A&A 367, 617-628 (2001)
DOI: 10.1051/0004-6361:20000459
C. Gry1,2 - E. B. Jenkins3
1 - ISO Data Center, ESA Astrophysics
Division, PO Box 50727, 28080 Madrid, Spain
2 -
Laboratoire d'Astronomie Spatiale,
BP 8,
13376 Marseille Cedex 12,
France
3 -
Princeton University Observatory,
Princeton, NJ 08544-1001, USA
Received 20 September 2000 / Accepted 5 December 2000
Abstract
The composition and physical properties of several local clouds, including the
Local Interstellar Cloud (LIC)
in which the Sun is embedded, are derived from absorption features
in the UV spectrum of the star CMa.
We derive temperatures and densities
for three components by combining our interpretations of
the ionization balance of magnesium and
the relative population of C II in an excited fine-structure level.
We find that for the LIC
=
cm-3 and
K.
We derive the ionization fractions of hydrogen and discuss
the ionizing processes. In particular the hydrogen and helium
ionizations in the LIC
are compatible with photoionization by the local EUV radiation fields
from the hot stars and the cloud interface with the hot gas.
We confirm the detection of high ionization species:
Si III is detected in all clouds and C IV in two of them, including the LIC,
suggesting the presence of
ionized interfaces around the local clouds.
Key words: ISM: solar neighbourhood - ISM: clouds -
ISM: ionization - ISM: structure - stars:
CMa -
ultraviolet: ISM
The star CMa (B2 II, V=1.50,
kms-1,
,
b=-11.3)
(Hoffleit & Jaschek 1982) at a distance
of 130 pc (Perryman et al. 1997) is by far the brightest extreme ultraviolet
source in the sky
(Vallerga et al. 1993) and thus the main photoionization source
in the Solar Neighborhood (Vallerga & Welsh 1995; Vallerga 1998).
This is principally due to the
extraordinary emptiness of the line of sight to
CMa, as we describe below.
A beneficial aspect of the emptiness and hence the simplicity
of the sight line is the opportunity for us to study with an
unusual level of detail individual diffuse clouds in the local
interstellar medium. This is the subject of this paper.
In particular, the star CMa provides an opportunity to observe the absorption
spectrum of the Local Interstellar Cloud (LIC)
surrounding our solar system. In most cases we obtained
a good signal-to-noise ratio for the absorption features, thereby
allowing us to derive
the chemical and physical properties within the clouds,
including depletion, temperature,
electron density and ionization.
The temperature of the LIC is usually derived from the width
of absorption lines by profile fitting. Different measurements applied to
various elements all point to a temperature of around 7000 K, but with a
relatively large error. The most precise measurements are
provided by
the observation of the HI L
line, because the low mass of
hydrogen offers the best discrimination between thermal and turbulent
line broadening when compared to the results from heavier elements. Using
this method, Linsky et al. (1995) found
K in the directions
toward Capella and Procyon.
The electron density in the LIC has been determined in the
lines of sight towards Sirius (Lallement et al. 1994) and CMa
(Gry et al. 1995) using the ratio N(Mg II)/N(Mg I), towards
Cas
with the ratio N(Na I)/N(Ca II) (Lallement & Ferlet 1997), and
with the ratio N(C II*)/N(C II) towards Capella (Wood & Linsky 1997)
and the white dwarf RE J1032+532 (Holberg et al. 1999).
All methods give results that are around 0.1 cm-3, which is roughly the same
order of magnitude as the neutral gas density.
There are strong indications that the LIC and
similar clouds in the Local Interstellar Medium (LISM)
are partly ionized.
The observed fractional ionization of hydrogen can be explained
by the EUV radiation from white dwarf and other stars, in particular
CMa and
CMa (Vallerga 1998).
Previous studies of the nearby line of sight toward
CMa with
the Goddard High Resolution Spectrograph (GHRS) on the Hubble Space
Telescope (Dupin & Gry 1998) and an independent facility, the Interstellar
Medium Absorption Profile Spectrograph (IMAPS) (Jenkins et al. 2000)
have shown that the two main clouds
in that sight-line present a very high ionization fraction of hydrogen,
which could be explained by photoionization due to
the combination of
CMa and
CMa if the clouds are located close
enough to the stars.
An outstanding problem is that these and other stars do not
produce enough photons with
energies above 24.6eV to explain the high fractional ionization of helium
in the LISM, as shown by the low value of n(He I)/n(H I) (equal
to 0.07 instead of the cosmic ratio of 0.1, which indicates that
helium is more ionized than hydrogen).
