Spatial patterns of hyporheic exchange and biogeochemical cycling around cross‐vane restoration structures: Implications for stream restoration design | Zendy

Gordon Ryan P. | Zendy; Lautz Laura K. | Zendy; Daniluk Timothy L. | Zendy

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Spatial patterns of hyporheic exchange and biogeochemical cycling around cross‐vane restoration structures: Implications for stream restoration design

Author(s) -

Gordon Ryan P.,

Lautz Laura K.,

Daniluk Timothy L.

Publication year - 2013

Publication title -

water resources research

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.863

H-Index - 217

eISSN - 1944-7973

pISSN - 0043-1397

DOI - 10.1002/wrcr.20185

Subject(s) - biogeochemical cycle , hyporheic zone , environmental science , stream restoration , cycling , hydrology (agriculture) , stream bed , flux (metallurgy) , streams , geology , ecology , geomorphology , environmental engineering , surface water , geography , materials science , geotechnical engineering , sediment , computer science , computer network , archaeology , metallurgy , biology

Key Points In‐stream restoration structures do not create single, deep hyporheic flow cells Patterns of flux around secondary pools and riffles dominate the streambed area Hyporheic exchange volumes are ∼0.4% of discharge in restored reaches of 45–55 m

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