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Erosion quantification in pastures with different slopes in the Ribeir?o Salomea Watershed

机译:Ribeir?o Salomea流域不同坡度牧场的侵蚀定量

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摘要

The water erosion is one of the main forms of soil degradation and it is highly affected by the soil cover and landscape slope. The objective of this work was to quantify the detachment rate and the soil loss due to water erosion under simulated rains in pastures, as well as to study the effect of land cover and the slope classes ( 9, 10-15, 25-30 and 35-40%) on soil loss in the Ribeirão Salomea wathershed. The treatments with four repetitions were: with and without pasture covering in four slope classes: 9, 10-15, 25-30 and 35-40%. Thirty-two simulated rains were applied in plots delimited by galvanized metallic foils fixed in the soil and having a gutter at their lower part for runoff sampling. The results showed that the land cover influenced soil loss only within each slope classes. Soil losses increased with increasing slope classes. This phenomenon was higher in uncovered land than in the covered ones. The erodibility was 1.48 x 105 kg s m-4 for the evaluated Mollisol.
机译:水蚀是土壤退化的主要形式之一,受到土壤覆盖和景观坡度的强烈影响。这项工作的目的是量化牧场中模拟降雨下由于水蚀造成的脱离率和水土流失,并研究土地覆盖和坡度等级的影响(<9,10-15,25-30和35-40%)的土壤流失在RibeirãoSalomea中。有四个重复的处理方法是:有和没有牧场覆盖率的四个坡度类别:<9、10-15、25-30和35-40%。在由固定在土壤中的镀锌金属箔界定的地块上,进行了3​​2次模拟降雨,并在其下部有一个排水沟以进行径流采样。结果表明,土地覆盖仅在每个坡度类别内影响土壤流失。土壤损失随着坡度等级的增加而增加。在未覆盖的土地上这种现象比在被覆盖的土地上更高。对于所评价的Mollisol,可蚀性为1.48×105kg s m-4。

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