A model for lateral hyporheic flow based on valley slope and channel sinuosity
Author:
Affiliation:
1. Department of Geological Sciences; University of Texas at Austin; Austin Texas USA
Publisher
American Geophysical Union (AGU)
Subject
Water Science and Technology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2008WR007442/fullpdf
Reference39 articles.
1. Effect of stream channel size on the delivery of nitrogen to the Gulf of Mexico;Alexander;Nature,2000
2. Lateral organization of aquatic invertebrates along the corridor of a braided floodplain river;Arscott;J. N. Am. Benthol. Soc.,2005
3. Biophysical controls on organic carbon fluxes in fluvial networks;Battin;Nat. Geosci.,2008
4. Simulation of solute transport in a mountain pool-and-riffle stream: A transient storage model;Bencala;Water Resour. Res.,1983
5. Sinuosity-driven hyporheic exchange in meandering rivers;Boano;Geophys. Res. Lett.,2006
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