228Ra and 226Ra in the Kara and Laptev seas.

Rutgers van der Loeff, Michiel, Kühne, Stephan, Wahsner, Monika, Höltzen, Heike, Frank, Markus, Ekwurzel, Brenda, Mensch, Manfred and Rachold, Volker (2003) 228Ra and 226Ra in the Kara and Laptev seas. Continental Shelf Research, 23 (1). pp. 113-124. DOI 10.1016/S0278-4343(02)00169-3.

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Abstract

The surface water in the Transpolar Drift in the Arctic Ocean has a strong signature of 228Ra. In an earlier study of 228Ra in the open Arctic we showed that the major 228Ra source had to be in the Siberian shelf seas, but only a single shelf station was published so far. Here we investigate the sources of this signal on the Siberian shelves by measurements of 228Ra and 226Ra in surface waters of the Kara and Laptev Sea, including the Ob, Yenisey and Lena estuaries.

In the Ob and Lena rivers we found an indication for a very strong and unexpected removal of both isotopes in the early stage of estuarine mixing, presumably related to flocculation of organic-rich material. Whereas 226Ra behaves conservatively on the shelf, the distribution of 228Ra is governed by large inputs on the shelves, although sources are highly variable. In the Kara Sea the maximum activity was found in the Baydaratskaya Bay, where tidal resonance and low freshwater supply favour 228Ra accumulation. The Laptev Sea is a stronger source for 228Ra than the Kara Sea. Since a large part of Kara Sea water flows through the Laptev Sea, the 228Ra signal in the Transpolar Drift can be described as originating on the Laptev shelf.

The combined freshwater inputs from the Eurasian shelves thus produce a common radium signature with a 228Ra/226Ra activity ratio of 4.0 at 20% river water. The radium signals of the individual Siberian rivers and shelves cannot be separated, but their signal is significantly different from the signal produced on the Canadian shelf (Smith et al., in press). In this respect, the radium tracers add to the information given by Barium. Moreover, with the 5.8 year half-life of 228Ra, they have the potential to serve as a tracer for the age of a water mass since its contact with the shelves.

Document Type: Article
Keywords: Polar oceanography; Radium isotopes; Tracers; Sediment–water exchanges
Research affiliation: AWI
Refereed: Yes
DOI etc.: 10.1016/S0278-4343(02)00169-3
ISSN: 0278-4343
Projects: Laptev Sea System, Permafrost
Date Deposited: 17 Mar 2015 10:58
Last Modified: 17 Mar 2015 10:58
URI: http://oceanrep.geomar.de/id/eprint/28053

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