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林业科学 ›› 2007, Vol. 43 ›› Issue (02): 15-20.doi: 10.11707/j.1001-7488.20070203

• 论文及研究报告 • 上一篇    下一篇

林冠截留在杉木林生态系统能量转换过程中的作用

康文星 邓湘雯 赵仲辉   

  1. 中南林业科技大学,长沙410004
  • 收稿日期:2006-01-04 修回日期:1900-01-01 出版日期:2007-02-25 发布日期:2007-02-25

Effects of Canopy Interception on Energy Conversion Processes in Chinese Fir Plantation Ecosystem

Kang Wenxing,Deng Xiangwen,Zhao Zhonghui   

  1. Central South University of Forestry and Technology Changsha 410004
  • Received:2006-01-04 Revised:1900-01-01 Online:2007-02-25 Published:2007-02-25

摘要:

根据会同生态站2000—2005年连续定位观测数据,研究杉木人工林林冠截留在杉木人工林生态系统能量转换过程中的作用。结果表明:林冠层每年吸收的辐射能为25.5430亿J·m-2,透过林冠层的辐射能为2.5306亿J·m-2,被冠层反射的辐射能为2.7432亿J·m-2,分别占到达林冠表面辐射能的82.7%、8.2%和9.1%;林冠截留水分的蒸发,使得系统获取的净辐射能向潜热能转化。每年林冠截留水分蒸发耗能6.3695亿J·m-2,占系统净辐射能的22.9%,占系统总蒸发散耗能的30.4%,是系统能量支出的一个重要组成部分;林冠截留使大气降水中的雨滴动能消耗在克服枝叶阻力的做功上,叶面水滴从冠层滴落下,是一个由势能转化为动能的过程;冠层叶片对水滴有汇聚作用,使冠滴水直径较冠上大气降水大,冠滴水的直径主要受冠层结构的影响,与大气降水量和降水强度的关系不大;林分郁闭度为0.9,枝下高7m,降水量大于3mm时,林冠层不能有效地降低雨滴动能,只有在雨量极小、林冠能截留大部分水量,或者雨强极大、直径大的雨滴在枝叶表面撞击分散的情况下,才能显示林冠对大气降水雨滴动能的降低作用。

关键词: 林冠层, 截留作用, 辐射能, 潜热能, 雨滴动能

Abstract:

The functions of canopy interception on energy conversion processes in a Chinese Fir plantation ecosystem were studied with the long-term observation data in Huitong. The results showed that the solar radiation absorbed, transmitted, and reflected were 2.554 30 billion (with a absorption ratio of 0.827), 0.253 06 billion (with a transmissivity of 0.082) and 0.274 32 billion J·m -2 a-1 (with a reflection ratio of 0.091) on the canopy, respectively. The conversion of net solar radiation to latent heat with the processes of evaporation from canopy interception amounts to 0.636 95 billion J·m-2 a-1 (accounting for 22.9% of the total ecosystem net radiation, and 30.4% of the ecosystem evapotranspiration.), which was an important part of the system energy budget. Canopy interception consumed the raindrop kinetic energy in overcoming the branches and leaves resistance, which gathered raindrops together by branches and leaves and then followed with potential energy in raindrops converted to kinetic energy with falling raindrops. In general, diameter of raindrops from the canopy is bigger than that of the raindrops above the canopy as result of gathering effect of canopy. The kinetic energy of raindrops from the canopy, therefore, was higher than that of raindrops in the atmosphere. And the drop_size distribution from the canopy was influenced by the structure of the canopy layer rather than amount of precipitation and precipitation intensity. The canopy had no significantly efficient effects on decreasing raindrop kinetic energy in the case study with branch height of 7 m and precipitation amount of over 3 mm. However, the canopy would play a key role in decreasing raindrop kinetic energy in both cases of a little amount of precipitation and heavy precipitation intensity, which the canopy could intercept most amount of precipitation in the former condition and the canopy could scatter bigger raindrops to smaller raindrops with striking to leaves in the latter.

Key words: canopy, crown-interception, radiation energy, latent heat energy, raindrop kinetic energy