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- W2076775326 abstract "Anthropogenic radionuclides in seawater have been used as transient tracers of processes in the marine environment. Especially, plutonium in seawater is considered to be a valuable tracer of biogeochemical processes due to its particle-reactive properties. However, its behavior in the ocean is also affected by physical processes such as advection, mixing and diffusion. Here we introduce Pu/(137)Cs ratio as a proxy of biogeochemical processes and discuss its trends in the water column of the North Pacific Ocean. We observed that the (239,240)Pu/(137)Cs ratio in seawater exponentially increased with increasing depth (depth range: 100-1000 m). This finding suggests that the profiles of the (239,240)Pu/(137)Cs ratios in shallower waters directly reflect biogeochemical processes in the water column. A half-regeneration depth deduced from the curve fitting the observed data, showed latitudinal and longitudinal distributions, also related to biogeochemical processes in the water column." @default.
- W2076775326 created "2016-06-24" @default.
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- W2076775326 date "2009-03-01" @default.
- W2076775326 modified "2023-10-03" @default.
- W2076775326 title "239,240Pu/137Cs ratios in the water column of the North Pacific: a proxy of biogeochemical processes" @default.
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- W2076775326 doi "https://doi.org/10.1016/j.jenvrad.2008.12.019" @default.
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