Relationship between topological order and glass forming ability in densely packed enstatite and forsterite composition glasses.

ABSTRACT: The atomic structures of magnesium silicate melts are key to understanding processes related to the evolution of the Earth's mantle and represent precursors to the formation of most igneous rocks. Magnesium silicate compositions also represent a major component of many glass ceramics, and depending on their composition can span the entire fragility range of glass formation. The silica rich enstatite (MgSiO(3)) composition is a good glass former, whereas the forsterite (Mg(2)SiO(4)) composition is at the limit of glass formation. Here, the structure of MgSiO(3) and Mg(2)SiO(4) composition glasses obtained from levitated liquids have been modeled using Reverse Monte Carlo fits to diffraction data and by density functional theory. A ring statistics analysis suggests that the lower glass formi

SUBMITTER: Kohara S 

PROVIDER: S-EPMC3169147 | biostudies-literature | 2011 Sep

REPOSITORIES: biostudies-literature