Issue |
A&A
Volume 520, September-October 2010
|
|
---|---|---|
Article Number | A25 | |
Number of page(s) | 18 | |
Section | Stellar structure and evolution | |
DOI | https://doi.org/10.1051/0004-6361/201014542 | |
Published online | 23 September 2010 |
White dwarf masses in intermediate polars observed with the Suzaku satellite![[*]](/icons/foot_motif.png)
T. Yuasa1 - K. Nakazawa1 - K. Makishima1,2 - K. Saitou3,4 - M. Ishida3,5 - K. Ebisawa3,4 - H. Mori3,6 - S. Yamada1
1 - Department of Physics, School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo 113-0033, Japan
2 - Cosmic Radiation Laboratory, The Institute of Physical and
Chemical Research (RIKEN), 2-1 Hirosawa, Wako, Saitama 351-0198, Japan
3 - Japan Aerospace Exploration Agency, Institute of Space and
Astronautical Science, 3-1-1 Yoshino-dai, Chuo-ku, Sagamihara, Kanagawa
252-5210, Japan
4 -
Department of Astronomy, School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo 113-0033, Japan
5 -
Department of Physics, Tokyo Metropolitan University, 1-1 Minami-Osawa, Hachioji, Tokyo 192-0397, Japan
6 -
Department of Astrophysics, School of Science, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8602, Japan
Received 30 March 2010 / Accepted 7 June 2010
Abstract
Context. White dwarfs (WDs) in cataclysmic variables (CVs)
are important experimental laboratories where the electron degeneracy
is taking place on a macroscopic scale. Magnetic CVs increase in number
especially in the hard X-ray band (
keV) thanks to sensitive hard X-ray missions.
Aims. From X-ray spectroscopy, we estimate the masses of nearby WDs in moderately-magnetized CVs, or Intermediate Polars (IPs).
Methods. Using the Suzaku satellite, we aquired wide-band
spectra of 17 IPs, covering 3-50 keV. An accretion column
model of Suleimanov et al. (2005, A&A, 435, 191) and an
optically-thin thermal emission code were used to construct a spectral
emission model of IPs with resolved Fe emission lines. By
simultaneously fitting the Fe line complex and the hard X-ray continuum
of individual spectra, the shock temperature and the WD mass were
determined with a better accuracy than in previous studies.
Results. We determined the WD masses of the 17 IPs with statistical fitting errors of
in many cases. The WD mass of a recently-found IP, IGR J17195-4100, was also estimated for the first time
.
The average WD mass of the sample is
.
When our results were compared with previous X-ray mass determinations,
we found significant deviation in a few systems although the reason of
this is unclear. The iron abundance of the accreting gas was also
estimated, and confirmed the previously reported sub-solar tendency in
all sources with better accuracy.
Key words: accretion, accretion disks - novae, cataclysmic variables - X-rays: binaries
1 Introduction
White dwarfs (WDs) are attractive experimental laboratories where the electron degeneracy plays an important role for supporting the stars against gravity. An accreting WD is of great importance in the universe because some of them probably cause type Ia supernovae as the WD mass reaches the Chandrasekhar limit, and deliver synthesized heavy elements out to the surrounding space. The mass of a WD is thus one of the critical physical parameters which determines the fate of the WD.
Forming a subgroup of cataclysmic variables (CVs), a magnetic
cataclysmic variable (mCV) involves a magnetized WD as a compact star.
mCVs are further classified into polars and intermediate polars (IPs),
according to whether their magnetic field strengths are 107-9 G or 105-7 G,
respectively. Polars are so named after their strong polarization in
the optical and infrared wavelengths, and sometimes referred to as AM
Her type following this prototype (for a review of polars, see Cropper 1990). The magnetic field of a polar is strong enough for the orbital and spin periods of its WD to be synchronized
.
In IPs, the two periods are asynchronous, typically
(for reviews of IPs, see Patterson 1994; Hellier 1996), and polarization is generally weak, although there are some recent measurements of polarization (e.g. Butters et al. 2009).
In both types of these binary systems, mass accretion is taking place
from non-degenerate companions, probably low-mass stars, via Roche-lobe
overflow. Polars do not have an accretion disk. Most IPs have accreting
disks, while in the inner region, the disk is truncated, and gas almost
freely falls onto a WD channeled along its magnetic field. Near the WD
surface, a stationary shock stands to convert the kinematic energy of
the bulk gas motion into thermal energy. Because the temperature of the
shock-heated gas is typically >10 keV, and the density is low,
hard X-rays are emitted via optically thin thermal emission. Then, the
heated gas forms a post shock region (PSR) with a temperature gradient,
wherein the gas descends while it cools via the X-ray emission (e.g. Wu et al. 1994; Aizu 1973; Frank et al. 1992; Wu 1994). As a result, the total spectrum from the PSR is observed as a sum of multi-temperature emission components (e.g. Ishida et al. 1994).
Although mCVs account for a small fraction
of all CVs, they dominate in the hard X-ray band (>10 keV), and most
of CVs detected in recent hard X-ray surveys with INTEGRAL/IBIS and Swift are magnetized (Landi et al. 2009; Barlow et al. 2006; Bird et al. 2010), including both known (e.g. Revnivtsev et al. 2004) and new objects (Landi et al. 2009; Butters et al. 2007; Sazonov et al. 2008; Ajello et al. 2006; Evans et al. 2008; Bonnet-Bidaud et al. 2007).
According to recent X-ray studies (Revnivtsev et al. 2008; Sazonov et al. 2006), mCVs form an important X-ray source population in the lower luminosity range
,
while low-mass X-ray binaries with neutron stars and black hole
binaries dominate in the high-luminosity range. It has also been
suggested that the Galactic ridge X-ray emission (GRXE, Ebisawa et al. 2005; Bleach et al. 1972; Iwan et al. 1982; Koyama et al. 2007a; Valinia & Marshall 1998; Worrall et al. 1982; Revnivtsev & Sazonov 2007; Revnivtsev et al. 2009; Kaneda et al. 1997; Tanaka 2002; Ebisawa et al. 2001; Koyama et al. 1986) and the Galactic Center X-ray emission (Yamauchi et al. 1990; Koyama et al. 1996,1989; Revnivtsev et al. 2007; Muno et al. 2004; Koyama et al. 2007a) mostly consist of numerous dim point sources (Revnivtsev et al. 2009,
and references therein) including RS CVn systems, dwarf novae, and
mCVs, each contributing to different X-ray energy regimes. Especially
in the hard X-ray band, mCVs are attractive candidates because of their
spectral resemblance to the GRXE (Revnivtsev et al. 2006; Krivonos et al. 2007),
including both continua and iron-K lines. If we obtain a reliable
``averaged mCV spectrum'' in the hard X-ray band, we can directly
compare it with that of the GRXE. For this purpose, the construction of
a wide-band spectral model of mCVs and estimation of WD masses are both
mandatory, because mCV spectra can be well expressed as a function of
the WD mass as described in Sect. 2.
