A&A 430, L69-L72 (2005)
DOI: 10.1051/0004-6361:200400131
M. A. Guerrero1 - Y.-H. Chu2 - R. A. Gruendl2 - M. Meixner3
1 - Instituto de Astrofísica de Andalucía, CSIC,
Apartado Correos 3004, 18080, Granada, Spain
2 -
Astronomy Department, University of Illinois,
1002 W. Green Street, Urbana, IL 61801, USA
3 -
Space Telescope Science Institute, 3700 San Martin Drive,
Baltimore, MD 21218, USA
Received 1 December 2004 / Accepted 19 December 2004
Abstract
The Eskimo Nebula (NGC 2392) is a double-shell planetary nebula (PN)
known for the exceptionally large expansion velocity of its inner shell,
90 km s-1, and the existence of a fast bipolar outflow with a
line-of-sight expansion velocity approaching 200 km s-1.
We have obtained XMM-Newton observations of the Eskimo and
detected diffuse X-ray emission within its inner shell.
The X-ray spectra suggest thin plasma emission with a temperature
of
2
106 K and an X-ray luminosity of
erg s-1, where d is the distance in parsecs. The diffuse X-ray emission shows noticeably different spatial
distributions between the 0.2-0.65 keV and 0.65-2.0 keV bands.
High-resolution X-ray images of the Eskimo are needed to determine
whether its diffuse X-ray emission originates from shocked fast wind
or bipolar outflows.
Key words: ISM: planetary nebulae: general - ISM: planetary nebulae: individual: NGC 2392 - stars: winds, outflows
Planetary nebulae (PNe) consist of the stellar material ejected
by low- and intermediate-mass stars (1-8
)
at the end
of the asymptotic giant branch (AGB) phase.
As such a star evolves off the AGB, the copious mass-loss strips
off the stellar envelope and exposes the hot stellar core.
A PN emerges when the stellar UV radiation ionizes the ejected
stellar material, causing it to emit in the optical.
PNe are expected to be diffuse X-ray sources. The central stars of PNe possess fast stellar winds with terminal velocities of 1000-4000 km s-1 (Cerruti-Sola & Perinotto 1985), while fast collimated outflows with velocities up to 1000 km s-1 are also observed in PNe and proto-PNe, e.g., MyCn 18 and Hen 3-1475 (O'Connor et al. 2000; Bobrowsky et al. 1995; Riera et al. 1995). The interactions of the fast stellar wind and/or collimated outflows with nebular material produce shocked gas that is hot enough to emit in X-rays.
In the interacting-stellar-winds model of PNe (Kwok et al. 1978), the fast wind emanating from the central star sweeps up the slow AGB wind to form a sharp nebular shell. The interior structure of a PN would be similar to that of a wind-blown bubble (e.g., Weaver et al. 1977). The central cavity of a PN is expected to be filled with shocked fast wind at 107-108 K, but this hot gas is too tenuous to produce appreciable X-ray emission. Dynamic or evaporative mixing of cool nebular material into the hot gas at their interface produces optimal conditions for soft X-ray emission, which will show a limb-brightened morphology within the nebular shell, as observed in NGC 6543 (Chu et al. 2001).
Fast collimated outflows or jets may also produce hot X-ray-emitting
gas.
When outflows with velocities
300 km s-1 initially impinge
on the AGB wind, bow shocks and X-ray emission can be produced
(e.g., Hen 3-1475, Sahai et al. 2003).
The prolonged action of collimated outflows may bore through the
AGB wind and form extended cavities filled by shocked hot gas
that emits X-rays (e.g., Mz 3, Kastner et al. 2003).
Diffuse X-ray emission from hot gas in PNe was hinted by ROSAT
observations (Guerrero et al. 2000), but was unambiguously resolved only by
Chandra and XMM-Newton observations.
Besides the aforementioned Hen 3-1475, Mz 3, and NGC 6543, diffuse
X-ray emission has been reported in only 4 other PNe: A 30,
BD+30
3639, NGC 7009, and NGC 7027
(Kastner et al. 2001; Chu et al. 1997; Kastner et al. 2000; Guerrero et al. 2002).
It is imperative to detect diffuse X-ray emission from a large number
of PNe to investigate whether shocked fast stellar wind, collimated
outflows or both are responsible for the X-ray emission from PNe.
