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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