Although the mass of a WD is a basic physical quantity, its
determination is generally not easy, since an uncertainty of the
inclination angle of the orbital plane degrades the accuracy of
estimation except for eclipsing systems. However, especially in mCVs,
X-ray spectroscopy provides an independent method; the X-ray spectrum
is primarily determined by the shock temperature, which in turn
reflects the M/R ratio, where M and R are the mass and radius of a WD, respectively. Combining the X-ray estimate on M/R with a theoretical WD mass-radius relation, for example one by Nauenberg (1972),
we can determine M.
The X-ray spectroscopic approach is in practice subdivided into two methods, the continuum method and the emission line method. The former requires a sensitive hard X-ray detector since the relevant spectral feature, namely exponential cutoff which reflects the shock temperature, appears in the hard X-ray range (energy >10 keV). The latter relies on the resolved emission lines (e.g. from Fe), hence requiring a detector with a relatively high energy resolution such as an X-ray CCD (charge coupled device) camera. The continuum method has been applied to the data taken with Ginga (Ishida 1991; Cropper et al. 1998), RXTE (Suleimanov et al. 2008,2005; Ramsay 2000), and Swift (Landi et al. 2009; Brunschweiger et al. 2009). Fujimoto & Ishida (1997) and Ezuka & Ishida (1999) applied the emission line method to the ASCA data, deriving the metal abundances as well.
Suzaku (Mitsuda et al. 2007),
which is the fifth Japanese X-ray astrophysical observatory, has a
wide-band (0.2-600 keV) energy coverage with a high sensitivity,
realized by the X-ray Imaging Spectrometer (XIS, Koyama et al. 2007b), which uses CCDs and the Hard X-ray Detector (HXD, Takahashi et al. 2007)
which consists of semiconductor detectors and scintillator crystals.
The hard X-ray response of the HXD allows us to directly measure the
thermal cutoff of an IP spectrum, and hence estimate its shock
temperature. At the same time, we can use the XIS to resolve emission
lines, especially Fe-K
lines, into three typical components; from almost neutral, He-like, and H-like species. Thus, Suzaku is expected to provide significantly advanced information on the masses of mCVs.
In the present paper, we report masses and iron abundances of IPs estimated by analyzing wide-band Suzaku spectra of 17 objects. Compared to IPs, hard X-ray emission from polars is weaker because cyclotron emission induced by the stronger magnetic field reduces their plasma temperatures. It is also difficult to incorporate the effect of strong magnetic field into a spectral model. Therefore, we only analyzed IPs.
In Sect. 2, we describe a numerically calculated emission model which is used to derive the mass estimations. Target information and data reduction procedure are given in Sect. 3. Section 4 deals with the WD mass estimation. In Sect. 5, we compare our results with previous reports.
2 Modeling of X-ray emission from an accretion column
2.1 Previous works
A number of works have been performed to model X-ray spectra emitted from PSRs of accretion columns in mCVs, and to estimate the PSR temperatures by comparing the model spectrum with observations. The temperatures were then translated into the M/R ratio of their WDs. As mentioned in Sect. 1, these works can be divided into continuum and emission line methods.
In the continuum method, the vertical structure of the accretion column (e.g., profiles of bulk velocity, temperature, and density) is calculated based on plausible physical assumptions, following which an X-ray spectral model can be constructed by convolving thin thermal emission models with the plasma profile. The M/R ratio is a free parameter of the synthesized model spectrum, and should be determined through its comparison with an observed spectrum. Aizu (1973) was the very first who explored this theoretical method. By neglecting the gravitational attraction inside accretion columns, Wu (1994) and Wu et al. (1994) presented profiles of plasma parameters in one-dimensional plane-parallel PSR in closed-integral formulae by considering plasma cooling via bremsstrahlung and cyclotron emission.
Ishida (1991) analyzed Ginga data of several IPs using an isothermal assumption to a PSR, and reported WD mass estimations (or lower limits) for the first time by fitting spectra with an isothermal emission model. By comparing the isothermal emission model with their more realistic spectral calculations, Wu et al. (1995) gave correction factors to the WD masses estimated by Ishida (1991). Cropper et al. (1998) and Ramsay et al. (1998) also used the model of Wu (1994) and fitted data obtained with Ginga, ASCA, and RXTE.
To construct a more physically realistic model, Cropper et al. (1999), Ramsay (2000) and Suleimanov et al. (2005)
calculated the accretion column structure by taking into account the
gravitational attraction, and found that the inclusion of the gravity
slightly reduces the WD mass estimates especially in systems with
higher WD masses (e.g.
,
Ramsay 2000). Brunschweiger et al. (2009) also applied the model of Suleimanov et al. (2005) to the data of 22 IP systems observed with the Swift/BAT, and gave mass estimates. Some authors considered more sophisticated emission models; for example, Suleimanov et al. (2008)
considered the effect of Compton up-scattering of photons by post-shock
plasmas although it was found to change the WD mass estimates only
slightly. Canalle et al. (2005)
calculated PSR temperature and density profiles by taking into account
the dipole magnetic field structure, and showed that this increases
estimated WD masses mainly in high mass (e.g.
)
systems.
As the first application of the emission line method, Ishida & Fujimoto (1995) and Fujimoto & Ishida (1997) analyzed the ASCA/SIS
data of EX Hya. They thus estimated the plasma temperature behind the
shock by comparing observed line-intensity ratios with those
theoretically predicted. Employing the PSR structure of Aizu (1973), they obtained a WD mass estimate of
,
which agreed with that of
derived with optical spectroscopic observations by Hellier (1996). Using the same line-ratio model, Hellier et al. (1996), Fujimoto (1996), and Ezuka & Ishida (1999) investigated WD masses in other systems, giving comparable results with those obtained with the X-ray continuum methods.
