The Department of Earth Sciences is looking for a highly motivated postdoctoral researcher with a PhD in Earth Sciences, Environmental Sciences, Biology or other appropriate field. You will work on the project ‘Investigating the impact of ocean acidification on the marine phosphorus cycle, a (bio)geochemical modelling approach’.
Your jobMicroscopic calcite (CaCO3) shells of plankton sink through ocean waters to the seafloor by the trillions each year, taking along essential nutrients such as phosphorus (P). Ocean acidification is likely to alter global CaCO3 fluxes, with so far unknown consequences for P cycling, ocean fertility and CO2 uptake. Our lack of knowledge regarding these feedbacks limits our insight in ocean functioning under environmental change, both in the (ancient) past and the human-impacted future.
The NWO-funded PHOSFLUX project aims to shed light on these unknowns, by quantifying the role of CaCO3 fluxes and acidification in global marine P cycling through a combination of field work in the North Atlantic Ocean, laboratory experiments and numerical modelling. A scientific cruise with our research vessel Pelagia will allow us to investigate CaCO3 – P interactions in the field. Through controlled lab experiments, we will dive deeper into the underlying chemical and mineralogical processes, to eventually capture them in physical-chemical models that predict the impact of acidification on marine P cycling.
The PHOSFLUX project is a collaboration between the NIOZ (Dr Peter Kraal) and Utrecht University (UU; Prof. Dr Mariëtte Wolthers), combining unique sea-going and on-shore experimentation with advanced analytical tools to understand mineral-water interactions from microscopic to ocean-basin scale. Besides PI’s Kraal and Wolthers, the PHOSFLUX team consists of a NIOZ-based PhD student performing experiments and analyses, and a Utrecht University-based postdoctoral researcher who focuses on modelling the CaCO3 – P interactions.
As postdoctoral researcher within PHOSFLUX, your role is to model P dynamics in sinking and deposited marine snow in relation to changing environmental conditions in the water column. To achieve this, you will create a reactive-transport model for P dynamics that will include processes such as CaCO3 dissolution, organic matter decomposition and adsorption/incorporation of PO4 into solid phases of marine snow. You will test the performance of your model by simulating experimental and field data in collaboration with the PHOSFLUX PhD candidate.
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