AMS measurements of 129I in seawater around Iceland and the Irminger Sea

Large amounts of iodine-129 were, and still are, released into the environment from nuclear facilities, in particular from two reprocessing facilities located on the east coast of the North Atlantic Ocean (Sellafield and La Hague). The main transport path of the releases from the two facilities is t...

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Published in:Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
Main Authors: Gómez-Guzmán, J.M., Villa, M., Le Moigne, F., López-Gutiérrez, J.M., García-León, M.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://eprints.soton.ac.uk/372014/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:372014 2023-07-30T04:01:07+02:00 AMS measurements of 129I in seawater around Iceland and the Irminger Sea Gómez-Guzmán, J.M. Villa, M. Le Moigne, F. López-Gutiérrez, J.M. García-León, M. 2013 https://eprints.soton.ac.uk/372014/ English eng Gómez-Guzmán, J.M., Villa, M., Le Moigne, F., López-Gutiérrez, J.M. and García-León, M. (2013) AMS measurements of 129I in seawater around Iceland and the Irminger Sea. Nuclear Instruments and Methods in Physics Research Section B Beam Interactions with Materials and Atoms, 294, 547-551. (doi:10.1016/j.nimb.2012.07.045 <http://dx.doi.org/10.1016/j.nimb.2012.07.045>). Article PeerReviewed 2013 ftsouthampton https://doi.org/10.1016/j.nimb.2012.07.045 2023-07-09T21:56:26Z Large amounts of iodine-129 were, and still are, released into the environment from nuclear facilities, in particular from two reprocessing facilities located on the east coast of the North Atlantic Ocean (Sellafield and La Hague). The main transport path of the releases from the two facilities is through the North Atlantic Current (NAC) and subsequently the Norwegian Coastal Current (NCC) to the Arctic Ocean. Iceland lies on the Scotland–Greenland ridge, which separates the Atlantic and Arctic oceans. 129I data available in that area are scarce despite their importance in modeling 129I dispersion through the North Atlantic and Arctic Oceans. For this reason, we have determined the 129I/127I ratio in seawater samples by means of Accelerator Mass Spectrometry (AMS) from three locations at the Iceland and Irminger Basins at different depths (from surface to 1000 m) in order to study the transport pathways of the anthropogenic releases to the waters. The measured 129I/127I ratios, compared to the pre-anthropogenic 129I/127I value, show the strong influence of the artificial 129I discharges in the North Atlantic waters. Article in Journal/Newspaper Arctic Arctic Ocean Greenland Iceland north atlantic current North Atlantic University of Southampton: e-Prints Soton Arctic Arctic Ocean Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms 294 547 551
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Large amounts of iodine-129 were, and still are, released into the environment from nuclear facilities, in particular from two reprocessing facilities located on the east coast of the North Atlantic Ocean (Sellafield and La Hague). The main transport path of the releases from the two facilities is through the North Atlantic Current (NAC) and subsequently the Norwegian Coastal Current (NCC) to the Arctic Ocean. Iceland lies on the Scotland–Greenland ridge, which separates the Atlantic and Arctic oceans. 129I data available in that area are scarce despite their importance in modeling 129I dispersion through the North Atlantic and Arctic Oceans. For this reason, we have determined the 129I/127I ratio in seawater samples by means of Accelerator Mass Spectrometry (AMS) from three locations at the Iceland and Irminger Basins at different depths (from surface to 1000 m) in order to study the transport pathways of the anthropogenic releases to the waters. The measured 129I/127I ratios, compared to the pre-anthropogenic 129I/127I value, show the strong influence of the artificial 129I discharges in the North Atlantic waters.
format Article in Journal/Newspaper
author Gómez-Guzmán, J.M.
Villa, M.
Le Moigne, F.
López-Gutiérrez, J.M.
García-León, M.
spellingShingle Gómez-Guzmán, J.M.
Villa, M.
Le Moigne, F.
López-Gutiérrez, J.M.
García-León, M.
AMS measurements of 129I in seawater around Iceland and the Irminger Sea
author_facet Gómez-Guzmán, J.M.
Villa, M.
Le Moigne, F.
López-Gutiérrez, J.M.
García-León, M.
author_sort Gómez-Guzmán, J.M.
title AMS measurements of 129I in seawater around Iceland and the Irminger Sea
title_short AMS measurements of 129I in seawater around Iceland and the Irminger Sea
title_full AMS measurements of 129I in seawater around Iceland and the Irminger Sea
title_fullStr AMS measurements of 129I in seawater around Iceland and the Irminger Sea
title_full_unstemmed AMS measurements of 129I in seawater around Iceland and the Irminger Sea
title_sort ams measurements of 129i in seawater around iceland and the irminger sea
publishDate 2013
url https://eprints.soton.ac.uk/372014/
long_lat ENVELOPE(-34.041,-34.041,63.054,63.054)
geographic Arctic
Arctic Ocean
Greenland
Irminger Sea
geographic_facet Arctic
Arctic Ocean
Greenland
Irminger Sea
genre Arctic
Arctic Ocean
Greenland
Iceland
north atlantic current
North Atlantic
genre_facet Arctic
Arctic Ocean
Greenland
Iceland
north atlantic current
North Atlantic
op_relation Gómez-Guzmán, J.M., Villa, M., Le Moigne, F., López-Gutiérrez, J.M. and García-León, M. (2013) AMS measurements of 129I in seawater around Iceland and the Irminger Sea. Nuclear Instruments and Methods in Physics Research Section B Beam Interactions with Materials and Atoms, 294, 547-551. (doi:10.1016/j.nimb.2012.07.045 <http://dx.doi.org/10.1016/j.nimb.2012.07.045>).
op_doi https://doi.org/10.1016/j.nimb.2012.07.045
container_title Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
container_volume 294
container_start_page 547
op_container_end_page 551
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