2.2 The constructed model
To make the best use of the capability of Suzaku (Sect. 1), we constructed a spectrum model by improving the PSR model of Suleimanov et al. (2005) in two ways. One is to include the Fe-K emission lines, while the other is to improve the plasma cooling function, which is used when solving hydrodynamical equations in the high-temperature regime ( >108.5 K; see the following section). Below we describe how we constructed our model.
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Figure 1: Assumed geometry of the accretion column of an IP. |
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As illustrated in Fig. 1, a one-dimensional cylindrical accretion column, or PSR, is assumed. Channeled by the magnetic field, gas is considered to fall into the accretion column with its supersonic free-fall velocity. At a certain height, a strong shock converts some of the bulk motion of the gas into thermal energy in the PSR. While the shock-heated gas falls subsonically down along the magnetic field lines, it cools by emitting X-rays. Finally, the gas is assumed to softly land onto the atmosphere of the WD. Because the magnetic fields of IPs are not as strong as those of polars, the dominant cooling process of the heated gas is optically thin thermal X-ray emission (free-free plus free-bound plus bound-bound), and the cyclotron cooling can be considered negligible (e.g. Eq. (2) of Wu et al. 1995). Including these, the assumptions made in the present model are summarized as
- 1-dimensional cylindrical accretion (curvature of magnetic field neglected);
- temperature before the shock to be zero;
- gas to be ideal;
- a strong shock;
- cooling via free-free, free-bound, and bound-bound process (cyclotron cooling to be negligible);
- gravitational force in the PSR taken into account;
- soft landing of cooled gas onto the WD surface.
2.3 Calculation of the model
With these assumptions, the accreting plasma flow can be described with hydrodynamical equations; conservations of the mass, the momentum, and the energy. Since these equations and initial conditions assumed in the numerical calculation have been already published by several authors (e.g. Suleimanov et al. 2005; Cropper et al. 1999), we do not recall them here, and follow the same formalization and notation as Suleimanov et al. (2005). Below, we describe major changes and some attentions related to the model calculation.
In the model used in Suleimanov et al. (2005) and Brunschweiger et al. (2009), the plasma cooling function
was taken from Sutherland & Dopita (1993). Although we could integrate the optically-thin emission code (
apec
; see below) to construct a cooling function, we also use the result of Sutherland & Dopita (1993) here. This is because spectra calculated with the emission code only cover E<50 keV currently, and this would artificially reduce cooling rates in higher plasma temperatures (e.g.
keV). However, for rather massive WDs, we need to specially treat a higher temperature regime which is not covered by Sutherland & Dopita (1993) (i.e.
T>108.5 K). In this regime, we extended the
cooling function using a thermally averaged relativistic free-free
Gaunt factor tabulated by Nakagawa et al. (1987).
We averaged the Gaunt factor over the frequency separately for hydrogen
and helium, and then converted the averaged values into the cooling
rate (or energy loss rate) in terms of the total power per unit volume
emitted by thermal bremsstrahlung (see e.g. Rybicki & Lightman 1979),
![]() |
(2) |
where




When a fraction f of the PSR cross section to the WD surface area is set, the specific accretion rate a can be related to the total accretion rate
via
.
Since the luminosity of a PSR is determined by liberated gravitational energy
,
the product af can be regarded as the model normalization. Although a and f can be free parameters in general (see e.g. Cropper et al. 1999; Suleimanov et al. 2005), and the numerical solution changes as a varies, we fixed them at a=1.0 g cm-2 s-1 and f=0.001
(0.1% of the WD surface area) for the sake of an easy comparison with
the previous reports. To rescale the model spectrum, a normalization
parameter, which linearly adjusts the normalization of the model
calculated with the fixed a and f, was introduced. Effects of changing a on our result are discussed in Sect. 5.4.2.
After setting
and a,
finding the solution of the three conservation equations is reduced to
solving an initial value problem of ordinary differential equations. As
explained for example in Cropper et al. (1999) and Suleimanov et al. (2005), this can be practiced with the so-called shooting algorithm. Each trial starts from an assumed shock height z=z0, where the initial parameters are set according to the strong shock limit of the Rankine-Hugoniot relation (Suleimanov et al. 2005). The lower limit of the calculation,
,
is specified by the WD mass-radius relation of Eq. (1). At the WD surface, another boundary condition of the bulk gas speed v=0
is imposed to fulfill the soft-landing assumption. In the algorithm, we
first solve the differential equations from a trial initial value of z0 (for example, 1.01
), and see how the final state of each quantity at
deviates from the conditions assumed above. By taking into account the deviation as a feedback to a new initial z0, we solve the equations again. Until the feedback becomes small enough, below
of derived z0, this procedure is repeated. Practically, this method converged in several to a few tens of iterations at each value of
.
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Figure 2: Results of the numerical solutions for the shock height from the WD surface (thick solid line) and the shock temperature (thin solid line), shown against the WD mass. For comparison, the dashed line shows the shock temperature calculated by assuming no-gravity in the PSR. |
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We executed the calculation over a range of
with a step of
.
Figure 2
shows the dependency of the shock height and the shock temperature on
the WD mass by interpolating data points with spline functions.
In the higher WD masses, the gas velocity at the shock height becomes
higher, and therefore the gas density falls for a given accretion rate.
This causes a decrease in the plasma cooling rate and cooling time,
yielding taller shock heights.
Cropper et al. (1999) showed that an inclusion of the gravitational attraction changes WD mass estimations especially in high mass
systems.
This can be confirmed with the comparison of the profiles of shock
temperature calculated with and without gravitational attraction shown
in Fig. 2. For example, at
,
no-gravity profile overestimates a shock temperature and following
by
compared with the present result. Note that in Cropper et al. (1999), they used an analytic free-free cooling rate (Wu 1994),
which is described in their Appendix A. Therefore, the resulting
shock temperatures (their Fig. 1) are slightly different from our
values (Fig. 2).
Based on the calculation results, we convolved profiles of the
temperature and the density along the accretion column with
(single-temperature) spectra calculated by the optically-thin emission
code apec
(Smith et al. 2001) to obtain a total multi-temperature emission spectrum.
Since we employed apec
spectra instead of the simple bremsstrahlung continuum which Suleimanov et al. (2005)
utilized, our model includes atomic (particularly Fe) emission lines,
which can be an important signature of the plasma temperature in the
present spectral analysis.
In this way, we prepared a series of model spectra for each
by changing the metal abundance of
apec
from 0.1
to 2.0
with a step of
.
