Structure and dissolution of silicophosphate glass

P(2)O(5)–SiO(2)–Na(2)O–CaO glasses are promising therapeutic ion-releasing materials. Herein, we investigated the state of silicon (Si) in P(2)O(5)–SiO(2)–Na(2)O–CaO glass using a model with a composition of 55.0P(2)O(5)–21.3SiO(2)–23.7Na(2)O (mol%), incorporating a six-fold-coordinated silicon structure (([6])Si). The model was constructed using a classical molecular dynamics method and relaxed using the first-principles method. Further, we experimentally prepared glasses, substituting Na(2)O for CaO, to investigate the dissolution of glass with varying ([6])Si and PO(4) tetrahedra (Q(P)(n)) distributions (n = number of bridging oxygens (BOs) to neighboring tetrahedra). ([6])Si in the glass model preferentially coordinated with Q(P)(3). When Si was surrounded by phosphate groups, phosphorus (P) induced the formation of ([6])Si by elongating the Si–O distance, and ([6])Si acted like a glass network former (NWF). Na(+) coordinated with ([6])Si–O–P bonds via electrostatic interactions with BO. (31)P and (29)Si magic-angle-spinning-nuclear-magnetic-resonance spectra of three experimental glass samples with the compositions of 55.0P(2)O(5)–21.3SiO(2)–xCaO–(23.7 − x)Na(2)O (mol%, x = 0, 12.4, and 23.7) showed that Q(P)(3) and ([6])Si increased with increasing Na(2)O. When each glass powder was immersed in a tris-HCl buffer solution at 37 °C, the dissolution of NWF ions and network modifier (NWM) ions increased almost monotonically with time for all samples, indicating that the solubility of the samples was suppressed by the coexistence of CaO and Na(2)O, attributed to the delocalization of the electron distribution of P in the ([6])Si-coordinated Q(P)(3) units compared to that in the P- or ([4])Si-coordinated Q(P)(3) units, which reduces hydrolysis.