Energetic Insight into the Formation of Solids from Aluminum Polyoxocations

The ε‐Keggin [AlO 4 Al 12 (OH) 24 (H 2 O) 12 ] 7+ ion (AlAl 12 7+ ) is a metastable precursor in the formation of aluminum oxyhydroxide solids. It also serves as a useful model for the chemistry of aluminous mineral surfaces. Herein we calculate the enthalpies of formation for this aqueous ion and its heterometal‐substituted forms, GaAl 12 7+ and GeAl 12 8+ , using solution calorimetry. Rather than measuring the enthalpies of the MAl 12 7/8+ ions directly from solution hydrolysis, we measured the metathesis reaction of the crystallized forms with barium chloride creating an aqueous aluminum solution monospecific in MAl 12 7/8+ . Then, the contributions to the heat of formation from the crystallized forms were subtracted using referenced states. When comparing the aqueous AlAl 12 7+ ion to solid aluminum (oxy)‐hydroxide phases, we found that this ion lies closer in energy to solid phases than to aqueous aluminum monomers, thus explaining its role as a precursor to amorphous aluminum hydroxide phases.