Titlebook: Subsurface Solute Transport Models and Case Histories; With Applications to Vyacheslav G. Rumynin Book 2011 Springer Science+Business Media

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Dynamics of Saltwater–Freshwater Interfacet of the interface between displacing and displaced fluids in a confined homogeneous aquifer is analyzed. In the second part of the chapter (Sect. 13.2) we will examine how some ideas of the two-phase flow theory can be used to model the migration of brine in fresh water aquifer systems.

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Book 2011nalysis coupled with modeling (analytical and numerical) tool application. The relevant theoretical developments are concerned mainly with the formulation and solution of deterministic mass-transport equations for a wide range of engineering issues in groundwater quality assessment and forecasting..

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Unsteady-State Hydrogeological Model of Evaporation-Induced Sedimentation in a Surface Reservoirey often involve some simplifying assumptions, for example, the evaporation rate from the water surface may be assumed constant (the dependence of evaporation rate form salt concentration in the solution is not taken into account), which is only true in a certain range of water mineralization values.

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Studying Subsurface Density-Induced Phenomena Using Numerical Modelingies dissolved in the water can vary substantially throughout the modeled area, affecting the flow pattern, and the latter, in turn, affects the change in concentration field. Thus, the flow and transport problems are coupled.

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