A 2-year study was conducted to evaluate the ecological status of 12 acid-sensitive and 12 non-acid-sensitive Maryland coastal plain streams during the spring, summer, and fall of 1992 to 1993. An index of biotic integrity (IBI) for fish, chemical parameters, and physical habitat conditions were eva
Hydraulic characteristics of a small Coastal Plain stream of the southeastern United States: effects of hydrology and season
✍ Scribed by Hwa-Seong Jin; G. Milton Ward
- Publisher
- John Wiley and Sons
- Year
- 2005
- Tongue
- English
- Weight
- 222 KB
- Volume
- 19
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.5878
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
Various physical and biological properties affect solute transport patterns in streams. We measured hydraulic characteristics of Payne Creek, a low‐gradient upper Coastal Plain stream, using tracer experiments and parameter estimation with OTIS‐P (one‐dimensional transport with inflow and storage with parameter optimization). The primary objective of this study was to estimate the effects of varying discharge, season, and litter accumulation on hydraulic parameters. Channel area A ranged from 0·081 to 0·371 m^2^ and transient storage area A~s~ ranged from 0·027 to 0·111 m^2^. Dispersion D ranged from 1·5 to 11·1 m^2^ min^−1^ and exchange coefficient α ranged from 0·009 to 0·038 min^−1^. Channel area and dispersion were positively correlated to discharge Q, whereas storage area and exchange coefficient were not. Relative storage size A~s~/A ranged from 0·17 to 0·59, and was higher during fall than other seasons under a similar Q. The fraction of median travel time due to transient storage $F_{\rm med}^{200}$ ranged from 8·8 to 34·5% and was significantly correlated with Q through a negative power function. Both metrics indicated that transient storage was a significant component affecting solute transport in Payne Creek, especially during the fall. Comparison between the measured channel area A~c~ and A suggested that surface storage was dominant in Payne Creek. During fall, accumulation of leaf litter resulted in larger A and A~s~ and lower velocity and D than during other seasons with similar discharge. Seasonal changes in discharge and organic matter accumulation, and dynamic channel morphology affected the magnitude of transient storage and overall hydraulic characteristics of Payne Creek. Copyright © 2005 John Wiley & Sons, Ltd.
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