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.)
Attention was first called to the probability of an extremely low
pressure in the reversing layer by R. H. Fowler and Milne,[62] in
advancing the form of ionization theory which is to be analyzed in
later chapters. The conclusion that the pressure in the reversing layer
is exceedingly low was a direct outcome of their discussion, and they
mentioned that the results from other methods converged in the same
direction.
Russell and Stewart,[63] in a specific discussion of the pressures
at the surface of the sun, have established beyond question, and on
quite other grounds, that the pressure for the solar reversing layer
is indeed of the order suggested by Fowler and Milne. The value
need then no longer be
regarded as a result of the Fowler-Milne theory, and may be used
without redundancy in deriving a stellar temperature scale from that
theory.
METHODS OF ESTIMATING REVERSING LAYER PRESSURES
Russell and Stewart examined the evidence for reversing layer pressures
derived from the following sources: (a) Shifts of spectral lines
due to pressure, (b) Sharpness of lines, (c) Widths of
lines, (d) Flash spectrum, (e) Equilibrium of outer
layers, (g) Ionization and chemical equilibrium in the solar
[Pg 38]
atmosphere. In addition to these we have (f) the observed limit
of the Balmer series in the hotter stars, where the hydrogen lines are
at or near their maximum. These sources of evidence will now be briefly
discussed.
(a) Shifts of Spectral Lines.—It was at one time supposed that
displacements of spectral lines, corresponding to pressures of several
atmospheres, could be found in stellar spectra. More recent work,[64]
however, has shown conclusively that the pressure shifts that occur are
so small that it is impossible to estimate a pressure from them with
any approach to accuracy. The estimated pressures are of the same order
as their probable errors. This being so, the most that can be expected
of the method based upon pressure effects is a demonstration of whether
or no the pressure exceeds 0.1 atmosphere, and this question has now
been satisfactorily answered in the negative.
[Pg 39]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account