Publications by authors named "S Savoye"

Article Synopsis
  • - The study investigates how salinity gradients affect the diffusion properties of clayey materials, specifically using through-diffusion experiments with vermiculite samples to compare conditions with and without these gradients.
  • - Two diffusion models were utilized: a classical Fickian model and a reactive transport code, CrunchClay, to analyze the multi-porosity diffusion processes in the presence of charged surfaces.
  • - The findings revealed that water primarily diffused through interparticle porosity rather than interlayer porosity, and highlighted the necessity for a model with at least three types of porous volumes to accurately represent the diffusion behavior of different species under varying salinity conditions.
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The Abinky formation, composed of analcimolites (i.e., rocks with <70 wt% analcime), underlies Tchirezrine II, which hosts the Imouraren (Niger) uranium deposit.

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Ra is an ultra-trace element with important environmental implications for many industries (including water treatment and oil and mineral extraction). Its extremely low concentrations in natural environments do not allow for direct observation and measurement of the Ra-bearing minerals governing Ra mobility. To better understand the retention processes for Ra in rocks and soil, a synthesized assemblage of Ra-doped minerals was made, combining montmorillonite, ferrihydrite and barite.

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Liquid-liquid partition coefficient is a useful tool to predict biological and environmental fate of organic compounds, for example bioaccumulation or toxicity of lipophilic contaminants. Conversely, the partitioning of ionizable compounds is poorly studied in contrast to that of neutral compounds. Yet, such topic deserves attention, since numerous organic contaminants are ionizable as well as their degradation products.

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Diffusion is the main transport process of water and solutes in clay-rich porous media owing to their very low permeability, so they are widely used as barriers against contaminant spreading. However, the prediction of contaminant mobility can be very complicated when these media are partially water-saturated. We conducted diffusion experiments for water (HTO and HDO) and ions (Na and I) through partially water saturated compacted kaolinite, a weakly charged clay material, to quantify the distinct diffusive behavior of these species.

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