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Stellar atmospheres

Chapter 13: TABLE VII
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This work presents a detailed analysis of stellar atmospheres, focusing on the physical principles underlying astrophysics. It explores the relationship between physics and astrophysics, examining properties of matter related to nuclear structure and atomic states. The text discusses the stellar temperature scale, including definitions and temperature variations among different types of stars. It also addresses the effects of temperature, pressure, and other conditions on stellar spectra, providing insights into the observational results from the Harvard Observatory. The analysis aims to contribute to the understanding of stellar atmospheres through extensive research and original investigations.

CHAPTER II
THE STELLAR TEMPERATURE SCALE

IT is well to distinguish the different meanings that are to be associated with the term “stellar temperature.” The observed energy distribution in the spectrum, combined with the theory of black-body radiation, lead to a quantity known as the “effective temperature” of the star. This is the temperature of a hypothetical black body, the spectrum of which would have the observed energy distribution of the star in question. It has often been emphasized that the effective temperature is merely a label, for it is not the actual temperature of any specific portion of the star. Presumably the temperature of a star falls off, from the center outwards, according to the laws expressed by the theory of radiative equilibrium, and though it might thus be possible to specify, on certain assumptions, the depth in a star at which the effective temperature coincides with the actual temperature, no observational significance could attach to the information.

The theory of radiative equilibrium[43] enables us to specify the temperature gradient, and in particular to determine the central temperature, the effective temperature, and the boundary temperature, corresponding to a given energy output. These three quantities are essentially arbitrary, and the second is the only one susceptible of direct measurement, while none of them represents the actual temperature of any assignable region. In order to clarify ideas it is useful to regard the effective temperature as representing roughly the temperature of the photosphere, that is, of the region in the star that gives rise to the approximately black continuous background of the spectrum. It must, however, be remembered that “the theory provides a definite relation between temperature and optical depth, involving only one constant, the effective temperature. Suppose now ... we arbitrarily select a certain temperature, and name it the photospheric temperature, and name the unknown depth at which it occurs the photospheric depth; this depth will be described by some unknown transmission coefficient, to be determined. If, taking account of absorption and emission, we proceed to calculate the transmission coefficient ... we shall simply recover the optical depth predicted by Schwarzschild’s theory.” (Milne.)[44] No method of measuring the effective temperatures of the stars by comparing their energy spectrum with that of a black body can remove the arbitrariness of the quantity thus measured.

The theory of thermal ionization permits estimates to be made of the temperatures in the reversing layers of stars. These temperatures refer to the average level at which are situated the absorbing atoms corresponding to the lines used. The differences of effective level[45] for different atoms render these “ionization temperatures” difficult to define consistently, but they represent actual temperatures of assignable regions in the star, and the extent of their agreement with the temperatures derived from the distribution of energy in the continuous spectrum is a matter of extreme interest. The material and theory from which the ionization temperatures are derived is the subject matter of Chapters VI to IX. The temperature scale used in calibration and in the discussion of the theory of thermal ionization is the scale derived from the measured effective temperatures.

The derivation of a definitive scale of effective temperatures from the numerous available observations is probably impossible at the present time. The methods employed differ widely, and the conditions for accurate intercomparison cannot be regarded as fully established. The material at present available, however, permits some general conclusions, and as the needs of astrophysics demand a working temperature scale, such conclusions are summarized in the present chapter.

In the discussion of the material a difficulty immediately arises. The scale to be derived must be based entirely, in the present stage of the observations, upon the apparently brighter stars, and it is notorious that they are not homogeneous in absolute magnitude. Theory predicts[46] that absolutely bright stars will have a lower effective temperature than stars of low luminosity belonging to the same spectral class, and this prediction is, on the whole, verified by observation. The material must therefore be selected on the basis of luminosity if a standard temperature scale is to be formed, and probably the temperature scale to be aimed at should refer to stars of some one absolute magnitude adopted as standard. Theoretically, standard mass might be preferable to standard luminosity, but, in the present state of the subject, so few masses are known that such a system would not be practicable. The ideal of referring to standard absolute magnitude was not attained by the earlier temperature scales, which were apparently based upon averages for all the available brighter stars.

The more comprehensive data for the study of the stellar temperature scale are the spectrophotometric measures of Wilsing and Scheiner,[47] of Wilsing,[48] of E. S. King,[49] and of Rosenberg.[50] The temperature scales derived by Wilsing and by Rosenberg differ by a linear factor; Rosenberg assigns higher temperatures to the hotter stars, and lower temperatures to the cooler stars. These temperature scales, and their intercomparison, have been very fully discussed by Brill,[51] who reduces all the measures to the scale given by Wilsing, and gives, for the principal Draper classes, the following comparative table for the corrected mean effective temperatures on the absolute centigrade scale.

In addition to the comprehensive data just quoted, there have been numerous determinations of the temperatures of individual bright stars, chiefly by Abbot,[52] Coblentz,[53] Sampson,[54] and H. H. Plaskett.[55] In the main these values confirm the scale given in Table V, but sometimes considerable differences occur in the values given for individual stars by different investigators. At the same time, each observer is usually reasonably self-consistent, and the deviations must therefore be ascribed to differences of method. Some of the results are reproduced, for illustration, in Table VI.