![]() |
Figure 1:
XMM-Newton and HST H |
| Open with DEXTER | |
The Eskimo Nebula (NGC 2392) offers an excellent opportunity to assess the effects of collimated outflows in a PN. The Eskimo is a double-shell PN: its bright elliptical inner shell has two blister-like protrusions on the south rim, and its round outer shell contains a set of complex low-ionization features (O'Dell et al. 2002). In addition, the Eskimo has a fast collimated outflow, detected in high-dispersion spectra of optical nebular lines; the outflow, with line-of-sight expansion velocities approaching 200 km s-1, is dynamically interacting with nebular material (Gieseking et al. 1985; O'Dell & Ball 1985; O'Dell et al. 1990; Maestro et al., in preparation). We have obtained XMM-Newton observations of the Eskimo and here we report the detection of diffuse X-ray emission from this nebula.
The Eskimo Nebula was observed with the XMM-Newton Observatory in Revolution 790 on 2004 April 2 using the EPIC/MOS1, EPIC/MOS2, and EPIC/pn CCD cameras. The two EPIC/MOS cameras were operated in the Full-Frame Mode for a total exposure time of 17.5 ks, while the EPIC/pn camera was operated in the Extended Full-Frame Mode for a total exposure time of 12.5 ks. For all observations, the Medium filter was used. The XMM-Newton pipeline products were processed using the XMM-Newton Science Analysis Software (SAS version 6.0.0) and the calibration files from the Calibration Access Layer available on 2004 June 10.
The event files were screened to eliminate events due to charged
particles or associated with periods of high background.
For the EPIC/MOS observations, only events with CCD patterns 0-12
(similar to ASCA grades 0-4) were selected;
for the EPIC/pn observation, only events with CCD pattern 0 (single
pixel events) were selected.
Time intervals with high background (i.e. count rates
0.3 cnts s-1 for the EPIC/MOS or
1.4 cnts s-1
for the EPIC/pn in the background-dominated 10-12 keV energy range)
were discarded. The resulting exposure times are 17.3 ks, 17.1 ks, and 11.6 ks for
the EPIC/MOS1, EPIC/MOS2, and EPIC/pn observations, respectively.
The XMM-Newton EPIC/MOS1, EPIC/MOS2, and EPIC/pn observations
of the Eskimo detect within the nebula a total of 180
15,
175
15, and 620
30 cnts, respectively.
In order to construct an X-ray image of the highest signal-to-noise
ratio, we merged together the event files of the three EPIC observations and extracted raw EPIC images in the 0.2-2.0, 0.2-0.65,
and 0.65-2.0 keV bands with a pixel size of 1
5 (Figs. 1-d).
The raw EPIC image in the 0.2-2.0 keV band is then adaptively
smoothed using Gaussian profiles with FWHM ranging from 4'' to 6''.
The contour map of this smoothed image is overplotted on a
Hubble Space Telescope (HST) Wide Field Planetary Camera 2
(WFPC2) H
image (Fig. 1b).
The alignment of X-ray and optical images is fine-tuned using
HD 59087, a star
100'' north of the Eskimo, which is
detected both in the XMM-Newton EPIC and HST WFPC2 images.
The X-ray emission from the Eskimo is clearly extended.
Its distribution is elongated along PA
25
(Fig. 1a),
and the 25% contour of the smoothed EPIC image follows closely
the outline of the the inner shell in the HST H
image (Fig. 1b).
The image in the 0.2-0.65 keV band shows a similar spatial
distribution, but in the 0.65-2.0 keV band the emission is
elongated along PA
70
,
i.e., roughly aligned
with the fast bipolar outflow detected at PAs of 50
-80
and 230
-260
,
as illustrated in Fig. 1d
(Gieseking et al. 1985; Maestro et al., in preparation).
These comparisons suggest that the diffuse X-ray emission from the
Eskimo is mostly confined within its inner shell, but some of the
harder X-ray emission in the 0.65-2.0 keV band may be produced by
the interaction of the fast bipolar outflow with nebular material.
![]() |
Figure 2:
(Top) XMM-Newton EPIC/pn background-subtracted spectrum of the Eskimo
overplotted with the best-fit MEKAL model.
