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400 | 8.48(-03)![]() |
4.95(-03) | 1.48(-02) | 2.47(-02) | 1.42(-02) | 4.05(-02) |
7.53(-06)![]() |
7.67(-07) | 2.31(-06) | 3.88(-06) | 4.32(-07) | 9.86(-06) | |
600 |
9.09(-03) | 5.04(-03) | 1.51(-02) | 2.51(-02) | 1.46(-02) | 4.26(-02) |
8.96(-05) | 6.94(-06) | 2.09(-05) | 3.50(-05) | 4.40(-06) | 7.09(-05) | |
900 |
9.46(-03) | 5.02(-03) | 1.50(-02) | 2.51(-02) | 1.50(-02) | 4.48(-02) |
4.76(-04) | 3.12(-05) | 9.37(-05) | 1.57(-04) | 2.28(-05) | 2.73(-04) | |
1350 |
9.39(-03) | 4.85(-03) | 1.46(-02) | 2.42(-02) | 1.52(-02) | 4.76(-02) |
1.45(-03) | 8.59(-05) | 2.58(-04) | 4.32(-04) | 7.53(-05) | 6.95(-04) | |
2000 |
8.91(-03) | 4.56(-03) | 1.37(-02) | 2.27(-02) | 1.55(-02) | 5.13(-02) |
2.97(-03) | 1.64(-04) | 4.93(-04) | 8.26(-04) | 1.80(-04) | 1.31(-03) | |
3000 |
8.14(-03) | 4.15(-03) | 1.25(-02) | 2.08(-02) | 1.58(-02) | 5.65(-02) |
4.75(-03) | 2.51(-04) | 7.54(-04) | 1.26(-03) | 3.62(-04) | 2.10(-03) | |
4500 |
7.23(-03) | 3.68(-03) | 1.11(-02) | 1.84(-02) | 1.62(-02) | 6.40(-02) |
6.23(-03) | 3.20(-04) | 9.60(-04) | 1.61(-03) | 6.36(-04) | 2.97(-03) | |
6700 |
6.30(-03) | 3.20(-03) | 9.60(-03) | 1.60(-02) | 1.68(-02) | 7.38(-02) |
7.08(-03) | 3.56(-04) | 1.07(-03) | 1.79(-03) | 1.01(-03) | 3.88(-03) | |
10000 |
5.37(-03) | 2.70(-03) | 8.09(-03) | 1.34(-02) | 1.76(-02) | 8.70(-02) |
7.23(-03) | 3.59(-04) | 1.08(-03) | 1.80(-03) | 1.50(-03) | 4.82(-03) |
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4.06(-03)![]() |
2.51(-03) | 7.50(-03) | 1.25(-02) | 7.35(-03) | 2.10(-02) | |
400 | 5.01(-04)![]() |
1.53(-04) | 4.60(-04) | 7.71(-04) | 2.92(-04) | 7.53(-04) |
1.82(-05)![]() |
1.32(-06) | 3.95(-06) | 6.67(-06) | 9.42(-07) | 1.26(-05) | |
4.06(-03) | 2.48(-03) | 7.41(-03) | 1.23(-02) | 7.45(-03) | 2.19(-02) | |
600 | 8.27(-04) | 2.31(-04) | 6.97(-04) | 1.16(-03) | 4.06(-04) | 9.84(-04) |
1.33(-04) | 8.38(-06) | 2.51(-05) | 4.23(-05) | 6.68(-06) | 6.98(-05) | |
4.04(-03) | 2.42(-03) | 7.26(-03) | 1.21(-02) | 7.59(-03) | 2.30(-02) | |
900 | 1.05(-03) | 2.75(-04) | 8.31(-04) | 1.38(-03) | 4.56(-04) | 1.06(-03) |
5.05(-04) | 2.94(-05) | 8.82(-05) | 1.48(-04) | 2.71(-05) | 2.26(-04) | |
3.96(-03) | 2.33(-03) | 7.00(-03) | 1.16(-02) | 7.75(-03) | 2.46(-02) | |
1350 | 1.09(-03) | 2.74(-04) | 8.29(-04) | 1.37(-03) | 4.38(-04) | 9.83(-04) |
1.22(-03) | 6.80(-05) | 2.04(-04) | 3.42(-04) | 7.61(-05) | 5.12(-04) | |
3.80(-03) | 2.21(-03) | 6.63(-03) | 1.10(-02) | 7.94(-03) | 2.68(-02) | |
2000 | 9.86(-04) | 2.42(-04) | 7.31(-04) | 1.20(-03) | 3.78(-04) | 8.31(-04) |
2.14(-03) | 1.15(-04) | 3.45(-04) | 5.79(-04) | 1.63(-04) | 8.96(-04) | |
3.58(-03) | 2.04(-03) | 6.12(-03) | 1.02(-02) | 6.26(-03) | 2.97(-02) | |
