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This article examines the comparison between the classical formulations used to describe silicates and that derived from the application of the extended Zintl–Klemm concept (EZKC). The ionic strength, I, for 25 silicate lattices is calculated taking into account both formulations, and the results show that, in every single one of the examples, the ionic strength of the Zintl polyanion is higher than that of the classical model which assigns a formal charge of 4+ for silicon. Our earlier study, firstly applied to the germanate (NH4)2Ge[6][Ge[4]6O15] [Vegas & Jenkins (2017). Acta Cryst. B73, 94–100] and to the polyanion [Ge[4]6O15]6− equivalent to the pseudo-As2O5 derived from it, explained satisfactorily the charge transfer that takes place in the Zintl compounds. The value of I = ½∑nizi2 for the Zintl polyanion was greater than for the compound as formulated in the classical way. In that article, a meaningful relationship was found between the electron transfers as defined by the EZKC and the ionic strength I of the anion [Ge[4]6O15]6− ≡ Ψ-As2O5. Because the ionic strength, I, of a lattice is directly proportional to the lattice potential energy, UPOT, the higher the I the greater the UPOT; thus it is harder to break up the lattice into its constituent ions and hence the lattice itself is more stable, giving support to the idea that the application of the EZKC and the resulting electron shifts yields structures which are inherently thermodynamically more stable than the starting configuration.

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