Percolative conductivity in alkaline earth silicate melts and glasses

Abstract

Ion conducting (CaO)x(SiO2)1-x glasses and melts show a threshold behaviour in dc conductivity near x=xt=0.50, with conductivities increasing linearly at x>xt. We show that the behaviour can be traced to a rigid (x<0.50) to floppy (x>0.50) elastic phase transition near x=xt. In the floppy phase, conductivity enhancement is traced to increased mobility or diffusion of Ca2+ carriers as the modified network elastically softens.

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