Effective diffusivity and mass flux across the sediment-water interface in streams

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Effective diffusivity and mass flux across the sediment-water interface in streams

[1] The exchange of water between a stream and its hyporheic zone (defined as the sediment beneath and immediately adjacent to a stream) underpins many ecological and hydrological functions in turbulent streams. Hyporheic exchange can be parameterized in terms of an effective diffusion coefficient Deff and considerable effort has gone into developing process-based models and empirical correlati...

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ژورنال

عنوان ژورنال: Water Resources Research

سال: 2012

ISSN: 0043-1397

DOI: 10.1029/2011wr011148