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Contraindre les échanges côte-large et la pompe biologique de carbone par modélisation inverse de deux radio-isotopes (radium228 et thorium234)

Abstract : The oceanic cycles of carbon and the main nutrients are poorly known since they are affected by many physical, chemical or biological sources and sinks that are difficult to estimate by direct measurements.One way to better constrain these important processes is to use the information contained in more simple tracers called "proxies". As radium 228 (228Ra) flows from the continental shelves, it is used as a proxy of water and mineral elements fluxes from the coast to the open ocean. In particular, it is often used to estimate the SGD (Submarine Groundwater Discharge). For its part, thorium 234 (234Th), an insoluble radio-isotope, is used to constrain the dynamics of the solid particles onto which it is adsorbed. The carbon flux from the surface to the deep ocean, called "biological carbon pump" (BCP), is often estimated by a 234Th-based method.During this PhD, a numerical model with a resolution of 2°, based on the circulation of the NEMO-OPA model and the particle fields of the PISCES model, was built for each of the two radioisotopes.Several unknown model parameters were constrained by observations using an inverse technique.The inverse modeling of 228Ra was used to constrain 228Ra fluxes from 38 coastal regions.However, the SGD fluxes are poorly constrained by this method, because SGD can be confused with another source of 228Ra: diffusion from sediments.The inverse modeling of 234Th produced estimates of partition coefficients, representing the affinity of different particle types for this isotope. It was also used to estimate the errors associated with some common simplifications made in 234Th-based BCP studies.
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Submitted on : Monday, September 17, 2018 - 12:58:10 PM
Last modification on : Wednesday, October 14, 2020 - 3:52:14 AM
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  • HAL Id : tel-01875401, version 1



Guillaume Le Gland. Contraindre les échanges côte-large et la pompe biologique de carbone par modélisation inverse de deux radio-isotopes (radium228 et thorium234). Sciences de la Terre. Université de Bretagne occidentale - Brest, 2018. Français. ⟨NNT : 2018BRES0032⟩. ⟨tel-01875401⟩



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