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首页> 外文期刊>Acta Oceanologica Sinica >Distribution of radium-224 in the western Arctic Ocean
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Distribution of radium-224 in the western Arctic Ocean

机译:镭224在北冰洋西部的分布

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摘要

Radium-224 activities in the western Arctic Ocean were measured via ship-board ~(220)Rn emanation technique during the Second Chinese National Arctic Expedition. The results showed that the ~(224)Ra activities in the study areas ranged from being less than 0.08 to 3.58 Bq/m~3, with an average of 0.23 Bq/m~3. The low ~(224)Ra concentration in the surface water was attributed to the influence of sea ice melted water. The horizontal distribution of surface ~(224)Ra in the western Arctic Ocean showed a high ~(224)Ra characteristics occurred along the slope around 160°W, providing evidence for the importance of ice-rafted sediments to controlling the distribution of radium isotopes in the Arctic Ocean. Mostly, ~(224)Ra concentrations increased with the depth in the shelf region and reached a maximum at 75 m at the central Canada Basin, which further confirms the importance of the transport of shelf bottom water to maintaining the upper halocline layer in the Canada Basin.
机译:在第二次中国全国北极考察中,通过船上的〜(220)Rn发射技术测量了北冰洋西部的Rad-224活性。结果表明,研究区的〜(224)Ra活度范围从小于0.08到3.58 Bq / m〜3,平均为0.23 Bq / m〜3。地表水中〜(224)Ra的低浓度归因于海冰融化水的影响。北冰洋西部〜(224)Ra表面的水平分布显示沿160°W附近的斜坡具有较高的〜(224)Ra特征,这提供了浮冰沉积物对控制镭同位素分布的重要性的证据在北冰洋。通常,〜(224)Ra浓度随架子区域的深度而增加,并在加拿大中部盆地75 m处达到最大值,这进一步证实了架子底水的运输对保持加拿大上层卤水层的重要性。盆地。

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