3000 | 8.04(-04) | 1.93(-04) | 5.86(-04) | 9.73(-04) | 2.28(-04) | 6.47(-04) |
3.04(-03) | 1.60(-04) | 4.81(-04) | 8.06(-04) | 3.04(-04) | 1.37(-03) | |
3.28(-03) | 1.83(-03) | 5.51(-03) | 9.18(-03) | 8.51(-03) | 3.39(-02) | |
4500 | 6.09(-04) | 1.45(-04) | 4.42(-04) | 7.32(-04) | 2.23(-04) | 4.81(-04) |
3.67(-03) | 1.90(-04) | 5.72(-04) | 9.57(-04) | 5.05(-04) | 1.88(-03) | |
2.94(-03) | 1.61(-03) | 4.84(-03) | 8.06(-03) | 8.89(-03) | 3.93(-02) | |
6700 | 4.51(-04) | 1.06(-04) | 3.22(-04) | 5.33(-04) | 1.61(-04) | 3.45(-04) |
3.91(-03) | 2.01(-04) | 6.04(-04) | 1.01(-03) | 7.70(-04) | 2.41(-03) | |
2.57(-03) | 1.37(-03) | 4.12(-03) | 6.85(-03) | 9.34(-03) | 4.65(-02) | |
10000 | 3.16(-04) | 7.53(-05) | 2.28(-04) | 3.76(-04) | 1.14(-04) | 2.42(-04) |
3.81(-03) | 1.94(-04) | 5.85(-04) | 9.77(-04) | 1.11(-03) | 2.96(-03) |
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2.53(-03) | 1.56(-03) | 4.67(-03) | 7.77(-03) | 4.79(-03) | 1.45(-02) | |
400 | 5.05(-04) | 1.41(-04) | 4.23(-04) | 7.04(-04) | 2.44(-04) | 5.92(-04) |
3.14(-05) | 1.97(-06) | 5.91(-06) | 9.99(-06) | 1.63(-06) | 1.64(-05) | |
2.53(-03) | 1.53(-03) | 4.59(-03) | 7.65(-03) | 4.88(-03) | 1.51(-02) | |
600 | 6.75(-04) | 1.77(-04) | 5.35(-04) | 8.89(-04) | 2.93(-04) | 6.76(-04) |
1.64(-04) | 9.55(-06) | 2.87(-05) | 4.84(-05) | 8.87(-06) | 7.27(-05) | |
2.50(-03) | 1.49(-03) | 4.47(-03) | 7.43(-03) | 4.96(-03) | 1.59(-02) | |
900 | 7.34(-04) | 1.85(-04) | 5.62(-04) | 9.29(-04) | 2.95(-04) | 6.63(-04) |
4.96(-04) | 2.77(-05) | 8.32(-05) | 1.40(-04) | 3.02(-05) | 2.03(-04) | |
2.43(-03) | 1.42(-03) | 4.27(-03) | 7.10(-03) | 5.08(-03) | 1.71(-02) | |
1350 | 6.89(-04) | 1.69(-04) | 5.11(-04) | 8.44(-04) | 2.62(-04) | 5.78(-04) |
1.03(-03) | 5.59(-05) | 1.68(-04) | 2.83(-04) | 7.49(-05) | 4.15(-04) | |
2.31(-03) | 1.33(-03) | 4.00(-03) | 6.64(-03) | 5.21(-03) | 1.87(-02) | |
2000 | 5.78(-04) | 1.40(-04) | 4.25(-04) | 6.96(-04) | 2.14(-04) | 4.67(-04) |
1.60(-03) | 8.61(-05) | 2.59(-04) | 4.35(-04) | 1.48(-04) | 6.83(-04) | |
2.15(-03) | 1.21(-03) | 3.65(-03) | 6.06(-03) | 5.39(-03) | 2.09(-02) | |
3000 | 4.49(-04) | 1.08(-04) | 3.26(-04) | 5.37(-04) | 1.63(-04) | 3.52(-04) |
2.10(-03) | 1.11(-04) | 3.35(-04) | 5.63(-04) | 2.61(-04) | 9.97(-04) | |
1.95(-03) | 1.08(-03) | 3.24(-03) | 5.39(-03) | 5.61(-03) | 2.40(-02) | |
4500 | 3.30(-04) | 7.91(-05) | 2.39(-04) | 3.94(-04) | 1.19(-04) | 2.56(-04) |
2.39(-03) | 1.25(-04) | 3.78(-04) | 6.33(-04) | 4.17(-04) | 1.34(-03) | |
1.72(-03) | 9.32(-04) | 2.81(-03) | 4.66(-03) | 5.86(-03) | 2.80(-02) | |
6700 | 2.36(-04) | 5.65(-05) | 1.70(-04) | 2.80(-04) | 8.50(-05) | 1.81(-04) |
