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山杨林地枯落物层对溅蚀的影响

The effects of litter layer on splash erosion in Populus davidiana woodland

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【作者】 韩冰吴钦孝刘向东汪有科赵鸿雁

【Author】 Han Bing;WuQin-Xiao;Liu Xiang-Dong;Wang You-Ke and Zhao Hong Yan(Northwestern Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100),

【机构】 中国科学院水利部西北水土保持研究院

【摘要】 天然降雨下30年生山杨林内溅蚀试验结果表明,当I_(30)(最大30分钟雨强)为0.076mm/min或P_o(林内降雨量)为3.3mm时,清除枯落物层林地发生溅蚀,在I_(30)为0.35mm/min或P_o为25.56mm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60%以上;在同一土壤和坡度条件下,I_(30)、P_o、H_1(枯落物层厚度)是溅蚀发生的主要因素,且溅蚀量(S_t)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他因素无关。溅蚀主要发生在清除枯落物层的林下,随枯落物层厚度增加,溅蚀量剧减,当枯落物层积累到1cm时防止土壤溅蚀量达97.50%。

【Abstract】 Under the condition of natural rainfall,the results of splash erosion experiment in the woodland of 30-year-old Populus davidiana have shown : if I30( maximum thirty-minute intensity of rain)=0.076 mm/min or Po(the precipitation inside woodland)=3.3 mm,the splash erosion will be occured by the removing of litter layer ,splash erosion is absent when litter layer is of 1 cm,I30= 0. 35 mm/min or Po= 25. 56 mm. Splash erosion in July and August occupies more the 60%of the total annual amount.Under the same status of soil and gradient,I30,Po and H1(litter layer thickness) are the major factors which control the occurence of splash erosion , and the splash erosion amount will express quadratic multinomial regression relation to them , but when the litter layer reached a certain thickness,splash erosion is not related with the other facter.Splash erosion mainly occures on the woodland which litter layer has been removed,with the increasing of litter layer,splash erosion intensely reduced , when the litter layer accumulation reachs 1 cm,it can prevent from 97.5%soil splash erosion.

【关键词】 枯落物层溅蚀土壤保持
【Key words】 litter layersplash erosionsoil conservation
【基金】 国家自然科学基金
  • 【文献出处】 植物资源与环境 ,Journal of Plant Resources and Environment , 编辑部邮箱 ,1994年04期
  • 【分类号】S792.114
  • 【被引频次】34
  • 【下载频次】151
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