Systematic variation of soil infiltration rates within and between the components of the vegetation mosaic in an Australian desert landscape
- 9 January 2002
- journal article
- research article
- Published by Wiley in Hydrological Processes
- Vol. 16 (1) , 119-131
Abstract
Vegetation mosaics have commonly been thought to include two principal zones with distinctly different hydrology: relatively bare and impermeable runoff source zones (intergroves) and more strongly absorbing vegetated runon zones (groves). However, the data required to verify the internal uniformity of hydrologic response within these components of mosaic landscapes have been lacking, as have data on the nature (abrupt or gradational) of the boundaries between them. This study examines the degree of internal uniformity of key soil properties in the intergroves and groves of an Australian vegetation mosaic.Infiltration rates, soil water content, shear strength, bulk density and texture were determined at intervals of 1·5–2·5 m across several grove–intergrove cycles of an Australian banded shrubland. Results demonstrate that order‐of‐magnitude variability in soil infiltration rates can occur across intergroves, with lesser variation in groves. Patterns of infiltration are systematically related to slope position. Rates are relatively high in the uppermost parts of the intergrove, and fall to low values only in the lowermost intergrove where soils are mechanically strong. Infiltration rates increase rapidly from the lowermost intergrove to reach maxima within the upper to middle grove, from where rates once again decline toward the next intergrove. However, there is only a gradational change in infiltration rates across the pioneer zone–grove boundary, which is the sharpest of the mosaic boundaries when identified using plant cover data.Hydrologic models built on the presumption that mapped plant cover units are equally distinct hydrologically may need to be refined to incorporate the presence of systematic internal variability of infiltration rates and gradational change in soil hydraulic properties. Copyright © 2002 John Wiley & Sons, Ltd.Keywords
This publication has 20 references indexed in Scilit:
- Soil measurements during HAPEX-Sahel intensive observation periodJournal of Hydrology, 2004
- Soil and water components of banded vegetation patternsCATENA, 1999
- Water balance in a banded vegetation patternCATENA, 1999
- Banded vegetation near Broken Hill, Australia: significance of surface roughness and soil physical propertiesCATENA, 1999
- The soil surface characteristics of vegetation stripes in Northern Mexico and their influences on the system hydrodynamicsCATENA, 1999
- The role of surface water redistribution in an area of patterned vegetation in a semi-arid environment, south-west NigerJournal of Hydrology, 1997
- Grass-mediated Capture of Resource Flows and the Maintenance of Banded Mulga in a Semi-arid WoodlandAustralian Journal of Botany, 1997
- Runoff and runon areas in a patterned chenopod shrubland, arid western New South Wales, Australia: characteristics and originJournal of Arid Environments, 1995
- Energy and water budgets of an area of patterned woodland in the SahelAgricultural and Forest Meteorology, 1993
- A runoff capability classification system based on surface features criteria in semi-arid areas of West AfricaJournal of Hydrology, 1992