The viscosities of nine coal ash slags were measured in air as a function of temperature. Selected
slags were also tested in reducing atmosphere and in air with 10% water vapor. In air, the
viscosities of the slags can be related to the mole ratio of basic to acidic oxides. An improved fit
is obtained from the ratio of oxide ions contributing to the bases to the oxide contributing to the
acids. The change in viscosity observed in using hydrogen instead of air appears to be related to
the amount of iron originally in the slag. When water vapor is present in air, the viscosity of a
high-silica glassy slag decreased. The viscosities of three other slags, with lower silica content,
increased slightly, with the increase in potassium content. In the former case, water likely enters
the slag and disrupts Si−O−Si bridges. In the latter case, water may form metal−hydroxide
complexes with the alkali cations such as potassium. A second effect of water vapor is to reduce
the temperature at which the slag begins to crystallize (the temperature of critical viscosity).
These effects of water on coal ash slag viscosity are similar to those on magmas, even if with
lower magnitude.