A sequential extraction method consisting of six operationally-defined frac
tions was used to determine the geochemical partitioning of natural (U, Th,
) and antropogenic (Pu, Am,Cs-137) radionuclides in three sediment samples
of different origin (Venice Lagoon, Adriatic Sea; Gaeta Gulf, Thyrrhenian S
ea; IAEA-367, Enewetak Atoll, Central Pacific Ocean). Fe, Mn, Al, Ti, Ca, S
r, Pb, Ba, K were also determined in the different fractions to get more in
formation about the chemical association of the single radionuclides. The e
xperimental results were compared to those described in the literature for
an IAEA-135 Sea Sediment collected in the Irish Sea in front of the Sellafi
eld Plant (UK).