The beneficial effect of jarosite seed on the rate of precipitation of
ammonium jarosite and sodium jarosite was confirmed, and it was shown
that the initial rate of precipitation increases linearly with the am
ount of seed present. A minimum degree of agitation is necessary to su
spend the seed, but higher agitation rates are without further effect.
Furthermore, the presence of seed extends the range of jarosite preci
pitation to lower pH values and to lower temperatures than is the situ
ation in the absence of seed. The presence of seed accelerates the ini
tial precipitation rate at all pH values and temperatures and generall
y eliminates any induction period. The activation energy for sodium ja
rosite precipitation in the presence of seed is 106 kJ/mol. In the pre
sence of sodium jarosite seed, the rate of sodium jarosite precipitati
on is nearly independent of ferric ion concentrations > 0.03 M Fe3+ wh
en the rate is expressed as a percentage of the initial Fe3+ concentra
tion. A more pronounced ferric ion concentration dependence is noted i
n the absence of seed. Increasing Na2SO4 concentrations cause the rate
of sodium jarosite precipitation, in the presence or absence of seed,
to increase to similar to 0.2 M Na2SO4 but to decrease at higher Na2S
O4 concentrations. This dependence seems to be related mostly to the c
hanging sodium ion concentration, as the rate is nearly independent of
ZnSO4 concentrations up to 2.0 M in the presence or absence of seed.