2.43(-03) | 1.27(-04) | 3.85(-04) | 6.42(-04) | 6.18(-04) | 1.68(-03) | |
1.49(-03) | 7.83(-04) | 2.36(-03) | 3.91(-03) | 6.17(-03) | 3.32(-02) | |
10000 | 1.64(-04) | 3.93(-05) | 1.19(-04) | 1.97(-04) | 5.92(-05) | 1.26(-04) |
2.29(-03) | 1.19(-04) | 3.62(-04) | 6.01(-04) | 8.73(-04) | 2.05(-03) |
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1.74(-03) | 1.05(-03) | 3.18(-03) | 5.28(-03) | 3.39(-03) | 1.06(-02) | |
400 | 4.41(-04) | 1.16(-04) | 3.51(-04) | 5.86(-04) | 1.93(-04) | 4.49(-04) |
4.40(-05) | 2.59(-06) | 7.75(-06) | 1.32(-05) | 2.40(-06) | 2.00(-05) | |
1.72(-03) | 1.04(-03) | 3.11(-03) | 5.18(-03) | 3.44(-03) | 1.10(-02) | |
600 | 5.17(-04) | 1.32(-04) | 3.97(-04) | 6.61(-04) | 2.10(-04) | 4.74(-04) |
1.81(-04) | 1.02(-05) | 3.06(-05) | 5.21(-05) | 1.07(-05) | 7.46(-05) | |
1.69(-03) | 1.00(-03) | 3.01(-03) | 5.00(-03) | 3.50(-03) | 1.18(-02) | |
900 | 5.11(-04) | 1.28(-04) | 3.84(-04) | 6.35(-04) | 1.97(-04) | 4.39(-04) |
4.65(-04) | 2.56(-05) | 7.68(-05) | 1.30(-04) | 3.19(-05) | 1.85(-04) | |
1.63(-03) | 9.50(-04) | 2.85(-03) | 4.73(-03) | 3.58(-03) | 1.26(-02) | |
1350 | 4.45(-04) | 1.10(-04) | 3.30(-04) | 5.45(-04) | 1.67(-04) | 3.65(-04) |
8.56(-04) | 4.66(-05) | 1.40(-04) | 2.37(-04) | 7.25(-05) | 3.50(-04) | |
1.53(-03) | 8.77(-04) | 2.65(-03) | 4.38(-03) | 3.69(-03) | 1.39(-02) | |
2000 | 3.60(-04) | 8.75(-05) | 2.63(-04) | 4.35(-04) | 1.31(-04) | 2.87(-04) |
1.24(-03) | 6.66(-05) | 2.01(-04) | 3.38(-04) | 1.35(-04) | 5.46(-04) | |
1.41(-03) | 7.92(-04) | 2.40(-03) | 3.96(-03) | 3.82(-02) | 1.57(-02) | |
3000 | 2.70(-04) | 6.57(-05) | 1.85(-04) | 3.25(-04) | 9.77(-05) | 2.12(-04) |
1.52(-03) | 8.15(-05) | 2.47(-04) | 4.14(-04) | 2.28(-04) | 7.72(-04) | |
1.27(-03) | 6.96(-04) | 2.11(-03) | 3.48(-03) | 3.99(-03) | 1.80(-02) | |
4500 | 1.94(-04) | 4.72(-05) | 1.42(-04) | 2.34(-04) | 7.04(-05) | 1.52(-04) |
1.65(-03) | 8.78(-05) | 2.68(-04) | 4.47(-04) | 3.54(-04) | 1.01(-03) | |
1.11(-03) | 5.95(-04) | 1.81(-03) | 2.98(-03) | 4.18(-03) | 2.12(-02) | |
6700 | 1.37(-04) | 3.33(-05) | 9.97(-05) | 1.65(-04) | 4.97(-05) | 1.07(-04) |
1.63(-03) | 8.60(-05) | 2.66(-04) | 4.40(-04) | 5.13(-04) | 1.26(-03) | |
9.45(-04) | 4.93(-04) | 1.51(-03) | 2.47(-03) | 4.39(-03) | 2.51(-02) | |
10000 | 9.47(-05) | 2.31(-05) | 6.91(-05) | 1.14(-04) | 3.42(-05) | 7.37(-05) |
1.49(-03) | 7.83(-05) | 2.46(-04) | 4.02(-04) | 7.12(-04) | 1.52(-03) |
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1.26(-03) | 7.63(-04) | 2.31(-03) | 3.81(-03) | 2.51(-03) | 8.07(-03) | |
400 | 3.62(-04) | 9.39(-05) | 2.82(-04) | 4.69(-04) | 1.50(-04) | 3.41(-04) |
5.44(-05) | 3.11(-06) | 9.32(-06) | 1.60(-05) | 3.18(-06) | 2.31(-05) | |
