Access the full text.
Sign up today, get DeepDyve free for 14 days.
C. Wilson, P. Smart (1984)
Pipes and pipe flow process in an upland catchment, WalesCatena, 11
K. Beven (1981)
Micro-, Meso-, Macroporosity and Channeling Flow Phenomena in SoilsSoil Science Society of America Journal, 45
M. Mosley (1982)
Subsurface flow velocities through selected forest soils, South Island, New ZealandJournal of Hydrology, 55
M. Mosley (1979)
Streamflow generation in a forested watershed, New ZealandWater Resources Research, 15
M. Sklash, M. Stewart, A. Pearce (1986)
Storm Runoff generation in humid headwater catchments 2. A case study of hillslope and low-order stream responseWater Resources Research, 22
Rowe Rowe (1979)
Rainfall interception by a beech‐podocarp‐hardwood forest near Reefton, North Westland, New ZealandJ. Hydrol. N. Z., 18
M. Mccaig (1983)
Contributions to storm quickflow in a small headwater catchment—the role of natural pipes and soil macroporesEarth Surface Processes and Landforms, 8
K. Perroux, P. Raats, D. Smiles (1982)
Wetting Moisture Characteristic Curves Derived from Constant-rate Infiltration into Thin Soil Samples1Soil Science Society of America Journal, 46
Pearce Pearce, Stewart Stewart, Sklash Sklash (1986)
Storm runoff generation in humid headwater catchments, 1, Where does the water come from?Water Resour. Res., 22
J. Bouma, A. Jongerius, O. Boersma, A. Jager, D. Schoonderbeek (1977)
The Function of Different Types of Macropores During Saturated Flow through Four Swelling Soil Horizons1Soil Science Society of America Journal, 41
J. McDonnell (1988)
The age, origin and pathway of subsurface stormflow in a steep humid headwater catchment.
Wilson Wilson, Smart Smart (1984)
Pipes and pipeflow in an upland catchmentCatena, 11
T. Stiphout, H. Lanen, O. Boersma, J. Bouma (1987)
The effect of bypass flow and internal catchment of rain on the water regime in a clay loam grassland soilJournal of Hydrology, 95
K. Smettem, S. Trudgill, A. Pickles (1983)
Nitrate loss in soil drainage waters in relation to by‐passing flow and discharge on an arable siteEuropean Journal of Soil Science, 34
P. Germann (1986)
Rapid drainage response to precipitationHydrological Processes, 1
J. McDonnell (1990)
The influence of macropores on debris flow initiationQuarterly Journal of Engineering Geology, 23
F. Stauffer, T. Dracos (1986)
Experimental and numerical study of water and solute infiltration in layered porous mediaJournal of Hydrology, 84
Clothier Clothier, Wooding Wooding (1983)
The soil diffusivity near saturationSoil Sci. Soc. Am. J., 47
A. Pearce, M. Stewart, M. Sklash (1986)
Storm runoff generation in humid headwater catchments 1
B. Clothier, R. Wooding (1983)
The Soil Water Diffusivity Near SaturationSoil Science Society of America Journal, 47
J. Bouma, J. Anderson (1973)
Relationships Between Soil Structure Characteristics and Hydraulic Conductivity 1
A. Abdul, R. Gillham (1984)
Laboratory Studies of the Effects of the Capillary Fringe on Streamflow GenerationWater Resources Research, 20
Jones Jones (1979)
Extending the Hewlett model of storm runoff generationArea, 11
J. McDonnell, M. Bonell, M. Stewart, A. Pearce (1990)
Deuterium variations in storm rainfall: Implications for stream hydrograph separationWater Resources Research, 26
K. Beven, P. Germann (1982)
Macropores and water flow in soilsWater Resources Research, 18
R. Ragan (1968)
An experimental investigation of partial area contribution., 76
J. Webster (1977)
The hydrologic properties of the forest floor under beech/podocarp/hardwood forest, North Westland
G. Thomas, R. Phillips, V. Quisenberry (1978)
CHARACTERIZATION OF WATER DISPLACEMENT IN SOILS USING SIMPLE CHROMATOGRAPHIC THEORYEuropean Journal of Soil Science, 29
J. Bouma (1981)
Soil morphology and preferential flow along macroporesAgricultural Water Management, 3
J. Hewlett, A. Hibbert (1967)
Factors affecting the response of small watersheds to precipitation in humid areas
R. Gillham (1984)
The capillary fringe and its effect on water-table responseJournal of Hydrology, 67
Scotter Scotter (1978)
Preferential solute movement through larger soil voids, 1, some computations using simple theoryAust. J. Soil Res., 16
Scotter (1978)
Preferential solute movement through larger soil voids. I. Some computations using simple theorySoil Research, 16
Bouma Bouma, Anderson Anderson (1973)
Relationships between soil structure characteristics and hydraulic conductivity, Field Soil Water RegimeSpec. Publ. Soil Sci. Soc. Am., 5
J. Jones (1987)
The effects of soil piping on contributing areas and erosion patternsEarth Surface Processes and Landforms, 12
R. Luxmoore (1981)
Micro-, Meso-, and Macroporosity of SoilSoil Science Society of America Journal, 45
M. Sklash, R. Farvolden (1979)
The Role Of Groundwater In Storm RunoffJournal of Hydrology, 43
Simultaneous observations of rapid preferential flow through macropores and isotopically “Old” water displacement remain unresolved in the Maimai (M8) catchment. Continuous, three‐dimensional soil moisture energy conditions were monitored in two discrete catchment positions for a series of storm events in 1987. Tensiometric response was related to the soil water characteristic curve, hillslope throughflow, and total catchment runoff. For events yielding ≪2 mm hr−1 peak runoff, near‐stream valley bottom groundwater systems discharged water volumes sufficient to account for storm period streamflow. This process was assisted by regular low (<−40 cm H2O) matric potential conditions and rapid filling of available soil water storage. For events yielding >2 mm hr−1 peak storm flow, hillslope hollow drainage into steeply sloping first‐order channels dominated old water production and most of the catchment storm flow. Highly transient macropore‐driven processes of crack infiltration (bypass flow), slope water table development, and lateral pipe flow enabled large volumes of stored water to be delivered to the first‐order channel bank at the appropriate time to satisfy catchment storm flow volumes and water isotopic and chemical composition.
Water Resources Research – Wiley
Published: Nov 1, 1990
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.