped 10-20 sequent bins and estimated the
deviation of source counts in each bin of a given group
from the mean value in the group.
This method revealed maximum deviation at a 2.9
level.
Since there exist the ROSAT PSPC data (
counts
collected in a 6.3ks exposure), we first checked whether the
LETGS and PSPC data yield consistent results in spectral fits.
The blackbody fits showed that the allowed domains of the
fitting parameters do not formally overlap with each other:
eV,
km (
d60=d/60 pc)
and
(the uncertainties are given at a 3
level)
with
for the PSPC data, and
eV,
km and
(
)
for the LETGS data.
The difference between the blackbody models given by
the two fits (see Fig. 2) is most likely
attributed to uncertainties in the calibration of
LETGS and PSPC.
The next step in analysing the LETGS spectrum is to
apply NS atmosphere models.
The results of P96 and P02 showed that the light
element, H and He, nonmagnetic atmosphere models
can be firmly ruled out because the models (i)
yield too small distances to RXJ1856,
(5-6)
pc and
(ii) overpredict the optical flux by a factor
of 20-30.
P02 found that heavier element atmosphere models can
be reconciled with the PSPC and optical data at
kT=57.4eV,
km for pure Fe, and
kT= 58.7eV,
km for Si-ash compositions,
assuming the gravitational parameter
(
is the Schwarzschild radius)
.
Varying
resulted in negligible changes in the
inferred model parameters unless the strong absorption line
at (unredshifted)
keV (due to
absorption by Fe XVIII ions) penetrates in lower
(redshifted) energies
keV
and significantly affects the quality of the PSPC spectral fits.
The effects of gravity on the emergent spectra are too small
to affect the results of the spectral fits.
The fit of the PSPC spectrum with Fe atmosphere models of
Pavlov & Zavlin (2000) yields
pc,
eV at R=10 km and
,
that are
well consistent with those obtained by P02.
Although the LETGS spectrum revealed no statistically
significant features, it is worthwhile trying the heavy
element atmosphere models on these data.
To fit the LETGS data, we fixed the distance at d=60 pc
and obtained best fitting parameters
,
kT=40.3eV,
km at
(see red curves in the left panels of Fig. 3).
The model fits well at (redshifted)
keV where
the atmosphere spectrum shows no strong spectral features.
However, the situation is drastically different at the
higher energies because of the strong absorption line at
keV (see above) of a
characteristic width
eV and a weaker absorption
complex at
keV.
We note that the LETGS spectrum shows a strong
instrumental feature at E= 0.61-0.63keV (POG).
Despite of a formally small value of
obtained
in this fit, the deviation between the model and LETGS spectra
at
keV are large enough to regard the fit as
unacceptable.
Increasing
(i.e. reducing the redshift) does not
improve the fit because the absorption lines remain within
the observed energy range (see an example of the spectral
fit at
,
R=9.8km and
in
the upper left panel of Fig. 3 [blue curve]).
The same strong Fe features are expected to be present in the Si-ash model spectra as Fe composes 68% of the ash (P02). Therefore, the situation with the Si-ash model fit to the LETGS spectrum should be similar to the Fe case. We also applied atmosphere models with a solar composition containing 2% heavy elements (Grevesse & Noels 1993). The model spectra show numerous prominent spectral features (mainly due to absorption by Fe, C and O ions) in the whole observed energy range (see right panels in Fig. 3, and also Rajagopal & Romani 1996) which are inconsistent with the LETGS data.
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Figure 1: Regions used for extracting the source and background dispersed spectra. The vertical red lines on either side of the gaps between the HRC-S detector plates indicate the the areas that are masked out to avoid getting artificial spectral features due to the dithering across the plate edges (see POG). |
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Figure 2: The best blackbody fit to the LETGS spectrum (red curve) with the blackbody model given by the best PSPC fit (blue curve). |
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Figure 3: The LETGS spectrum fitted with the Fe ( left) and solar mixture ( right) atmosphere models (see text for details). |
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Regardless of the chemical composition,
radiation emitted from the surface of a magnetized
NS should exhibit spectral lines of the
electron (at
keV) and
proton (at
eV) cyclotron resonances
(B12 is the strength of magnetic field in units of 1012G).
The lack of significant features in the LETGS spectrum (0.15-0.82keV)
may appear to exclude the magnetic fields
G
and
G.
But we note that these restrictions on B
are not very stringent because these lines
may be rather faint if the surface layers are only weakly ionized.
Besides, nonuniformity of the magnetic field over the
surface should lead to a strong smearing of the lines
(Zavlin et al. 1995).
Remarkably, the X-ray spectrum of the other isolated NS,
RX J0720.4-3125, obtained with XMM-Newton also
shows no significant spectral features and is well fitted
with a blackbody model of
eV
(Paerels et al. 2001).
P02 argued that a two-component blackbody model
can be reconciled with both the optical and X-ray data
on RXJ1856.
In this model the hard component of
eV
is emitted from a
fractional area on the NS surface
and fits the X-ray data, whereas the soft component of
eV represents radiation from the
cool surface and matches the optical data.
The required non-uniform distribution of the surface
temperature may be due to the strong dependance of thermal
conductivity of the NS crust on the magnetic field at
G (Greenstein & Hartke 1983).
At temperatures
eV and magnetic fields
G hydrogen (if present on the surface) can be
in form of polyatomic molecules and/or a condensed liquid
(Lai & Salpeter 1997).
Although, to our knowledge, no reliable calculations have
been done, one may speculate that such a condensed matter
surface emits radiation close to the blackbody spectrum at
a temperature close to that of the surface,
as suggested by Pavlov (2000)
.
Then, the two-component blackbody interpretation may be
considered as a simplified model of the thermal radiation
from such a magnetized and relatively cool NS.
New important information for elucidating the nature of RXJ1856 is expected to come from the forthcoming 50ks XMM-Newton and 450ks Chandra observations. They will yield an order of magnitude more counts in the dispersed spectra than in the data presented above. This will allow one to take more advantage of the high spectral resolution. Additionally, the new data would enable an unambiguous detection of X-ray pulsations from the source even if the pulsed fraction is as low as 3%. Once the period is found in the new data, it could be traced back to the earlier ROSAT and Chandra data. This would give estimates on the period derivative and, as consequence, magnetic field and age of RXJ1856. The latter, compared with the estimate derived from the optical observations, would shed more light on the nature of this enigmatic source.
Acknowledgements
We thank Fred Walter, George Pavlov and Frits Paerels for intensive discussions. This research was supported by Deutsches Zentrum für Luft- und Raumfahrt grant 50OX0001.