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- W2058936701 abstract "Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equation with fractional time derivative of order γ, which may vary from 0 to 1. Accounting for diffusion in the surrounding rock mass leads to the introduction of an additional fractional time derivative of order 1∕2 in the equation for solute transport. The closed-form solutions for concentrations in the aquifer and surrounding rocks are obtained for the arbitrary time-dependent source of contamination located in the inlet of the aquifer. Based on these solutions, different regimes of contamination of the aquifers with different physical properties are modeled and analyzed." @default.
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- W2058936701 date "2007-03-30" @default.
- W2058936701 modified "2023-09-28" @default.
- W2058936701 title "Simulation of Contaminant Transport in a Fractured Porous Aquifer" @default.
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- W2058936701 doi "https://doi.org/10.1115/1.2754327" @default.
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