1.24(-03) | 7.45(-04) | 2.25(-03) | 3.71(-03) | 2.56(-03) | 8.46(-03) | |
600 | 3.88(-04) | 9.84(-05) | 2.95(-04) | 4.88(-04) | 1.52(-04) | 3.39(-04) |
1.87(-04) | 1.04(-05) | 3.13(-05) | 5.34(-05) | 1.22(-05) | 7.49(-05) | |
1.21(-03) | 7.13(-04) | 2.16(-03) | 3.57(-03) | 2.60(-03) | 9.00(-03) | |
900 | 3.59(-04) | 9.00(-05) | 2.68(-04) | 4.45(-04) | 1.36(-04) | 3.00(-04) |
4.23(-04) | 2.34(-05) | 7.01(-05) | 1.19(-04) | 3.28(-05) | 1.69(-04) | |
1.16(-03) | 6.70(-04) | 2.04(-03) | 3.34(-03) | 2.67(-03) | 9.79(-03) | |
1350 | 3.01(-04) | 7.44(-05) | 2.22(-04) | 3.66(-04) | 1.11(-04) | 2.44(-04) |
7.14(-04) | 3.91(-05) | 1.18(-04) | 2.00(-04) | 6.96(-05) | 3.00(-04) | |
1.09(-03) | 6.16(-04) | 1.88(-03) | 3.08(-03) | 2.75(-03) | 1.08(-02) | |
2000 | 2.34(-04) | 5.78(-05) | 1.72(-04) | 2.84(-04) | 8.54(-05) | 1.87(-04) |
9.68(-04) | 5.27(-05) | 1.60(-04) | 2.69(-04) | 1.24(-04) | 4.51(-04) | |
9.88(-04) | 5.52(-04) | 1.69(-03) | 2.75(-03) | 2.86(-03) | 1.22(-02) | |
3000 | 1.72(-04) | 4.25(-05) | 1.27(-04) | 2.09(-04) | 6.26(-05) | 1.36(-04) |
1.14(-03) | 6.17(-05) | 1.89(-04) | 3.16(-04) | 2.02(-04) | 6.20(-04) | |
8.78(-04) | 4.80(-04) | 1.48(-03) | 2.39(-03) | 2.99(-03) | 1.41(-02) | |
4500 | 1.22(-04) | 3.03(-05) | 9.01(-05) | 1.48(-04) | 4.35(-05) | 9.61(-05) |
1.19(-03) | 6.42(-05) | 2.00(-04) | 3.30(-04) | 3.06(-04) | 7.98(-04) | |
7.66(-04) | 4.06(-04) | 1.28(-03) | 2.03(-03) | 3.13(-03) | 1.66(-02) | |
6700 | 8.54(-05) | 2.12(-05) | 6.33(-05) | 1.03(-04) | 3.10(-05) | 6.75(-05) |
1.14(-03) | 6.13(-05) | 1.95(-04) | 3.17(-04) | 4.36(-04) | 9.81(-04) | |
6.47(-04) | 3.32(-04) | 1.07(-03) | 1.66(-03) | 3.29(-03) | 1.99(-02) | |
10000 | 5.88(-05) | 1.46(-05) | 4.35(-05) | 7.15(-05) | 2.14(-05) | 4.67(-05) |
1.02(-03) | 5.46(-05) | 1.80(-04) | 2.86(-04) | 5.97(-04) | 1.17(-03) |
Multiplet | C V | N VI | O VII | Ne IX | Mg XI | Si XIII |
w | 307.88 | 430.65 | 574.00 | 921.82 | 1357.07 | 1864.44 |
(40.27) | (28.79) | (21.60) | (13.45) | (9.17) | (6.65) | |
x+y | 304.41 | 426.36 | 568.74 | 915.02 | 1343.28 | 1853.29 |
(40.73) | (29.08) | (21.80) | (13.55) | (9.23) | (6.69) | |
z | 298.97 | 419.86 | 561.02 | 905.00 | 1331.74 | 1839.54 |
(41.47) | (29.53) | (22.10) | (13.70) | (9.31) | (6.74) |
We note that for all temperatures (low and high), we have included in the line ratio calculations, RR contribution (direct + upper-level radiative cascade), and collisional excitations inside the n=2 shell. For high temperature plasmas, the CE contribution (direct + resonance + cascade) from the ground level (n=1 shell, 1s2) should be included in the calculations as well as DR (direct + cascade). Figure 5 displays these different contributions which populate a given n=2 level.