The two main proposals to explain this phenomenon are i)
the LISM is still recombining from
a much more
highly ionized state produced by a supernova-related energetic event
in the recent past (Reynolds 1986; Frisch & Slavin 1996; Lyu & Bruhweiler
1996) and ii) the ionization of He is maintained by the diffuse
EUV radiation emitted by conductive interfaces between the cloud edges
and the hot gas filling the "Local Bubble'' in which they are embedded
(Slavin 1989; Slavin & Frisch 1998).
In this paper we present GHRS spectra of
CMa over limited wavelength intervals between 1190 Å and 1550 Å, ones that
include the lines of N I, O I,
C II and C II*, S II, Si II, Si III, and C IV at a wavelength resolution
.
We consider also a profile
of O I at 1039 Å, recorded by
IMAPS at
.
We
show how they shed light on the knowledge of characteristics of
the nearby diffuse clouds such as temperatures, electron densities,
abundances, and degree of ionization.
Most of the observations presented here have been performed in late 1996 with
the Ech-A grating of GHRS.
All data were taken with the 0
25 Small Science Aperture
(SSA), the procedure FP-SPLIT = 4 and a substepping of 4 samples per diode
(for details of the instrumentation, see Soderblom et al. 1995).
For data processing, we used the standard STSDAS procedures working in the
IRAF environment. We assigned wavelengths from the standard
calibration tables. An error of
1 resolution element on the wavelength
assignment is expected to arise from magnetic drifts.
The signal-to-noise ratio (S/N) for all Ech A data is about 200 when the flux is at the level of the stellar continuum. However there is a degradation of signal quality for features that appear in the bottoms of strong stellar lines. For most interstellar lines the S/N ranges between 100 and 200, but it is 80 for C II and C II* and 30 in the extreme case of Si III where the stellar line is the deepest.
Observations in the far-UV lines were carried out
by IMAPS when it was operated on the
ORFEUS-SPAS II mission that flew in
late 1996 (Hurwitz et al. 1998). IMAPS is an objective-grating echelle
spectrograph that was designed to record the spectra of bright,
early-type stars over the wavelengths from 950 Å to
1150 Å with a high spectral resolution. For more details on the
instrument see Jenkins et al. (1996).
The IMAPS spectra were extracted from the echelle spectral images using
special procedures developed by one of us (EBJ) and his collaborators on
the IMAPS investigation team. The S/N obtained
for the interstellar lines observed by IMAPS
is of the order of 25 to 30.
In both sets of spectra, there is an uncertainty related to the
background correction for scattered light on the echelle format.
For the GHRS Ech-A data, the error in the background correction
is smaller than a few percent of the continuum and is only a concern for
strong lines that almost reach the zero intensity level in their deepest points.
In the case of a species for which several lines with different
oscillator strengths are available, such as Si II, the uncertainty
is eliminated by comparing the different profiles, which must have relative
strengths that follow their oscillator strengths.
For very strong lines like H I Ly
and C II 1334 Å,
the zero level is determined by the base of the saturated line.
The situation for the O I 1302 Å line is reported in
Sect. 3.1.
![]() |
Figure 1: Example of the continuum normalization for the Si II line at 1260.4 Å. The stellar line is fitted by a polynomial (shown here superimposed on the spectrum) over the velocity interval [-30 kms-1, 40 kms-1] |
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Stellar lines were
fitted with one low-order polynomial over a velocity range covering the
interstellar components (Sect. 3), by considering the points
bluewards of Component 4 up to V=-30 kms-1 or -40 kms-1,
redwards of Component 1 up to V=+40 kms-1, as well as the velocity range
which is not affected by any interstellar absorption between
Components 2 and 3. The spectra are then
normalized to these stellar lines to create the interstellar profiles
with a level continuum. An example of the stellar line
fitting is illustrated in Fig. 1 for the
Si II 1260 Å line.
For strong or moderately strong lines the uncertainty added to the
column density estimates by this normalization process is small.
However, for very faint lines (Mg I, C II*, S II), it is a major
source of error. This uncertainty was taken into account when we listed
the column density results in Table 2. The most difficult
case is that for S II, where
all three interstellar lines are very faint and
appear on top of a steep slope of a stellar line. In this
configuration there is a lot of
freedom for the location of the synthetic stellar lines which
can artificially enhance the
interstellar line or, alternatively, make it disappear almost completely.
We thus use several options for the S II absorption profiles defined
by an envelope of
around the fitted continuum.
We derive the column densities by using the line fitting software "Owens''
developed by Martin Lemoine. Each interstellar absorption component is
represented by the convolution
of a theoretical Voigt profile with the instrumental profile. The instrumental
profile for the GHRS Echelle data was assumed to be a Gaussian
with a FWHM of 0.92 diodes
(Soderblom et al. 1995).