TABLE V

Class   Wilsing   Rosenberg E.S. King
Color Temperature  
E.S. King
Total Radiation
12300° 30000° 22700° 22700°
11450  18000  15200  14900 
10250   1200 11600  11300 
  9000   9000   8800   8600
  7950   7850   7900   7700
  6880   6930   7000   6800
  5980   6000   6040   5870
  5250   5200   5090   4950
  4570   4570   4570   4440
  3860   3840   3640   3550
  3550   3580   3430   3340

It is seen that the effective temperatures of individual hotter stars vary widely among themselves. This is largely a result of the difficulty of making the appropriate correction for atmospheric extinction. It must, then, be supposed that the temperatures derived by spectrophotometric methods are not trustworthy for stars hotter than Class . The values determined by the earlier observers for the and classes are almost certainly too low. Rosenberg’s value of 30,000° for is, however, most probably too high, as will be inferred later from the ionization temperature scale.

For the cooler stars small discrepancies also occur among the different observers. In the writer’s opinion, the lowest estimates for the temperatures of the cooler stars are probably nearest to the truth.

TABLE VI

Star Abott
Radiometric  
Coblentz
Thermoelectric
Plaskett
Wedge Method  
Sampson
Photoelectric
Ori() 13000° 25000°
Cas() 15000° 30000 
Per() 15000  14000
Ori() 16000° 10000  14800
Lyr() 14000   8000 11600
() 11000 12800
( Cyg()  9000  9000 10900
Aql()  8000
Cas()  9000 10700
()  6000  8300
Aur()  5800  6000 5500-6000   5500 *
()  4000  4200
Gem()  5500 5000-5500  4200
Tau()  3000  3500  3400
Ori()  2600  3000  3400
Peg()  2850  3200

* Temperature assumed in calibration of scale.

It was mentioned at the outset that dwarf stars appear to be at a higher temperature than giants of the same spectral class. The following table summarizes the differences in temperature, as compiled by Seares.[56]

TABLE VII

Class    Effective Temperature
Giant Dwarf
6080° 6080°
5300  5770 
4610  5500 
3860  4880 
3270  4120 
3080  3330 

A more detailed list of giant and dwarf temperatures was compiled in 1922 by Hertzsprung[57] from all the material then available. The tabulation that follows contains his values for (the “reciprocal temperature,” where is 14,600), and the corresponding absolute temperature, in degrees centigrade.

TABLE VIII

Mt. W. Class Giant Dwarf Temperature
Giant
Temperature
Dwarf
2.00 7300°
2.16 6770 
2.08 6990 
2.26 6460 
2.30 6350 
2.11 6920 
2.30 6350 
2.29 6370 
2.34 6240 
2.36 6190 
2.48 5880 
2.30 2.51 6340° 5810 
2.45 5970 
2.71 5100 
2.83 2.62 5170  5580 
2.92 2.68 5020  5440 
2.92 2.64 5020  5530 
3.15 4730 
3.09 4820 
3.15 4730 
3.25 2.76 4480  5300 
3.20 4560 
3.29 4430 
3.39 3.03 4300  4840 
3.48 3.11 4180  4700 
3.50 3.05 4160  4790 
3.54 4130 
3.83 3810 
3.86 3870 
4.14 3530 
4.33 3370 
4.36 3350 
4.35 3360 
4.49 3250 
4.45 3280 
3.93 3720 

The difference in temperature between giant and dwarf stars of the same spectral class is clearly shown in the foregoing tables. The relation of absolute magnitude to effective temperature within a given class must be regarded as definitely established by observation.

The temperatures for the cooler giant stars in both these lists are somewhat lower than those given for the corresponding classes in Table V. The temperature of , for instance, is placed nearer to 4000° than to 4500°. The fact that the sun, a typical dwarf, has an effective temperature of 5600° seems to favor these lower values.

TABLE IX

Class Temperature Class Temperature
3000° 9000°
3000  10000  
3500  13500  
4000  15000  
5000  17000  
5600  18000  
7000  20000  
7500  25000  
8400  35000  

In concluding the summary of stellar temperatures, the ionization temperature scale is given in the foregoing table. The discussion on which the table is based is contained in Chapters VI to IX, and it is merely placed here for comparison with the preceding tabulations.

FOOTNOTES:

[43] Eddington, Zeit. f. Phys., 7, 351, 1921.

[44] Phil. Trans., 223A, 201, 1922.

[45] Chapter IX, p. 136.

[46] Chapter XIV, p. 195.

[47] Wilsing and Scheiner, Pots. Pub., 24, No. 74, 1919.

[48] Pots. Pub., 24, No. 76, 1920.

[49] H. A., 76, 107, 1916.

[50] A.N., 193, 356, 1912.

[51] A. N., 218, 210, 1923; ibid., 219, 22 and 354, 1923; Die Strahlung der Sterne, Berlin, 1924.

[52] Rep., Smithsonian Ap. Obs., 1924.

[53] Pop. Ast., 21, 105, 1923.

[54] M. N. R. A. S., 85, 212, 1925.

[55] Pub. Dom. Ap. Obs., 2, 12, 1923.

[56] Ap. J., 55, 202, 1922.

[57] Lei. An., 14, 1, 1922.