Because the currently available version of apec
does not calculate the spectrum above E>50 keV, we can miss the exponential cutoff feature, which is crucial in the calculation of high temperature layers (
kT>20-30 keV). Although this energy range is not
directly employed in our data analysis, the model shapes in that range
are considered important, because the HXD has the broad spectral
redistribution function, and photons with E>50 keV sometimes produce signals in significantly lower energies.
Therefore, above E>50 keV, we substituted spectra estimated by meka
model (which still provides a spectrum in that energy range), with its
normalization set 5.5% smaller than that of the corresponding apec
model. This renormalization is done to make the two spectra match smoothly at E=50 keV
under high temperatures where this substitution is of particular
importance.
In this manner, the model was calculated over the 0.1-100 keV
band. Note however that we only used it only above 3 keV in
spectral fitting to avoid modeling of complex absorption in lower
energies, which is less important for WD mass estimations (see
Sect. 4.1).
Near the WD surface, where the density of a PSR plasma rapidly
increases, the optically-thin assumption will be invalid, and
optically-thick emission will emerge. Although this can alter a PSR
spectrum in the lower energy range (e.g.
keV), we simply used
apec
because our analysis (Sect. 3) utilizes spectra in higher energies (E>3 keV).
Finally, a set of total spectra calculated in this way were converted
to a so-called ``local model'' file of the spectral analysis software Xspec
(Arnaud 1996).
The free parameters of the model are the WD mass, the metal abundance,
and the model normalization. In this local model, spectra for masses
and abundances that are in between the calculation grid points (see
above) are generated by interpolating spectra of the surrounding four
grid points.
Table 1: Suzaku observations of intermediate polars analyzed in the present study.
In Fig. 3 we present normalized profiles of the temperature and density for an IP with a WD mass of 0.7 ,
for comparison with the results of Suleimanov et al. (2005). The shock height of 0.013
,
which we derived, is somewhat different from that of Suleimanov et al. (2005), 0.018
.
This difference might arise from difference of implementation of the
algorithm. In the present study, we do not investigate this difference
since the shock temperatures in the two cases differ only by
.
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Figure 3:
Temperature and density profiles of a PSR calculated for an IP of
|
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3 Observations and data reduction
We assembled our IP sample of 17 systems observed with Suzaku. Table 1 lists information of their Suzaku observations together with their background-subtracted count rates from each detector.
The XIS consists of four X-ray imaging charge coupled device (CCD) cameras as a focal plane detector of the X-ray Telescope (XRT; Serlemitsos et al. 2007). Three (XIS0, 2, and 3) use front-side illuminated (FI) CCD chips, while the other is back-side illuminated (BI; XIS1). The energy coverage is nominally 0.2-12 keV (Koyama et al. 2007b). Since 2006 November, one of the FI sensors, XIS2, has not been operational, and therefore, we utilize data taken with the other three XIS sensors for observations performed after that date.
The HXD is a non-imaging collimated X-ray detector that consists of two main detection parts; silicon p-intrinsic-n diodes (hereafter PIN) and gadolinium silicate (GSO) crystals. They cover the energy range of 10-70 keV (PIN) and 40-600 keV (GSO). In the present analysis, we only utilize PIN data because signals from IPs were hardly detected by GSO.
Since the sample has been constructed by combining different
observations, it is heterogeneous and incomplete, although it can be
regarded as a flux-limited sample in the hard X-ray band. To perform a
detailed spectral analysis, we only selected targets with enough
statistics in the hard X-ray band; sources with background-corrected
HXD count rates higher than 0.04 counts s-1 are used in the present analysis. This rate is equivalent to 10% of the typical HXD background count rate (Fukazawa et al. 2009; Kokubun et al. 2007), or mCrab in terms of flux. With these criteria, AE Aqr, GK Per, and the IP-like object SAX J1748.2-2808 (Nobukawa et al. 2009) were excluded from the sample, although the XIS clearly detects their spectra.
The typical energy bands utilized in the present study are 3-12 keV and 12-50 keV for the XIS and the HXD (Table 1). We limited ourselves to use the XIS data above 3 keV since lower energy spectral shape are affected by the intrinsic multi-column absorption; the time-averaged spectrum is integrated over multiple azimuthal angles, and thus including spectra absorbed by different column density. The higher floor bound of the XIS in some sources are explained in the section below. In some observations, especially in that of FO Aqr, we applied higher floor bound for the HXD data since an enhanced electrical noise contaminated the data therein. The HXD data above 40 keV are discarded when source signals were below 5% of the background.
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Figure 4:
A calculated total spectrum from a PSR of an IP with a WD mass of 0.7 |
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All observations were performed in the normal operation mode of the XIS and HXD. Obtained data were processed with the Suzaku off-line
processing software version 2. We utilized the analysis software
package HEASOFT of version 6.6.2 together with a detector
calibration database (CALDB) version 2009-05-11. We excluded the XIS
and HXD/PIN data taken when the target is occulted by the Earth, or the
spacecraft was in the South Atlantic Anomaly. To reduce the
contamination from scattered Solar X-rays, we also removed the XIS data
taken while the target elevation angle above the Sun-lit Earth rim was
less than .
We applied the same event filtering criteria as used for creating nominal cleaned event files, as described at the Suzaku website
.
In the XIS data analysis, we extracted time-averaged spectra of the targets using circular regions with radii of 2'. Background spectra were also extracted from the same observation data, excluding apparent point sources if any. This background spectrum contains both non-X-ray background (NXB) and diffuse X-ray background (DXB). Because the signal-to-noise ratio is sufficiently high for all targets, the background subtraction ignored the vignetting effect of the XRT (Serlemitsos et al. 2007). We generated redistribution matrices and auxiliary response files of the XIS/XRT using xisrmfgen version 2009-02-28 and xissimarfgen (Ishisaki et al. 2007) version 2009-01-08, respectively (both contained in HEASOFT). In the spectral analysis, we summed the spectra taken by the FI sensors, and used a detector response averaged over them.
Table 2: The best-fit spectral parameters obtained with the partial-covering absorber model.
We accumulated a time-averaged PIN spectrum of each target, and
subtracted the non X-ray background events extracted from the NXB event
file, which in turn was produced from a modeling method by Fukazawa et al. (2009) and distributed via the PIN NXB release website.
The version keyword of the NXB file we used is METHOD=LCFITDT, i.e.
so-called tuned background. We subtracted the DXB component simulated
after Boldt (1987), and subtracted it from the observed spectrum.
This procedure is summarized in the website of NASA Goddard Space Flight Center
.
Since the present sample objects are located off the Galactic plane, we
neglected contributions from the GRXE.
