Titlebook: Mathematical Modeling of Groundwater Pollution; Ne-Zheng Sun Book 1996 Springer Science+Business Media New York 1996 Adsorption.Filtration

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Numerical Solutions of Advection-Dominated Problems,we have stated that when the FDM is used for solving advection-dominated problems, two kinds of errors, numerical dispersion and overshoot, will occur. As a result, oscillations will appear around concentration fronts and steep concentration fronts cannot be accurately calculated. In Chapter 5, we p

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es are de- pendent on groundwater. As an "open" system, groundwater may exchange mass and energy with its neighboring systems (soil, air, and surface water) through adsorption, ion-exchange, infiltration, evaporation, inflow, outflow, and other exchange forms. Consequently, both the quantity and qua

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Book 1996 pendent on groundwater. As an "open" system, groundwater may exchange mass and energy with its neighboring systems (soil, air, and surface water) through adsorption, ion-exchange, infiltration, evaporation, inflow, outflow, and other exchange forms. Consequently, both the quantity and quality of gr

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Finite Difference Methods and the Method of Characteristics for Solving Hydrodynamic Dispersion Equown function are obtained. These discrete values approximately describe the time-space distribution of the unknown variable. We will see that exactly the same steps can be used to solve advection-dispersion problems.

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978-1-4757-2560-5Springer Science+Business Media New York 1996

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