At Ranger uranium mine it was proposed to calcine local magnesite and
use it instead of imported lime to neutralize tailings. A pilot-scale
study comparing a bed of tailings neutralized in this way with one neu
tralized with lime showed that magnesite settled less and consolidated
more slowly, resulting in an increased short-term storage requirement
. To find out why, the relative humidities of solutions of calcium and
magnesium sulphates and of samples from the beds dried to known water
contents were determined. Other samples were dried intermittently in
linear shrinkage moulds under a constant, low evaporative demand. Prec
ipitation of magnesium sulphate eventually caused a skin to form on ma
gnesite, greatly reducing the rate of drying. To explain the shrinkage
patterns and low bulk densities of the slurries after oven-drying, it
is suggested that the clay-sized particles present form a framework i
n which the larger particles are held. It is deduced that the earlier
results were due to the smaller clay content of lime and the lower rel
ative humidity of magnesite at a given water content. With a large eva
porative demand, a skin could increase the long-term drying rate of st
ored tailings.