The adsorption of sulfate at different pH in the presence of different
concentrations of sodium perchlorate, sodium nitrate or sodium chlori
de by two variable charge soils with contrasting surface charge proper
ties was studied. The adsorption decreased with the increase in pH. Fo
r the Ferralsol carrying net positive surface charge at natural pH inc
reasing the concentration of NaClO4 or NaNO3 resulted in a decrease in
sulfate adsorption at low pH and an increase in sulfate adsorption at
high pH. There was an intermediate pH al which the salt concentration
had no effect on adsorption. This point of zero salt effect (PZSE) on
adsorption for NaClO4 and NaNO3 was 5.5 and 5.8, respectively. In the
presence of NaCl the adsorption-pH curves converged at pH 7 at which
the soil practically did not adsorb sulfate, For the Ferric luvisol wi
th a net negative surface charge at natural pH a PZSE on adsorption oc
curred at pH 5.7 only in the presence of NaClO4. The adsorption-pH cur
ves converged at pH 6.4 in the presence of NaNO3 and were nearly paral
lel to one another in the presence of NaCl. These results were explain
ed by the combined effect of competitive adsorption and the change in
electrical potential at the adsorption plane, It was suggested that th
e more abundant the positive surface charge relative to negative surfa
ce charge of a soil at natural pH, the more likely the occurrence of a
point of zero salt effect on sulfate adsorption, and that chloride io
ns were more effective in inducing the increases in negative surface c
harge and surface potential of soils than nitrate and perchlorate ions
.