When fitting a PIN spectrum, we employed an appropriate redistribution
matrix file contained in CALDB, depending on the pointing mode and the
observation date. Because the observation of XY Ari was performed at an
off-axis position of the HXD, the effective area of PIN decreased by
;
we took this effect into account by applying an additional auxiliary file calculated with hxdarfgen.
In some observations, XIS images contained weak point sources other
than target IPs. These sources could contaminate the data of PIN
because PIN has a wider field of view (
bottom to bottom). However, their contributions in the PIN energy band are estimated to be
% in XY Ari, and much lower in other observations. Therefore, we simply neglected them in the present analysis.
4 Spectral analysis and results
4.1 Fitting to the XIS/HXD spectra with the partial covering model
Using the tabulated model (Sect. 2; hereafter ip_psr
),
we performed chi-square fitting to the spectra of individual IPs. The
lower energy band (<3 keV) was ignored because analyses in this
band are hampered by multi-column and ionized absorption caused by
pre-shock gas (e.g., Cropper et al. 1999; de Martino et al. 2001). To account for the intrinsic multi-column absorption, we utilized a model with a partial-covering (PC) absorber expressed by vphabs
(available in Xspec
).
A Gaussian was added to the model to express the neutral (or low ionized) Fe K
emission line at
keV. In addition, the entire model spectrum was subjected to interstellar absorption using
phabs
. The total model expression is thus
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|||
![]() |
|||
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where
constant
is a renormalization factor for the two detectors (see Suzaku Memo 2008-06![[*]](/icons/foot_motif.png)

ip_psr
components are constrained to have a common set of parameters. The Fe abundance of vphabs
was equalized to that of ip_psr
, considering that the X-ray absorbing and emitting gas must have the same chemical composition.
First, we fitted the wide-band spectra using all XIS data starting from
3 keV. The HXD spectra were fitted over the energy ranges listed
in Table 1. The table also gives the shock temperatures, which are related to
through Fig. 2.
Hereafter, the quoted errors are at 90% confidence levels unless
otherwise noted. Note that the WD mass of IGR J17195-4100 was estimated
for the first time as far as we know.
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Figure 5:
Observed XIS and HXD spectra (black crosses) of individual IPs compared with the best-fit model (solid line). Left panels: raw spectra, wherein the detector responses are not removed. The lower panels show the data-to-model ratio. Right panels: the same spectra, shown after removing of the detector responses and multiplied by E2. Equivalent to the |
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In the present fitting, we considered fits with a null-hypothesis
probability higher than 1% as acceptable. Based on this criterion,
acceptable fits were obtained with this partial covering model in 11
systems; FO Aqr, EX Hya, NY Lup, V2400 Oph, V1223 Sgr, and RX J2133 are
remainders. The best-fit parameters are listed in Table 2 and Figs. 5 and A.1
show the spectra and the best-fit models of individual IPs. For the
remaining six objects, we listed results obtained after prescriptions
described in the paragraphs below. The average WD mass and the mean
iron abundance associated with their 1
standard deviations were
and
,
respectively.
When fitted with the partial covering model, EX Hya showed large
bipolar residuals in the energy band slightly below the H-like Fe K
line. As reported by Hellier & Mukai (2004) with Chandra/HETG
data, the highly ionized Fe lines from EX Hya have complex shapes with
considerable contribution from unresolved dielectric satellite lines.
Although this might be a cause of the residual, we leave this
speculation as a future task because it is difficult to diagnose the
line structure with the energy resolution of the XIS. In the present
study, we therefore put the original fitting result obtained with the
partial covering model in Table 2.
The estimated WD mass did not change within errors even if the H-like
Fe emission line was ignored in the fitting since the thermal cutoff is
clearly detected in the PIN spectrum, and it strongly constrains the
shock temperature (and hence a WD mass).
In NY Lup, V1223 Sgr, and RX J2133, positive residuals were observed near the lower bound of the XIS data. We suspect that these residuals reflect the complex absorption structure in the lower energy spectra, which are not as so important when determining shock temperatures and WD masses. Therefore, we gradually changed the lower bound of the XIS spectrum, and found that fits become acceptable when the lower bound energies listed in Table 1, 3.5 keV for NY Lup, and 4 keV for V1223 Sgr and RXS J2133, were employed. These changes did not significantly affect the best-fit parameters, and therefore we simply regarded the resultant parameters of these fittings with the narrower energy bands as the current best estimations.
In FO Aqr and V2400 Oph, the partial covering model did not
give an acceptable fit even when the employed energy ranges were
changed. Instead, the fits improved significantly to an acceptable
level when an additional absorbed ip_psr
component was incorporated. Since these sources are supposed to have high accretion rates (Suleimanov et al. 2005),
we consider that taking this additional absorbed component into account
is reasonable. Therefore, we estimated WD masses in these sources using
this modified model. The column densities of the additional absorbed
component are also listed below those of the primary PC model in
Table 2.
In systems with special accreting and viewing geometries, the Fe
emission lines (6.7 keV) could be artificially enhanced or
suppressed by ``resonance trapping'' of the Fe-K line photons (Terada et al. 2001), because the optical depth of the process is higher than 1 (e.g. 25 by Done et al. 1995). This could affect our abundance measurements, and in turn, those of
.
However, this effect is only of a importance when the column is
observed either pole-on (the Fe-K line enhanced) or side-on
(suppressed) through a large fraction of the spin phase (Terada et al. 2001).
Because our 17 IPs are more or less pulsating at their spin periods, they are not likely to be either pole-on or side-on, and the enhancement or suppression, if any, can be averaged out by the WD spin (changing viewing angle). We therefore consider that this effect is negligible for the present study, and that the derived sub-solar abundances reflect a true property of the accreting gases.
4.2 HXD/PIN-only fitting
We also fitted the HXD/PIN spectra alone to confirm the result of
the partial covering model at the energy band where even the strongest
absorption little changes the spectral model. In the fitting, we fixed
.
The results of this analysis are compared with those from the wide-band fitting (Sect. 4.1) in Fig. 6. Large y-axis errors are simply due to lower statistics in the PIN data. The masses derived with the two methods thus agree with each other within errors. In particular, we do not find any systematic differences between the two sets of estimates. This self-calibration ensures the consistency of the continuum and line methods.
