The fate of neptunium in the aquatic environment is dependent upon, am
ongst other processes, the extent of uptake by particulate material. I
n oxic natural waters it exists predominantly in the V-valent state. A
number of laboratory experiments have been carried out, using Np-239
tracer, particulate material prepared from Irish Sea sediment and vari
ous synthetic solutions, to determine the influence of chemical parame
ters on the sorption behaviour of Np(V) in marine waters. The data sug
gest that uptake is highly dependent upon solution pH both as a result
of changes in charge on particle surfaces and, at high pH values (>9.
0), from the formation of hydrolysis species. Np(V) uptake by marine p
articulate material was essentially independent of ionic strength with
in the pH range of natural seawater. The presence of Mg2+, Ca2+ and HC
O3- ions was found to inhibit Np(V) sorption; removal of Np(V) was, ho
wever, increased from solutions which were supersaturated with respect
to CaCO3. The data indicate that, although Np(V) sorption in seawater
is controlled by interactions between Mg2+, Ca2+ and HCO3- ions, the
effect of the combined presence of all three constituents is more comp
lex than might be expected from the action of individual components.