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A conceptual and empirical model for the combined influence
of oxidation/reduction reactions and transport processes on
the fate of selenium contaminated sediments in the Central Valley
has been developed and evaluated. Interestingly, in the presence
of a fluctuating water table, the combined effects of these
processes enable a net transport of selenium in the opposite
direction of the net flux of water. From a macroscopic perspective,
the processes are now well understood and more than decade of
field monitoring data is available to both calibrate and test
this model. When examined however from a more fundamental point
of view many outstanding issues remain. Chief among these, and
critical to a satisfactory understanding of the problem, are
the factors that control the kinetics of selenium oxidation/reduction
reactions and how and why these vary in space and time.
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