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Land-use change from indigenous management to cattle grazing initiates the gullying of alluvial soils in northern Australia

机译:从土著管理到放牧的土地利用变化引发了澳大利亚北部冲积土壤的淤积

摘要

Catchments in northern Australian have undergone dramatic land-use changes from traditional Aboriginal management to widespread cattle grazing post-European settlement. Quantifying the soil erosion impacts of these changes is essential to the future sustainable management of the soils in these catchments. Rates of gully erosion in alluvial soils were measured using recent GPS surveys and historical air photographs. The results indicated that median erosion rates currently and historically are within the same order of magnitude (0.1 to 1m per year). Historic air photo analysis demonstrated rapid increases in gully area of 2 to 10 times their initial 1949 area. Extrapolation of gully area growth trends backward in time suggested that most gullies initiated between 1880 and 1950. European cattle were introduced into the lower Mitchell catchment in the 1880's, suggesting the contribution of land use intensification to either gully initiation or acceleration. It is hypothesized that intense cattle grazing concentrated in the riparian zones during the dry season decreased perennial vegetation cover along hollows and steep river banks, increasing the potential for gully erosion. Once initiated on steep banks into dispersible sub-soils, alluvial gullies can rapidly progress in consuming and degrading the most productive part of the landscape, the riparian zone.
机译:从传统的原住民管理到欧洲定居后广泛放牧的牲畜,澳大利亚北部的集水区发生了戏剧性的土地利用变化。量化这些变化对土壤侵蚀的影响对于这些流域未来土壤的可持续管理至关重要。使用最新的GPS调查和历史航空照片测量了冲积土壤中的沟壑侵蚀率。结果表明,当前和历史上的中值侵蚀率处于同一数量级(每年0.1至1m)。历史的航空照片分析表明,沟壑面积迅速增加,是其1949年最初面积的2至10倍。沟壑面积增长趋势的倒推显示,大多数沟壑始于1880年至1950年。欧洲牛群在1880年代被引入米切尔河下游流域,这表明土地利用集约化对沟壑萌芽或加速的贡献。据推测,干旱季节集中在河岸带的大量放牧牛减少了沿空洞和陡峭河岸的多年生植被覆盖,增加了沟壑侵蚀的可能性。冲积沟一旦在陡峭的河岸上开始形成可分散的底土,便会迅速消耗和降解景观中最富生产力的部分-河岸带。

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