Stellar atmospheres : $b A contribution to the observational study of high temperature in the reversing layers of starsPayne-Gaposchkin, Cecilia
Science
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.)
The absorption bands of titanium oxide, TiO₂, are the characteristic
flutings[300][301]
of the stars of Class , and the strength of these
bands has been proposed[302] as a criterion of class for the stars
in which they are found. It is perhaps noteworthy that titanium,
zirconium, and carbon, the only elements which give oxides in stellar
spectra (hydrogen excepted) belong to the fourth group of the periodic
system.
VANADIUM (23)
The vanadium lines are best identified by intensity from Rowland’s
table. The following multiplets[303] are present in the solar
spectrum: , , ,
, , ,
. The multiplet is well seen in
stellar spectra from onwards, and increases in strength as
cooler stars are approached.[304] Slipher[305] called attention to
the strength in Ceti of the vanadium group near 4400,
presumably the two multiplets , ,
with excitation potential 0.28 volts.
[Pg 76]
IONIZED VANADIUM
Three multiplets, all far in the ultra-violet, are tabulated for
ionized vanadium by Meggers, Kiess, and Walters,[306] and two of them
are within the range of Rowland’s table. All the lines of these, the
and multiplets, have been satisfactorily
identified with solar lines. The strength of the ultimate lines of
ionized vanadium, which occur in the multiplet last named, is a little
greater, in the solar spectrum, than that of the strongest lines of the
neutral atom, at 4379, which are also ultimate lines.
The following tabulation contains, in the same form as Table XI, the
data respecting the two multiplets which are identified in the solar
spectrum.
TABLE XII
Series
Wave-Lenght
Int.
Cl.
Attribution
Int.
Wave-Lenght
3727.348
20
-
1
3727.488
3760.230
5
-
1
3760.364
3718.163
3
-
3718.291
3750.873
15
-
2
3751.015
3778.359
3
-
(Fe
3
3778.463)
3743.63
3
-
(Cr
1
37243.726)
3770.976
10
2
3771.116
*
3093.10
40
III Er
3093.229
3121.144
20
IV E
V
4
3121.270
*
3102.301
40
III Er
V
3
3102.404
3145.35
-
-
3
3145.484
3126.221
25
IV E
V, Fe
5
3126.319
*
3110.710
30
III Er
Ti, V
?
3110.810
3145.979
5
V Er
Zr
1
3146.091
3130.270
25
III E
V
3
3130.380
*
3118.382
30
III Er
V
3
3118.498
3145.344
10
IV E
3
3145.484
3133.336
20
III E
V
2
3133.449
*
3125.286
40
III Er
5
3125.399
[Pg 77]
CHROMIUM (24)
The lines of chromium were classified by Catalan,[307] and those which
occur in the sun are comprised in the following multiplets:[308]
, , ,
, , ,
, , ,
, , .
The ultimate lines , at 4254, 4274, 4289 increase
with advancing type.[309] The maximum for subordinate lines[310] is at
.
IONIZED CHROMIUM
Of the six multiplets of ionized chromium tabulated by Meggers, Kiess,
and Walters,[311] only two are within the measured range of the solar
spectrum, but every line in these two multiplets accords satisfactorily
in wave-length and intensity with a line in Rowland’s table. The
ultimate lines are in the neighborhood of 2800, and are therefore
unattainable. The lines, and the solar intensities, are contained in
the appended table.
TABLE XIII
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