Quantifying Macropore Recharge: Examples from a Semi‐Arid Area
- 1 November 1997
- journal article
- Published by Wiley in Groundwater
- Vol. 35 (6), 1097-1106
- https://doi.org/10.1111/j.1745-6584.1997.tb00182.x
Abstract
No abstract availableThis publication has 19 references indexed in Scilit:
- An Isotopic Study (2H and 18O) of Water Movements in Clayey Soils Under a Semiarid ClimateWater Resources Research, 1996
- Chemical and Isotopic Methods for Quantifying Ground‐Water Recharge in a Regional, Semiarid EnvironmentGroundwater, 1995
- Improvements in the gaseous hydrogen-water equilibration technique for hydrogen isotope-ratio analysisAnalytical Chemistry, 1991
- Interpretation of solute profile dynamics in irrigated soilsIrrigation Science, 1990
- A method to extract soil water for stable isotope analysisJournal of Hydrology, 1990
- Inferences about solute transport in macroporous forest soils from time series modelsGeoderma, 1990
- Preferential flow and the generation of runoff: 2. Boundary-layer flow theoryWater Resources Research, 1990
- Estimating Macroporosity in a Forest Watershed by use of a Tension InfiltrometerSoil Science Society of America Journal, 1986
- Groundwater recharge estimation using chloride, deuterium and oxygen-18 profiles in the deep coastal sands of Western AustraliaJournal of Hydrology, 1985
- The Function of Different Types of Macropores During Saturated Flow through Four Swelling Soil HorizonsSoil Science Society of America Journal, 1977