![]() |
Figure 6: Comparison of the WD masses estimated from the partial covering model using the XIS and HXD/PIN data, with those determined by the HXD/PIN data alone ignoring the partial covering. Source names are abbreviated. |
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5 Discussion
5.1 Comparison with previous reports: WD masses
5.1.1 Based on X-ray data
Table 3 compares the present Suzaku XIS+HXD results with the WD masses reported by the previous studies in the X-ray band. In Fig. 7 we plot correlations between our WD masses and those from the RXTE/PCA+HEXTE data by Suleimanov et al. (2005) and the Swift/BAT data by Brunschweiger et al. (2009); the spectral models and the energy band used in these three studies are very similar to one another.
Table 3: Estimated WD masses compared with previous reports in the X-ray band.
In Figs. 7a and b, our results derive higher WD masses, especially for massive
systems, although rough correlations are seen among the three
measurements. For a few sources, for example V709 Cas, BG CMi, and PQ
Gem, this discrepancy amounts to
.
Reasons for these differences are unclear at present. Unfortunately, the WD masses of Suleimanov et al. (2005) and Brunschweiger et al. (2009)
show the same level of disagreement as seen in these figures, although
the two studies use the same spectral model calculated in the former.
This might indicate that the results suffer from rather large
systematic uncertainties, which could exceed the quoted statistical
fitting errors. We are aware that our analysis is not free either of
possible systematic uncertainties (Sect. 5.4)
involved in the detectors and the spectral model. Yet our result may be
less subject to various systematic effects, because we jointly utilized
the Fe-K line spectroscopy and the hard-band continuum shape, and the
wide-band fitting result is consistent with that from the PIN-only
fitting (Fig. 6).
![]() |
Figure 7: Comparison of the WD masses estimated in the present study with those by a) Suleimanov et al. (2005) and b) Brunschweiger et al. (2009). |
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From X-ray light curve analysis in the eclipsing IP XY Ari, Hellier (1997) estimated
to be
.
Our result,
,
nicely agrees with this value, and this agreement provides a convincing calibration to the present methodology (see also Brunschweiger et al. 2009).
5.1.2 Other methods
It is also meaningful to compare the derived WD masses with those
estimated from binary kinematics based mainly on optical/IR
spectroscopy. Using references in the CV catalog by Ritter & Kolb (2003), we collected reports on
of IPs, and then plotted them as shown in Fig. 8.
Note that most of the reports employed an assumption of a Roche-lobe
filling Zero Age Main Sequence star to estimate radius and mass of the
secondary (non-degenerate) stars, and this may be a cause of systematic
uncertainties in their WD mass estimations.
![]() |
Figure 8:
Comparison of the WD masses estimated in the present study with those in the optical and infra-red wavelengths. References are Hellier (1997) for XY Ari, Penning (1985) for BG CMi, Hellier (1993) for TV Col, Haswell et al. (1997) for YY Dra, and Beuermann et al. (2004) for V1223 Sgr. For EX Hya, two different values are presented;
|
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All masses agree (with rather large errors) except for EX Hya. For
this object, WD masses determined spectroscopically in optical/IR
wavelength have been somewhat controversial. The difference of the WD
masses are mainly caused by different radial velocity estimations.
Based on NaI and CaII line profiles, Beuermann & Reinsch (2008) estimated the amplitude of a radial velocity of the secondary (non-degenerate) star K2 to be
km s-1 by assuming that of the primary WD K1 of
km s-1 (Belle et al. 2003; Hoogerwerf et al. 2004). From these values, they obtained
.
On the contrary, Mhlahlo et al. (2007) derived
km s-1 from H
,
H
,
and H
lines, and used K2 of
km s-1 reported by Vande Putte et al. (2003), leading to the WD mass
which disagrees with the former value by more than four times the error range.
Independently of the radial velocities, the PIN spectrum of EX Hya
clearly shows a cutoff in the 10-20 keV band (Sect. 4.1),
and because of this cutoff together with the Fe line structure, the
lower WD mass is favored by the fitting. The cutoff cannot be explained
by a WD of 0.7
since
our model implies a shock temperature of 30 keV and a similar
cutoff-energy, and even multiple absorption or reflection cannot fake a
lower cutoff energy from a spectrum of the high shock temperature. The
inconsistency with the WD mass of Beuermann & Reinsch (2008) might imply the necessity of some modifications to the assumptions of the geometry and the physical processes (Sect. 2.2) in this object.
5.2 The WD mass spectrum and its average
Figure 9
shows the distribution of the WD mass of our sample, compared with
those of CVs determined kinematically, mainly based on optical/IR
spectroscopy (Ritter & Kolb 2003). The two distributions give the mean masses of
for the present study and
for the optical sample (errors are 1
standard deviations), and the Kolmogorov-Smirnov probability is 0.39.
Therefore it is inferred with this limited sample that the mass spectra
of CVs and IPs are statistically not largely different. With this
distribution, although the systematic uncertainties (Sect. 5.4)
should be examined carefully, we consider that the WD masses of IPs are
truly distributed, not extracted from a single common value with errors
caused by the analysis method.
![]() |
Figure 9: WD mass spectrum of our sample IPs (shaded histogram), compared with that of 104 CVs (histogram with dashed line; taken from Ritter & Kolb 2003). |
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The mean WD mass of our IP sample,
,
can be compared with the value of
inferred by Krivonos et al. (2007) based on the analysis of Galactic Ridge X-ray Emission (GRXE) in the hard X-ray band with INTEGRAL/SPI.
This comparison is intriguing because IPs are thought to have deep
connection with the origin of the GRXE (especially in the hard X-ray
band). However, before examining any discussion about the discrepancy
of the two values, we should consider the incompleteness of our sample.
The current sample only consists of IPs localized to the solar vicinity
(
pc)
because of their intrinsic low luminosity. Because their selection is
usually flux-limited, it can be biased to IPs with higher WD masses
which give higher fluxes in the hard X-ray band. In addition, the GRXE
spectrum may be decomposed into various types of X-ray sources over a
wide energy range (e.g. Revnivtsev et al. 2006).
Among them, RS CVn systems and dwarf novae have softer spectra, and if
their contribution is considered simultaneously with IPs, the IP
component in the GRXE spectrum may become harder, leading to a higher
WD mass. Then the difference of the two values may be reduced.
5.3 Comparison of Fe abundances
Fujimoto & Ishida (1997), Ezuka & Ishida (1999), and Evans et al. (2004)
estimated metal abundances of IPs by analyzing the resolved Fe line
complex (6-7 keV) and X-ray continua with the multi-temperature
PSR model. Fujimoto & Ishida (1997) obtained the Fe abundance of EX Hya as
,
which was later revised by Ezuka & Ishida (1999) to
together with measurements of the Fe abundances of 12 other IPs.
