Abstract:
The Brigalow Catchment Study (BCS) was established to determine the impact on hydrology when brigalow
land is cleared for cropping and grazing. The paired catchment study was commenced in 1965 using catchments of
approximately 15 ha, with natural vegetation dominated by brigalow scrub (Acacia harpophylla). Three contiguous
catchments were selected near Theodore in central Queensland to represent the extensive brigalow bioregion of central and
southern Queensland and northern New South Wales (∼40 Mha). The hydrology of the 3 catchments was characterised
during a 17-year calibration period (1965–81). The catchments were considered hydrologically similar, with sufficient data
available for an empirical comparison between catchments. In 1982, two of the catchmentswere cleared, with one developed
for cropping and the other sown to improved pasture. The third catchment was used as an uncleared control. Hydrologic
characteristics were then compared for the following 21 years. In their virgin state, the catchments behaved similarly, with
average annual runoff being 5% of annual rainfall. Once cleared, total runoff from the cropping catchment increased to
11% of annual rainfall and total runoff from the pasture catchment increased to 9% of annual rainfall; however, timing of
the individual runoff events varied between land uses. In order to confirm that changes in hydrology were a function of
land use and not just seasonal variability or sampling error, several analytic techniques were used: a simple comparison of
runoff totals, comparison of events, comparison of probability of exceedance for daily runoff, and comparison of predicted
and observed runoff using a water balance modelling approach