Rare earth elements in the Arctic Ocean

Stig Westerlund , Peder Öhman
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引用次数: 32

Abstract

In this paper we present the first data set for rare earth elements (REE) in the Arctic Ocean. The data are from unfiltered samples. The concentrations are La: 18.8–41.3 pM; Ce: 5.7–25; Pr: 1.4–9.9; Nd: 14.6–39.6; Sm: 2.7–7.3; Gd: 3.8–13.4; Dy: 3.7–12.3; Er: 3.6–9.6; and Yb: 2.9–8.1. The concentrations found in the deep water are lower than deep-water concentrations found elsewhere and are oceanographically consistent. Our data show that the distribution of REE are influenced by riverine input in the northern part of the investigated area. Transport of resuspended material into the water from the Barents Sea Shelf is suggested to influence the concentrations of REE in the southern part of the Nansen Basin. The covariation between REE and nutrients is opposite to that found in other oceans. The fresh water end member concentrations for the REE in the northern surface water have been calculated.

北冰洋中的稀土元素
在本文中,我们提出了北冰洋稀土元素(REE)的第一个数据集。数据来自未经过滤的样本。浓度为La: 18.8 ~ 41.3 pM;Ce: 5.7 -25;公关:1.4 - -9.9;Nd: 14.6 - -39.6;Sm: 2.7 - -7.3;Gd: 3.8 - -13.4;Dy: 3.7 - -12.3;呃:3.6 - -9.6;Yb: 2.9-8.1。在深海中发现的浓度低于其他地方发现的深海浓度,并且在海洋学上是一致的。结果表明,研究区北部稀土元素的分布受河流输入的影响。从巴伦支陆架向水体输运的重悬浮物质影响了南森盆地南部的稀土元素浓度。稀土元素与营养物之间的共变与其他海洋相反。计算了北方地表水中稀土元素的淡水端元浓度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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