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K. Northcote, G. Hubble, R. Isbell, C. Thompson, E. Bettenay (1975)
A description of Australian soils.
Zaslavsky Zaslavsky, Sinai Sinai (1981a)
Surface hydrology: I. Explanation of phenomenaJournal of the Hydraulics Division; Proceedings, American Society of Civil Engineers, 107
A. Shirmohammadi, W. Knisel, J. Sheridan (1984)
An approximate method for partitioning daily streamflow dataJournal of Hydrology, 74
R. George, A. Conacher (1993)
Interactions between perched and saprolite aquifers on a small, salt‐affected and deeply weathered hillslopeEarth Surface Processes and Landforms, 18
J. Turner, D. Macpherson, R. Stokes (1987)
The mechanisms of catchment flow processes using natural variations in deuterium and oxygen-18Journal of Hydrology, 94
M. Anderson, T. Burt (1982)
The contribution of throughflow to storm runoff: An evaluation of a chemical mixing modelEarth Surface Processes and Landforms, 7
Turner Turner, MacPherson MacPherson, Stokes Stokes (1987)
The mechanisms of catchment flow using natural variations in deuterium and oxygen‐18Journal of Hydrology, 94
Zaslavsky Zaslavsky, Sinai Sinai (1981b)
Surface hydrology: III. Causes of lateral flowJournal of the Hydraulics Division; Proceedings, American Society of Civil Engineers, 107
J. Ruprecht, N. Schofield (1989)
Analysis of streamflow generation following deforestation in southwest Western AustraliaJournal of Hydrology, 105
A. Conacher, S. Neville, P. King (1983)
Evaluation of throughflow interceptors for controlling secondary soil and water salinity in dryland agricultural areas of southwestern Australia : II. Hydrological studyApplied Geography, 3
Journal of Hydrology, Special Edition, 94
D. Mcghie (1980)
The contribution of the mallet hill surface to runoff and erosion in the Narrogin region of Western AustraliaSoil Research, 18
W. Nutter, W. Sopper (1968)
Two Weirs for Accurate Stream-Gaging of Small WatershedsWater Resources Research, 4
T. Burt (1979)
The relationship between throughflow generation and the solute concentration of soil and stream water, 4
M. Anderson, T. Burt (1978)
The role of topography in controlling throughflow generationEarth Surface Processes and Landforms, 3
D. Williamson, R. Stokes, J. Ruprecht (1987)
Response of input and output of water and chloride to clearing for agricultureJournal of Hydrology, 94
B. Sadler, P. Williams (1981)
The evolution of a regional approach to salinity management in Western AustraliaAgricultural Water Management, 4
Pearce Pearce, Stewart Stewart, Sklash Sklash (1986)
Storm runoff generation in humid headwater catchments, 1. Where does the water come from?Water Resources Research, 22
A. Conacher (1975)
Throughflow as a mechanism responsible for excessive soil salinisation in non-irrigated, previously arable lands in the Western Australian wheatbelt: A field studyCatena, 2
J. Bosch, J. Hewlett (1982)
A REVIEW OF CATCHMENT EXPERIMENTS TO DETERMINE THE EFFECT OF VEGETATION CHANGES ON WATER YIELD AND EVAPOTRANSPIRATIONJournal of Hydrology, 55
J. Turner, D. Macpherson (1990)
Mechanisms Affecting Streamflow and Stream Water Quality: An Approach via Stable Isotope, Hydrogeochemical,and Time Series AnalysisWater Resources Research, 26
A. Pearce, M. Stewart, M. Sklash (1986)
Storm runoff generation in humid headwater catchments 1
McArthur McArthur, Churchwood Churchwood, Hick Hick (1977)
Landforms and soils of the Murray River catchment areaCSIRO Australian Division, Land Research Management Series, 3
Department of Agriculture, Technical Report, 81
George George (1990)
The 1989 saltland surveyJournal of Agriculture, Western Australia, 31
E. O'Loughlin (1986)
Prediction of Surface Saturation Zones in Natural Catchments by Topographic AnalysisWater Resources Research, 22
Burt Burt (1979)
The relationship between throughflow generation and solute concentration of stream and soil‐waterEarth Surface Processes, 4
M. Sklash, R. Farvolden (1979)
The Role Of Groundwater In Storm RunoffJournal of Hydrology, 43
Sadler Sadler, Williams Williams (1981)
The evolution of a regional approach to salinity managementAgricultural Water Management, 4
This paper considers the contributions of overland flow, throughflow and deep seepage to the generation of streamflow in a salt‐affected, deeply weathered landscape. Runoff mechanisms on a small hillslope in south‐western Australia were dependent on the extent and development of variable source areas. In winter, streamflow generation was controlled by returnflow, saturation overland flow and throughflow. In summer, post‐ponding, infiltration‐excess and saturation overland flow dominated. The extent of the variable source area and the magnitude of streamflow were due to antecedent soil moisture, rainfall and slope morphology. Concave hillslope sections accumulated soil moisture due to both saturated and unsaturated lateral flow processes. Throughflow provided the mechanism and vehicle for solute movement from the groundwater discharge area to the stream. However, discharge from the deep aquifer was the primary mechanism responsible for soil salinity and maintaining the core of the variable source area. Estimates of throughflow which only take account of soil‐water movement and disregard returnflow, will underestimate the magnitude of throughflow.
Earth Surface Processes and Landforms – Wiley
Published: Jun 1, 1993
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