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Thallium dynamics in the southern North Sea

机译:北海南海的铊动态

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摘要

In open ocean waters thallium (Tl) belongs to the group of conservative elements, even though deviations from this trend have been observed in NW German coastal waters. Here, we report on tidal, seasonal and spatial dynamics of Tl along with Mo and Mn in the water column of a backbarrier tidal flat close to the island of Spiekeroog, the Jade system (Inner Jade and Jade Bay) and the adjacent offshore region. Dissolved thallium (Tl-diss) displays strong tidal and seasonal variations (similar to 25-60 pM) unrelated to salinity. In all study areas, Tl-diss clearly deviates from conservative behavior. In general, Tl-diss is low during low tide (with a loss of up to 50%) and inversely related to Mn-diss, except in summer. The tidal Tl variations as well as the loss of Tl in the water column may be due to Tl removal from pore waters in reducing sediments and drainage of Tl-free but Mn-rich pore waters into the water column during low tide. The negative Tl anomaly can be traced offshore for more than 40 km to the island of Helgoland.
机译:在开阔的海洋水域中,铊(TL)属于保守元素组,尽管在NW德国沿海水域中已经观察到这种趋势的偏差。在这里,我们报道了TL的潮汐,季节和空间动态以及莫和Mn在靠近Spiekeroog岛,玉器系统(内玉和玉湾)和邻近的海上地区。溶解的铊(TL-plas)显示出强烈的潮汐和季节性变化(类似于25-60 pm)与盐度无关。在所有研究领域,TL-SMY清楚地偏离了保守行为。通常,在低潮中的TL-vers低(损失高达50%),除夏季除外,与MN粉不相关。潮汐T1变异以及水柱中的T1的损失可能是由于从孔隙中除去了在低潮期间减少了沉积物和富含含量的富含TL但MN的孔隙水的沉积物和排出的沉积物和排出。负TL异常可以追溯到60多公里到Helgoland岛。

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