THE EFFECTS OF WILDFIRE ON SOIL WETTABILITY AND HYDROLOGICAL BEHAVIOR OF AN AFFORESTED CATCHMENT

A wildfire in February 1986 destroyed most of an afforested research catchment in the southwestern Cape region of South Africa. The hydrological consequences of the fire were quantified using monitored pre-fire and post-fire stream flow and sediment data from the burned catchment and a nearby control catchment. Soil loss and soil wettability were also measured. In the first year after the fire, weekly stream flow totals increased by 12%, quick flow volumes increased by 201%, peak flow rates increased by 290% and catchment response ratio increased by 242%. Soil loss on overland flow plots ranged from 10 to 26 t ha-1, and suspended sediment and bedload yields each increased roughly four-fold following the fire. Wettability of the soils was greatly reduced by the passage of fire. Surface soil layers (0-10 mm) were burned clean of any inherent water repellency by the passage of a hot fire, but more severe repellency, in broader bands, was induced in deeper soil levels by the heating of the soil. It is postulated that the widespread development of water repellency in the soil led to overland flow during larger rainstorms, which in turn caused the markedly altered hydrological behaviour of the catchment and the high soil losses relative to the unburned condition.