진학프로석·박사 채용 접수 플랫폼

Metals’ Fate During Extreme Floods 

Mobilization of metals in contaminated wetlands under climate forcing, by coupling multi-tracer isotopic system and spectroscopic speciation

Background

Demographic growth, the energy transition and the increase in living standards result in an exponential increase in the quantities of metals extracted, while technological developments lead to a diversification of the metals necessary for industrial development, causing an unprecedented increase in releases of metals in the environment. Metals are considered toxic (e.g., Cd, Pb) or as micronutrients (e.g., Cu, Zn), but increasing their concentrations beyond certain thresholds degrades the quality of ecosystems and threatens human and animal health (concept “One Health”) in contaminated areas.

Climate models predict that the frequency, intensity and number of short-term extreme precipitation events and flood variability will increase as the global climate changes. This state of affairs no longer makes it possible to precisely constrain the fate and source-sink balance of metals in the Earth critical zone (ECZ) and consequently, the overall contributions of the continent to the oceans. In the ECZ, soils are metal sinks, especially wetlands. Their hydrological cycle (high water/low water) favors the formation of chemical gradients and biogeochemical processes controlling the metal cycle. Extreme floods are characterized by water levels and flows significantly higher than the oscillatory levels observed over time. The source-sink balance of metals in wetlands is then unbalanced, increasing the metals exported in very short periods of time (“flash pollution”) and in partially known physicochemical forms, possibly toxic and in quantities and concentrations that we have to estimate.

Keywords

• Climate changes
• Soil biogeochemistry
• Metal contamination
• Isotopic systems
• Solid spectroscopy
• Iron and carbon cycles
• Redox gradient

Objectives

During extreme rains in contaminated wetlands

• Identifying the biogeochemical processes responsible of the metal remobilization (focus on organic matter and Fe speciation)
• Using antagonistic isotopic behavior to decipher the remobilization of metals from various anthropogenic sources and their subsequent interactions with soil components.

Methods

The subject will include

• Laboratory experiments to mimic observed conditions to work under controlled conditions and identify metal remobilization processes. The basic tools of geochemistry and mineralogy will be coupled with isotopic geochemistry, speciation at the molecular scale (spectroscopic techniques at Synchrotron facility and Mossbauer spectroscopy) and microbiology.
• Field campaign for collecting samples from contaminated wetlands and leading laboratory experiments.
• Analytical platforms: Elemental geochemistry, Controlled cultures, soil/bacteria/plants (https://lpg-umr6112.fr/plateformes-angersnantes/), and GEOBIOSE platform (https://ccem.ifremer.fr/Actualites/Plateforme-GEOBIOSE)

Supervision: Gildas Ratié (gildas.ratie@univ-nantes.fr)

Collaborators: Daniel F. Araújo (IFREMER), Diego Baragaño (CSIC), Veronika Veselská (CATRIN).