Electrochemical analysis revealed acidity scales in sulfuric acid differ by 12 orders, indicating flaws in current definitions of acidity function.
We report on the considerable difference between the distinct pH and Hammett's H 0 acidity function in the entire H 2 O‐H 2 SO 4 mixing range. The Hammett acidity for 100 wt% H 2 SO 4 is accepted with H 0 = −11.9. We measured the pH acidity using two different electrochemical cells, operating with at least one hydrogen electrode, giving for 100% sulfuric acid as −24 ± 2. This value was confirmed by high‐level compound calculations using the DLPNO‐CCSD(T) level at the basis set limit and COSMO‐RS solvation. Thus, the difference between both scales amounts to − H 0 = −12 or 12 orders of magnitude. It results from the Gibbs transfer energies of the (protonated) Hammett‐indicator bases B (BH + ) used to define and determine H 0 . High‐level computations of these Gibbs transfer energies confirm our experimental as well as our computational findings. A general method to convert H 0 values of acids other than sulfuric acid into values is given. Hence, this huge (pH − H 0 )‐difference clearly delineates that the often used but erroneous assumption of the H 0 values constituting an extension of pH acidity to the realm of negative pH values is wrong. The distinctive protochemical potential curve progression is discussed as a function of sulfuric acid concentration and physical properties, together with the assignment of the potential‐determining species in the respective mixtures. Finally, superacidity is defined in a universal manner, i.e., applicable to all media, i.e., liquid, solid, or gaseous.
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Radtke et al. (2025) studied this question.
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