In connection with recent measurements of the dispersion of oxygen down to 1920A, the continuous absorption of oxygen between 1750 and 1300A has been investigated quantitatively with a small fluorite spectrograph by the photographic-photometric method. The results are given in a graph, which shows that the absorption co-efficient α as function of the wave number ν has a relatively sharp maximum at 6.8×{}10⁴ cm^-1 (λ=1450A) and falls off rather symmetrically on both sides. The maximum absorption coefficient reduced to N.P.T. is about 490 cm^-1. The absorption in this region of the spectrum is so strong that during a few minutes exposure a great part of the oxygen disappears, being dissociated and probably absorbed by the metal walls of the tube. By integration of the absorption curve one gets the corresponding f-value according to the equation ∫α(ν)dν=πNfe²mc²=(2.38×10⁷)f. The f-value calculated from this expression is 0.193 compared with 0.202 calculated from the dispersion measurements. The corresponding resonance wave-length from the dispersion measurements is 1468 in fairly good agreement with the observed position of the maximum of absorption. A dispersion formula which takes into account the distribution of absorption in a continuous band is given, and is applied to the dispersion of oxygen.
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Ladenburg et al. (1933) studied this question.
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