Distribution of [formula omitted]Cs in the Lena River Estuary–Laptev Sea System

Abstract

Surface sediment samples in the Laptev Sea have average 137 Cs content of 7.1 Bq kg −1, a value intermediate 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 137 Cs in the Laptev Sea sediments show significant variability, and the influence of a variety of environmental factors. 137 Cs concentrations in the Laptev Sea surface sediments range from 0.8 to 16 Bq kg −1. There is a marked increase in 137 Cs content of surface sediment samples collected near the Lena River delta, and a local enrichment in the 137 Cs inventories at these sites is also evident. Fine-grained mixed-layer illite/smectite rich sediments in the estuary provide effective adsorption sites to fix 137 Cs, in spite of desorption processes associated with low salinities in estuarine mixing. The Lena River–Laptev Sea mixing zone is a major site of sea-ice production. River and shelf sediments are incorporated into sea-ice formed in this region ( Holmes and Creager, 1974). The irregular 137 Cs activity profiles of the Lena River estuary cores indicate disturbance or removal of 137 Cs-laden sediments via sea-ice related processes. Lena River and Estuary sediments may have served as a secondary source (i.e. other than direct fallout) of 137 Cs in sea-ice. North-east of the Lena River estuary, sediment contains a thin layer of 137 Cs-bearing material over an erosion surface. The 137 Cs-laden surface layer may be the result of transient deposition of estuarine sediments being delivered by sea-ice or spring floods.