As emphasized previously, the cascade contribution from n>2 levels, especially for the
3S1 level, should be taken into account in line ratio calculations since this
level is responsible for the forbidden component (z) line, which appears in both
ratios R and G. For a pure photoionized plasma, when no upper level radiative
cascade contribution is included in the RR rates, R and G could be
underestimated by 6-10% (for O VII). In a hybrid plasma, where collisional
processes from the ground level are not negligible, the ratio R is lower by
% at
K, when no cascades from upper levels are taken into
account. In a similar way, the value of G would be underestimated.
We also point out the importance of taking into account the branching ratios in the
calculations of x and y lines.
), and
)
are respectively the branching ratios
of the x and y lines (
being the transition probability
from level j to level i, see Fig. 1). Branching ratios are very important in
the case of light nuclear charge (Z), as shown in Fig. 6, for C V,
as well
.
When Z increases, most
branching ratios become less important but nevertheless some of them should be included in
the calculations. Without these branching ratios the intensities of the intercombination
lines x and y could be overestimated, resulting in an underestimate of the ratio
R. This could lead to huge discrepancies for the value of R as well as for
G.
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Figure 6:
Simplified Gotrian diagrams for C V and Si XIII. Thick curves
correspond to the strongest radiative transitions (
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Figure 7:
G (=(x+y+z)/w) is reported as a function of electronic temperature (![]() ![]() ![]() ![]() |
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Figure 9:
In case of hybrid plasmas (partially photoionized: recombination plus collisional
excitation from the ground level), the ratio
R (=z/(x+y)) is reported as a function of
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Figure 11:
O VII theoretical spectra constructed using the RGS (XMM) resolving power
(
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At higher temperatures, i.e. large enough to permit excitation from the ground level to
upper levels, G becomes sensitive to both parameters (,
). High values of
favour mainly DR (H-like ions
towards He-like ions), but for photoionized plasma such high temperatures (where
G<4) are probably extreme cases (i.e. not realistic) for WA plasmas.
On the contrary,
for lower values of
the lines are produced mainly by collisional
excitation ("hybrid'' plasma in our nomenclature). A value of G<4 will be the
signature of a plasma where collisional processes are no longer negligible and even be
dominant compared to recombination. We should notice that this is no more the case when G is sensitive to
,
i.e. when the resonance w line becomes sensitive
to density due to the depopulation of the 1s2s1S0 level to the 1s2p1P1 level (see also Figs. 4-6-9 in Gabriel & Jordan [1972]).
In conclusion, the relative intensity of the resonance w line, compared to the
forbidden z and the intercombination (x+y) lines, contains informations
about the ionization processes that occur: a weak w line compared to the z
or the (x+y) lines corresponds to a pure photoionized plasma. It leads to a ratio of
G=(z+x+y)/w>4. On the contrary a strong w line corresponds to a hybrid plasma (or
even a collisional plasma), where collisional processes are not negligible and may even
dominate (see Sect. 3.3.2). In this case, w is at least as intense as the
z or x+y lines.
For low values of
corresponding to the density range where G is
independent of
(Fig. 8), R is almost insensitive
to temperature.
But in the case of high temperature (with a high
value so that the
medium is dominated by recombination), the value of R is larger. Thus in the density
range where R takes a constant value (i.e. low density values), a high value of R corresponds to a high temperature. This also imply a very intense H-like line
(K
)
since the ratio
= H-like/He-like need to be large enough so
that the gas is dominated by recombinations (see caption of the Fig. 7).
Copyright The European Southern Observatory (ESO)