Abstract
The reflecting and absorbing powers, and hence dispersion, of H2SO4 solutions were determined as a function of concentration and of wave‐length between 50μ and 150μ. Pure H2SO4 reflects and absorbs the far infrared less than water as is to be expected from the Debye theory on dipole orientation. A broad band around 60μ, similar to the 60μ band in water, was observed in both concentrated and dilute H2SO4. This band appears to be of interatomic origin and possibly a fundamental vibration frequency of the sulphate radical, SO4, due to bending. The reflecting and absorbing powers of H2SO4 solutions are much greater than of pure H2O or H2SO4. This is accounted for by the presence of ions which move in translation to follow the alternations of the electromagnetic waves in the far infrared. The structure of these ions is discussed in reference to other physical properties observed in H2SO4 solutions. It is suggested that in adding less than 5 percent water to H2SO4 possibly ions of SO4‐‐ and OH4++ might be formed; on further dilution, ions of H and H3SO5 are formed (hydrated HSO4, with the water making stable six‐ring of S–O–H–O–H–O–S); on still further dilution, ions of H+ and SO4‐‐ become most abundant.

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