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Sinking velocity of particulate radiocesium in the northwestern North Pacific
Sinking particles (SP) were collected by time series sediment traps at two depths in the northwestern Pacific before and after the Fukushima Daiichi Nuclear Power Plant accident, and accident‐derived particulate radiocesium was measured. Radiocesium (137Cs) was first detected at 500 m (4810 m) about...
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Published in: | Geophysical research letters 2014-06, Vol.41 (11), p.3959-3965 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Sinking particles (SP) were collected by time series sediment traps at two depths in the northwestern Pacific before and after the Fukushima Daiichi Nuclear Power Plant accident, and accident‐derived particulate radiocesium was measured. Radiocesium (137Cs) was first detected at 500 m (4810 m) about 2 weeks (1 month) after the accident. 137Cs of SP collected over 1 year revealed that the time lag between two depths was larger than that for the first 137Cs detection (about 2 weeks). We estimated the transient sinking velocity (SV) from the cumulative temporal 137Cs flux and the time lags at the two depths. Although the SV of SP collected in very early period was large, the estimated SV of most particulate 137Cs (about 80%) was about 50 m d−1. Based on comparison of 137Cs concentration in total SP with that in SP without organic materials, we suspect that most of the 137Cs was likely incorporated into aluminosilicates.
Key Points
Radiocesium from the Fukushima in sinking particle was measured
Estimated sinking velocity was slower than that estimated previously
Radiocesium in sinking particle is mainly adsorbed onto aluminosilicates |
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ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1002/2014GL060126 |