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    坝上地区典型防护林水源涵养功能对林分结构的响应

    Response of water conservation function of typical protective forests in Bashang area of northern China to stand structure

    • 摘要:
      目的 坝上是京津冀地区重要的生态屏障和水源涵养地,探究典型防护林林分结构对枯落物层和土壤层水源涵养功能的影响,为该地区防护林的抚育管理与林分优化提供科学依据。
      方法 选取坝上地区御道口林场3种典型防护林(樟子松林、华北落叶松林、樟子松华北落叶松混交林)为研究对象,调查胸径、树高、林龄、密度、郁闭度和叶面积指数等林分结构指标,通过室内浸水法和环刀法进行枯落物层和土壤层持水性能的测定,运用冗余分析探究防护林结构对枯落物层和土壤层持水性能的影响机制。
      结果 (1)樟子松华北落叶松混交林的枯落物层厚度、蓄积量、枯落物最大持水量和有效拦蓄量均大于纯林,其中总枯落物厚度差异显著(P<0.05)。(2)土壤总孔隙度、含水量和最大持水量都随着土层的增加而减小。其中土壤总孔隙度和最大持水量在0 ~ 30 cm土层表现为华北落叶松林 > 樟子松华北落叶松混交林 > 樟子松林,在30 ~ 60 cm土层表现为华北落叶松林 > 樟子松林 > 樟子松华北落叶松混交林。(3)冗余分析表明,林分结构与水源涵养功能密切相关,林分密度和树高对不同防护林枯落物层水源涵养能力影响显著,而树高和林龄对不同防护林土壤层水源涵养能力影响显著(P < 0.05)。
      结论 3种防护林中枯落物层和土壤层水源涵养能力最好的分别是樟子松华北落叶松混交林和华北落叶松林,林分密度、树高和林龄可以较好地解释水源涵养功能的变化。本研究对坝上地区生态平衡维护与可持续发展具有积极意义。

       

      Abstract:
      Objective The Bashang area, a crucial ecological barrier and water-conserving region in the Beijing-Tianjin-Hebei region of northern China, is the focus of this study. Our aim is to explore the influence of stand structure of typical protective forests on water conservation function of litter layer and soil layer.
      Method Three types of typical protective forests (Pinus sylvestris var. mongolica forest, Larix principis-rupprechtii forest, Pinus sylvestris var. mongolica and Larix principis-rupprechtii mixed forest) in the Yudaokou Forest Farm of the Bashang area were selected as research objects. Stand structure parameters such as DBH, tree height, stand age, stand density, canopy closure, and leaf area index (LAI) were investigated. The water-holding capacity of both litter layer and soil layer was assessed using the indoor immersion method and the ring-knife technique. Redundancy analysis was employed to explore the influence mechanism of protective forest structure on the water-holding properties of litter layer and soil layer.
      Result (1) The thickness of litter layer, volume of litter, maximum water holding capacity of litter and effective storage capacity of the mixed forest were greater than those of pure forest, and the difference of thickness was significant (P < 0.05). (2) The total soil porosity, water content and maximum water holding capacity of soil decreased as the soil layer deepened. The total soil porosity and maximum water holding capacity in the 0−30 cm soil layer showed Larix principis-rupprechtii forest > Pinus sylvestris var. mongolica and Larix principis-rupprechtii mixed forest > Pinus sylvestris var. mongolica forest, and in the 30−60 cm soil layer, it was showed as Larix principis-rupprechtii forest > Pinus sylvestris var. mongolica forest > Pinus sylvestris var. mongolica and Larix principis-rupprechtii mixed forest. (3) Redundancy analysis demonstrated that stand structure was closely related to the function of water conservation. Stand density and tree height had a significant influence on water conservation capacity of litter layer in different protection forests. Additionally, tree height and stand age had a significant impact on the water conservation capacity of soil layer in different protection forests (P < 0.05).
      Conclusion Among the three types of typical protective forest, the Pinus sylvestris var. mongolica and Larix principis-rupprechtii mixed forest and Larix principis-rupprechtii forest have the best water-conserving capacity in litter layer and soil layer, respectively. Stand density, tree height, and stand age have a significant effect on their hydrological effects. Therefore, when conducting afforestation in the Bashang area, appropriate tree species, reasonable density, and scientific thinning methods should be selected according to the actual situation to improve the efficiency of moisture utilization. This study provides an important scientific basis for the tending management and stand optimization of typical protective forest in the Bashang area and has positive significance for maintaining ecological balance and sustainable development in this area.

       

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