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

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Dynamic Equilibrium of Freshwater–Saltwater Interfacept interface are considered under steady-state conditions. Classical approaches to the determination of the shape of the interface at equilibrium related to the two benchmark problems, seawater intrusion in a costal aquifer, and saltwater upcoming beneath a partially penetrating pumping well, are re

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Studying Subsurface Density-Induced Phenomena Using Numerical Modelingerent scenarios of leakage of industrial waste from surface reservoirs, as well as a scenario of upward saltwater movement from a deeper saltwater zone into the freshwater zone in response to pumping into a well using different modeling technique. Numerical modeling emerged here as one of the primar

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Advection and Dispersion of Dissolved Species in Aquifersn in homogeneous and heterogeneous aquifers. In this chapter, we will consider the migration models that describe the motion of solutions miscible with groundwater in homogeneous aquifers. The solute migration processes in heterogeneous (stratified and fracturedporous) systems will be discussed in separate chapters.

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One-Dimensional Hydrodynamic Mixing Models for Regional Flow Systems Under Areal Recharge Conditionsn in homogeneous and heterogeneous aquifers. In this chapter, we will consider the migration models that describe the motion of solutions miscible with groundwater in homogeneous aquifers. The solute migration processes in heterogeneous (stratified and fracturedporous) systems will be discussed in separate chapters.

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Conceptual Lumped-Parameter Models for Coupled Transient Flow and Solute Transport in Catchmentsy simplifies the search of solute transport problem that makes practically possible the long-range prediction of chemical component distributions between the near-surface domain and the aquifer system relying on a restricted number of hydrogeological parameters.

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Models for Tracer Test Analysis and Interpretationtion about solute transport properties of systems featuring natural hydrogeochemical stratification. Those models are next modified to account for density difference between the fluids in contact (see Secs. 12.3 and 14.2).