Table 1:
Lines used for the integral inversion and for evaluating
the elemental abundances.
is our
preferred laboratory wavelength and
the
"corrected'' observed wavelength in
Brooks et al. (1999).
is the peak
temperature of line formation. Since one line per ion at
most is used in the integral inversion, we indicate with
"i'' the lines used in the integral inversion and "f''
the lines compared with observations in the forward sense,
i.e. by comparing the intensities predicted using the DEM
with the observed intensities. The source for the adopted
wavelengthis is denoted by E for Edlén (1983a,1984,1985c,b,a,1983b), F
for Fawcett (1975), K for Kelly (1987), N for
Martin et al. (1995), and O for Wiese (1985),
respectively.
Ion |
 |
Transition |
 |
 |
i/f |
O III |
525.797 |
2s2 2p2 1D2-2s 2p3 1P1 |
525.801 |
4.95 |
f |
O III |
599.598 |
2s2 2p2 1D2-2s 2p3 1D2 |
599.596 |
5.00 |
i |
O IV |
553.329 |
2s2 2p2P1/2-2s 2p2 2P3/2 |
553.343 |
5.20 |
f |
O IV |
554.076 |
2s2 2p 2P1/2-2s 2p2 2P1/2 |
554.076 |
5.20 |
f |
O IV |
554.513 |
2s2 2p 2P3/2-2s 2p2 2P3/2 |
554.512 |
5.20 |
f |
O IV |
555.263 |
2s2 2p 2P3/2-2s 2p2 2P1/2 |
555.270 |
5.20 |
i |
O IV |
608.397 |
2s2 2p 2P1/2-2s 2p2 2S1/2 |
608.312 |
5.20 |
f |
Ne IV |
543.886 |
2s2 2p3 4S3/2-2s 2p4 4P5/2 |
543.881 |
5.30 |
i |
O V |
629.732 |
2s2 1S0-2s 2p 1P1 |
629.735 |
5.40 |
i |
Ar VII |
585.754 |
3s2 1S0-3s 3p 1P1 |
585.694 |
5.50 |
f |
Ne V |
359.375 |
2s2 2p2 3P2-2s 2p3 3S1 |
359.374 |
5.50 |
i |
Ne VII |
561.72 |
2s 2p 3P2-2p2 3P2 |
561.725 |
5.70 |
i |
Al VII |
356.892 |
2s2 2p3 4S3/2-2s 2p4 4P5/2 |
356.922 |
5.75 |
f |
Ca VIII |
582.845 |
3s2 3p 2P1/2-3s 3p2 2D3/2 |
582.872 |
5.75 |
f |
Ca X |
557.759 |
3s 2S1/2-3p 2P3/2 |
557.764 |
5.80 |
i |
Al VIII |
328.183 |
2s2 2p2 3P2-2s 2p3 3P2 |
328.249 |
5.90 |
f |
Al VIII |
328.230 |
2s2 2p2 3P2-2s 2p3 3P1 |
|
5.90 |
f |
Si VIII |
316.218 |
2s2 2p3 4S3/2-2s 2p4 4P3/2 |
316.215 |
5.90 |
f |
Si VIII |
319.839 |
2s2 2p3 4S3/2-2s 2p4 4P5/2 |
319.840 |
5.90 |
f |
Mg VIII |
311.772 |
2s2 2p 2P1/2-2s 2p2 2P3/2 |
311.750 |
5.90 |
f |
Mg VIII |
313.743 |
2s2 2p 2P1/2-2s 2p2 2P1/2 |
313.758 |
5.90 |
i |
Mg VIII |
335.231 |
2s2 2p 2P1/2-2s 2p2 2S1/2 |
335.233 |
5.90 |
f |
Fe XI |
352.661 |
3s2 3p4 3P2-3s 3p5 3P2 |
352.671 |
6.05 |
f |
Si IX |
341.950 |
2s2 2p2 3P0-2s 2p3 3D1 |
341.952 |
6.05 |
i |
Al X |
332.788 |
2s2 1S0-2s2p 1P1 |
332.785 |
6.10 |
f |
Al XI |
550.04 |
2s 2S1/2-2p 2P3/2 |
550.050 |
6.15 |
f |
Si X |
347.408 |
2s2 2p 2P1/2-2s 2p2 2D3/2 |
347.402 |
6.15 |
i |
Fe XII |
364.468 |
3s2 3p3 4S3/2-3s 3p4 4P5/2 |
364.467 |
6.15 |
f |
Si XII |
520.662 |
2s 2S1/2-2p 2P1/2 |
520.685 |
6.30 |
i |
Source LaTeX |
All tables |
In the text