An application of the plaster dissolution method for quantifying water velocity in the shallow hyporheic zone of an Appalachian stream system
Author:
Affiliation:
1. *United States Forest Service, Northeastern Forest Experiment Station, Timber and Watershed Laboratory, Parsons, WV 26287, U.S.A.
2. †Department of Biology, Marshall University, Huntington, WV 25755, U.S.A.
Publisher
Wiley
Subject
Aquatic Science
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-2427.1998.00280.x
Reference44 articles.
1. Adams M.B. Kochenderfer J.N. Wood F. Angradi T.R. Edwards P.1994Forty years of hydrometeorological data from the Fernow Experimental Forest West Virginia USDA Forest Service Northeastern Forest Experiment Station General Technical Report NE‐184.
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3. Stream ecology and surface-hyporheic hydrologic exchange: Implications, techniques and limitations
4. Spatial distribution and taxonomic composition of the hyporheos of several Sonoran Desert streams.;Boulton A.J.;Archiv für Hydrobiologie,1992
5. Differentiation between epigeic and hypogeic fauna in gravel streams
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