植物生态学报 ›› 1988, Vol. 12 ›› Issue (3): 181-188.

• 论文 • 上一篇    下一篇

海南岛尖峰岭热带林土壤渗透水的初步研究

卢俊培   

  • 发布日期:1988-03-10
  • 通讯作者: 卢俊培

Seepace Water of Soil in Tropical Forest at Jianfengling, Hainan Island, China

Lu Jun-pei   

  • Published:1988-03-10
  • Contact: Li Yong-hong

摘要: 本文应用开口托盘式集水器收集不同土层的渗透水,研究尖峰岭热带山地雨林,半落叶季雨林及其游耕地的土壤渗透水状况,分析了不同植被—土壤类型与利用状况的渗透特点、降水与渗透水的关系、渗透水量与水质的动态变化,初步揭示了尖峰岭热带林对水分的输导—涵贮性能,及热带林生态系统中物质迁移的特点,并据此分析了游耕农业的生态恶果。

Abstract: The characteristics of percolation of different vegetation-soil types and land uses were studied at Jianfengling in Hainan Island, China. Seepage water was collected by a number of open dish collectors from different layers of soil. The relationship between rainfall and seepage water in the area, and characteristics of substance movement in tropical forest ecosystem were analysed. According to two-year observation, it was shown that the annual percolation within 100cm depth of the lateritic yellow soil under the mountain rain forest was 355 mm, equal to 15.9% of the annual rainfall, while in the cinnamon latosol under the semideciduous monsoon forest it had only 30mm which was 1.8% of the annual rainfall. The litter cover and the upper 30cm of surface soil hold the maximum seepage water. The forest has an excellent function of soil and water conservation. The seepage capacity is positively correlated with rainfall, but the deeper the soil, the less the significant correlation is.