Several sampling campaigns were carried out in the Seine estuary in or
der to study the behaviour of plutonium isotopes Versus salinity (Pu-2
38 and Pu-239,Pu-240), in 0.45 mu m filtered waters. During estuarine
mixing, the plutonium has a non-conservative behaviour: plots of Pu ac
tivities versus salinity display an excess of dissolved Pu-238 (RI = P
u-238/Pu-239,Pu-240 > 1) in low salinity waters (0.5 and 1.5 g l(-1))
and a depletion (RI < 1) in the zone of intermediate salinities (8 to
15 g l(-1)), with respect to conservative dilution. Laboratory experim
ents showed that Pu(V) present in seawater is reduced to the III, IV s
tates and sorbed onto particles with a maximum in low salinity waters
which could explain the depletion observed at intermediate salinity in
the Seine estuary. Reduction occurs prior to sorption and is connecte
d with the Seine river colloidal and dissolved species (humic acids).
The Pu associated with estuarine sediments desorbs from the ''oxide-hy
droxide'' fraction in contact with river water, thus partly explains t
he plutonium excess measured in low salinity filtered waters of the Se
ine.