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are conducted to characterize the transport of these agents into both saturated and unsaturated porous media using non-Newtonian solutions. The reactivity of the reducers on chlorinated solvents will also be
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of dissolved substances in heterogeneous, partially-saturated porous media. In order for these models to be predictive, the impact of saturation degree on point velocity statistics and their correlation
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Title: Capillary pressure, relative permeability and wettability at critically-low saturated porous media (CRISP) Application deadline: as long as possible until Dec 24 Research theme: Porous Media
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are difficult to model and simulate accurately, and in porous media the multiple disparate lengthscales further complicates matters. However, this multi-scale setting also provides beautiful mathematical
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in English (level B2 to C1 Common Framework of Reference for Languages). He/she will be familiar with basic concepts in fluid mechanics and statistics. Fluid flow in porous media plays a central role
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this manufacturing process. We will start with standard models for flow in porous media and adapt them to the particularities of electrode wetting. Such models can later be extended to describe more complex phenomena
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are difficult to model and simulate accurately, and in porous media the multiple disparate lengthscales further complicates matters. However, this multi-scale setting also provides beautiful mathematical
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» Computational physicsEducation LevelMaster Degree or equivalent Skills/Qualifications good konwledge in solid mechanics, damage mechanics, fracture mechanics, fluid flow in porous media, discretization of PDE
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fundamental and in more applied directions. The center works to advance the understanding of porous media by developing theories, principles, tools and methods to replace ad hoc approaches to porous media with
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storage and evaporative flow requires a very good understanding of the phenomena in porous media. Evaporation in a porous medium is a complex phenomenon where water vapor diffusion, liquid water flow and