Abstract
Variations in the absorption characteristics of periodate solutions with pH and temperature have been used to better determine the species present in dilute aqueous solutions. The species H5IO6, H4IO6−, IO4− and H3IO6− and their equilibria were sufficient to completely explain the spectrophotometric and potentiometric data of periodate solutions in pH ranges 0-7 and temperature ranges 0-70°. Apparent and true constants for these ionization and hydration equilibria have been evaluated at 25° as αH+(αH4IO6−)/αH5IO6 = K1 = 5.1 × 10−4 αH+(αH3IO6−)/αH4IO6− = K2 = 2.0 × 10−7 (αIO4−/(αH4IO6−) α2H2O = KD = 40 [αH+(αIO4− + αH4IO6−)]/αH5IO6 = K1´ = 2.3 × 10−2 αH+(αH3IO6−)/(αIO4−+ (αH4IO6−) = K2´ = 4.35 × 10−9. © 1951, American Chemical Society. All rights reserved.
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CITATION STYLE
Crouthamel, C. E., Hayes, A. M., & Martin, D. S. (1951). Ionization and Hydration Equilibria of Periodic Acid. Journal of the American Chemical Society, 73(1), 82–87. https://doi.org/10.1021/ja01145a030
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