For plotting purposes, both the spectrum and model are binned in 30 eV
wide energy bins. (Inset) |
| Open with DEXTER | |
To analyze the properties of the diffuse X-ray emission from the Eskimo,
we extracted a spectrum from the EPIC/pn event file using a circular
source aperture of 20'' radius, large enough to include all X-ray
emission from the nebula. The background level was assessed from an annular region exterior to
the source aperture and 9 times larger in area. The background-subtracted EPIC/pn spectrum of the Eskimo is shown in Fig. 2. This spectrum shows a broad peak between 0.4 and 0.6 keV,
a plateau below 0.4 keV, and a sharp decline above 0.6 keV. Low-intensity emission peaks are discernible at
0.9 keV,
1.1 keV, and
1.8 keV.
The overall spectral shape indicates thermal plasma emission, and
the peaks correspond to the He-like triplets of
N VI at
0.43 keV,
O VII at
0.57 keV,
Ne IX at
0.92 keV,
Na X at
1.13 keV, and
Si XIII at
1.86 keV.
We have also extracted EPIC/MOS spectra; they show similar spectral
features at lower signal-to-noise ratios, so we will concentrate
only on the EPIC/pn spectrum in the analysis below.
The observed spectrum can be modeled to determine the physical
conditions of the X-ray-emitting gas and the amount of foreground
absorption. We have adopted the MEKAL optically-thin plasma emission model
(Liedhal et al. 1995; Kaastra & Mewe 1993) and nebular abundances,
although we note that these may differ from those of the
X-ray-emitting gas (e.g., Maness et al. 2003).
The abundances of He, C, N, O, Ne, Ar, and S relative to
hydrogen by number, as determined from optical and UV spectra
of the Eskimo, are 0.076, 2.2
10-4, 1.1
10-4,
2.8
10-4, 6.4
10-5, 1.4
10-6, and
4.3
10-6, respectively (Barker 1991; Henry et al. 2000).
For elements that do not have available nebular abundances, we adopt
solar abundances (Grevesse & Sauval 1998).
We have also assumed solar abundances for the foreground interstellar
absorption, and adopted absorption cross-sections from Balucinska-Church & McCammon (1992).
The spectral fit is carried out by folding the absorbed MEKAL model
spectrum through the EPIC/pn response matrix, and comparing the
modeled spectrum to the observed EPIC/pn spectra in the 0.2-2.5 keV
energy range using the
statistics.
The best-fit model with nebular abundances has a large reduced
,
2.5, with excessive positive residuals at
0.4 keV and
0.9 keV and negative residuals at
0.6 keV.
These energies are coincident with the N VI, Ne IX, and
O VII lines, respectively; thus the residuals suggest that
the N/O and Ne/O abundance ratios are higher than those of the
adopted nebular values. We have therefore made spectral fits that allowed the abundances of N
and Ne to vary, and subsequently the reduced
is improved to
1.5.
The best-fit model, overplotted on the EPIC/pn spectrum in Fig. 2, has
a plasma temperature of
T = (2.0+0.1-0.3)
106 K (or
kT = 0.175
+0.01-0.03 keV), an absorption column density
1020 cm-2, and a volume
emission measure of (1.2
0.3)
10
cm-3, where d is the distance in parsecs and has been reported
to be 1150 pc (Perryman et al. 1997). The quality of the spectral fits is illustrated by the plot of
the reduced
of the fits as a function of kT and
shown in the inset of Fig. 2. Adopting a typical gas-to-dust ratio (Bohlin et al. 1978), the best-fit
absorption column density corresponds to a logarithmic extinction at
the H
line of
=
0.2+0.3-0.1, in
agreement with that determined from the Balmer decrement (Barker 1991).
The N and Ne abundances are enhanced with respect to the nebular
abundances by 3.5
1.2 and 3.0
1.0, respectively, thus
resulting in N/O
1.4 and Ne/O
0.7.
The residuals of the best-fit model may also indicate enhanced Na and
Si abundances, but the number of counts is too small to warrant
spectral fits allowing these abundances to vary.
The observed (absorbed) X-ray flux in the 0.2-2.5 keV energy range
is
10-14 erg cm-2 s-1,
and the intrinsic (unabsorbed) X-ray flux is
10-13 erg cm-2 s-1.
The X-ray luminosity in the same energy range is
erg s-1.
The sharp rim of the Eskimo's inner shell suggests compression by
supersonic shocks.
Indeed, the inner shell of the Eskimo, expanding at
90 km s-1 into the much slower outer shell, has an expansion
velocity notably high among PNe (O'Dell & Ball 1985).
