Table 3 lists the observed fluxes of the
lines.
The most intense
lines are the S(0) (
)
and S(1) (
)
lines, with typical
fluxes of 0.5-1 10-19 and 1-2 10-19 W cm-2, respectively.
Unfortunately, the S(2) line was only observed in the two clouds
already discussed in detail by Rodríguez-Fernández et al. (2000).
The S(3) line is very weak and it has only been detected
in the sources with more intense S(1) emission.
Even in some sources which show emission in the S(4) and S(5) lines,
the S(3) line has not been detected.
This is due to strong dust absorption produced by the solid state
band of the silicates at
m (Martín-Pintado et al. 1999a).
The pure rotational lines of
arise due to electric quadrupole transitions.
The quadrupole transition probabilities are small
(Turner et al. 1977)
and thus the rotational lines remain optically thin.
In this case, the column density of the upper level involved
in a transition from level i to level j can be obtained from the
line fluxes Fij of Table 3 using the following expression:
Figure 4 shows the population diagrams for one
of the sources for which more than four lines were detected:
M
-0.32-0.19.
We have used the extinction law derived by Lutz (1999)
towards the Galactic center using hydrogen recombination lines.
This extinction law differs from that of Draine (1989)
for silicate-graphite mixtures of grains
in that there is no deep minimum at m and there is
a slightly higher value for the
ratio,
where
the visual extinction (at 0.55
)
and
is the extinction at 9.7
.
For instance, in the case of M
-0.32-0.19 one sees that 15 mag
of visual extinction (squares in Fig. 4) is a lower limit
to the extinction
while 45 mag (stars in Fig. 4) is an upper limit.
The best result is obtained for a visual extinction of
around 30 mag (triangles).
Using this method for the other sources with more than four
lines detected, we
also derive a visual extinction of
30.
This value should be considered as a lower limit to the actual extinction
for the sources where the S(3) line was not detected.
It is not possible to know how much of this extinction is caused
by material in the line-of-sight towards the GC (foreground extinction)
and how much is intrinsic to the GC clouds.
Nevertheless, a visual extinction of
30 mag is
in agreement with the average foreground extinction
as measured by Catchpole et al. (1990) using
stars counts and suggests that the
emission can arise
from the clouds surfaces (see also Pak et al. 1996).
In the other sources where we cannot estimate the extinction
from our
data we have applied a correction of
mag.
For those clouds located farther from the center of the Galaxy
and/or the Galactic plane, we have corrected the observed fluxes
by 15 mag (see Table 4). This value was derived
by Rodríguez-Fernández et al. (2000) by
analyzing the far infrared dust emission toward two sources in
the "Clump 2" and the
complexes.
In any case, the extinction correction has a minor
impact in the main results of this paper (see below).
Figure 5 shows the extinction corrected population
diagrams for all the sources presented in this paper.
![]() |
Figure 5: Population diagrams for all the sources corrected for the extinctions listed in Table 4. The filled circles are connected when more than three lines are detected. Arrows indicate upper limits. The error-bars are smaller than the circles (even taking into account both calibration and Gaussian fitting errors) |
The values of extinction required to give a smooth population diagram
would be somewhat smaller if the
ortho-to-para (OTP) ratio
were lower than the local thermodynamic equilibrium (LTE) ratio.
This is obvious since the
method to derive the extinction depends mainly
on the extinction at the wavelength of an ortho level (J=5).
Non-equilibrium OTP ratios measured with the lowest rotational lines
has been found in two clouds of our sample
(Rodríguez-Fernández et al. 2000).
Unfortunately, for the clouds presented in this paper,
it is difficult to estimate the OTP ratio
since the S(2) line has not been observed
and the S(3) line is completely extincted in most of them.
Current data do not show any evidence for a non-equilibrium
OTP ratio, but we cannot rule it out a priori.
For instance, assuming OTP ratios of
2
we still can find a smooth
population diagrams, i.e. without
the typical zig-zag shape characteristic of non-equilibrium OTP ratios
(see e.g. Fuente et al. 1999).
In this case, the extinction would be of
20-25 mag instead of 30 mag.
On the contrary, assuming OTP ratios of
1
one finds, in general, rather artificial diagrams, which suggests that
OTP ratios as low as
1 are not compatible with the data.
Although one must bear in mind these considerations, in the following
we assume that the OTP ratios are LTE.
Table 4 lists the results derived from the
lines
after applying the extinction corrections.
Source | ![]() |
T32 | T76 |
![]() |
K | K | 1022 cm-2 | ||
M -0.96+0.13 | 15 | 157(6) | - | 1.10(9) |
M -0.55-0.05 | 30 | 135(5) | - | 2.7(3) |
M -0.50-0.03 | 30 | 135(4) | - | 2.3(2) |
M -0.42+0.01 | 30 | 167(6) | - | 1.03(8) |
M -0.32-0.19 | 30 | 188(5) | 650(90) | 1.03(5) |
M -0.15-0.07 | 30 | 136(6) | - | 2.6(4) |
M +0.16-0.10 | 30 | 157(7) | 900(200) | 1.17(13) |
M +0.21-0.12 | 30 | 186(13) | 670(110) | 0.64(7) |
M +0.24+0.02 | 30 | 163(2) | - | 1.73(6) |
M +0.35-0.06 | 30 | 195(11) | 700(200) | 0.66(5) |
M +0.48+0.03 | 30 | 174(7) | ![]() |
1.03(9) |
M +0.58-0.13 | 30 | 149(5) | - | 1.3(2) |
M +0.76-0.05 | 30 | 181(4) | - | 1.77(8) |
M +0.83-0.10 | 30 | 178(5) | 550(60) | 1.59(6) |
M +0.94-0.36 | 15 | 146(7) | - | 0.95(10) |
M +2.99-0.06 | 15 | 152(3) | - | 1.40(9) |
Obviously, T32 lacks of physical sense if the ortho-
and para-
abundances are not in equilibrium.
As mentioned, we can obtain smooth population diagrams
assuming OTP ratios lower than the LTE ratio.
The temperature T32 derived in
this case (
)
is higher than the one
derived directly from the observations (T32).
For instance, assuming OTP ratios
2 one obtains a
which is
10% larger than T32.
It is possible to estimate the total warm
column densities (
)
by extrapolating the populations in the J=2 level to the
J=1 and J=0 levels at the temperature T32.
The derived warm
are listed in Table 4 and should
be considered lower limits to the actual amount of warm molecular gas
since the lowest levels can be populated with colder,
although still warm, gas.
The total column density of warm
varies from source to source
but it is typically of 1-2 1022 cm-2.
These column densities are
only a factor of 1.2 higher than those one would obtain without any
extinction correction.
Thus, in regard to the derived gas temperatures and
total column densities, the extinction correction is not critical.
On the other hand, extrapolating the column densities in the
J=6 and J=7 to lower levels at the temperature T76, one finds
that the amount of gas at
600 K is less
than 1% of the column densities measured at
150 K.
The
total column densities at temperatures
assuming an OTP ratio of
2 are lower
than those of Table 4 by a factor of 1.8.
Note, that in this case the total column density should be
derived extrapolating
the observed population in the J=3 to the J=1 level
and the population in the J=2 to the J=0 levels,
as two different species at temperature
.
Of course, these column densities are still lower limits
to the actual warm
column densities.
These results are the first direct estimation of the
column densities and the structure of the warm gas in the GC clouds.
They show the presence of large column densities
of warm molecular gas with large temperature gradients (150-700 K),
extending the results derived by Hüttemeister et al. (1993)
from their NH3 data.
© ESO 2001