An iterative
procedure which minimizes the sum of the squared differences between
model profiles and
the data points allows us to determine the most likely column densities of the
absorbing elements N(cm-2), the radial velocity of the cloud (kms-1)
and the velocity dispersion (b-value) (kms-1) of each interstellar absorption
component. The
software also allows us to fit the lines from several elements simultaneously,
which leads directly to a coherent solution for all species in
terms of velocity, temperature and turbulent velocity.
The wavelengths and f-values are listed
in Table 1.
Element | wavelength (Å) | f-value | |
IMAPS | O I | 1039.230 |
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Ech A | S III | 1190.203 |
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Si II | 1190.416 |
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|
Si II | 1193.290 |
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|
N I | 1199.550 |
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|
N I | 1200.223 |
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|
N I | 1200.710 |
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|
Si III | 1206.500 |
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|
D I | 1215.339 |
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|
H I | 1215.670 |
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|
S II | 1250.584 |
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|
S II | 1253.811 |
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|
S II | 1259.519 |
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|
Si II | 1260.422 |
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|
O I | 1302.168 |
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|
Si II | 1304.370 |
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|
C II | 1334.532 |
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|
C II* | 1335.708 |
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|
Si IV | 1393.755 |
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|
Si IV | 1402.770 |
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|
C IV | 1548.195 |
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|
C IV | 1550.770 |
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|
Ech B | Mg II | 2803.503 |
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Mg II | 2796.352 |
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|
Mg I | 2852.964 |
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|
Fe II | 2344.214 |
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|
Fe II | 2382.765 |
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|
Fe II | 2586.650 |
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1 Wavelengths and f-values are from a private communication by Morton,
updating data from Morton (1991).
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Figure 2:
Ech-B (first six plots) and new Ech-A spectra of ![]() ![]() |
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Comp. | 1 | 2 | 3 | 4 | 5 |
V | 17 kms-1 | 10 kms-1 | -10 kms-1 | -19 kms-1 | -65 kms-1 |
Fe II |
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- | - |
Mg II |
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- |
Mg I |
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- | - |
Si II |
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- |
Si III |
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C II a |
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C II* |
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- | - |
O I |
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- | - |
N I |
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- | - |
S II |
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- | - |
C IV |
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- |
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- | - |
S III |
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- | - |
Si IV |
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- | - |
N V |
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- | - |
a The upper limits for Components 1 and 2 are determined from N(S II) as explained in Sect. 3.2. |
The three principal components had heliocentric velocities of 17, 10 and -10 kms-1. In the previous papers, they were identified as Components 1, 2 and 3, respectively. Two of the components have been identified by Gry et al. (1995) as the two clouds detected in the line of sight to Sirius by Lallement et al. (1994) and described further by Hébrard et al. (#H&). As Sirius is located at a distance of only 2.7 pc, these two components must be situated very close to the Sun.
Component 1 is recognized as the Local Interstellar Cloud (LIC) in which the Sun is embedded, for which the motion has been characterized by Lallement & Bertin (1992). Component 2, called the "Blue Cloud,'' is also in front of Sirius but is distinct from the LIC. Another component (Component 4) was detected on the blue side of Component 3 in the strongest lines at -19 kms-1, while a fifth component was detected only in the line of Si III at -65 kms-1, and confirmed in H I because it mimics a very strong D I absorption (too strong to be due to D I with a reasonable D/H ratio), for its H I absorption turns out to coincide with the expected D I feature from Component 1 (see Sect. 3.3). Finally, a "Component 0'' had been introduced in the red wing of Component 1 to improve the fit of some of the profiles, but our reanalysis with more complete data indicates that this component may not be real. Its introduction in the previous Ech B data analysis was probably a consequence of using a slightly distorted line spread function. We have chosen to omit the component in our more refined analysis.
We have performed the line fitting for Components 1 to 4 over
all elements available in the Echelle A
and Echelle B data, as well as for the O I
line recorded by IMAPS.
All lines of O I, N I, Mg I, Mg II, Fe II,
Si II, Si III, C II, C II**, and S II were fitted simultaneously
with a unique line-of-sight
velocity structure and a unique column density that was consistent
with different lines of the same species. As the absolute wavelength
calibration
had a precision of one resolution element (about 3 kms-1),
an individual velocity shift is allowed for each data set, whereas the
relative velocity of the components had to be the same for all lines.
The resulting velocity shifts for all elements have a dispersion of
kms-1, in agreement with the precision of the wavelength calibration.
The derived velocity for Component 1 is
kms-1, in agreement
with its identification as the Local Interstellar Cloud.
The velocity shifts of the other components relative to Component 1
are known with more precision:
kms-1 for Component 2,
kms-1 for Component 3, and
kms-1 for Component 4.
