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作 者:韩冰[1] 吴钦孝[1] 刘向东[1] 江有科 赵鸿雁[1]
出 处:《水土保持研究》1994年第3期14-18,共5页Research of Soil and Water Conservation
摘 要:28年生油松人工林内天然降雨的溅蚀试验结果表明,当I30为0.07mm/min或P0为3.57mm时,无枯落物层覆盖的林地发生溅蚀,当I30为0.25mm/min或Po为45.8mm时,具1cm枯落物层的林地不发生溅蚀。从溅蚀月动态看出,7、8月份占全年溅蚀量的70%以上。在同一土壤和同一坡度条件下,I30、P0、H1是溅蚀发生的主要因素,且溅蚀量与其呈二次多项式回归关系。但当枯落物层具有一定厚度时溅蚀与其它因素无关。具有1cm厚的枯落物层即可防止土壤溅蚀量的79.7%。The results of the experiment in prevention of splash erosion under the condition of natural rainfall in the woodland of 28-year-old chinese pine have shown that when I30=0.07 mm,min-1 or P0=3.57mm the splash erosion in the woodland with out litter occured;and when I30=0.25mm.min-1or P0=45.8mm itdid not occured in the woodland with litter of 1cm.Splash erosion monthly dynamic indicated that the splash erosion in July and August amounts to more than 70% of the total splash erosion.Under the conditions of same soil and slope,I30、P0and H1are the major factors affecting the splash erosion,and there is a multinomial regression equation among splash erosion and I30, P0,H1e.But when the litter layer reached a certain thickness,splash erosion has nothing to do with the other factors.When the litter layer accumulatedto a depth of 1cm,it can prevent soil splash erosion of 79.7%.
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