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  • Access by Xinjiang University

Ionospheric Absorption by N2 and O2 of Certain Extreme Ultraviolet Solar Wavelengths

K. C. Clark

  • University of Washington, Seattle, Washington

Phys. Rev. 87, 271 – Published 15 July, 1952

DOI: https://doi.org/10.1103/PhysRev.87.271

Abstract

Measurements are reported of the coefficients of absorption by the gases N2 and O2 of the emission from the H Lyman series 2-7, the resonance line 584A of He I, and twenty lines of H2 between 980A and 850A, the atomic lines likely being strong in solar radiation. For an atmosphere of constant relative composition the absorption coefficients are related to the atmospheric heights of maximum photoionization and maximum electron concentration by equations which allow for a constant temperature gradient, the inverse square decrease of gravity, and a recombination process which may vary with height. With these laboratory measurements for N2 and O2 and the known calculated absorption for O, ionosphere layer heights are computed for the simple case which assumes complete O2 dissociation above 100 km, no N2 dissociation, and two-body recombination. Although only the first assumption is probably secure, it appears that photoionization is capable of producing layers at heights which agree with observation.

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