The viscous flow of inorganic glasses is considered from the point of view of valence theory and free-volume theory. It is shown that the "hole formation" corresponds to local fluctuation deformation of the glass network and the "transition of a particle into a micro-cavity," to the switching of the bridging atoms. A possible refinement of the valence theory of flow is discussed; this is based on the assumption that in silicate glasses there are oxygen atoms with vacant bonds.
Origin
Unknown
Journal Title
The Soviet Journal Of Glass Physics And Chemistry 1976 2 (6) 498-502
Sector
Primary Papers
Class
PP 597