“…where C is the maximum initial variation in C, L is the effective diffusion distance between the two phases, D is the temperature-dependent diffusion coefficient and t is the homogenisation time (Carruthers, 1977). Application of the equation to At-Sh melts (Ang and Lacy 1979), which represent the class of liquids under consideration, shows that even when the compositional fluctua.tion yields a pure phase, a soaking period of 15 rain should homogenise the melt at temperatures where D =I x 10-Sere z sec-L In practice, however, even holding for as long as 4 hr is insufficient to bring about uniformity in composition. Ang and Lacy (1979) have developed an elegant analysis in which a parameter H defined by…”