The influence of hillslope gradient, regolith texture, stone size and stone position on the presence of a vesicular layer and related aspects of hillslope hydrologic processes: a case study from the Australian arid zone
- 29 February 1996
- Vol. 26 (1-2) , 71-84
- https://doi.org/10.1016/0341-8162(95)00034-8
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- Runoff and runon areas in a patterned chenopod shrubland, arid western New South Wales, Australia: characteristics and originJournal of Arid Environments, 1995
- PARTITIONING SMALL SCALE SPATIAL VARIABILITY OF RUNOFF AND EROSION ON SAGEBRUSH RANGELAND1Jawra Journal of the American Water Resources Association, 1994
- Effects of rock fragments on soil erosion by water at different spatial scales: a reviewCATENA, 1994
- Runoff and sediment yield from topsoils with different porosity as affected by rock fragment cover and positionCATENA, 1992
- Numerical Study of the Maximum Boundary Shear Stress Induced by Raindrop ImpactWater Resources Research, 1991
- Morphology and genesis of silt and clay coatings in the vesicular layer of a desert loam soilSoil Research, 1991
- The hydrological response of soil surfaces to rainfall as affected by cover and position of rock fragments in the top layerEarth Surface Processes and Landforms, 1990
- Reclamation of a scalded, red duplex soil by waterpondingSoil Research, 1989
- Influences of quaternary climatic changes on processes of soil development on desert loess deposits of the Cima volcanic field, CaliforniaCATENA, 1986
- Factors influencing infiltration and sediment production of semiarid rangelands in NevadaWater Resources Research, 1975