The comparison of the synthetic profiles with the data
suggested that the velocity shift between Component 3 and Component 1
could be slightly different for Si III from what we found for
the other elements. We thus decided to decouple the Si III velocity
from the determinations for other species,
and we found that indeed the velocity shift
between Component 3 and Component 1 for Si III is -28.48 kms-1, i.e.,
1 kms-1 more than for the other elements. This velocity
shift however is only one-third of a resolution element and must be compared to
the velocity dispersion of material in the clouds which is more than
a factor of three higher.
Comp. | 1 | 2 | 3 | 4 |
C II | ![]() |
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Fe II |
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When we derived b-values that had the best fit to the data, we imposed the requirement that various elements should have common values for the turbulent and thermal doppler contributions within each velocity component. Differences in the outcomes for b across different elements were therefore governed only by variations in atomic mass. Table 3 shows the b-values for two elements that represent the two extremes in mass: carbon and iron.
The derived column densities for Components 1 to 4
are listed in Table 2, and the fits of the
lines are presented in Fig. 2.
Specific considerations for a few elements are
discussed individually below.
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Figure 3:
IMAPS spectra of ![]() ![]() |
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Guidance on the correct zero level of the O I line at 1302 Å was available from the observed zero level of the nearby C II line at 1334 Å which is known to be heavily saturated. The presence of clearly visible component structures at the bottom of the line indicates that the profile remains above zero or, at most, it hits zero over a range of just a few points, in accord with the expected noise level. However an uncertainty on the exact zero level location still remains, and this is manifested as an uncertainty in the column densities for Components 1 and 2. It is thus useful to check the results using the weaker line of O I at 1039 Å, which is available in the IMAPS data.
The interstellar O I feature observed with IMAPS is unfortunately contaminated by
telluric O I absorption,
as revealed by the presence of a strong, narrow O I** absorption line
at 1041 Å.
However we can estimate the expected telluric contribution for O I. In the
Earth's upper atmosphere, the fine-structure levels
should be populated in accord with their statistical weights.
With this in mind, we performed a
fit of the far-UV O I and O I** lines together with the other species
(leaving out the O I 1302 Å line), but with the addition of a
telluric component satisfying the constraint that
(O I**).
The resulting fits are illustrated in Fig. 3.
They give results for the O I column densities of Components 1 and 2
that agree with the range of values derived from the O I 1302 Å line
alone, giving an assurance that the
background assignment for that line was not erroneous.
Table 2 lists the O I
column densities which are consistent with both O I lines.
There are substantial uncertainties with
the C II column density determinations for
Components 1 and 2 because the line is so strong.
Over the velocity range covered by Component 1, the profile shows nearly zero
intensity - a situation that is consistent with arbitrarily high column
densities. Therefore, while some lower limit for N(C II) could be gathered
from the profile fitting, we derived
upper limits from the upper limits for N(S II) multiplied by the
cosmic abundance ratio,
(Anders & Grevesse
1989). In effect, S II and C II are both the dominant
ionization states in diffuse neutral gas, and even if these two elements are in a
partially ionized medium, they should have
about the same fraction
of atoms elevated to higher stages of ionization
(Jenkins et al. 2000). While this may be true, we also know that
carbon is usually more depleted
than sulfur in the ISM, implying that N(C II)/N(S II) is probably
lower than the cosmic abundance ratio. The upper limits for N(C II) listed in
Table 2 for Components 1 and 2 reflect these considerations.
For Component 3, the line is not
as saturated, and we derived both the lower and the upper limits
from the line fitting, and we note that the upper limit we measure
is very close to the value we would estimate from S II.
![]() |
Figure 4:
The four interstellar components of H I and D I fitted on the
stellar Lyman ![]() ![]() |
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In principle, the low column density of neutral matter present in the line of
sight toward CMa is favorable for studying D/H because
the bottom of the H I line is not wide enough to bury the deuterium
line.
Indeed, as seen in Fig. 4, the D I feature is clearly seen
in the wing of the H I profile.
Unfortunately, as already noted by Gry et al. (1995) with the G160M data,
it is very difficult to derive H I and D I column densities
from the Lyman
line because
i) the H I stellar line is narrow compared to the interstellar profile
and is thus very difficult to define with any accuracy;
ii) the D I feature
is probably blended with an H I absorption from the small component at
-65 kms-1.
Although this component is very weak and probably mostly ionized, for
it is detected only in Si III and C II, a neutral hydrogen
column density of only 1013 cm-2 could dominate over a deuterium
feature if
;
iii) since the mass of deuterium is low, its b-value is
high and the absorption features from the different components
are not resolved very well, unlike the cases for the other elements. This makes it
impossible to distinguish the contribution of each component to the
D I profile, which might otherwise allow us to separate a blend of three or four
D I components from the one H I high
velocity component.