Evans et al. (2004) gave the metal abundance of
for FO Aqr (whilst they did not take their result as evidence of genuine sub-solar abundance).
Since our IP sample is well covered by that of Ezuka & Ishida (1999), we compare our result with theirs in Table 4 and Fig. 10. Although the two results consistently indicate sub-solar abundances, they exhibit no particular correlation. Considering that the Suzaku data have a much wider spectral coverage, higher statistics, and a somewhat better energy resolution than those from ASCA which Ezuka & Ishida (1999) used, our results may be seen as more updated. Note also that Ezuka & Ishida (1999) did not take into account partial covering or the reflection component.
![]() |
Figure 10: Fe abundances determined in the present study, compared with the measurements by Ezuka & Ishida (1999). Source names are abbreviated. |
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Table 4: Comparison of the Fe abundances with values reported by Ezuka & Ishida (1999) associated with 90% confidence intervals.
When our 17 objects are divided into seven objects with
and the other 10 with
,
the former and latter sub-samples have averaged Fe abundances of
and
,
respectively. The lack of significant difference ensures that our
abundance determinations are not strongly affected by the continuum
shape. We suppose that these different sub-solar values reflect various
metal abundances of the accreting gas and the companion
(non-degenerate) stars.
Previous studies of summed (unresolved) Fe lines also reported sub-solar Fe abundances in IPs.
Using Ginga, Beardmore et al. (2000) reported an underabundance of metals by a factor of
relative to solar for V1223 Sgr. This roughly agrees with our result,
.
de Martino et al. (2004) gave
for PQ Gem (RE0751+14), which is also comparable to ours
.
5.4 Limitations and systematic uncertainties of our assumptions
In this section, we discuss the limitations in our assumptions of the present model calculation
and the WD mass estimation. As a whole, these may cause systematic uncertainties, and affect our WD mass results (Table 2)
to some extent. Nevertheless, we regard the present results as
meaningful, because the estimated systematic effects are not
significantly larger than the statistical precision associated with our
determinations of
.
More detailed spectral analyses, which are less subject to the
limitations will be possible with data taken with future
high-resolution and wide-band instruments, such as the X-ray
microcalorimeter and the hard X-ray imager onboard the ASTRO-H satellite (Takahashi et al. 2008).
5.4.1 Dynamics of accreting gas and system geometries
As detailed in Suleimanov et al. (2005) and Brunschweiger et al. (2009),
the assumption that the accreting gas falls freely from an infinite
distance is not necessarily warranted, since the gas may well form an
accretion disk and radiate away part of its energy release there. If
such a disk is truncated, under plausible parameters, at a radius of
cm in an IP with a WD of
,
the shock temperature, and hence
,
would be underestimated by
.
Similarly, a fast spin of a WD would also cause the present method to underestimate
because of the centrifugal force. If corrected for this effect, the WD masses in Table 2 of two rapid rotators in our sample, V709 Cas (with a spin period of 312.78 s) and YY Dra (
s), could increase by a few tens of percent depending on their accretion rates.
In addition to this, a fast spinning WD might obey a different (equatorially elongated) mass-radius relation (e.g. Nauenberg 1972; Geroyannis & Papasotiriou 1997). However, precise numerical treatment of this effect exceeds the scope of our present study, and we leave it untouched.
According to Canalle et al. (2005), the inclusion of the dipole curvature in the PSR calculation
reduces the calculated shock temperature by
for
under typical accreting colatitudes, and <2-3% for
.
At present, it is hardly possible to observationally constrain the
magnetic field structure near the WD magnetic poles. Therefore, we
reluctantly neglected the curvature of the WD magnetic field when
calculating the PSR structure (Sect. 2.2). In Table 2, five systems have upper WD mass limits below 0.8
,
and we suppose this systematic effect can be safely neglected at least for these light systems.
5.4.2 Accretion rate dependence
In the spectral fitting, we freely varied the normalization (i.e. accretion rate) of the PSR spectral model, which was calculated assuming a fixed specific accretion rate of 1.0 g cm-2 s-1 (Sect. 2.3). Strictly speaking, this means a self-inconsistency, because the calculated shock height and the shock temperature should increase and decrease, respectively, as the accretion rate decreases; this, in turn, is because the free-free cooling rate is proportional to the plasma density squared (e.g. Aizu 1973).
![]() |
Figure 11: Result of the numerical calculation of the PSR model when changing the accretion rate. Shock temperatures are plotted with solid, long dashed, short dashed, and dotted lines for accretion rates of 0.1, 1, 5, and 10 g cm-2 s-1. |
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To examine the accretion-rate dependence of our numerical result, we
performed calculations with several different accretion rates as shown
in Fig. 11. As noted above, a lower value of a gives a lower shock temperature at any
.
For higher
,
difference of the resulting shock temperatures is more or less conspicuous. At
,
we see a difference of a factor of 1.13 between the results of a=0.1 and 1.0 g cm-2 s-1, and a factor of 1.02 between a=1.0 and 10 g cm-2 s-1. Correspondingly, at
,
the difference increases to factors of 1.33 (a=0.1 to a=1.0) and 1.10 (a=1.0 to a=10). In most systems we analyzed (except for V709 Cas), WD masses are below 1.2
,
and therefore we consider that this uncertainty affects the WD mass estimates only slightly, much less than
.
Especially in lower
,
the a
dependence is small, and therefore we presume that the estimated shock
temperatures and WD masses are considerably secure in this mass range.
5.4.3 PSR base temperature
In the present study, the PSR temperature was assumed to fall to zero at its base although irradiating hard X-rays from the PSR may heat the WD photosphere (e.g. Cropper et al. 1998). Indeed, non-zero base temperatures have been suggested observationally by several authors (see. Ezuka & Ishida 1999, and references therein).
This uncertainty could be avoided by iteratively calculating the PSR emission model with a finite base temperature until a model fit converges into a self-consistent result. We did not perform this because of the limitation on the computation time and the statistical quality of the data. Furthermore, as noted in Sect. 2.3, emission will become thick near the WD surface, and therefore a more sophisticated spectral model which takes this effect into account is needed to be constructed for performing this analysis.
5.4.4 Reflection component
The spectra of the present IP sample show clear detections of the fluorescent Fe line at keV.
