Estimation of Soil Erosion Using Field and Modelling Approaches in an Undisturbed Arnhem Land Catchment, Northern Territory, Australia

Geographical Research - Tập 46 Số 3 - Trang 333-349 - 2008
G. R. Hancock1, R.J. Loughran1, K. G. Evans2,1, RICHARD M. BALOG3
1School of Environmental and Life Sciences, The University of Newcastle, Callaghan, New South Wales 2308, Australia
2Hydrological and Ecological Processes Program, Environmental Research Institute of the Supervising Scientist, Darwin, Northern Territory, Australia.
3Philippine Nuclear Research Institute, Commonwealth Avenue, Diliman, Quezon City, Philippines

Tóm tắt

AbstractAn assessment of slope erosion at Tin Camp Creek catchment, Arnhem Land, Northern Territory, Australia, was carried out using the fallout environmental radioisotope caesium‐137 (137Cs) as an indicator of soil erosion status, two numerical models (SIBERIA and the Revised Universal Soil Loss Equation (RUSLE)) and erosion pins. This undisturbed drainage basin is situated in the seasonally wet‐dry tropics, with high energy storms and a mean annual rainfall of 1389 mm. Tin Camp Creek catchment is unaffected by European agriculture or pastoral activities, but often experiences fire during the dry season. Two transects were sampled for 137Cs in 2002 and 2004, and two models were used to convert 137Cs measurements into soil loss estimates. Two methods using the theoretical Profile Distribution Model (PDM) gave net soil redistribution rates between +2.72 and –22.19 t ha−1 yr−1 and +2.95 and –24.06 t ha−1 yr−1, respectively, while an Australian empirical model (AEM) for uncultivated soils produced estimates between +1.84 and –7.00 t ha−1 yr−1 (negative values indicate soil erosion, positive, deposition). The RUSLE gave estimated soil losses for the two transects of approximately 10 t ha−1 yr−1, while the SIBERIA model produced values between 0.5 and 2 t ha−1 yr−1 for the transects and between 3.5 and 11 t ha−1 yr−1 for the total catchment. Average net soil losses of 14 and 15 t ha−1 yr−1 for the total catchment and slopes, respectively, were measured by erosion pins. The soil losses in the catchment are similar to those for some other transects in the Northern Territory and the Kimberley region of Western Australia (measured by the 137Cs AEM), even though these areas are affected by pastoral activities. This may be at least partly explained by erosion in Tin Camp Creek catchment during high intensity rainstorms at the commencement of the wet season, especially if the slopes have been affected by fire during the previous dry season.

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Geographical Research

Tập 46 Số 3

333-349

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