One-Dimensional Hydrodynamic Mixing Models for Regional Flow Systems Under Areal Recharge Conditions and Their Application to the Interpretation of Isotopic Data

  • Vyacheslav G. RumyninEmail author
Part of the Theory and Applications of Transport in Porous Media book series (TATP, volume 25)


The transfer of chemical components that, when in solutions, have no effect on the physical properties of aquifer materials and groundwater, is inseparable from the groundwater flow. Their advective transport involves micro- and macrodispersion processes, which control the extent of solute dispersion 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.


Groundwater Flow Groundwater Vulnerability Liquid Radioactive Waste Tritium Concentration Radioactive Waste 
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© Springer Science+Business Media B.V. 2011

Authors and Affiliations

  1. 1.Geological DepartmentThe Russian Academy of Sciences Institute of Environmental Geology Saint Petersburg Division Saint Petersburg State UniversitySt. PetersburgRussian Federation

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