Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study

A numerical model based upon residual circulation has been developed to simulate the long-term (years) transport of non-conservative radionuclides in the English Channel. The transfer of radionuclides between water, suspended matter and bottom sediments has been described in terms of kinetic transfe...

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Autor: Periáñez Rodríguez, Raúl
Tipo de recurso: artículo
Estado:Versión enviada para evaluación y publicación
Fecha de publicación:2003
País:España
Institución:Universidad de Sevilla (US)
Repositorio:idUS. Depósito de Investigación de la Universidad de Sevilla
OAI Identifier:oai:idus.us.es:11441/133932
Acceso en línea:https://hdl.handle.net/11441/133932
https://doi.org/10.1016/S0272-7714(02)00115-4
Access Level:acceso abierto
Palabra clave:English Channel
Advection–diffusion
Distribution coefficient
Sediment
Suspended matter
Cs
Pu
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spelling Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study Periáñez Rodríguez, Raúl English Channel Advection–diffusion Distribution coefficient Sediment Suspended matter Cs Pu A numerical model based upon residual circulation has been developed to simulate the long-term (years) transport of non-conservative radionuclides in the English Channel. The transfer of radionuclides between water, suspended matter and bottom sediments has been described in terms of kinetic transfer coefficients, so that the model can be applied in situations out of equilibrium. The model has been used to study and compare the effects of direct discharges of radionuclides, the case of a continuous release and the redissolution of radionuclides from a contaminated sediment. These numerical experiments have been carried out for two radionuclides with a different geochemical behaviour: 137Cs and 239,240Pu. It has been found that natural equilibrium in the partition of radionuclides between the liquid and solid phases is reached in the case of instantaneous releases and in the case of redissolution from a contaminated sediment. However, in the case of a continuous release such partition remains out of natural equilibrium. Also, the behaviour of 137Cs and 239,240Pu is similar, but the time scales of the processes are clearly different due to the different affinities of both radionuclides to remain fixed to the solid phases. European Commission FIGE-CT-2000-00085 Elsevier https://hdl.handle.net/11441/133932 https://doi.org/10.1016/S0272-7714(02)00115-4
title Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
spellingShingle Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
Periáñez Rodríguez, Raúl
English Channel
Advection–diffusion
Distribution coefficient
Sediment
Suspended matter
Cs
Pu
title_short Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
title_full Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
title_fullStr Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
title_full_unstemmed Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
title_sort Redissolution and long-term transport of radionuclides released from a contaminated sediment: a numerical modelling study
author Periáñez Rodríguez, Raúl
author_facet Periáñez Rodríguez, Raúl
author_role author
topic English Channel
Advection–diffusion
Distribution coefficient
Sediment
Suspended matter
Cs
Pu
topic_facet English Channel
Advection–diffusion
Distribution coefficient
Sediment
Suspended matter
Cs
Pu
description A numerical model based upon residual circulation has been developed to simulate the long-term (years) transport of non-conservative radionuclides in the English Channel. The transfer of radionuclides between water, suspended matter and bottom sediments has been described in terms of kinetic transfer coefficients, so that the model can be applied in situations out of equilibrium. The model has been used to study and compare the effects of direct discharges of radionuclides, the case of a continuous release and the redissolution of radionuclides from a contaminated sediment. These numerical experiments have been carried out for two radionuclides with a different geochemical behaviour: 137Cs and 239,240Pu. It has been found that natural equilibrium in the partition of radionuclides between the liquid and solid phases is reached in the case of instantaneous releases and in the case of redissolution from a contaminated sediment. However, in the case of a continuous release such partition remains out of natural equilibrium. Also, the behaviour of 137Cs and 239,240Pu is similar, but the time scales of the processes are clearly different due to the different affinities of both radionuclides to remain fixed to the solid phases.
publishDate 2003
format article
status_str submittedVersion
url https://hdl.handle.net/11441/133932
https://doi.org/10.1016/S0272-7714(02)00115-4
eu_rights_str_mv openAccess
publisher Elsevier
institution Universidad de Sevilla (US)
collection idUS. Depósito de Investigación de la Universidad de Sevilla
reponame_str idUS. Depósito de Investigación de la Universidad de Sevilla
instname_str Universidad de Sevilla (US)
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publishDateSort 2003
author_browse Periáñez Rodríguez, Raúl
publisherStr Elsevier
score 6,924472