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Absolute Structures of a Mirror Pair of Infinite Na(H2O)4+‑Connected ε‑Keggin–Al13 Species

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posted on 2024-04-25, 21:13 authored by Hui Wang, Jin-Liang Gu, Yu-Wei Guo, Yu Ma, Ning-Ning Yu, Zhong Sun
The absolute structures of a pair of infinite Na­(H2O)4+-connected ε-Keggin–Al13 species (Na−ε-K–Al13) that were inversion structures and mirror images of each other were determined. Single crystals obtained by adding A2SO4 (A = Li, Na, K, Rb, or Cs) solution to NaOH-hydrolyzed AlCl3 solution were subjected to X-ray structure analyses. The statistical results for 36 single crystals showed that all the crystals had almost the same unit cell parameter, belonged to the same F4̅3m space group, and possessed the same structural formula [Na­(H2O)4AlO4Al12(OH)24(H2O)12]­(SO4)4·10H2O. However, the crystals had two inverse absolute structures (denoted A and B), which had a crystallization ratio of 1:1. From Li+ to Cs+, with increasing volume of the cation coexisting in the mother solution, the degree of disorder of the four H2O molecules in the Na­(H2O)4+ hydrated ion continuously decreased; they became ordered when the cation was Cs+. Absolute structures A and B are the first two infinite aluminum polycations connected by statistically occupied [(Na1/4)4(H2O)4]+ hydrated ions. The three-dimensional structure of the infinite Na−ε-K–Al13 species can be regarded as the assembly of finite ε-K–Al13 species linked by [(Na1/4)4(H2O)4]+ in a 1:1 ratio. In this assembly, each [(Na1/4)4(H2O)4]+ is connected to four ε-K–Al13 and each ε-K–Al13 is also connected to four [(Na1/4)4(H2O)4]+ in tetrahedral orientations to form a continuous rigid framework structure, which has an inverse spatial orientation between absolute structure A and B. This discovery clarifies that the ε-K–Al13 (or ε-K–GaAl12) species in Na­[MO4Al12(OH)24(H2O)12]­(XO4)4·nH2O (M = Al, Ga; X = S, Se; n = 10–20) exists as discrete groups and deepens understanding of the formation and evolution process of polyaluminum species in forcibly hydrolyzed aluminum salt solution. The reason why Na+ statistically occupies the four sites was examined, and a formation and evolution mechanism of the infinite Na−ε-K–Al13 species was proposed.

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