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Radionuclides as tracers of water fronts in the South Indian Ocean—ANTARES IV Results

机译:放射性核素作为南印度洋水滨的示踪剂—ANTARES IV结果

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Anthropogenic 90Sr, 239,240Pu and 241Am were used as tracers of water mass circulation in the Crozet Basin of the South Indian Ocean, represented by three main water fronts—Agulhas (AF), Subtropical (STF) and Subantarctic (SAF). Higher 90Sr concentrations observed north of 43°S were due to the influence of AF and STF, which are associated with the south branch of the Subtropical gyre, which acts as a reservoir of radionuclides transported from the North to the South Indian Ocean. On the other hand, the region south of 43°S has been influenced by SAF, bringing to the Crozet Basin Antarctic waters with lower radionuclide concentrations. The 238Pu/239,240Pu activity ratios observed in water and zooplankton samples indicated that, even 35 years after the injection of 238Pu to the Indian Ocean from the burn-up of the SNAP-9A satellite, the increased levels of 238Pu in surface water and zooplankton are still well visible. The radionuclide concentrations in seawater and their availability to zooplankton are responsible for the observed 210Po, 239,240Pu and 241Am levels in zooplankton.
机译:人类活动的90Sr,239,240Pu和241Am被用作印度洋南部克罗泽特盆地水质循环的示踪剂,以三个主要水位为代表:Agulhas(AF),亚热带(STF)和亚南极(SAF)。在43°S以北观测到更高的90Sr浓度归因于AF和STF的影响,它们与亚热带回旋的南分支相关,后者是从北向南印度洋运输的放射性核素的储集层。另一方面,南半球43°以南的区域受到了SAF的影响,从而将放射性核素浓度较低的南极水带到了克罗泽盆地。在水和浮游动物样本中观察到的238Pu / 239,240Pu活度比表明,即使在SNAP-9A卫星燃尽向印度洋注入238Pu之后的35年,地表水和浮游动物中238Pu的水平也有所增加仍然清晰可见。海水中放射性核素的浓度及其对浮游动物的利用是导致浮游动物中观测到的210Po,239,240Pu和241Am水平的原因。

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