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Featured researches published by M. Rozet.


Journal of Environmental Radioactivity | 2010

A study of the atmospheric dispersion of a high release of krypton-85 above a complex coastal terrain, comparison with the predictions of Gaussian models (Briggs, Doury, ADMS4)

C. Leroy; Denis Maro; D. Hébert; L. Solier; M. Rozet; S. Le Cavelier; O. Connan

Atmospheric releases of krypton-85, from the nuclear fuel reprocessing plant at the AREVA NC facility at La Hague (France), were used to test Gaussian models of dispersion. In 2001-2002, the French Institute for Radiological Protection and Nuclear Safety (IRSN) studied the atmospheric dispersion of 15 releases, using krypton-85 as a tracer for plumes emitted from two 100-m-high stacks. Krypton-85 is a chemically inert radionuclide. Krypton-85 air concentration measurements were performed on the ground in the downwind direction, at distances between 0.36 and 3.3 km from the release, by neutral or slightly unstable atmospheric conditions. The standard deviation for the horizontal dispersion of the plume and the Atmospheric Transfer Coefficient (ATC) were determined from these measurements. The experimental results were compared with calculations using first generation (Doury, Briggs) and second generation (ADMS 4.0) Gaussian models. The ADMS 4.0 model was used in two configurations; one takes account of the effect of the built-up area, and the other the effect of the roughness of the surface on the plume dispersion. Only the Briggs model correctly reproduced the measured values for the width of the plume, whereas the ADMS 4.0 model overestimated it and the Doury model underestimated it. The agreement of the models with measured values of the ATC varied according to distance from the release point. For distances less than 2 km from the release point, the ADMS 4.0 model achieved the best agreement between model and measurement; beyond this distance, the best agreement was achieved by the Briggs and Doury models.


Journal of Environmental Radioactivity | 2017

The VATO project: An original methodology to study the transfer of tritium as HT and HTO in grassland ecosystem

D. Maro; F. Vermorel; M. Rozet; C. Aulagnier; D. Hébert; S. Le Dizès; C Voiseux; L. Solier; Catherine Cossonnet; C. Godinot; Bruno Fiévet; P. Laguionie; O. Connan; O. Cazimajou; Mehdi Morillon; M. Lamotte

Tritium (3H) is mainly released into the environment by nuclear power plants, military nuclear facilities and nuclear reprocessing plants. The construction of new nuclear facilities in the world as well as the evolution of nuclear fuel management might lead to an increase of 3H discharges from the nuclear industry. The VATO project was set up by IRSN (Institut de Radioprotection et de Sûreté Nucléaire) and EDF (Electricité de France) to reduce the uncertainties in the knowledge about transfers of 3H from an atmospheric source (currently releasing HT and HTO) to a grassland ecosystem. A fully instrumented technical platform with specifically designed materials was set up downwind of the AREVA NC La Hague reprocessing plant (Northwest of the France). This study, started in 2013, was conducted in four main steps to provide an hourly data set of 3H concentrations in the environment, adequate to develop and/or validate transfer models. It consisted first in characterizing the physico-chemical forms of 3H present in the air around the plant. Then, 3H transfer kinetics to grass were quantified regarding contributions from various compartments of the environment. For this purpose, an original experimental procedure was provided to take account for biases due to rehydration of freeze-dried samples for the determination of OBT activity concentrations in biological samples. In a third step, the 3H concentrations measured in the air and in rainwater were reconstructed at hourly intervals. Finally, a data processing technique was used to determine the biological half-lives of OBT in grass.


Journal of Environmental Radioactivity | 2009

Solid partitioning and solid-liquid distribution of 210Po and 210Pb in marine anoxic sediments: roads of Cherbourg at the northwestern France

O. Connan; Dominique Boust; G. Billon; L. Solier; M. Rozet; S. Bouderbala

A sequential extraction protocol has been used to determine the solid-phase partition of (210)Po and (210)Pb in anoxic marine sediment from the roads of Cherbourg (France) in the central English Channel. Measurements were also obtained in pore waters, in which (210)Po activities range between 1 and 20 mBq L(-1) and (210)Pb activities between 2.4 and 3.8 mBq L(-1), with highest activities in the topmost layer. These activities are higher than in seawater, suggesting that sediment act as a source of both (210)Po and (210)Pb for overlying water. The (210)Po profile in the pore waters is apparently correlated with those obtained for Fe, Mn and SO(4)(2)(-), suggesting an influence of early diagenetic processes on the (210)Po solid-liquid distribution. In the sediment, (210)Po is predominantly bound to organic matter or chromium reducible sulphides, and residuals (clay minerals and refractory oxides). Our results indicate that (210)Po is not significantly bound to AVS, i.e. acid volatile sulphides: bioturbation could play a role by the early redistribution of (210)Po bound to acid volatile sulphides in the sediment. (210)Po, (210)Pb and Pb exhibit differences in terms of distribution, probably due to a different mode of penetration in the sediment. This work provides information on solid and liquid distribution of (210)Po and (210)Pb in marine sediment. These data are very scarce in the literature.


