Host phases of fallout Pu-239,Pu-240 and Am-241 were studied in the surface
sediments obtained in 1994 from abyssal basins of relatively small area of
the western North Pacific. An analytical procedure involving sequential ch
emical extraction was employed for partitioning the host phases of the nucl
ides in sediment into five fractions: (1) exchangeable, (2) bound to carbon
ate, (3) bound to hydrous Fe-Mn oxides, (4) bound to organic matter and (5)
residual. Decrease of total Pu-239,Pu-240 concentration with decreasing as
sociation of Pu-239,Pu-240 with organic matter, high Am-241/Pu-239,Pu-240 a
ctivity ratio in carbonate phase and somewhat high proportion of oxidized P
u-239,Pu-240 in leachable phases suggest a possibility of post-depositional
diagenetic remobilization of Pu from sediment to water column.