Radium in Arctic surface water ...

The transpolar drift is strongly enriched in 228Ra accumulated on the wide Arctic shelves with subsequent rapid offshore transport. We present new data of Polarstern expeditions to the central Arctic and to the Kara and Laptev seas. Because 226Ra activities in Pacific waters are 30% higher than in A...

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Main Authors: Rutgers van der Loeff, Michiel M, Cai, Pinghe, Stimac, Ingrid, Bauch, Dorothea, Hanfland, Claudia, Roeske, Tobias, Moran, S Bradley
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.772682
https://doi.pangaea.de/10.1594/PANGAEA.772682
id ftdatacite:10.1594/pangaea.772682
record_format openpolar
spelling ftdatacite:10.1594/pangaea.772682 2024-09-09T19:20:42+00:00 Radium in Arctic surface water ... Rutgers van der Loeff, Michiel M Cai, Pinghe Stimac, Ingrid Bauch, Dorothea Hanfland, Claudia Roeske, Tobias Moran, S Bradley 2012 application/zip https://dx.doi.org/10.1594/pangaea.772682 https://doi.pangaea.de/10.1594/PANGAEA.772682 en eng PANGAEA https://dx.doi.org/10.1029/2011jc007478 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CTD/Rosette In situ pump Expendable CTD ARK-XI/1 ARK-XXII/2 Polarstern Marine Geochemistry @ AWI AWI_MarGeoChem article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.77268210.1029/2011jc007478 2024-07-03T13:10:33Z The transpolar drift is strongly enriched in 228Ra accumulated on the wide Arctic shelves with subsequent rapid offshore transport. We present new data of Polarstern expeditions to the central Arctic and to the Kara and Laptev seas. Because 226Ra activities in Pacific waters are 30% higher than in Atlantic waters, we correct 226Ra for the Pacific admixture when normalizing 228Ra with 226Ra. The use of 228Ra decay as age marker critically depends on the constancy in space and time of the source activity, a condition that has not yet adequately been tested. While 228Ra decays during transit over the central basin, ingrowth of 228Th could provide an alternative age marker. The high 228Th/228Ra activity ratio (AR = 0.8-1.0) in the central basins is incompatible with a mixing model based on horizontal eddy diffusion. An advective model predicts that 228Th grows to an equilibrium AR, the value of which depends on the scavenging regime. The low AR over the Lomonosov Ridge (AR = 0.5) can be due to either rapid ... : Supplement to: Rutgers van der Loeff, Michiel M; Cai, Pinghe; Stimac, Ingrid; Bauch, Dorothea; Hanfland, Claudia; Roeske, Tobias; Moran, S Bradley (2012): Shelf-basin exchange times of Arctic surface waters estimated from 228Th/228Ra disequilibrium. Journal of Geophysical Research: Oceans, 177, C03024 ... Article in Journal/Newspaper Arctic laptev Lomonosov Ridge DataCite Arctic Central Basin ENVELOPE(43.000,43.000,73.500,73.500) Pacific
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic CTD/Rosette
In situ pump
Expendable CTD
ARK-XI/1
ARK-XXII/2
Polarstern
Marine Geochemistry @ AWI AWI_MarGeoChem
spellingShingle CTD/Rosette
In situ pump
Expendable CTD
ARK-XI/1
ARK-XXII/2
Polarstern
Marine Geochemistry @ AWI AWI_MarGeoChem
Rutgers van der Loeff, Michiel M
Cai, Pinghe
Stimac, Ingrid
Bauch, Dorothea
Hanfland, Claudia
Roeske, Tobias
Moran, S Bradley
Radium in Arctic surface water ...
topic_facet CTD/Rosette
In situ pump
Expendable CTD
ARK-XI/1
ARK-XXII/2
Polarstern
Marine Geochemistry @ AWI AWI_MarGeoChem
description The transpolar drift is strongly enriched in 228Ra accumulated on the wide Arctic shelves with subsequent rapid offshore transport. We present new data of Polarstern expeditions to the central Arctic and to the Kara and Laptev seas. Because 226Ra activities in Pacific waters are 30% higher than in Atlantic waters, we correct 226Ra for the Pacific admixture when normalizing 228Ra with 226Ra. The use of 228Ra decay as age marker critically depends on the constancy in space and time of the source activity, a condition that has not yet adequately been tested. While 228Ra decays during transit over the central basin, ingrowth of 228Th could provide an alternative age marker. The high 228Th/228Ra activity ratio (AR = 0.8-1.0) in the central basins is incompatible with a mixing model based on horizontal eddy diffusion. An advective model predicts that 228Th grows to an equilibrium AR, the value of which depends on the scavenging regime. The low AR over the Lomonosov Ridge (AR = 0.5) can be due to either rapid ... : Supplement to: Rutgers van der Loeff, Michiel M; Cai, Pinghe; Stimac, Ingrid; Bauch, Dorothea; Hanfland, Claudia; Roeske, Tobias; Moran, S Bradley (2012): Shelf-basin exchange times of Arctic surface waters estimated from 228Th/228Ra disequilibrium. Journal of Geophysical Research: Oceans, 177, C03024 ...
format Article in Journal/Newspaper
author Rutgers van der Loeff, Michiel M
Cai, Pinghe
Stimac, Ingrid
Bauch, Dorothea
Hanfland, Claudia
Roeske, Tobias
Moran, S Bradley
author_facet Rutgers van der Loeff, Michiel M
Cai, Pinghe
Stimac, Ingrid
Bauch, Dorothea
Hanfland, Claudia
Roeske, Tobias
Moran, S Bradley
author_sort Rutgers van der Loeff, Michiel M
title Radium in Arctic surface water ...
title_short Radium in Arctic surface water ...
title_full Radium in Arctic surface water ...
title_fullStr Radium in Arctic surface water ...
title_full_unstemmed Radium in Arctic surface water ...
title_sort radium in arctic surface water ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.772682
https://doi.pangaea.de/10.1594/PANGAEA.772682
long_lat ENVELOPE(43.000,43.000,73.500,73.500)
geographic Arctic
Central Basin
Pacific
geographic_facet Arctic
Central Basin
Pacific
genre Arctic
laptev
Lomonosov Ridge
genre_facet Arctic
laptev
Lomonosov Ridge
op_relation https://dx.doi.org/10.1029/2011jc007478
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.77268210.1029/2011jc007478
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