| Element | Ionization Potential | Authority |
|---|---|---|
| C++ | 45 | Payne |
| N+ | 24 | Ibid. |
| N++ | 45? | Ibid. |
| O+ | 32 | Ibid. |
| O++ | 45 | Fowler and Milne |
| Si | 8.5 | Menzel, Payne |
| S+ | 20 | Payne |
| S++ | 32 | Ibid. |
| Sc+ | 12.5 | Menzel |
| Ti+ | 12.5 | Ibid. |
| Fe | 7.5 | Ibid. |
| Fe+ | 13 | Ibid. |
The value of
is dependent on the effective level, and hence upon the excitation potential. Without the introduction of unjustified assumptions, more than one critical potential cannot be deduced from observations of intensity maximum. The excitation potential corresponding to a line could be roughly inferred from the observed maximum, by observing the shift of predicted maximum produced by the level effect (discussed in [Chapter IX]) if the ionization potential were known. There are, however, no data as yet that could be used in drawing inferences of this kind.
DURATION OF ATOMIC STATES
The successful application of theory to the astrophysical determination of the life of an atom requires the fulfilment of special conditions. The requirements of the idea developed by Milne[434] demand that the atom shall exist in appreciable quantities in only two states simultaneously. This condition is fulfilled by the ionized atoms of the alkaline earth elements, and it is with calcium that the estimates here discussed are concerned.
The investigation relates to the calcium present in the high-level chromosphere, where, owing to remoteness from the photosphere, thermal ionization is negligible. Photoelectric ionization may be operative in removing the first electron from the calcium atom, but the sun is too deficient in light of wave-length 1040 for second stage photoelectric ionization to be appreciable. The calcium present in the high-level chromosphere is probably largely in the once ionized condition, since an atom once ionized is likely to remain so for a long time, owing to the scarcity of free electrons in the tenuous outer regions of the sun. The present investigation neglects altogether the neutral and doubly ionized calcium atoms, and furthermore assumes that the transfers corresponding to the
and
