4.7 Editorial Material

Modeling the Effects of Turbulence on Hyporheic Exchange and Local-to-Global Nutrient Processing in Streams

Journal

WATER RESOURCES RESEARCH
Volume 54, Issue 9, Pages 5883-5889

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2018WR023078

Keywords

streams; turbulence; nutrients; hyporheic; biogeochemistry; sediment

Funding

  1. U.S. NSF Partnerships for International Research and Education [OISE-1243543]
  2. UC Office of the President Multi-campus Research Program Initiative award [MRP-17-455083]
  3. USGS River Corridor Powell Center
  4. U.S. Department of Energy (DOE), Office of Biological and Environmental Research (BER), as part of BER's Subsurface Biogeochemistry Research Program (SBR)
  5. Australian Research Council [DP120102500]

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New experimental techniques are allowing, for the first time, direct visualization of mass and momentum transport across the sediment-water interface in streams. These experimental insights are catalyzing a renaissance in our understanding of the role stream turbulence plays in a host of critical ecosystem services, including nutrient cycling. In this commentary, we briefly review the nature of stream turbulence and its role in hyporheic exchange and nutrient cycling in streams. A simple process-based model, borrowed from biochemical engineering, provides the link between empirical relationships for grain-scale turbulent mixing and nutrient processing at reach, catchment, continental, and global scales.

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