4.5 Article

Spatial and vertical distributions of natural and anthropogenic radionuclides and cesium fractionation in sediments of the Var river and its tributaries (southeast France)

Journal

Publisher

SPRINGER
DOI: 10.1007/s10967-013-2491-1

Keywords

Natural radioactivity; Sediment; Var river; Cs-137; Sequential extraction; Radionuclide speciation

Funding

  1. Atomic Energy Commission of Syria (AECS)
  2. Conseil General des Alpes Maritimes
  3. Agence de l'Eau RMC
  4. Conseil Regional PACA
  5. Syndicat Mixte d'Etudes de la Basse Vallee du Var

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This paper reports results on the natural and anthropogenic radionuclides activity concentrations in sediments of the Var river and its tributaries. Natural (U-238, Th-232 and K-40) and artificial (Cs-137) radionuclides activities were measured using high purity germanium detector. Measured activity concentrations differ widely; they depend on the pertinent environmental situation such as the presence of dams, and sediments type. Other factors controlling the distribution of the studied radioisotopes have been discussed. A sequential extraction method consisting of six operationally-defined fractions has been used for determining the geochemical partitioning of anthropogenic radionuclide Cs-137 in a 405-410 cm deep sediments collected in the lower valley of the Var river. This method corresponds to a modification of the three-stage sequential extraction procedure proposed by the Commission of the European Communities Bureau of Reference (BCR, now Standards, Measurements and Testing Program). Two steps with weak reagents, (fraction A: water; fraction B: nitric acid 0.001 M), were added before the first step of BCR (carbonate fraction) in order to better detect anthropogenic components. A total acid digestion of solid residues by microwave assisted was also added. The 6-steps extraction method was tested and validated by certified reference materials. Cs-137 was found mostly in the hydrosoluble fraction (20-24 %), oxide and hydroxide fraction (22-25 %) and in the residue (51-58 %), while Cs-133 was mostly found in the residual fraction (> 97 %).

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