Journal of Environmental Radioactivity | 2013

Dating of sediment record at two contrasting sites of the Seine River using radioactivity data and hydrological time series

Anne Vrel; Dominique Boust; Patrick Lesueur; Julien Deloffre; Carole Dubrulle-Brunaud; L. Solier; M. Rozet; Coralie Thouroude; Catherine Cossonnet; Sandrine Thomas

Sediment cores were collected at the outlet of the highly anthropogenized catchment of the Seine River at two contrasting sites: a flood plain of the lower Seine River and a quasi-permanently submerged harbour basin (or wet dock) in the upper tidal estuary. Analyses of artificial radionuclides ((137)Cs and plutonium isotopes), coupled with hydrological and bathymetric data, lead to a precise dating of the sediment cores collected at the two sites. (137)Cs signals originating from global fallout (early 1960s) and from the Chernobyl accident (1986) are identified, but at different levels due to the incomplete nature or variable continuity of the records. Anomalous (238)Pu concentrations found at both sites (1-2 Bq kg(-1)) are attributed to unknown industrial releases originating from upstream. Interpolating (137)Cs sediment activities under the assumption of a constant sediment rate, those releases were dated back to 1975 ± 1, thus providing a local but reliable time-marker. Age models have highlighted a very contrasting sediment filling dynamics in these two sites. This study presents the first sediment record of alpha- and gamma-emitting artificial radionuclides obtained at the outlet of the huge catchment area of the River Seine, over a period covering the last 50 years.


Journal of Environmental Radioactivity | 2008

Water to atmosphere fluxes of 131I in relation with alkyl-iodide compounds from the Seine Estuary (France)

O. Connan; Emmanuel Tessier; Denis Maro; David Amouroux; D. Hébert; M. Rozet; C Voiseux; L. Solier

This study presents an original work on measurements of stable and radioactive iodinated species in the Seine estuary (France), with estimates fluxes of volatile gaseous species from water to the atmosphere. Various iodinated compounds were identified in water and air in particular 131I in water, what is unusual. Concentrations and behaviour of iodinated elements in the Seine estuary seem similar to what has been observed in other European estuaries. MeI (Methyl Iodide) and Total Volatile Iodine (TVI) fluxes from water to air vary between 392 and 13949 pmol m(-2) d(-1) and between 1279 and 16484 pmol m(-2) d(-1), respectively. Water to air flux of TVI for the Seine river was estimated in the range 4-46 kg y(-1). Measurements of (131)I in water varying between 0.4 and 11.9 Bq m(-3). Fluxes of (131)I from water to atmosphere are in the range 2.4 x 10(5)-1.3 x 10(7)Bq y(-1), close to an annual discharge of (131)I by a nuclear reactor.


Fusion Science and Technology | 2015

Modeling and Validating Tritium Transfer in a Grassland Ecosystem in Response to 3h Releases

Séverine Le Dizès; Denis Maro; M. Rozet; D. Hébert

Abstract In this paper a radioecological model for tritium transfer in a grassland ecosystem developed on an hourly time-step basis is proposed and compared with the first data set obtained in the vicinity of the AREVA NC reprocessing plant of La Hague (France).


WIT Transactions on Ecology and the Environment | 2015

Modeling And Validating Tritium Transfer In A Grassland Ecosystem In Response To 3H Release

S. Le Dizès; H. Renard; F. Vermorel; D. Maro; C. Aulagnier; M. Rozet; D. Hébert; L. Solier

In this paper a radioecological model for tritium transfer in a grassland ecosystem developed on an hourly time-step basis is proposed and compared with the first data set obtained in the vicinity of the AREVA NC reprocessing plant of La Hague (France).


Journal of Environmental Radioactivity | 2006

Transfer of radiocarbon liquid releases from the AREVA La Hague spent fuel reprocessing plant in the English Channel.

Bruno Fiévet; C Voiseux; M. Rozet; Michel Masson; Pascal Bailly du Bois


Atmospheric Environment | 2011

Atmospheric dispersion of an elevated release in a rural environment: Comparison between field SF6 tracer measurements and computations of Briggs and ADMS models

O. Connan; C. Leroy; F. Derkx; D. Maro; D. Hébert; Pierre Roupsard; M. Rozet


Radionuclides in the Oceans, RADOC 96 - 97 | 1997

Improving Knowledge of Water-Mass Circulation in the English Channel Using Radioactive Tracers

Pascal Bailly Du Bois; M. Rozet; K Thoral; Jean-Claude Salomon

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Dive into the M. Rozet's collaboration.

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D. Hébert

Institut de radioprotection et de sûreté nucléaire

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L. Solier

Institut de radioprotection et de sûreté nucléaire

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O. Connan

Institut de radioprotection et de sûreté nucléaire

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D. Maro

Institut de radioprotection et de sûreté nucléaire

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C Voiseux

Institut de radioprotection et de sûreté nucléaire

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Denis Maro

Institut de radioprotection et de sûreté nucléaire

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Dominique Boust

Institut de radioprotection et de sûreté nucléaire

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P. Laguionie

Institut de radioprotection et de sûreté nucléaire

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Bruno Fiévet

Institut de radioprotection et de sûreté nucléaire

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Catherine Cossonnet

Institut de radioprotection et de sûreté nucléaire

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