We plot in Fig. 4 some representative fits to the
Lyman
profile simply to illustrate
the complexity arising from the overlapping
individual absorbers. In this example
the Lyman
profile has been fitted using information from the
other elements, without any additional constraints. This solution
is not acceptable because it implies an H I column
density for
Component 2 which is incompatible with the limit set by O I or S II.
We have checked nevertheless that the H I column densities derived from
O I in Sect. 4.1 produce a synthetic Lyman
profile
which is compatible with the observed profile.
Some absorption features can
be seen on the EchA spectra at the bottom of the two C IV stellar lines
(Fig. 5). They were already apparent at lower resolution
in the G160M data (Gry et al. 1995).
If we fit a stellar
continuum outside the range where the contributions from Components 1 and 3 are
expected, the normalized
spectra show two components with a velocity separation which is compatible
with the separation between Components 1 and 3 with
column densities of
and
cm-2,
respectively.
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Figure 5:
The C IV profiles of ![]() |
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There is a shift of about -5 kms-1 in the absolute velocity of the components, compared to the velocities of these components measured for the other species. This shift is a bit too high to be attributed to an uncertainty in the wavelength calibration, which should be less than 3 kms-1 (this has been verified with the other elements). However, velocity discrepancies between highly ionized species and lower ionization stages are not unusual; see, e.g., Sembach et al. (1994).
We have also performed an evaluation of the C IV lines with a fit to the stellar and interstellar lines simultaneously over a velocity interval that includes the region covered by Components 1 to 3 and without specifying the velocity of the interstellar components. This approach eliminates the possible bias that could arise from the a priori choice of the location of the interstellar features when defining the stellar continuum. The result of the fit was virtually the same as that found with our standard way of deriving a normalized spectrum. Once again, a velocity separation equivalent to that between Components 1 and 3 was found. This separate exercise reinforces our proposal that the C IV lines are real and not simply a consequence of our incorporating information from other elements in lower stages of ionization.
Absorption features from the O VI doublet have been looked for in the IMAPS spectrum but they are not visible. None of the other high ionization species Si IV, S III and N V have been detected in the GHRS spectrum.
The ionization fractions of oxygen and nitrogen are coupled to that
of hydrogen via resonant charge exchange reactions. In particular,
the rate coefficient for charge exchange of O II with H I is exceptionally
strong, 10
(Field & Steigman 1971),
and O I is therefore a very good tracer of H I. We can thus derive
the column densities of neutral hydrogen in the components from their respective
O I column
densities through the relation
(H I) = N(O I)/(O/H)
,
where (O/H)
is
the abundance of oxygen relative to hydrogen in the interstellar medium.
If we adopt the value derived by Meyer et al. (1998),
(O/H)
,
we find that
(H I) =
4.4+1.6-0.6 1017 cm-2 for Component 1,
(H I) =
0.9 1017 cm-2 for Component 2 and
(H I) =
0.6 1015 cm-2 for Component 3.
With these numbers, we arrive at a total H I column density in the
range 7 1017 to 1.1 1018 cm-2, which is
compatible with that derived from the absorption of the extreme
ultraviolet
flux from the star based on EUVE spectra (Vallerga et al. 1993;
Cassinelli et al. 1995).
If we adopt a different tactic by assuming that the diffuse clouds in the local
ISM are
undepleted and the oxygen abundance is equal to the
abundance in B stars, (O/H)
,
then the H I column density is lower, ranging from 4.8 1017 to 7.2 1017 cm-2 for the whole line of sight, with
(H I)
=3.0+1.1-0.4 1017 cm-2 for Component 1,
(H I)
cm-2 for Component 2 and
(H I)
cm-2 for Component 3.
We can also derive the H I column
densities implied by the N I column densities. If we again use
the abundance of nitrogen in the interstellar medium derived by Meyer et al.
(1997), (N/H)
,
we find
(H I)
cm-2 for Component 1,
(H I)
cm-2 for Component 2, and
(H I)
cm-2 for Component 3.
We note that in all three components, the neutral column density derived
from N I is significantly lower than that derived from O I.
This N I deficiency in the local ISM has already been noticed by
Jenkins et al. (2000) from far-UV spectra
of white dwarf stars observed with FUSE. They have shown that
the N I deficiency, as that of
Ar I, favors the existence of a source of ionizing
photons with eV in the local ISM to explain the He I ionization.
For the subsequent discussions, we will adopt for N(H I) the ranges
derived from N(O I), keeping both options for the oxygen depletion.
S II is traditionally used as an indicator of the total
(i.e. neutral plus ionized) gas column density in the interstellar medium because
i) sulphur has little or no depletion onto dust grains (see, e.g.,
Savage & Sembach 1996; Fitzpatrick & Spitzer 1997) and ii) the
ionization potential of S II (23 eV) is high and therefore S II is often
assumed to be the dominant ionization stage both in HI and HII regions.
