Evaluation of changes in post-fire recharge under native woodland using hydrological measurements, modelling and remote sensing

SummaryThis paper examines the use of a controlled fuel reduction burn in native woodland to increase recharge to a shallow aquifer system for water supply in south-western Australia. Soil moisture trends from neutron probe measurements and watertable dynamics from piezometers under adjacent burned and unburned plots were compared to determine the difference in recharge resulting from the fire. Remotely sensed evapotranspiration (ET) subtracted from rainfall was used to independently estimate groundwater and soil moisture recharge and compare against a physically based model of soil–water fluxes. The use of naturally occurring chemicals (n-alkanes and cycloalkanes) produced in the fire as tracers of the recharge pulse in the winter following the fire was tested. It was found that in the winter following the fire (annual rainfall 701 mm), water storage in the 9 m thick unsaturated zone increased by about 300 mm but recharge to the watertable was only about 60 mm. In the subsequent year (rainfall 630 mm), leaf area index in the burned woodland recovered to be about 10% less than the unburned plot, remotely sensed ET rose above that in the unburned plot and recharge was lower in the burned than unburned plot. This trend continued and, after 3 years, increased ET negated any early recharge gains, and there was a net decrease in recharge resulting from the fire. The combination of water balance measurements, modelling and remote sensing provides a robust method to gain hydrological understanding of recharge mechanisms. Further work is required to refine the use of burn residue chemicals as soil water tracers, particularly in improving instrument design for groundwater sample collection in fine textured soils. As climate continues to change and regions with growing water shortages seek innovative solutions, approaches such as controlled burning may be needed; however, in this example, the approach was unproductive and further the environmental consequences need to be evaluated to make an appropriate assessment of trade-offs and viability of this approach.

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► The effect of forest fire on groundwater recharge was examined.
► Soil moisture and watertable hydrographs were examined to estimate recharge.
► After initial increase in water storage, evapotranspiration removed most of this over 3 years.
► Remotely sensed evaporation subtracted from rainfall agreed with measurements of soil moisture change.
► Biophysical modelling with WAVES gave similar estimates of recharge to measurements.