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Excess ~(222)Rn profiles in the bottom layer of the Japan Sea and their implication for bottom water dynamics

机译:日本海底层过量的〜(222)Rn剖面及其对底水动力学的影响

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摘要

Vertical profiles of excess radon-222 (~(222)Rn; half life: 3.82 days) in bottom seawaters between 8 and 780 m above the seafloor were measured in the Japan Sea, a semi-closed deep marginal sea in the northwest Pacific Ocean. All of the profiles observed at three locations (two profiles in the Japan Basin and one in the Yamato Basin) show curious zigzag patterns with ~(222)Rn maxima and minima, in contrast to a generally known steady-state profile of ~(222)Rn exponentially decreasing with the distance above the bottom. The observed ~(222)Rn profiles demonstrate the existence of horizontal supplies of ~(222)Rn-enriched waters in the bottom layer of the Japan Sea with timescales as short as the half-life of ~(222)Rn, probably in relation with the interaction between bottom currents and topographic features.
机译:在日本海(西北太平洋的半封闭深边缘海)日本海中测量了海底以上8至780 m之间底部海水中过量of222(〜(222)Rn;半衰期:3.82天)的垂直剖面。与通常已知的〜(222)稳态剖面相比,在三个位置(日本盆地中的两个剖面和大和盆地中的一个剖面)观察到的所有剖面都显示出具有〜(222)Rn最大值和最小值的奇怪的锯齿形图案。 Rn随着距离底部的距离呈指数下降。观测到的〜(222)Rn分布图表明,日本海底层存在〜(222)Rn富集水域的水平供给,时间尺度短于〜(222)Rn的半衰期,可能与与底流和地形特征之间的相互作用。

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  • 来源
    《Progress in Oceanography》 |2014年第2期|94-97|共4页
  • 作者

    Toshitaka Gamo;

  • 作者单位

    Department of Chemical Oceanography. Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba 277-8564, Japan;

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