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.)
The most important factor involved in the theory is ,
the partial pressure of electrons in the reversing layer.
By assuming constant at about
, and treating
as the unknown, a temperature scale which agrees substantially
with those derived from measurements of radiation may be deduced from
the observed positions of the maxima. The first discussion of the
data then available was made by Fowler and Milne in their original
paper.[379] Subsequent investigations of the positions of maxima
have been published by Menzel[380] and by the writer.[381] These
observations, and the scale derived from them, will be discussed in the
two following chapters.
The value of has been recently shown by several kinds of
investigation to be at least as low as was assumed by Fowler and
Milne, so that their assumption that a uniform mean pressure can be
used, as a first approximation, in deriving a temperature scale from
their formula appears to be justified. Milne[382] points out that “on
whatever specific assumptions” the theory rests, “the mean pressure for
a maximum of intensity in an absorption line is found to depend on the
absolute value of the absorption coefficient. In fact ... it is clear
[Pg 110]
that the greater the absorbing power of the atoms in question, the more
opaque is the stellar atmosphere in the frequency concerned, and so
the greater the height and the smaller the pressure at which the line
originates.” That the absorption coefficient in the stellar atmosphere
is very high is suggested by the reorganization times (“lives”) of such
atoms as have been investigated,[383] and Milne’s discussion of the
life of the excited calcium atom from astrophysical data lends weight
to the suggestion. A high absorption coefficient leads at once
to low pressures in the reversing layer, and theory has gone
far towards indicating that pressures of the order of
are to be expected
on a priori grounds.[384]
The observational evidence bearing on pressures in the reversing layer
will be found[385] in Chapter III. The case appears to be a strong
one, resting on evidence of many different kinds—notably pressure
shifts, line sharpness, and series limits. Russell and Stewart,[386]
in their exhaustive discussion of the question, conclude that “all
lines of evidence agree with the conclusion that the total pressure of
the photospheric gases is less than 0.01 atmosphere, and that
the average pressure in the reversing layer is not greater than
0.0001 atmosphere.”
The observational evidence gives the total pressure, but the
partial electron pressure will not differ greatly from this. Although
even in the hottest stars three ionizations is the greatest number
observed, most of the elements that constitute the stellar atmosphere
are appreciably ionized at temperatures greater than 4000°, so that the
partial electron pressure is at least half the total pressure.
PHYSICAL ASSUMPTIONS
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