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Models for Assessment of Transverse Diffusive and Advective Transfer in Regional Two-Layer Systems

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

Abstract

In many groundwater systems, the porous media have near-horizontal layered structures that have been formed by natural sedimentology processes. Diffusive transfer of solute mass between layers differing in hydraulic conductivity is a key smoothing mechanism of concentration profiles in such stratified groundwater systems. A result of this process is the higher rate of mass transfer in layers with lower permeability and its lower rate in layers with higher permeability.

Keywords

Solute Transport Permeable Layer Transverse Dispersion High Iodine Concentration Single Fissure 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© 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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