To assess whether the hot gas in the central cavity is responsible
for driving such a fast expansion, we derive the thermal pressure
of the X-ray-emitting gas and compare it to those of the surrounding
nebular shells.
Assuming a prolate ellipsoidal central cavity, the volume occupied
by the X-ray-emitting gas is
1.1
cm3, where
is the filling factor and
may be
0.5. From this volume and the aforementioned volume emission measure,
we derive an rms electron density of
35
cm-3.
This rms electron density and the plasma temperature of 2.0
106 K
imply that the thermal pressure of the X-ray-emitting gas,
,
is
2
dynes cm-2.
The inner and outer shells of the Eskimo have densities of 2500 and 900 cm-3, respectively, and a temperature of 14 500 K (Barker 1991). The thermal pressure of the inner and outer shells are
1
10-8 and
3
10-9 dynes cm-2, respectively.
The X-ray-emitting gas has slightly higher thermal pressure than the inner shell, and much higher than the outer shell, thus the thermal pressure of the hot gas in the Eskimo's central
cavity drives the expansion of its inner shell into the outer shell.
The temperature of the X-ray-emitting gas in the Eskimo,
2.0
106 K, is similar to that found in other elliptical PNe;
however, the terminal velocity of the Eskimo's fast wind is low,
only
400 km s-1 (Pauldrach et al. 2003).
For an adiabatic shock, the expected temperature of the shocked wind
would be
1.9
106 K for such a velocity, barely
reaching the temperature indicated by the X-ray spectrum, in sharp
contrast to other PNe whose shocked stellar winds are 10-100 times
hotter than the hot gas detected (e.g., Chu et al. 2001; Kastner et al. 2000).
If the hot gas in the Eskimo indeed originates from the shocked
fast stellar wind, the low expected post-shock temperature implies
that no significant mixing of nebular material has taken place.
The mass of the hot gas,
3
,
can be supplied by the fast stellar wind in
1800 yr at a
constant mass loss rate of 1.8
10
yr-1(Pauldrach et al. 2003).
If the X-ray emission from the Eskimo does not originate
from a shocked fast stellar wind, then there are two other possibilities.
First, the X-ray emission can be partially attributed to the central
star as in the case of NGC 6543 or to a late-type binary companion
as in the case of NGC 7293 (Guerrero et al. 2001).
The angular resolution of XMM-Newton, however, is insufficient
to resolve a point source from the diffuse emission from the Eskimo.
Second, the diffuse X-ray emission can be produced by the dynamical
interaction of the fast bipolar outflow with the inner shell.
This collision will produce shock-excited gas along the direction
of the outflow which is detected as the harder X-ray emission in
the 0.65-2.0 keV band, and also as shock-excited [Fe II] 1.26 and 1.64
m line emissions (Hora et al. 1999; Hollenbach & McKee 1989).
Similar situation is observed in BD+30
3639, whose diffuse
X-ray emission shows an asymmetric spatial distribution in hard
energies and reveals spectral evidence of enhanced Ne/O abundance
ratio (Kastner et al. 2002).
As suggested for BD+30
3639 (Soker & Kastner 2003), the hottest gas
in the Eskimo may have been produced by a fast,
500 km s-1,
collimated post-AGB wind that is no longer present.
Alternatively, the observed 200 km s-1 outflow may have a
large inclination with respect to the line-of-sight, so that its
real expansion velocity is large enough to power the hottest gas
in the Eskimo.
Our XMM-Newton observations of the Eskimo Nebula have detected diffuse X-ray emission from hot gas within its central cavity. The high thermal pressure of this hot gas is responsible for the high expansion velocity of its innermost shell. The origin of this hot gas, however, is uncertain, and may consist of several components: shocked fast stellar wind, shocks associated with the fast bipolar outflow, and emission from its central star or a binary companion. X-ray observations at the highest spatial resolution afforded by Chandra are needed to determine accurately the origin of X-ray emission from the Eskimo Nebula, a very interesting and complex PN.
Acknowledgements
M.A.G. is grateful to the VILSPA staff for his help and hospitality during the 4th SAS Workshop held in VILSPA on June 8-12, 2004. M.A.G. also acknowledges support from the grant AYA 2002-00376 of the Spanish MCyT (cofunded by FEDER funds). Y.-H.C. acknowledges support from the NASA grant NNG04GE63G.