Sinking velocity of particulate radiocesium in the northwestern North Pacific
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- Makio C. Honda
- Department of Environmental Geochemical Cycle Research; Japan Agency for Marine-Earth Science and Technology (JAMSTEC); Yokosuka Japan
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- Hajime Kawakami
- Public Relations Department, JAMSTEC; Yokosuka Japan
書誌事項
- 公開日
- 2014-06-06
- 資源種別
- journal article
- 権利情報
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- http://doi.wiley.com/10.1002/tdm_license_1
- http://onlinelibrary.wiley.com/termsAndConditions
- DOI
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- 10.1002/2014gl060126
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
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.
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 41 (11), 3959-3965, 2014-06-06
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1360004229801924736
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- ISSN
- 00948276
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- 資料種別
- journal article
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- データソース種別
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- Crossref
- KAKEN
- OpenAIRE

