A multiscale model coupling macroscale transport to microscale moving boundaries for colloid deposition is shown to admit weak solutions when pores do not fully clog, with numerical experiments quantifying the resulting changes to dispersion and storage capacity.
Coupling scales in process-based soil organic carbon modeling including dynamic aggregation
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A mathematical model for colloids deposition in porous media combined with a moving boundary at the microscale: Solvability and numerical simulation
A multiscale model coupling macroscale transport to microscale moving boundaries for colloid deposition is shown to admit weak solutions when pores do not fully clog, with numerical experiments quantifying the resulting changes to dispersion and storage capacity.