Stellar atmospheres : $b A contribution to the observational study of high temperature in the reversing layers of starsPayne-Gaposchkin, Cecilia
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Stellar atmospheres : $b A contribution to the observational study of high temperature in the reversing layers of stars
Payne-Gaposchkin, Cecilia
Astrophysics; Stars -- Spectra; Stars -- Temperature; Thesis (Ph. D.)
In two papers, Russell[396] has given a discussion of the solar
and sunspot spectra, showing that ionization theory offers a very
satisfactory interpretation of most of the observed phenomena.
Attention was called to the anomalous behavior of barium and
lithium,[397] and it was suggested that the theory of thermal
ionization, while taking account of the temperature of the reversing
layer, omitted to consider the effect of the absorption of photospheric
radiation. This omission might cause a deviation such as is observed
for barium, but appears inadequate to account for the behavior of
lithium. In the case of lithium, low atomic weight, and a consequent
high velocity of thermal agitation, has been suggested as the cause of
the anomaly. The question of the absorption of photospheric radiation
has more recently been discussed by Saha,[398] in the form of a
correction to his own ionization equations. It has been pointed out by
Woltjer[399] that the correction introduced by Saha and Swe may also be
derived from considerations advanced by Einstein[400] and Milne.[401]
The correction can be evaluated, but appears in every case to be rather
small. The effect of the photospheric radiation is certainly one that
must be included in a satisfactory theory, but at present, observation
is probably not of sufficient accuracy to demand such a refinement.
The work just quoted was qualitative. A more quantitative test of
ionization theory in the solar spectrum can also be made[402] by
comparing the intensities of solar lines corresponding to different
excitation potentials, but belonging to the same atom. The
[Pg 114] atoms which
give a large number of lines in the solar spectrum are those of the
first long period of the periodic table, and these, as is well known,
consist of multiplets, with components of very different intensities.
It appears to be legitimate to select the strongest line associated
with any energy level for the comparison; the strength of this line
probably represents fairly well the tendency of the atom to be in the
corresponding state.
Atom
Excitation
Potential
Intensity
Atom
Excitation
Potential
Intensity
Calcium
0.00
20
Chromium
0.00
10
1.88
15
0.94
5
2.53
8
1.02
5
2.70
5
2.89
2
2.92
4
Titanium
0.00
5
Iron
0.00
40
0.82
4
0.94
30
0.90
3
1.54
30
1.05
3
2.19
8
1.44
3
2.46
10
1.50
2
2.84
8
1.87
1
2.96
7
1.98
1
3.25
7
2.08
0
3.38
6
2.16
1
3.64
8
2.24
2
4.13
-
2.26
0
4.23
-
2.28
0
4.35
-
2.33
0
4.40
-
2.39
00
2.47
-
2.56
000
2.67
000
Public-domain text, read in full here on John Shaqi.
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