Access the full text.
Sign up today, get DeepDyve free for 14 days.
R. Freeze, P. Witherspoon (1968)
Theoretical Analysis of Regional Ground Water Flow: 3. Quantitative InterpretationsWater Resources Research, 4
G. Pinder, S. Sauer (1971)
Numerical Simulation of Flood Wave Modification Due to Bank Storage EffectsWater Resources Research, 7
J. Tóth (1963)
A Theoretical Analysis of Groundwater Flow in Small Drainage BasinsJournal of Geophysical Research, 68
P. Wiberg, J. Smith (1991)
Velocity distribution and bed roughness in high‐gradient streamsWater Resources Research, 27
S. Hendricks, D. White (1991)
Physicochemical Patterns within a Hyporheic Zone of a Northern Michigan River, with Comments on Surface Water patterns'Canadian Journal of Fisheries and Aquatic Sciences, 48
K. Prestegaard (1983)
Bar resistance in gravel bed streams at bankfull stageWater Resources Research, 19
N. Castro, G. Hornberger (1991)
Surface-subsurface water interactions in an alluviated mountain stream channelWater Resources Research, 27
Q. Singewald (1955)
Sugar Loaf and St. Kevin mining districts, Lake County, Colorado
Bencala Bencala, McKnight McKnight, Zellweger Zellweger (1990)
Characterization of transport in an acidic stream based on lithium tracer injection and simulations of transient storageWater Resour. Res.
B. Levy, R. Chambers (1987)
Bromide as a conservative tracer for soil-water studiesHydrological Processes, 1
F. Triska, V. Kennedy, R. Avanzino, G. Zellweger, K. Bencala (1989)
RETENTION AND TRANSPORT OF NUTRIENTS IN A THIRD-ORDER STREAM IN NORTHWESTERN CALIFORNIA: HYPORHEIC PROCESSES'Ecology, 70
G. Grant, F. Swanson, M. Wolman (1990)
Pattern and origin of stepped-bed morphology in high-gradient streams, Western Cascades, OregonGeological Society of America Bulletin, 102
K. Bencala, D. McKnight, G. Zellweger (1990)
Characterization of transport in an acidic and metal-rich mountain stream based on a lithium tracer injection and simulations of transient storageWater Resources Research, 26
J. Bear (1975)
Dynamics of Fluids in Porous MediaSoil Science, 120
M. Kirkby, K. Beven (1979)
A physically based, variable contributing area model of basin hydrology, 24
W. Gburek, J. Urban (1990)
The Shallow Weathered Fracture Layer in the Near–Stream ZoneGround Water, 28
V. Kennedy, A. Jackman, S. Zand, G. Zellweger, R. Avanzino (1984)
Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 2. Mathematical modelingJournal of Hydrology, 75
S. Savant, D. Reible, L. Thibodeaux (1987)
Convective transport within stable river sedimentsWater Resources Research, 23
T. Dunne, R. Black (1970)
Partial Area Contributions to Storm Runoff in a Small New England WatershedWater Resources Research, 6
L. Thibodeaux, J. Boyle (1987)
Bedform-generated convective transport in bottom sedimentNature, 325
D. McKnight, B. Kimball, K. Bencala (1988)
Iron Photoreduction and Oxidation in an Acidic Mountain StreamScience, 240
D. White, Charles Elzinga, S. Hendricks (1987)
Temperature Patterns within the Hyporheic Zone of a Northern Michigan RiverJournal of the North American Benthological Society, 6
By Cooper, M. Rorabaugh, GROUND-WATER Hydraulics, William Pecora (1963)
Ground-water movements and bank storage due to flood stages in surface streams
A. Elliott (1990)
Transfer of solutes into and out of streambeds
K. Bencala, V. Kennedy, G. Zellweger, A. Jackman, R. Avanzino (1984)
Interactions of solutes and streambed sediment: 1. An experimental analysis of cation and anion transport in a mountain streamWater Resources Research, 20
R. Freeze (1972)
Role of subsurface flow in generating surface runoff: 2. Upstream source areasWater Resources Research, 8
J. Whittaker (1987)
Modelling bed-load transport in steep mountain streamsIAHS-AISH publication
T. Winter (1983)
The interaction of lakes with variably saturated porous mediaWater Resources Research, 19
E. Keller, F. Swanson (1979)
EFFECTS OF LARGE ORGANIC MATERIAL ON CHANNEL FORM AND FLUVIAL PROCESSESEarth Surface Processes and Landforms, 4
Vaux Vaux (1968)
Intragravel flow and interchange of water in a streambedFish. Bull.
R. Bowman (1984)
Evaluation of Some New Tracers for Soil Water StudiesSoil Science Society of America Journal, 48
A numerical hydrological simulation suggested that water exchange between stream channels and adjacent aquifers is enhanced by convexities and concavities in streambed topography. At St. Kevin Gulch, an effluent stream in the Rocky Mountains of Colorado, subsurface hydraulic gradients and movement of ionic tracers indicated that stream water was locally recharged into well‐defined flow paths through the alluvium. Stream water‐filled flow paths in the alluvium (referred to as substream flow paths) returned to the stream a short distance downstream (1 to 10 m). Recharge to the substream flow paths occurred where stream water slope increased, at the transition from pools (<1%) to steeper channel units (5–20%). Return of substream flow paths to the stream occurred where stream water slope decreased, at the transition from steeper channel units to pools. A net water flux calculation is typically used to characterize water and solute fluxes between surface and subsurface zones of catchments. Along our study reach at St. Kevin Gulch the net inflow of water from subsurface to stream (1.6 mL s−1 m−1) underestimated the gross inflow (2.7 mL s−1 m−1) by 40%. The influence of streambed topography is to enhance hydrological fluxes between stream water and subsurface zones and to prolong water‐sediment contact times; these effects could have important consequences for solute transport, retention, and transformation in catchments.
Water Resources Research – Wiley
Published: Jan 1, 1993
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.