This strongly indicates that some of the incident X-rays are emitted
from a PSR reflected by cold gas near the WD surface or pre-shock
region (see Ezuka & Ishida 1999, and references therein). However, in the present spectral fitting (Sect. 4.1)
we did not take into account a reflection component from the WD surface
explicitly because the computation power needed to precisely calculate
the reflection is unaffordable at this moment. Qualitatively, its
effect may be represented to some extent by the strongly absorbed
component in the partial-covering model, which has a similar spectral
shape to a reflection component, both contributing mainly in the PIN
energy band.
Cropper et al. (1998) revealed that
an inclusion of a reflection component changes the obtained WD masses
only slightly from those of their partial covering fittings. By
analyzing a wide-band spectrum of V1223 Sgr with a reflection
component, Revnivtsev et al. (2004) derived a WD mass of
.
Our result,
well agrees with their value, and thus an effect of the reflection
component can be considered not as very large. A full treatment of a
reflection component is left as our future work.
6 Summary
We numerically solved the hydrostatic equations for PSRs of mCVs of Suleimanov et al. (2005), and updated it (Sect. 2.2) in terms of (1) the additional cooling function at higher temperatures and (2) the optically thin thermal emission code, which includes Fe emission lines. By constructing the spectral model file (Sect. 2.2), we fitted 17 IPs observed with Suzaku, and successfully reproduced the Fe line structures in the 6-7 keV band and at the same time the thermal cutoff detected in the hard X-ray band (Sect. 4.1). From the best-fit models, we estimated the WD masses and the Fe abundances. The average WD mass for the present sample were


The derived WD masses are compared with previous reports (Sect. 5.1), and a rough correlation was confirmed, although results on a few systems differ significantly
.
We also tentatively compared the mean WD mass with the value inferred
from the analysis of the GRXE in the hard X-ray band (Sect. 5.2), and found a difference by
,
although this may arise from various systematic biases.
T.Y. is financially supported by the Japan Society for the Promotion of Science. This research has made use of data and softwares obtained from the Data Archive and Transmission System at JAXA/ISAS and the High Energy Astrophysics Science Archive Research Center at NASA Goddard Space Flight Center.
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Online Material
Appendix A: Spectral fitting result
In Fig. A.1 we present the observed spectra overlaid with the best-fit model spectra (online version only).
![]() |
Figure A.1: Continued from Fig. 5. |
Open with DEXTER |
![]() |
Figure A.1: continued. |
Open with DEXTER |
![]() |
Figure A.1: continued. |
Open with DEXTER |
![]() |
Figure A.1: continued. |
Open with DEXTER |
Footnotes
- ... satellite
- Appendix A is only available in electronic form at http://www.aanda.org
- ...website
- http://www.astro.isas.jaxa.jp/suzaku/process/v2changes/criteria_xis.html
- ... website
- http://www.astro.isas.ac.jp/suzaku/analysis/hxd/pinnxb/
- ... Center
- http://heasarc.gsfc.nasa.gov/docs/suzaku/analysis/pin_cxb.html
- ... 2008-06
- ftp://legacy.gsfc.nasa.gov/suzaku/doc/xrt/suzakumemo-2008-06.pdf
All Tables
Table 1: Suzaku observations of intermediate polars analyzed in the present study.
Table 2: The best-fit spectral parameters obtained with the partial-covering absorber model.
Table 3: Estimated WD masses compared with previous reports in the X-ray band.
Table 4: Comparison of the Fe abundances with values reported by Ezuka & Ishida (1999) associated with 90% confidence intervals.
All Figures
![]() |
Figure 1: Assumed geometry of the accretion column of an IP. |
Open with DEXTER | |
In the text |
![]() |
Figure 2: Results of the numerical solutions for the shock height from the WD surface (thick solid line) and the shock temperature (thin solid line), shown against the WD mass. For comparison, the dashed line shows the shock temperature calculated by assuming no-gravity in the PSR. |
Open with DEXTER | |
In the text |
![]() |
Figure 3:
Temperature and density profiles of a PSR calculated for an IP of
|
Open with DEXTER | |
In the text |
![]() |
Figure 4:
A calculated total spectrum from a PSR of an IP with a WD mass of 0.7 |
Open with DEXTER | |
In the text |
![]() |
Figure 5:
Observed XIS and HXD spectra (black crosses) of individual IPs compared with the best-fit model (solid line). Left panels: raw spectra, wherein the detector responses are not removed. The lower panels show the data-to-model ratio. Right panels: the same spectra, shown after removing of the detector responses and multiplied by E2. Equivalent to the |
Open with DEXTER | |
In the text |
![]() |
Figure 6: Comparison of the WD masses estimated from the partial covering model using the XIS and HXD/PIN data, with those determined by the HXD/PIN data alone ignoring the partial covering. Source names are abbreviated. |
Open with DEXTER | |
In the text |
![]() |
Figure 7: Comparison of the WD masses estimated in the present study with those by a) Suleimanov et al. (2005) and b) Brunschweiger et al. (2009). |
Open with DEXTER | |
In the text |
![]() |
Figure 8:
Comparison of the WD masses estimated in the present study with those in the optical and infra-red wavelengths. References are Hellier (1997) for XY Ari, Penning (1985) for BG CMi, Hellier (1993) for TV Col, Haswell et al. (1997) for YY Dra, and Beuermann et al. (2004) for V1223 Sgr. For EX Hya, two different values are presented;
|
Open with DEXTER | |
In the text |
![]() |
Figure 9: WD mass spectrum of our sample IPs (shaded histogram), compared with that of 104 CVs (histogram with dashed line; taken from Ritter & Kolb 2003). |
Open with DEXTER | |
In the text |
![]() |
Figure 10: Fe abundances determined in the present study, compared with the measurements by Ezuka & Ishida (1999). Source names are abbreviated. |
Open with DEXTER | |
In the text |
![]() |
Figure 11: Result of the numerical calculation of the PSR model when changing the accretion rate. Shock temperatures are plotted with solid, long dashed, short dashed, and dotted lines for accretion rates of 0.1, 1, 5, and 10 g cm-2 s-1. |
Open with DEXTER | |
In the text |
![]() |
Figure A.1: Continued from Fig. 5. |
Open with DEXTER | |
In the text |
![]() |
Figure A.1: continued. |
Open with DEXTER | |
In the text |
![]() |
Figure A.1: continued. |
Open with DEXTER | |
In the text |
![]() |
Figure A.1: continued. |
Open with DEXTER | |
In the text |
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