Particle mixing processes of Chernobyl fallout in deep Norwegian Sea sediments: Evidence for seasonal effects
A 1430 m deep station in the Norwegian Sea (Voering Plateau) was occupied five times between May 1986 and February 1987 to investigate the seasonal variation in sediment mixing rates. Cherbnbyl-derived radiocesium, identified by its high proportion of short-lived 134Cs, was used as a tracer for mixi...
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Veröffentlicht in: | Geochimica et cosmochimica acta 1996-09, Vol.60 (18), p.3425-3433 |
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