Formation mechanism of an Al13 Keggin cluster in hydrated layered polysilicates

An Al13 ϵ-Keggin cluster, AlO4Al12(OH)24(H2O)127+, is a predominant intermediate during the hydrolysis and polymerization of aluminum as well as a highly toxic substance to plants and fishes. However, no one could clearly explain why and how a cage-like Al13 ϵ-Keggin cluster is formed even though it...

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Published inDalton transactions : an international journal of inorganic chemistry Vol. 49; no. 15; pp. 4920 - 4926
Main Authors Park, Man, Yun-Ju, Kang, Jeong-Hun Jang, Jae-Deok Seo, Kim, Junhyung, Seung-Min Paek, Woo-Taik Lim, Komarneni, Sridhar
Format Journal Article
LanguageEnglish
Published Cambridge Royal Society of Chemistry 21.04.2020
Subjects
Aluminum
Cation exchanging
Clusters
Hydrolysis
Inhomogeneity
Morphology
NMR
Nuclear magnetic resonance
Sediments
Trimers
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Summary:An Al13 ϵ-Keggin cluster, AlO4Al12(OH)24(H2O)127+, is a predominant intermediate during the hydrolysis and polymerization of aluminum as well as a highly toxic substance to plants and fishes. However, no one could clearly explain why and how a cage-like Al13 ϵ-Keggin cluster is formed even though it could be readily synthesized by the forced hydrolysis of Al3+. We found that the Al13 ϵ-Keggin cluster was spontaneously formed not in monocrystalline octosilicate but in polycrystalline magadiite by the cation-exchange reaction with unhydrolyzed Al3+. Furthermore, the Al13 ϵ-Keggin cluster was hardly detected in disaggregated magadiite crystals whose morphology was changed into monocrystalline crystals like octosilicate. Our findings prove that Al13 formation is necessary to relieve localized inhomogeneity and rationalize that Al13 is formed by the simultaneous co-assembly of four planar trimers and one octahedral monomer. In addition, the spontaneous formation of Al13 in heterogeneous systems could be a vital clue to its evaluation in soils and sediments.
ISSN:1477-9226
1477-9234
DOI:10.1039/d0dt00529k