西双版纳热带雨林恢复对土壤氮素积累和分配时空变化的影响

Effect of tropical rainforest restoration on temporal and spatial changes of soil nitrogen accumulation and allocation in Xishuangbanna

  • 摘要: 为探明热带雨林恢复对土壤氮素积累和分配时空变化的影响,本研究选取西双版纳热带森林中代表不同恢复阶段的白背桐(Mallotus paniculatus)、崖豆藤(Mellettia leptobotry)和高檐蒲桃(Syzygium oblatum) 3个典型群落为研究对象,采用土壤化学分析方法,对全氮、水解氮、铵态氮和硝态氮质量比及其分配比例w(水解氮)∶w(全氮)、w(铵态氮)∶w(全氮)和w(硝态氮)∶w(全氮)进行了系统测定,并分析了植被多样性与土壤理化性质变化对土壤氮素积累与分配的影响. 结果表明,随着恢复推进,土壤各氮组分质量比显著增加(p<0.05),其中恢复后期较初期水解氮和铵态氮质量比分别增加70.2%和64.2%. 土壤氮组分质量比及其分配比例在不同月份和土层间存在显著差异,其中6月质量比与占比最高,且随土层深度增加逐渐下降. 与此同时,雨林恢复显著提高了植物多样性和土壤养分积累,乔木和林下植被Shannon多样性指数在恢复后期分别为初期的1.43倍和1.55倍. 结构方程模型分析进一步揭示,植物多样性、土壤温度、总有机碳和微生物量碳是调控土壤氮素动态的主控因子,分别解释氮素组分质量比与分配变异的82%~94%和28%~52%. 因此,热带森林恢复通过重塑植物多样性、微气候与土壤碳库,显著促进了土壤氮素组分质量比的积累与分配. 本研究结果也为进一步阐明热带雨林恢复背景下的土壤氮循环机制提供了新的实证依据.

     

    Abstract: To investigate how tropical rainforest restoration influences the spatiotemporal dynamics of soil nitrogen accumulation and partitioning, we selected three representative communities in Xishuangbanna that span successive restoration stages: Mallotus paniculatus (early stage), Mellettia leptobotry (mid-stage), and Syzygium oblatum (late stage). Using standard soil chemical analyses, we quantified total nitrogen (TN), hydrolysable nitrogen (HN), ammonium-nitrogen (NH4+-N) and nitrate-nitrogen (NO3-N), along with their allocation ratios (HN/TN, NH4+-N/TN, \mathrmNO_3^ - _3^ + -N/TN). The effects of vegetation diversity and soil physicochemical properties on soil nitrogen accumulation and allocation were also analyzed. The results showed that all nitrogen fractions increased significantly with restoration progression (p < 0.05), relative to the early stage, hydrolysable nitrogen and ammonium nitrogen in the late stage rose by 70.2% and 64.2%, respectively. Nitrogen fractions and their allocation exhibited significant monthly and depth-related variations, peaking in June and decreasing with increasing soil depth. Meanwhile, restoration markedly enhanced plant diversity and soil nutrient accumulation, the Shannon diversity indices of both the tree layer and the understory were 1.43-fold and 1.55-fold higher, respectively, at the late stage than at the early stage. Structural equation modeling further revealed that plant diversity, soil temperature, total organic carbon, and microbial biomass carbon were the dominant controlling factors regulating soil nitrogen dynamics, jointly explaining 82% ~ 94% of the variation in nitrogen fractions and 28% ~ 52% of the variation in their allocation. Therefore tropical forest restoration, through reshaping plant diversity, microclimate, and soil carbon pools, significantly promotes the accumulation and redistribution of soil nitrogen fractions. This study provides new empirical evidence for unraveling the mechanisms of soil-nitrogen cycling under tropical rainforest restoration.

     

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