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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.","descriptionType":"Abstract"},{"description":"Supplement to: Rutgers van der Loeff, Michiel M; Kühne, Stephan; Wahsner, Monika; Höltzen, Heike; Frank, Markus; Ekwurzel, Brenda; Mensch, Manfred; Rachold, Volker (2003): 228Ra and 226Ra in the Kara and Laptev seas. 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    <title>Radium 228 and Radium 226 in surface water of the Kara Sea and Laptev Sea</title>
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  <publisher>PANGAEA</publisher>
  <publicationYear>2003</publicationYear>
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    <subject subjectScheme="Parameter">Elevation of event</subject>
    <subject subjectScheme="Parameter">DEPTH, water</subject>
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    <subject subjectScheme="Parameter">Radium-226</subject>
    <subject subjectScheme="Parameter">Radium-226, standard deviation</subject>
    <subject subjectScheme="Parameter">Radium-228</subject>
    <subject subjectScheme="Parameter">Radium-228, standard deviation</subject>
    <subject subjectScheme="Parameter">Radium-228/Radium-226 activity ratio</subject>
    <subject subjectScheme="Parameter">Radium-228/Radium-226 activity ratio, standard deviation</subject>
    <subject subjectScheme="Parameter">δ18O, water</subject>
    <subject subjectScheme="Parameter">δ18O, standard deviation</subject>
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    <subject subjectScheme="Method">Sampling by hand</subject>
    <subject subjectScheme="Method">Box corer</subject>
    <subject subjectScheme="Method">van Veen Grab</subject>
    <subject subjectScheme="Method">Water sample</subject>
    <subject subjectScheme="Method">Kasten corer RUS</subject>
    <subject subjectScheme="Method">Multiple investigations</subject>
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    <subject subjectScheme="Campaign">ARK-IX/4</subject>
    <subject subjectScheme="Basis">AWI Arctic Land Expedition</subject>
    <subject subjectScheme="Basis">Dmitry Mendeleev</subject>
    <subject subjectScheme="Basis">Polarstern</subject>
    <subject subjectScheme="Project">Laptev Sea System (LSS)</subject>
    <subject subjectScheme="Project">Marine Geochemistry @ AWI (AWI_MarGeoChem)</subject>
    <subject subjectScheme="Project">Paleoenvironmental Reconstructions from Marine Sediments @ AWI (AWI_Paleo)</subject>
    <subject subjectScheme="Project">Permafrost Research (Periglacial Dynamics) @ AWI (AWI_PerDyn)</subject>
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    <date dateType="Collected">1993-08-12T10:00:00/1999-09-04T00:00:00</date>
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    <description descriptionType="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.<br/>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.<br/>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.</description>
    <description descriptionType="Other">Supplement to: Rutgers van der Loeff, Michiel M; Kühne, Stephan; Wahsner, Monika; Höltzen, Heike; Frank, Markus; Ekwurzel, Brenda; Mensch, Manfred; Rachold, Volker (2003): 228Ra and 226Ra in the Kara and Laptev seas. Continental Shelf Research, 23(1), 113-124</description>
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