It is interesting to look for theoretical correlations between different
radiative or plasma properties such as the integrated intensities, optical depths, electron temperature, or gas pressure. This helps us to understand the
physical processes that are at work in the line formation. Such a task has been
done by Heinzel et al. (1994) for the hydrogen spectrum in 1D isothermal isobaric
prominence models. Our aim here is to look for correlations between integrated
intensities. For clarity we have restricted our study to only one value of the
prominence thickness (1000 km).
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Figure 11: Half emergent line profiles for one slab width (1000 km) at 6000 K (four top panels) and 18000 K (four bottom panels). Solid line: P=0.02; dots: P=0.05; short dashes: P=0.1; long dashes/dots: P=0.2; long dashes: P=0.5. Same units as in Fig. 5. |
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Figure 12: Integrated intensities (in cgs units) for 4 lines as a function of the pressure computed for one slab width (1000 km) and 8 temperatures. Same symbols as in Fig. 6. |
We present in Fig. 16 the relation between
and
for 40 models with a slab thickness of 1000 km. This
relation between these optically thin triplet lines is clearly linear. This
linearity would only disappear in the case where at least one of the lines
becomes optically thick and begins to saturate at line center. This may
marginally happen for the 10830 line. In this case the ratio between the
10830 line intensity and another triplet line would slightly decrease. We
stress that this linear relation is valid in the optically thin case for all
the triplet lines we have studied. The only thing which varies from one line pair
to another is of course the slope of the relation. This is due to the fact that
in the triplet line source function the scattering term is dominant over the
collisional term for a wide range of physical conditions. Thus the triplet line
ratios mainly depend on the ratio of the incident line intensities. Here we
obtain a constant ratio
for the 40 models
represented in Fig. 16. In the following we will only consider
the D3 line, keeping in mind that all the results presented for this line can
easily be transposed to any other triplet line such as He I
10830, 7065, 3889, 3188 or 4471 Å if the
intensity ratio is known. Table 6 summarizes the different
triplet line ratios for 40 models computed with
and a slab thickness of 1000 km.
The relation between the optically thin He I 6678 Å and
the optically thick resonance line He I
584 Å is
represented in Fig. 17. These two lines have a common level
which is the lower level of the 6678 transition (see Fig. 2). We can see that at low temperatures the 584 line is
completely saturated and is independent of the model parameters (see Sect. 4.2) while the pressure variations decrease the 6678 line
intensity. At a given temperature the line ratio depends on the pressure: an
increase in the pressure leads to an increase of
E(6678)/E(584). This is
particularly true at high temperatures where the collisional excitation plays
an important role in the 584 line wing emission.
The relation between optically thin singlet and triplet lines is not as simple
as for the triplet-triplet case. We have in this case to consider how the
helium statistical equilibrium is reached for the whole atom. In the singlet
system the presence of the resonance lines provides an efficient way to
deexcite the
states by spontaneous emission. In the triplet system
the
metastable level acts as a ground state. The intersystem
collisions tend to drive the electrons from triplet to singlet states. Moreover
we have already noticed in Sect. 4 the weakness of the singlet
lines relative to the triplet lines. Figure 18 illustrates the
pressure dependance of the relation between the singlet
Å line integrated intensity and its triplet
equivalent D3 line intensity.
At low pressures (0.02 dyn/cm2) the relation
between the two lines is almost linear. Landman & Illing (1976) have found a similarly
linear relation between the two lines for one observed prominence (see their
Fig. 3). The observed range of intensities was smaller than that
represented in our Fig. 18: the D3 maximum intensity was less
than
erg s-1 cm-2 sr-1, and the maximum
6678 intensity was about 50 erg s-1 cm-2 sr-1. But we can
see that if the pressure is higher the relation between the two lines is no
longer linear at all. At 0.05 dyn/cm2 the integrated intensities are almost
constant whatever the temperature, giving a limit ratio. If we increase the
pressure this same limit value for the line ratio will be found for the lower
temperatures. In this situation the formation of the two lines is mainly due to
the scattering of the incident radiation because of a high optical thickness in
the incident continuum radiation. For high pressure, high temperature models,
the same optical depth is reduced and collisional excitation becomes
important: this gives an increasing ratio of the two lines with the
temperature and the pressure.
