Wastes that can be treated by supercritical water oxidation often contain s
alts. Salts are almost insoluble under supercritical conditions and can res
ult in severe fouling. A simple heat- and mass-transfer model was developed
and tested experimentally for sodium sulfate in a fully turbulent flow of
ater at 25 MPa. This model uses empirical heat-transfer correlations to est
imate mass-transfer rates. The diffusion coefficient of the salt is calcula
ted from the Stokes-Einstein relation using a hydrodynamic diameter of 2 to
6 Angstrom. New measurements to solubility showed that the solubility of s
odium sulfate decreases by a factor of about 1,000 as the temperature incre
ases from 380 degrees C to 400 degrees C. Salt deposition rates, inferred f
rom the outside temperature of a heated test section, were reasonably close
to the model predictions.