A Study on the Transport of ¹³⁷Cs and ⁹⁰Sr in Marine Biota in a Hypothetical Scenario of a Nuclear Accident in the Western Mediterranean Sea

A Lagrangian model which simulates the transport of radionuclides released from nuclear accidents in the western Mediterranean Sea was recently described. This model was developed in spherical coordinates and includes three-dimensional mixing due to turbulence, advection by currents, radioactive dec...

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Detalles Bibliográficos
Autores: Periáñez Rodríguez, Raúl, Cortés Parejo, María del Carmen
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2023
País:España
Institución:Universidad de Sevilla (US)
Repositorio:idUS. Depósito de Investigación de la Universidad de Sevilla
OAI Identifier:oai:idus.us.es:11441/149573
Acceso en línea:https://hdl.handle.net/11441/149573
https://doi.org/10.3390/jmse11091707
Access Level:acceso abierto
Palabra clave:Mediterranean Sea
Lagrangian model
Nuclear accident
Biological uptake
Descripción
Sumario:A Lagrangian model which simulates the transport of radionuclides released from nuclear accidents in the western Mediterranean Sea was recently described. This model was developed in spherical coordinates and includes three-dimensional mixing due to turbulence, advection by currents, radioactive decay, and radionuclide exchanges between water and bed sediments. Water circulation was downloaded from the HYCOM global ocean model. Water–sediment interactions were described using a dynamic model based on kinetic transfer coefficients. Mixing, decay, and water–sediment interactions were solved using a stochastic method. Now, a dynamic biological uptake model consisting of four species (phytoplankton, zooplankton, non-piscivorous fish, and piscivorous fish) has been integrated within the transport model to be able to assess the effects of a potential accident in biota and fishery regions. The model has been set up for ¹³⁷Cs and ⁹⁰Sr due to the radiological relevance of these radionuclides. Several hypothetical accidents were simulated, resulting in ¹³⁷Cs concentrations in biota significantly higher than background levels. In contrast, ⁹⁰Sr accumulates in the food chain to a considerably weaker extent.