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重庆缙云山典型林分的坡面糙率系数及影响因素

Surface roughness coefficient and its influencing factors on the slope of typical forests in Jinyun mountain of Chongqing

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【作者】 韩小杰齐实刘登峰吴云陈林

【Author】 Han Xiaojie1,Qi Shi1,Liu Dengfeng1,Wu Yun2,Chen Lin2(1.College of Soil and Water Conservation,Beijing Forest University;Key Lab. of Soil & Water Conservation and Desertification Combating,Ministry of Educatio,100083,Beijing;2.Chongqing Jinyunshan National Nature Protection Region Management Bureau,400700,Chongqing: China)

【机构】 北京林业大学水土保持学院,水土保持与荒漠化防治教育部重点实验室重庆缙云山国家级自然保护区管理局

【摘要】 根据2008年4月实测数据,以三峡库区重庆缙云山4种典型林分(马尾松纯林、马尾松阔叶混交林、常绿阔叶林和楠竹林)为研究对象,并以农耕地作对照,在野外径流小区实验的基础上,通过曼宁公式,对重庆缙云山林地坡面糙率系数n值进行研究。结果表明:地表糙率系数n值介于0.007 9~0.270 4之间,其中,马尾松纯林的糙率系数n值最小,马尾松阔叶混交林的糙率系数n值最大,大小排序为马尾松阔叶混交林>阔叶林>楠竹林>马尾松纯林;糙率系数n(y)与枯落物厚度(x)的关系为y=0.020 5e0.543 6x,R2=0.923 7;地表水分渗透量(y)随着糙率系数n(x)增加而增大,其关系式为y=37.25lnx+188.47,R2=0.778 2。

【Abstract】 Surface roughness coefficients on the slope of forestland in Jinyun mountain of Chongqing by using the Manning Formula are conducted based on the measured field experiments data in 4 typical forests(Pinus massoniana,mixed with Pinus massoniana and broadleaf trees,broadleaf forest and Phyllostachys pubescens),compared to crop-land,in Jinyun mountain,Chongqing City of the Three Gorges Reservoir Area in April 2008.The results show that the values n of the surface roughness coefficient vary from 0.007 9 to 0.270 4.The value n of Pinus massoniana is minimum and the value n of the mixed with Pinus massoniana and broadleaf trees is maximum.The descending order of surface roughness coefficient of 4 typical forests is as follows: mixed with Pinus massoniana and broadleaf trees,broadleaf forest,Phyllostachys pubescens,Pinus massoniana.The relationships between surface roughness coefficient and litter depth is shown as linear relationship,the formula of surface roughness coefficient(y) and litter depth(x) is: y=0.020 5e0.543 6x,R2 is 0.923 7 respectively,and there is a logarithmic relationship between surface roughness coefficient(x) and infiltration capacity of surface water(y),the formula is: y=37.25lnx+188.47,R2 is 0.778 2.The infiltration capacity of surface water increases with the increase of surface roughness coefficient.

【基金】 国家自然科学基金“三峡库区以流域为单元森林植被对洪水的影响研究”(30571486);“十一五”科技支撑计划“重庆北部水源区水源涵养林构建技术试验示范”(2006BAD03A1802)
  • 【文献出处】 中国水土保持科学 ,Science of Soil and Water Conservation , 编辑部邮箱 ,2009年03期
  • 【分类号】S714
  • 【被引频次】10
  • 【下载频次】165
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