2008
DOI: 10.1016/j.jenvrad.2007.07.010
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Tracing anthropogenic nuclear activity with 129I in lake sediment

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Cited by 16 publications
(16 citation statements)
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References 27 publications
(29 reference statements)
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“…The iodine in marine sediment mainly originates from decomposition of biota debris with high iodine content (marine algae: 10-6000 μg/g, most values: 200-300 μg/g, mineral ˂ 1 μg/g), which absorbs and concentrates iodine from seawater (around 50 μg/L) (Hou et al, 2010;Hou et al, 1998;Price and Calvert, 1973). The 127 I concentrations in CORE-1 (5.0-37.0 μg/g) and CORE-2 (15.0-42.5 μg/g) is lower than that in most marine sediments, including those from Oregon (98-243 μg/g), Kattegat (100-200 μg/g) and Baltic Sea (42.7-75.9 μg/g) (Moran et al 1998;López-Gutiérrez et al, 2004;Aldahan et al, 2007), but higher than most values of lake sediments collected from Sweden (5.0-10.0 μg/g) and Philippines (2.97-20 μg/g) (Englund et al, 2008;Zhang et al, 2018). The values are in the similar level with that in the mixed zone of river and ocean, such as Jiaozhou Bay (20-36 μg/g) and the Mississippi River Delta (5.7-34.3 μg/g) (Fan et al, 2016;Oktay et al, 2000) (Table SI2).…”
Section: I and 129 I Level In The Sediment Cores From The Ecsmentioning
confidence: 63%
“…The iodine in marine sediment mainly originates from decomposition of biota debris with high iodine content (marine algae: 10-6000 μg/g, most values: 200-300 μg/g, mineral ˂ 1 μg/g), which absorbs and concentrates iodine from seawater (around 50 μg/L) (Hou et al, 2010;Hou et al, 1998;Price and Calvert, 1973). The 127 I concentrations in CORE-1 (5.0-37.0 μg/g) and CORE-2 (15.0-42.5 μg/g) is lower than that in most marine sediments, including those from Oregon (98-243 μg/g), Kattegat (100-200 μg/g) and Baltic Sea (42.7-75.9 μg/g) (Moran et al 1998;López-Gutiérrez et al, 2004;Aldahan et al, 2007), but higher than most values of lake sediments collected from Sweden (5.0-10.0 μg/g) and Philippines (2.97-20 μg/g) (Englund et al, 2008;Zhang et al, 2018). The values are in the similar level with that in the mixed zone of river and ocean, such as Jiaozhou Bay (20-36 μg/g) and the Mississippi River Delta (5.7-34.3 μg/g) (Fan et al, 2016;Oktay et al, 2000) (Table SI2).…”
Section: I and 129 I Level In The Sediment Cores From The Ecsmentioning
confidence: 63%
“…This event released large amounts of radioactive substances including 1.3-6 kg 129 I into the environment (Hou et al, 2009b). Although most of this radioactive material was deposited in the vicinity of Chernobyl NPP, an enhanced signals of 129 I and 137 Cs have been observed at locations of great distances (Englund et al, 2008;Hou et al, 2003;Michel et al, 2015;Paul et al, 1987). Chernobyl derived radionuclides including 131 I have also been measured in a large area in China in various environmental samples including aerosols, vegetables and milk, and relatively high levels of 131 I were found the north part of China after the accident, including the Jiaozhou Bay area and the catchments of the Yellow River and others flowing into the bay.…”
Section: Record Of the Chernobyl Nuclear Accidentmentioning
confidence: 99%
“…In western and northern Europe, 129 I recorded in sediments is dominated by NFRP releases. The signals of the NWTs and nuclear accidents (Englund et al, 2008) (Englund et al, 2007;Gallagher et al, 2005). In Ireland, even the large releases of radioactive iodine during the Windscale accident in 1957 have been obscured by the 129 I releases from NFRPs (Gallagher et al, 2005).…”
Section: Contribution Of Nuclear Fuel Reprocessing Plantsmentioning
confidence: 99%
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“…Analysis of the sediment core can be used to retrieve deposits/events in the past. The distributions of 129 I in marine sediment cores collected in Kattegat [54] and in lake sediment collected from Sweden [41,55] and UK [56] have been reported. Fig.…”
mentioning
confidence: 99%