2017
DOI: 10.1007/s10872-017-0439-8
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Horizontal and vertical distributions of 137Cs in seabed sediments around the river mouth near Fukushima Daiichi Nuclear Power Plant

Abstract: profile of the 137 Cs distributions suggest that they are related to pulse input caused by heavy-rain events. Change in the 137 Cs inventories with depth in this study are larger than those reported in previous studies, indicating earlier results of 137 Cs inventories per unit in seabed sediments in shallow seas, especially near the river mouth, which drains a radiologically highly-contaminated basin, were underestimated.

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Cited by 16 publications
(12 citation statements)
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“…The comparison result varied widely. This may have been due to the heterogeneous 137 Cs concentration in the coastal areas, as stated by past research 7,22,23 . The comparison result between the interpolation map, which is shown in Fig.…”
Section: Validation Of Towed Radiation Surveymentioning
confidence: 82%
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“…The comparison result varied widely. This may have been due to the heterogeneous 137 Cs concentration in the coastal areas, as stated by past research 7,22,23 . The comparison result between the interpolation map, which is shown in Fig.…”
Section: Validation Of Towed Radiation Surveymentioning
confidence: 82%
“…The radiocesium in the sediment more than 10 km off the coast of Fukushima is spread approximately 10 cm from the sediment surface, as indicated by considerable eld data 6,20,21 . The radiocesium depth pro le in nearshore and estuary areas is complex; a radiocesium peak has been observed at a depth of over 50 cm 7 . Towed radiation survey cannot evaluate all types of radiocesium depth pro les.…”
Section: Calibrationmentioning
confidence: 99%
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“…Considering that the tsunami has induced a subsidence of 37 cm in this area [43], the difference of sea level δh is finally of h 2 − h 1 + 0.37. The slope at the shoreline was produced by a bathymetric survey [44] with a resolution of 2-3 m and an accuracy of 2%. The bathymetric survey was acquired after the tsunami in 2013 but, because this map was only used to calculate the slope at the shoreline, the subsidence correction of the map was of no use.…”
Section: Methodsmentioning
confidence: 99%