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    植被恢复年限对塞罕坝华北落叶松人工林土壤碳氮磷储量的影响

    Effects of vegetation recovery years on soil carbon, nitrogen and phosphorus stocks of Larix gmelinii var. principis-rupprechtii plantations in Saihanba

    • 摘要:
      目的 揭示植被恢复对塞罕坝华北落叶松人工林土壤碳、氮、磷储量的影响机制,为人工林固碳、保肥功能精准提升提供科学依据。
      方法 本研究以塞罕坝不同恢复年限(15,25,36,52年)华北落叶松人工林为研究对象,以退化沙地为对照,通过测定0 ~ 1 m土层碳、氮、磷储量及相关环境因素,揭示植被恢复过程中土壤碳、氮、磷储量变化及其影响因素。
      结果 (1)不同恢复年限华北落叶松人工林土壤碳、氮、磷储量平均值分别为(211.5 ± 46.1)、(16.0 ± 3.1)、(5.8 ± 0.8)t/hm2。土壤碳、氮、磷储量随恢复年限增加显著增加(P < 0.05),土壤碳和磷储量于36年达最大值,而氮储量在52年时显著大于其他恢复年限(P < 0.05)。(2)方差分解结果显示,土壤和植被因素共同解释土壤碳、氮、磷储量84.46%、82.73%和65.29%的变异。其中,土壤黏粒含量单独解释率分别为25.79%、28.08%和34.16%;植被地下生物量单独解释率分别为58.67%、54.65%和31.13%。(3)结构方程结果表明,恢复年限对土壤碳、氮、磷储量仅具间接作用,恢复年限既可通过增加植被地下生物量间接提高土壤碳、氮、磷储量(占总效应的58.6%、53.0%和35.3%),又可通过增加植被地下生物量和凋落物层现存量来改变土壤机械组成,从而提高土壤磷储量(占总效应的38.3%)。
      结论 植被恢复年限通过增加植被地下生物量和改善土壤机械组成有效提升土壤碳、氮、磷储量,故人工林管理实践需加强土壤机械组成改良与根系生物量维持,同时注重土壤固碳保肥功能的长期发挥。

       

      Abstract:
      Objective This study aimed to reveal the influence mechanisms of vegetation restoration on soil carbon, nitrogen and phosphorus stocks of Larix gmelinii var. principis-rupprechtii plantations in Saihanba, and to provide a basis for precise improvement of carbon sequestration and fertility maintenance function.
      Method In this study, L. gmelinii var. principis-rupprechtii plantations with different years of recovery (15, 25, 36, 52 year) were compared against the degraded sandy land used as controls in Saihanba. Soil carbon, nitrogen and phosphorus stocks (0-1 m) and associated environmental factors were measured. Variation in soil carbon, nitrogen and phosphorus stocks and its influencing factors during vegetation restoration will be clarified.
      Result (1) Soil carbon, nitrogen and phosphorus stocks of L. gmelinii var. principis-rupprechtii plantations during different vegetation recovery years are (211.5 ± 46.1) t/ha, (16.0 ± 3.1) t/ha, (5.8 ± 0.8) t/ha. Soil carbon, nitrogen and phosphorus stocks increased with increasing vegetation recovery years (P < 0.05). Soil carbon and phosphorus stocks reached maximum at 36 years, while soil nitrogen stocks at 52 years were significantly higher than other vegetation recovery years. (2) Soil and vegetation factors together explained 84.46%, 82.73% and 65.29% of the variation in soil carbon, nitrogen and phosphorus stocks, respectively; and soil clay content individually explained 25.79%, 28.08% and 34.16% of the variation. Vegetation belowground biomass individually explained 58.67%, 54.65% and 31.13% of the variation in soil carbon, nitrogen and phosphorus stocks. (3) Structural equation models demonstrated that vegetation recovery years had no significant direct effect on soil carbon, nitrogen and phosphorus stocks. Vegetation recovery years indirectly increased soil carbon, nitrogen and phosphorus stocks by increasing vegetation belowground biomass (58.6%, 53.0% and 35.3%), and indirectly increased soil phosphorus stocks through affecting soil texture (by increasing vegetation belowground biomass and litter biomass, 38.3%).
      Conclusion Vegetation recovery years increased soil carbon, nitrogen and phosphorus stocks through indirect pathways mediated by soil texture and vegetation belowground biomass. Therefore, for practice and management of plantations, it is necessary to strengthen the management of soil texture and maintenance of vegetation belowground biomass as well as to focus on the long-term soil carbon sequestration and fertility maintenance function.

       

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