If we trust that assumptions i) and ii) are valid, we can derive the
total column densities
for Components 1, 2 and 3 from the expression:
,
where (S/H)
is the cosmic abundance ratio taken from Anders & Grevesse (1989):
(S/H)
.
In this context, we obtain
cm-2 for Component 1,
cm-2 for Component 2, and
cm-2 for Component 3.
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Figure 6: Curves of the electron density n(e) versus temperature T governed by Eqs. (2) and (3), for the permitted values of the ratios n(C II*)/n(C II) and N(Mg II)/N(Mg I). For each of the three components the shaded area where the two sets of curves intersect determines the possible values for n(e) and T |
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We follow the method of Jenkins et al. (2000) to derive
both the temperature and the electron density in a component by combining
the information from two ratios which depend
in different manners on these two physical parameters.
The relative populations of the fine-structure levels of C II are
governed by the balance between collisions and radiative de-excitation. In the
diffuse warm medium, the collisions are dominated by electrons. The
condition for equilibrium
To see the conditions from a different perspective, we make use of the equation
for the equilibrium between the two lowest
ionization levels of magnesium which is given by
We derive
5700<T<8200 K with
cm-3 for the LIC
(Component 1),
K with
cm-3 for Component 2, and
6000<T<8400 K with
cm-3 for Component 3.
Comp. | 1 (LIC) | 2 | 3 |
T (K) | 5700-8200 | 8200-30000 | 6000-8400 |
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0.08-0.17 | 0.016-0.088 | 0.18-0.28 |
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<0.55 | <0.43 | 0.955-0.985 |
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>0.14 | >0.034 | 0.18-0.29 |
p/k (cm-3K) | >1300 | >440 | 2300-5000 |
length (pc) | <1.3 | <3.3 | 0.17-0.45 |
Note that our results confirm the temperature of K commonly
found for the LIC in most studies, and our electron density of
cm-3 confirms the ranges found
independently in the LIC in other sight-lines by Wood & Linsky (1997)
and Holberg et al. (1999).
From our results, the LIC and Component 3 have similar temperatures
while Component 2 could be warmer.
From the comparison of the total and the neutral hydrogen column densities
derived from N(S II) and N(O I) respectively (see Sect. 4),
we estimate the
ionization fractions /
,
listed in Table 4.
Component 3 is ionized
by more than 95%, making its ionization comparable to that of the
two main
components (C and D) in the line of sight to CMa (Jenkins et al. 2000). As for Components C and D, the main ionizing source for
Component 3 is
probably the star
CMa and its high hydrogen ionization
fraction requires that it is located closer to the star, further away
from the Sun.
Component 1 (the LIC) can be at most 55% ionized, its maximum ionization fraction corresponding to the case of no oxygen depletion in the local cloud. However, formally the column density ranges allow the LIC to be neutral.
Since for Component 2 the neutral gas and total gas column density ranges
are nearly coincident, Component 2 is most probably neutral although
formally its ionization fraction can be as high as 43% in the case
of no oxygen depletion.
![]() |
Figure 7: Predicted densities versus H I attenuation column density in a local cloud exposed to the local photoionization field (due to hot stars and hot-gas conductive interface) |
Open with DEXTER |
In order to compare these numbers to the expected ionization fractions,
we have calculated the photoinionization equilibria in the local
ISM for varying depths of shielding by neutral H and He following the equations
described by Sofia & Jenkins (1998). We consider the effect of Vallerga's
(1998) composite stellar radiation field supplemented by Slavin's (1989)
calculated flux from the cloud conductive interface. The results are shown
in Fig. 7.
The calculation is the
same as that used to produce Fig. 2 of Jenkins et al. (2000) except
for a higher pressure p/k, in better agreement with the electron density
derived
in Sect. 5 for the LIC as well as with the neutral density
derived
from EUV stellar spectra and inside the heliosphere (Vallerga 1996;
Quémarais et al. #Qu&).
We derive the expected ionization fraction in the two local
clouds from
Fig. 7
and from the estimate of the mean attenuation of the ionizing flux received in
the clouds.
Since most of the
EUV radiation comes from the direction of CMa where
nearly all the neutral gas is included in one of these
two components, the attenuation is derived from their H I column densities
given in Sect. 4.1.
If we assume that Component 2 is located outside of the LIC, further out
toward CMa, it
should be shielded only by its own H I material,
with a mean H I attenuation of 1/2 N(H I), in all cases lower than
2.3 1017 cm-2. With this upper limit,
Fig. 7 predicts for Component 2 a minimum ionization
fraction of 0.44, which is inconsistent with the slightly lower maximum
ionization fraction permitted by
the observations. Note that the temperature of Component 2
derived in Sect. 5
is higher than that used in Fig. 7,
optimized to match the characteristics of the LIC.
