Sodium
phosphosilicate glasses with high phosphate contents represent
an unusual case in glass science as they are known to contain large
amounts of six-coordinated silicon species (SiO6/2 units,
Si(6)). Although the network connectivity of these units
has been previously investigated, the overall structural organization
of this system at the medium-range order level is still incompletely
understood. In the present study, this issue is addressed by using
a comprehensive suite of homo- and heteronuclear dipolar recoupling
studies involving the nuclear isotopes 23Na, 29Si, and 31P on isotopically enriched glasses in the systems xSiO2–(1 – x)(0.45Na2O–0.55P2O5) (x = 0.0, 0.1, and 0.2) and 0.2SiO2–0.2Na2O–0.6P2O5. Four- and six-fold coordinated
silicon species (Si(4) and Si(6)) coexist in
these glasses. Invariably, Si(6) selectively connects with
phosphate species, which are exclusively of the P(3) type,
whereas the Si(4) species are coordinated to both P(2) and P(3) units. 29Si ↔ 23Na and 31P ↔ 23Na rotational
echo double resonance experiments indicate much closer sodium/phosphorus
than sodium/silicon proximities. Evidently, the bond valence gradient
of the Si(6)–O–P(3) linkages redistributes
the anionic charge onto the phosphate nonbridging oxygen species,
which attract Na+ cations. The Si(6)(P(3))6Na2 superstructural units (stoichiometry
Na2SiP6O18) thus formed represent
an exceptionally high degree of medium-range order, accounting for
high thermal and mechanical stability of these glasses. The Na+ ions neutralize the negative charge located at nonbridging
oxygen atoms of P(3) tetrahedra, whereas the bridging oxygen
atoms in the Si(6)–O–P bonds are electrically
neutral. Finally, we show that the structural speciations of silicon
and phosphorus in SiO2–Na2O–P2O5 glasses can be predicted straightforwardly from
the elemental glass compositions in excellent agreement with experimental
results.