Chronological analysis of Omura Bay bottom sediment by measurement of environmental radioactivity
Chronological analysis of Omura Bay bottom sediment by measurement of environmental radioactivity
批准号:
14580552
负责人:
TAKATSUJI Toshihiro
金额:
$2.24万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2002
资助国家:
日本
项目状态:
已结题
起止时间:
2002 至 2003
中文摘要
分析了大村湾底部的沉积物。用锗半导体探测器对放射性进行了分析。采用电感耦合等离子体原子发射光谱法(ICP-AES)对主要元素进行了分析。微量元素的分析主要采用电感耦合等离子体质谱法(ICP-MS)。根据Pb-210的放射性,对水平分离的沉积物岩心样品进行了测年。沿岸的沉积速率往往比海湾中部快。这一趋势与直教湾和大阪湾相同。铯-137的垂直分布没有显示出核试验全球沉降物的明显峰值,用铯-137的分布进行测年是困难的。主元素P、Ti、K、Mg、Na、Al和Ca的垂直和水平分布基本均匀。K、Ti、Y、Rb、Sr、Zr、Nb、Cs、Hf、Th、Na、Zn、W、Pb和Cd的浓度高于地壳平均浓度。元素中Na、Zn、W、Pb、Cd的浓度呈上升趋势。Cu的浓度也明显升高。不能轻易下结论说流入海湾的微量元素随着年份的增加而增加,因为这些元素可能会液化到地表。而在缺氧条件下易液化的Fe和Mn的浓度则呈下降趋势。在向上增加的元素中,Cd是一个重要的环境因子,如果它越来越多地涌入海湾,可能是人类活动造成的,结果非常值得注意。
英文摘要
Sediments at the bottom of the Omura bay was analyzed. The radioactivity was analyzed by a Germanium semiconductor detector. The principal elements were analyzed by the inductively coupled, plasma atomic emission spectrometry (ICP-AES). The trace elements were mainly analyzed by the inductively coupled plasma mass spectrometry (ICP-MS).From the radioactivity of Pb-210, horizontally separated core samples of the sediments were dated. The sedimentation rate along the coast tends to be faster than the middle of the bay. The tendency is same as Zbkyo bay and Osaka bay. The vertical distribution of Cs-137 did not show clear peak of the Global fallout of the nuclear tests and the dating with Cs-137 distribution was difficult.The distributions of the principal elements, P, Ti, K, Mg, Na, Al, and Ca were almost uniform vertically and horizontally. The concentration of K, Ti, Y, Rb, Sr, Zr, Nb, Cs, Hf, Th, Na, Zn, W, Pb and Cd was higher than the average concentration of the earth's crust. In the elements, concentration of Na, Zn, W, Pb and Cd were increasing upward. The concentration of Cu was also clearly increasing upward. It is not appropriate to conclude easily that these trace elements pouring into the bay increase with the years because these elements may liquate out up to the surface. But concentration of Fe and Mn, which is known to liquate in anoxic condition, was decreasing upword oppositely. In the elements increasing upward, Cd is an important environmental factor, and if it is increasingly pouring into the bay, it may be the sake of human activity, and very noteworthy result.
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Nakamura, T., Hoel, D.G.: "Comparing cancer risks between radiation and dioxin exposure based on two-stage model"Environmetrics(Europe). 14. 203-211 (2003)
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高辻俊宏, 吉川勲, 藤安得博, 中村成孝, 松瀬美智子, 石井保裕 他: "西彼杵半島及び大村湾周辺の岩石中の放射性物質について、他"第4回環境放射能・放射線-夏の学校 プロシーディング. 64-77 (2003)
Toshihiro Takatsuji、Isao Yoshikawa、Tokuhiro Fujiyasu、Shigetaka Nakamura、Michiko Matsuse、Yasuhiro Ishii 等:“西园半岛和大村湾等岩石中的放射性物质 - 第 4 届环境放射性/辐射 - 暑期学校论文集”。 (2003)
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鬼塚昌彦, 遠藤暁, 石川正純, 星正治, 櫻井良憲, 高辻俊宏 他: "硼素含有壁を持つ組織等価比例計数管を用いた重水場の線質評価"京都大学原子炉実験所学術講演会報文集. 37. Web (2003)
Masahiko Onizuka、Akira Endo、Masazumi Ishikawa、Masaharu Hoshi、Yoshinori Sakurai、Toshihiro Takatsuji 等人:“使用含硼壁的组织等效正比计数管评估重水场中的辐射质量”京都大学反应堆研究所学术会议 37. Web (2003)
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高辻俊弘: "ポアソン照射の問題点と、単一粒子照射への期待"放射線科学. 45・9. 278-288 (2002)
高辻俊弘:“泊松照射的问题和单粒子照射的期望”《放射科学》278-288(2002)。
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共 21 条
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