“…[13][14][15][16][17][18][19][20] With capturing of the Keggin-Fe 13 clusters in water, [14,15,20,21] especiallyt he experimental evidence of Keggin-Fe 13 clusters as precursor of the ferrihydrite formation,t he nonclassic growth mode has been widely adopted in the literature. [13,14,[16][17][18][19][20][21] Althought he single phase modelo ft he ferrihydrite [13] clearly demonstrates that ferrihydrite consistso fd-Fe 13 Kegginu nits, it remains unclear why the Keggin-Fe 13 cluster can undergo rotational isomerization ( Figure 1). [14,20] In an effort to answer this question,N yman andc o-workers, [14] based on the comparison of the pair distance distribution function of Bi 6 Fe 13 L 12 dissolved in ethanolw ith that of two simulated dimers (the dimer of dodecaniobate a-Keggin ions linked by as ingle alkali, [22] and the dimer derived from the ferrihydrites tructure), deduced that the conversion of Keggin-Fe 13 clusters to ferrihydrite probablyi nvolvesl acunary Keggin-Fe 13 clusters.…”