Fungi in the Hyporheic Zone of a Springbrook
✍ Scribed by F. Bärlocher; L. G. Nikolcheva; K. P. Wilson; D. D. Williams
- Publisher
- Springer
- Year
- 2006
- Tongue
- English
- Weight
- 364 KB
- Volume
- 52
- Category
- Article
- ISSN
- 0095-3628
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Saturated flow is typically assumed for seepage from a stream underlain by an alluvial aquifer. However, if the water table falls a sufficient distance below a semipervious streambed, the head losses in this less conductive layer will cause the region beneath the stream, or hyporheic zone, to become
## Abstract Dam operations commonly cause large, frequent fluctuations in river stage, which persist for long distances downstream. The stage fluctuations force river water into and out of the banks, defining lateral hyporheic exchange paths. To evaluate the penetration distance and rates of dam‐in