Mechanisms responsible for streamflow generation on a small, salt‐affected and deeply weathered hillslope
- 1 June 1993
- journal article
- research article
- Published by Wiley in Earth Surface Processes and Landforms
- Vol. 18 (4), 291-309
- https://doi.org/10.1002/esp.3290180402
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Interactions between perched and saprolite aquifers on a small, salt-affected and deeply weathered hillslopeEarth Surface Processes and Landforms, 1993
- Analysis of streamflow generation following deforestation in southwest Western AustraliaJournal of Hydrology, 1989
- Response of input and output of water and chloride to clearing for agricultureJournal of Hydrology, 1987
- The mechanisms of catchment flow processes using natural variations in deuterium and oxygen-18Journal of Hydrology, 1987
- An approximate method for partitioning daily streamflow dataJournal of Hydrology, 1984
- A review of catchment experiments to determine the effect of vegetation changes on water yield and evapotranspirationJournal of Hydrology, 1982
- The role of groundwater in storm runoffJournal of Hydrology, 1979
- The relationship between throughflow generation and the solute concentration of soil and stream waterEarth Surface Processes and Landforms, 1979
- Throughflow as a mechanism responsible for excessive soil salinisation in non-irrigated, previously arable lands in the Western Australian wheatbelt: A field studyCATENA, 1975
- Two Weirs for Accurate Stream‐Gaging of Small WatershedsWater Resources Research, 1968