As the ionization fraction increases with temperature because the
recombination rate is a decreasing function of T,
the predicted ionization fraction for Component 2 is even higher
than that which appears in
Fig. 7, amplifying further the discrepancy with the value
derived from the observations.
This inconsistency would be eliminated if
Component 2 were shielded by the LIC, which would imply that it
is located within the Local Cloud, a configuration already proposed
by Gry (1996) for some of the small components detected close to the Sun in
several lines of sight.
For the LIC, the mean attenuation due to the cloud itself ranges from 1.5 1017 to 2.2 1017 cm-2depending on the assumed oxygen depletion value. From Fig. 7, this implies an ionization fraction between 0.45 and 0.5. If we were to add the attenuation effect due to Component 2 (which is maximum if Component 2 is external and shielding the LIC as a whole), the range of possible absorbing column is extended up to 4 or 6 1017 cm-2 and we would get an ionization fraction down to 0.34 or 0.24. These values are all compatible with the range derived for the LIC from the measured column densities.
Figure 7 also predicts that the ratio n(He I)/n(H I) is almost constant over the range of H I column densities measured toward the white dwarf stars observed by EUVE (around 11018 cm-2) and is close to the measured ratio of 0.07 (Dupuis et al. 1995). We conclude from the adequate prediction of the hydrogen ionization fraction as well as of the n(He I)/n(H I) ratio that the photoionization by the EUV radiation field due to the combination of the hot stars and the cloud conductive interface is a likely representation of the ionization processes in the LIC.
From the comparison of the ionization
fractions and the electron density,
we infer the total hydrogen density
(or its lower limit) for
each of the three
components. These are listed in Table 4.
In fact the numbers are compatible
with all three components having a similar total density close to
0.2-0.3 cm-3 but different
electron densities depending on their
ionization state.
The thermal pressures in the components are also listed in
Table 4.
To estimate the thermal pressure in the clouds from p/k=nT we sum up over
all particles: hydrogen (
), helium (0.1
)
and electrons (
).
For the LIC, if we adopt the
range of Vallerga (1996),
i.e. 0.15 to 0.34 cm-3, with our ranges for
and T,
we derive p/k=1900 to 6000 cm-3K, in
agreement with the thermal pressure found in Component 3, as is expected if
they are in equilibrium with a
surrounding medium that is common to both of them.
The thicknesses of the components
along the line of sight are estimated from the ratio of the total
column density
N(H
)
derived in Sect. 4.2 to the total density
.
The lengths of
the components (listed in Table 4) are all very small
compared to the length of the
line of sight: they occupy a total of less than 5 pc. This
implies that at least 96% of the sight-line is empty or filled with
more highly ionized gas.
Substantial amounts of Si III are detected in all components.
We find that
in Component 1 and more than
in Component 3. While
is only about 10% the
value of
in Component 2, it is 7.5 times
in Component 4.
In principle Si III cannot come from the same region as the other species because charge exchange with even small amounts of neutral hydrogen tends to shift the Si to lower stages of ionization (Jenkins et al. 2000). Nevertheless, it seems clear that Si III arises at velocities that coincide with all components, including even the less ionized Component 2. This makes it is very likely that Si III is located in regions associated with the clouds, perhaps in their outermost layers.
It is interesting
to note that Si III is not detected
in the spectrum of CMa (Hébrard et al. 1999) up to a limit of
2 1011 cm-2.
This limit corresponds to our detection for Component 2, but it is more than
10 times lower than the column density we derive for the LIC.
This discrepancy could be interpreted as Si III coming from a completely unrelated cloud, which coincidently has about
the same velocity as the LIC, as proposed by Hébrard et al. (1999).
A difficulty with the above proposal is that this
component probably would contaminate other lines,
and thus it should influence the column density determinations for
other elements. This hypothetical extra component would be likely to have
elemental abundance ratios different from the LIC - due in particular to
different ionization fractions - and thus create large perturbations in the
column density ratios.
Yet, if we compare the results
for the four species for which we have reliable results for both
CMa and
CMa sight-lines (i.e. derived from unsaturated lines):
N I, Si II, Fe II and Mg II, the
column density ratios between
CMa and
CMa are very similar
for all elements: N(
CMa)/N(
CMa
cm-2.
As an example of the kind of differences one can expect
between two different components, the column density ratios between
Component 1 and Component 3 for the three
ionized species Si II, Fe II and Mg II present a dispersion of 60%.
Even worse, the N I column density ratio between
Component 1 and Component 3 is more than a factor of 10
higher than the ratios for the other elements.
