Gas transfer velocity (k600) increases with discharge in steep streams but not in low‐slope streams

Abstract Gas transfer velocity (k600) controls gas fluxes between aquatic ecosystems and the atmosphere. In streams, k600 is controlled by turbulence and, thus, local hydrology and geomorphology. Resultantly, variability in k600 can be large and modeling k600 from physical parameters can have large...

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Bibliographic Details
Main Authors: Kelly S. Aho, Kaelin M. Cawley, Robert O. Hall Jr., Robert T. Hensley, Walter K. Dodds, Nicolas Harrison, Keli J. Goodman
Format: Article
Language:English
Published: Wiley 2025-06-01
Series:Limnology and Oceanography Letters
Online Access:https://doi.org/10.1002/lol2.70003
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