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Distribution of ~137Cs in the Lena River Estuary-Laptev Sea System

机译:莉娜河口-拉普捷夫海洋系统中〜137Cs的分布

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Surface sediment samples in the Laptev Sea have average ~137Cs content of 7.1 Bq kg~-1,a value intemediate between that of the western Kara Sea (23 Bq kg~-1) and the East Siberian Sea (4.2 Bq kg~-1). Both surface sediment content And sediment inventory of ~137Cs in the Laptev Sea sedi- Ments show significant variability, and the influence of a Variety of environmental factors. ~137Cs concentrations in The Laptev Sea surface sediments range from 0.8 to 16 Bq Kg~-1. There is a marked increase in ~137Cs content of Surface sediment samples collected near the Lena River Delta, and a local enrichment in the ~137Cs inventories at These sites is also evident. Fine-grained mixed-layer illite/ Smectite rich sediment sin the estuary provide effective Adsorption sites to fix ~137Cs, in spite of desorption pro- Cesses associated with low salinities in estuarine mixing.
机译:拉普捷夫海的地表沉积物样本的平均〜137Cs含量为7.1 Bq kg〜-1,介于喀拉海西部(23 Bq kg〜-1)和西伯利亚东部(4.2 Bq kg〜-1)之间)。拉普捷夫海沉积物中约137 Cs的表层沉积物含量和沉积物存量都表现出显着的变异性,并受到各种环境因素的影响。拉普捷夫海表层沉积物中〜137Cs的浓度范围为0.8至16 Bq Kg〜-1。在利纳河三角洲附近收集的地表沉积物样本中〜137Cs含量显着增加,并且这些地点的〜137Cs清单中也有局部富集。尽管在河口混合过程中存在低盐度的解吸过程,但河口细粒混合层伊利石/富含蒙脱石的沉积物仍可提供有效的吸附位点固定约137Cs。

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