Ionized helium is coupled to neutral helium in several different ways in our model atom. Radiative bound - free transitions (photoionization and collisional ionization) are allowed between all neutral helium states and the ground state of He II. The photoionization of the He I ground level plays an important role since it is the main way to populate the excited levels by recombinations (PR process) when the temperature is not high enough to produce significant collisional excitation from the ground level towards the triplet states.
The relation between He II 304 Å and
He I
584 Å shown in Fig. 19 indicates a
decreasing ratio
E(304)/E(584) with the temperature: the 304 line intensity
also grows with the temperature, but more slowly than the 584 line intensity.
At high temperatures the 584 line emission increases with the pressure because
of collisional excitation while the 304 line is saturated and is formed by
scattering of the incident radiation. A decrease of the temperature increases
the
E(304)/E(584) ratio up to a limit value which corresponds to a situation
where both lines are formed by the scattering of the incident radiation.
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Figure 14:
Half emergent line profiles for two different models: T=6000 K, P=0.02 dyn/cm2 and W=1000 km (four top panels); ![]() ![]() ![]() ![]() ![]() |
The intensity ratio between the helium D3 line and the hydrogen Balmer lines
has been measured by several observers (Landman & Illing 1976, 1977; Landman et al. 1977; Stellmacher 1979; Stellmacher & Wiehr 1995, 1997; de Boer et al. 1998, for instance).
Figure 20 shows the
theoretical behaviour of the
ratio with the
different physical parameters already considered in this work. First we can see
that this ratio decreases with the slab thickness.
increases
with the slab thickness (Fig. 6), but more slowly than the H
intensity.
is not very sensitive to the
temperature at low pressure. We can see that at a fixed temperature the
increase of the pressure causes the ratio to decrease because of a decrease of the mean helium ionization ratio. For the highest pressures where the ionization is low the
only way to observe a significant
value is
to have high temperatures. The evolution of the ratio with helium abundance
reflects the evolution of the D3 intensity with
(see Fig. 15) but with a higher slope. An increase of a factor of 4 in
helium abundance leads to an increase of a factor of 3 for the intensity ratio in
the case of a low pressure, low temperature model (
in Fig. 20, bottom
right panel). This corresponds to a decrease of about 15% of the H
intensity with the abundance increase.
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Figure 15:
Integrated intensities (in cgs units) for 4 lines as a function of the abundance
computed for 2 models: T=6000 K, P=0.02 dyn/cm2 and W=1000 km
(![]() ![]() ![]() |
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Figure 16:
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Figure 17:
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Figure 18:
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Figure 19:
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Heasley & Milkey (1976)
have already discussed (see their Fig. 1) the theoretical behaviour of this
relation relative to temperature, pressure, and column mass. If we increase the
total column mass (increase of the H
intensity) the prominence becomes
optically thick in the Lyman continuum and the excitational and ionizing
radiation penetrates less deeply in the slab, thus decreasing the ionization of
helium. An increase in the pressure has the same effect: we obtain an
increase of the recombination rates, thus reducing the helium ionization.
Finally, a decrease in the temperature leads to a decrease of hydrogen and
helium ionization (or an increase of the Lyman continuum optical thickness).
We know that the recombination from the He II ground state is the main
mechanism which populates the helium triplet states. This is consistent with
the photoionization-recombination (PR) scheme which is believed to be the main
population mechanism for helium in the solar atmosphere for temperatures below
20000 K (see e.g., Andretta & Jones 1997). These effects are also seen in
our Fig. 3 (see Sect. 3.2). The tendancy of a lowering
of the curve with increasing H
intensities is also visible in the
Fig. 6 of, e.g., de Boer et al. (1998). Our conclusion about helium excitation and
ionization conditions are that as the hydrogen density increases, the
ratio decreases, but more rapidly at slab
center where there is much less UV continuum radiation. This produces a too
weak ionization at slab center to populate helium triplet states.
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Figure 20:
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Copyright ESO 2001