The microstructure, phase content, and thermal conductivity of salvaged con
ventional silica bricks from float glass and TV-panel glass production furn
aces were examined as a function of position through the brick, and compare
d with the original, unaltered brick materials. The silica brick from the f
loat glass furnace was in service for approximately 10 years while that for
the TV-panel glass furnace was for approximately 6 1/2 years. The microstr
ucture and phase content in both salvaged bricks showed gradients, from tri
dymite at the bricks' cold-face ends, to cristobalite at their hot-face end
even though both bricks were an initial mixture of tridymite and cristobal
ite to begin with. The thermal conductivity of both bricks had increased as
a consequence of these phase and microstructural changes. A thermal analys
is model predicted that such changes would result in an increase in the bri
cks' cold-face temperature and heat content during service. The initially-p
roduced temperature gradients and environment caused microstructural change
s in the silica brick; however, the cause-and-effect relationship between t
emperature/environment and microstructural changes in the brick likely beca
me mutually reversible once the microstructural changes initiated and the t
hermal conductivity of the brick started to change as a consequence.