In batch equilibrium experiments, it was found that orthophosphate inc
reased Cd adsorption and decreased its desorption by three representat
ive soils. Ion activity products in the equilibrium solution indicated
that cadmium activity was under saturated with respect to Cd-3(PO4) (
a) on the Red earth(Typic Hapludult) and the Yellow-brown earth(Typic
Hapludalf). With the calcareous Yellow fluvo-aquic soil(Typic Haplaque
nt), phosphate enhanced Cd adsorption at lower Cd concentration but it
decreased the adsorption at high Cd level. Ion activity products and
solubility diagrams suggested that at high Cd level Cd-3(PO4)(2) had f
ormed and the activity of Cd in solution was controlled by this precip
itate. This implies that the formation of Cd-3(PO4)(2) (s) is unable t
o decrease Cd activity so long as soil adsorption sites are unsaturate
d by Cd. It is suggested from these results that one could not expect
decreasing soil Cd availability by phosphate fertilization unless a si
multaneous rise in soil pH also occurs.