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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-10-3839-2013</article-id>
<title-group>
<article-title>Iodine-129 concentration in seawater near Fukushima before and after the accident at the Fukushima Daiichi Nuclear Power Plant</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Suzuki</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Otosaka</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kuwabara</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kawamura</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kobayashi</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Japan Atomic Energy Agency, Ibaraki, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Japan Atomic Energy Agency, Aomori, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>06</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>6</issue>
<fpage>3839</fpage>
<lpage>3847</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 T. Suzuki et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/3839/2013/bg-10-3839-2013.html">This article is available from https://bg.copernicus.org/articles/10/3839/2013/bg-10-3839-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/3839/2013/bg-10-3839-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/3839/2013/bg-10-3839-2013.pdf</self-uri>
<abstract>
<p>Anthropogenic radionuclides were released into the environment in large
quantities by the Fukushima Daiichi Nuclear Power Plant (1FNPP) accident. To
evaluate accident-derived &lt;sup&gt;129&lt;/sup&gt;I, the &lt;sup&gt;129&lt;/sup&gt;I concentrations in
seawater before and after the accident were compared.
&lt;br&gt;&lt;br&gt;
Before the accident (2008–2009), the &lt;sup&gt;129&lt;/sup&gt;I concentrations in the
western margin of the North Pacific between 32&amp;deg; N and 44&amp;deg; N
showed a latitudinal gradient that was expressed as a linear
function of latitude. The highest and average &lt;sup&gt;129&lt;/sup&gt;I concentrations after
the accident were 73 times and approximately 8 times, respectively, higher
than those before the accident in this study area. Considering the
distribution of &lt;sup&gt;129&lt;/sup&gt;I in surface seawater, the accident-derived
&lt;sup&gt;129&lt;/sup&gt;I in the southern and northern stations of the 1FNPP was
predominantly supplied by seawater advection and atmospheric deposition
(including microbial volatilization), respectively.
&lt;br&gt;&lt;br&gt;
As of October 2011, depth profiles of &lt;sup&gt;129&lt;/sup&gt;I revealed that &lt;sup&gt;129&lt;/sup&gt;I
originating from the 1FNPP existed mainly in the upper 100 m depth. From the
depth profiles, the cumulative inventories of accident-derived &lt;sup&gt;129&lt;/sup&gt;I
were estimated to be (1.6–9.6) × 10&lt;sup&gt;12&lt;/sup&gt; atoms m&lt;sup&gt;−2&lt;/sup&gt; in this
study area.
&lt;br&gt;&lt;br&gt;
On the basis of the &lt;sup&gt;129&lt;/sup&gt;I data in the seawater near Fukushima, the
effective dose of &lt;sup&gt;129&lt;/sup&gt;I from seafood ingestion was much smaller than the
annual dose limit.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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