Published March 2016 | Version v1
Journal article

Meridional distribution of Fukushima-derived radiocesium in surface seawater along a trans-Pacific line from the Arctic to Antarctic Oceans in summer 2012

  • 1. Research and Development Center for Global Change, Japan Agency for Marine-Earth Science and Technology, Kanagawa (Japan)
  • 2. Fukushima University, Fukushima (Japan). Institute of Environmental Radioactivity
  • 3. Kanazawa University, Ishikawa (Japan). Low Level Radioactivity Laboratory

Description

In summer 2012, we measured activity concentration of radiocesium in surface seawater collected in the Arctic Ocean, Bering Sea, western Pacific Ocean, and Antarctic Ocean. The radiocesium derived from the Fukushima Dai-ichi Nuclear Power Plant accident in March 2011 was found in the Bering Sea and western North Pacific between 25 deg N and 63 deg N, which agrees with model simulation results of atmospheric deposition. A semi-synoptic view suggests that a main body of radiocesium discharged directly had been transported eastward to 170 deg W. northward to 50 deg N, and southward to 30 deg N by summer 2012, about one and half years after the accident. (author)

Additional details

Identifiers

Publishing Information

Journal Title
Journal of Radioanalytical and Nuclear Chemistry
Journal Volume
307
Journal Issue
3
Journal Page Range
p. 1703-1710
ISSN
0236-5731
CODEN
JRNCDM

Conference

Title
10. International Conference on Methods and Applications of Radioanalytical Chemistry
Acronym
MARC X
Dates
12-17 Apr 2015
Place
Kailua-Kona (United States)

Optional Information

Notes
54 refs. Record from MARIS; Source key: DL9TNC3B; Archive location: 635