Thus, in view of the small dispersion in the column density ratios between
the LIC
in the CMa sight-line and the LIC in the
CMa sight-line
in the various elements, we strongly support the idea that there is only
one absorbing component at the LIC velocity in the
CMa sight-line, and
thus that the Si III absorption is related to the LIC component.
The fact that N(Si III) is at least a factor of 10 lower in the Sirius
sight-line than in the CMa sight-line suggests
that the region where the Si III originates is extended and that more than
90% of it lies beyond Sirius. The possible very small
velocity shift
between the Si III absorption and the absorption from less ionized species
could be explained by the presence of a slight positive velocity gradient
toward the outer layer of the cloud.
The detection of Si III in the LIC has an interesting
consequence for the relative location of the two local clouds.
Since by definition the LIC is the cloud in which the Sun is
embedded, the presence of an extended LIC Si III layer past Sirius
implies that the LIC and its extended layer occupy the full line of sight
toward Sirius. It follows that Component 2
(the "Blue Component'' in the CMa sight-line)
should be embedded in the LIC or at least in its extended Si III
layer, corroborating the suggestion made in Sect. 6.
There is a significant difference between the gas responsible for the Si III absorption and the gas responsible for the C IV absorption: while the widths of the Si III profiles are compatible with Si III being at the same temperature as the less ionized elements, the profiles for C IV are clearly broader, implying temperatures of the order of 100000 to 200000 K. This favours the existence of collisional ionization due to a high temperature. Indeed, our C IV column densities and our Si IV upper limits are compatible with the outcome from Slavin's (1989) model for the conduction layer between the Local Cloud and the hot gas that is supposed to fill the Local Bubble. He calculated that N(C IV) = 2.7 1012 cm-2 and N(Si IV) = 1 1011 cm-2 through an interface of this sort, assuming minimal inhibiting effects from magnetic fields. His prediction for N(Si III) of 5 1010 cm-2 is far below our observed column density.
We have analysed the interstellar absorption lines in the high spectral
resolution (
)
UV spectrum
of
CMa (130 pc).
We derive column densities for 11 different elements in the three main clouds
and for a few elements with the strongest lines in two additional
very weak components.
Two of the main components (Components 1 and 2) are identified with the two
components detected in the much shorter line of sight
toward CMa (Sirius) which is not far from
CMa in the sky.
One of them (Component 1) is the Local Interstellar Cloud (LIC)
in which the Sun is embedded. For the four elements for which reliable
measurements exist for the two lines of sight (i.e. performed with unsaturated
lines) we find a constant ratio of 1.5 between the column densities of the LIC
toward
CMa and the column densities of the LIC toward
CMa.
We derive the neutral hydrogen column density from our measurement of O I
which is a good tracer of H I.
Depending on the oxygen abundance we adopt, we find a neutral gas
column density for the whole line of sight between
cm-2 if we consider that the local gas is not depleted (adopting the B stars
abundance)
and
cm-2 if we adopt the mean ISM oxygen abundance of
Meyer et al. (1998).
With the same two alternatives, we derive for the LIC a neutral gas
column density between 3.0
+1.1-0.4 1017 cm-2 and
4.4
+1.6-0.6 1017 cm-2.
We estimate the temperatures and electron densities in the three main
components by combining the information of the two ratios N(C II*)/N(C II)
and N(Mg II)/N(Mg I). In particular for the LIC we find
=
cm-3 and
K, both in agreement
with previous determinations having similar error bars.
We compare the neutral gas column densities with the total (neutral
and ionized) gas column densities derived from the S II measurements,
to conclude that Component 3 is ionized by more than 95%, that Component 2
is probably neutral but could be as much as 43% ionized and that the LIC
can be at most 55% ionized.
We conclude from
these numbers that Component 3 must be located further away on the line of
sight and is
thus almost fully ionized by CMa and that the ionization fraction in the
LIC is compatible with the gas
being ionized by the local EUV radiation
fields from the hot stars and the cloud interface with hot gas.
In contrast,
it is hard to explain the low state of ionization of Component 2 unless
it is included within the LIC which shields it from the ionizing radiation.
We detect high ionization species. Si III is detected in all clouds but more significantly in the LIC and Component 3, and is probably located in extended layers in the outer regions of the clouds. C IV is also detected in the LIC and Component 3, but with small velocity offsets from the lower ionization species. The derived amount of highly ionized gas and the derived high temperature are consistent with the predictions of Slavin (1989) for a conductive interface between the Local Cloud and the surrounding hot gas from the Local Bubble.
Acknowledgements
The GHRS data reduction and a preliminary spectral analysis have been performed in collaboration with Olivier Dupin as part of his Ph.D. Thesis, presented in April 1998. CG is very grateful to Martin Lemoine for his absorption line fitting software "Owens'' and his helpful advices. EBJ was supported by NASA grant NAG5-616 to Princeton University.