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Global variability and controls on the accumulation of fallout radionuclides in cryoconite.
Clason, Caroline C; Baccolo, Giovanni; Lokas, Edyta; Owens, Philip N; Wachniew, Przemyslaw; Millward, Geoff E; Taylor, Alex; Blake, Will H; Beard, Dylan B; Poniecka, Ewa; Selmes, Nick; Bagshaw, Elizabeth A; Cook, Joseph; Fyfe, Ralph; Hay, Melanie; Land, Deborah; Takeuchi, Nozomu; Nastasi, Massimiliano; Sisti, Monica; Pittino, Francesca; Franzetti, Andrea; Ambrosini, Roberto; Di Mauro, Biagio.
Afiliação
  • Clason CC; Department of Geography, Durham University, Durham, UK. Electronic address: caroline.clason@durham.ac.uk.
  • Baccolo G; Laboratory of Environmental Chemistry, Paul Scherrer Institut, Villigen, Switzerland; Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland.
  • Lokas E; Institute of Nuclear Physics PAS, Department of Mass Spectrometry, Krakow, Poland.
  • Owens PN; Department of Geography, Earth and Environmental Sciences, University of Northern British Columbia, Prince George, Canada.
  • Wachniew P; Faculty of Physics and Applied Computer Science, AGH University of Science and Technology, Krakow, Poland.
  • Millward GE; School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.
  • Taylor A; School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.
  • Blake WH; School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.
  • Beard DB; School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.
  • Poniecka E; International Institute of Molecular and Cell Biology, Warsaw, Poland.
  • Selmes N; Plymouth Marine Laboratory, Plymouth, UK.
  • Bagshaw EA; Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, BS8 1SS, UK.
  • Cook J; Department of Environmental Science, Aarhus University, Aarhus, Denmark.
  • Fyfe R; School of Geography, Earth and Environmental Sciences, University of Plymouth, Plymouth, UK.
  • Hay M; Department of Pathobiology and Population Sciences, Royal Veterinary College, University of London, London, UK.
  • Land D; Natural England, York, UK; British Exploring Society, London, UK.
  • Takeuchi N; Department of Earth Sciences, Chiba University, Chiba, Japan.
  • Nastasi M; National Institute of Nuclear Physics, Milano-Bicocca section, Milan, Italy; Department of Physics, University Milano-Bicocca, Milan, Italy.
  • Sisti M; National Institute of Nuclear Physics, Milano-Bicocca section, Milan, Italy.
  • Pittino F; Department of Environmental and Earth Sciences, University Milano-Bicocca, Milano, Italy.
  • Franzetti A; Department of Environmental and Earth Sciences, University Milano-Bicocca, Milano, Italy.
  • Ambrosini R; Department of Environmental Science and Policy, University of Milano, Milan, Italy.
  • Di Mauro B; Institute of Polar Sciences, National Research Council, Milan, Italy.
Sci Total Environ ; 894: 164902, 2023 Oct 10.
Article em En | MEDLINE | ID: mdl-37343877
ABSTRACT
The accumulation of fallout radionuclides (FRNs) from nuclear weapons testing and nuclear accidents has been evaluated for over half a century in natural environments; however, until recently their distribution and abundance within glaciers have been poorly understood. Following a series of individual studies of FRNs, specifically 137Cs, 241Am and 210Pb, deposited on the surface of glaciers, we now understand that cryoconite, a material commonly found in the supraglacial environment, is a highly efficient accumulator of FRNs, both artificial and natural. However, the variability of FRN activity concentrations in cryoconite across the global cryosphere has never been assessed. This study thus aims to both synthesize current knowledge on FRNs in cryoconite and assess the controls on variability of activity concentrations. We present a global database of new and previously published data based on gamma spectrometry of cryoconite and proglacial sediments, and assess the extent to which a suite of environmental and physical factors can explain spatial variability in FRN activity concentrations in cryoconite. We show that FRNs are not only found in cryoconite on glaciers within close proximity to specific sources of radioactivity, but across the global cryosphere, and at activity concentrations up to three orders of magnitude higher than those found in soils and sediments in the surrounding environment. We also show that the organic content of cryoconite exerts a strong control on accumulation of FRNs, and that activity concentrations in cryoconite are some of the highest ever described in environmental matrices outside of nuclear exclusion zones, occasionally in excess of 10,000 Bq kg-1. These findings highlight a need for significant improvements in the understanding of the fate of legacy contaminants within glaciated catchments. Future interdisciplinary research is required on the mechanisms governing their accumulation, storage, and mobility, and their potential to create time-dependent impacts on downstream water quality and ecosystem sustainability.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Total Environ Ano de publicação: 2023 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Total Environ Ano de publicação: 2023 Tipo de documento: Article