Abstract
The domain structural transition and structural heterogeneity (SH) in GeO(2) glass at 300 K and pressures up to 100 GPa are studied by means of molecular dynamics (MD) simulation. The results demonstrate that the structure of GeO(2) glass comprises domain D4, domain D5, or domain D6, which depends strongly on pressure, where domain Dx (x = 4, 5, or 6) is a cluster of connected GeO (x) units, in which all Ge atoms possess the same coordination number of x. In the range of 9-18 GPa, GeO(2) glass undergoes a structural transformation from domain D4 to domain D6 via domain D5. Under densification, structural evolution occurs along with the O (xx) → O (xy) atom variation, which comprises the processes of both merging and splitting of domain Dx and the exchange of domain-boundary (DB) atoms. The densification leads to a decrease of the Voronoi polygon (VP) volume of atoms. We found that the coexistence of separate domain structures is the origin of spatial SH in GeO(2) glass. Pressure-dependent structural heterogeneity in GeO(2) glass is also discussed in detail.