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The role of olive trees in rainfall erosivity and runoff and sediment yield in the soil beneath

机译:橄榄树在降雨侵蚀力,下层土壤径流和沉积物产量中的作用

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The modification of raindrops by the canopy of olive treesincreases the kinetic energy of the rain per unit area. The kinetic energycomputed from the measured drop size distribution under the tree canopy insimulated rainfall experiments is greater than that received in the open, 17.1 J mm-1, as against 15.7 J mm-1 . This causes higher soildetachment and loss than that observed outside the canopy. Tillage treatments ofthe soil modify its erodibility, accelerate soil detachment and reduce,simultaneously, the velocity of runoff. Both effects reduce the amount ofsediment compared to that observed in the non-tilled soil. The average values ofsoil lost per unit of rain depth and unit area were 5.81 g mm-1 m-2(conventional tillage) and 4.02 g mm-1 m-2 (zero tillage)under the canopy compared to 0.89 g mm-1 m-2 (conventionaltillage) and 0.95 g mm-1 m-2 (zero tillage) in the open.
机译:橄榄树冠对雨滴的修饰增加了单位面积雨水的动能。根据树冠模拟降雨实验下测得的液滴尺寸分布计算出的动能大于开放条件下的动能17.1 J mm -1 ,而15.7 J mm -1 。这导致比在树冠外观察到的更高的土壤分离和损失。土壤的耕作处理改变了土壤的易蚀性,加速了土壤的脱离并同时降低了径流速度。与在非倾斜的土壤中观察到的相比,这两种作用都减少了沉积物的量。每单位雨深和单位面积的土壤流失平均值分别为5.81 g mm -1 m -2 (常规耕作)和4.02 g mm -1 < / sup> m -2 (零耕作),而冠层下为0.89 g mm -1 m -2 (常规耕作)和0.95 g mm -1 m -2 (零耕种)在露天。

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