南亚热带植被恢复重建对土壤有机碳及养分的影响

    Effects of vegetation restoration and reconstruction on soil organic carbon and nutrients in the southern subtropical region

    • 摘要:
      目的 探讨植被恢复重建对土壤有机碳(SOC)及土壤养分的影响,以及不同树种配置模式的恢复效果。
      方法 以种植枫香Liquidambar formosana和木荷Schima superba 2个树种作为对照模式(CK),设计多树种选择模式(配置Ⅰ)、珍贵树种套种模式(配置Ⅱ)、针阔叶树混交模式(配置Ⅲ),共4种树种配置模式,设立固定样地,于2012(造林前)、2014(造林2年后)、2016(造林4年后)、2024(造林12年后)年持续调查植物及SOC和土壤养分。
      结果 2012年共种植63个树种,2024年调查发现,保存35个树种,高脂马尾松Pinus massoniana生长表现最好,平均胸径17.22 cm,平均树高8.65 m。造林后,SOC含量呈现降低−升高趋势,12年后平均为19.88 g·kg−1,接近造林前水平,0~20 cm层土壤SOC含量达20.33 g·kg−1,比造林前增加38.21%。造林12年后,CK的SOC含量最低,为8.45 g·kg−1;树种配置Ⅰ、Ⅱ、Ⅲ之间SOC含量差异不明显;配置Ⅲ的SOC含量在造林前最低(9.34 g·kg−1),而造林12年后,达各树种配置最高值(13.25 g·kg−1)。造林后,土壤全氮(TN)、全磷(TP)、全钾(TK)、碱解氮(AN)、有效磷(AP)含量呈现降低−升高−降低趋势,速效钾(AK)含量呈现降低−升高趋势;与造林前相比,造林12年后土壤养分含量均下降,树种配置间差异不显著,但CK配置模式各养分含量均比配置Ⅰ、Ⅱ、Ⅲ低,除CK的TP含量比配置Ⅲ稍高外。本次试验TP含量平均为0.21 g·kg−1,远低于全国平均水平(0.56 g·kg–1)。
      结论 在几近荒山植被恢复过程中,针阔混交模式配置Ⅲ表现出较好的恢复效果,多树种混交的恢复效果优于仅有2个树种混交模式。

       

      Abstract:
      Objective This study aimed to investigate the effects of vegetation restoration and reconstruction on soil organic carbon (SOC) and soil nutrients, as well as the recovery efficacy of different tree species configuration patterns.
      Method Four tree species configuration modes were designed: A control mode (CK) planting two species of Liquidambar formosana and Schima superba, a multi-species selection mode (Configuration I), a valuable species intercropping mode (Configuration II), and a conifer-broadleaf mixed mode (Configuration III). Permanent sample plots were established, and plants, SOC, and soil nutrients were continuously surveyed in 2012 (pre-planting), 2014 (2 years post-planting), 2016 (4 years post-planting), and 2024 (12 years post-planting).
      Result A total of 63 tree species were planted in 2012. By 2024, 35 species remained, with Pinus massoniana (high-fat variety) showing the best growth performance, with an average diameter at breast height (DBH) of 17.22 cm and an average tree height of 8.65 m. After afforestation, SOC content showed a trend of decrease followed by an increase, averaging 19.88 g·kg1 after 12 years, close to the pre-planting level. In the 0−20 cm soil layer, SOC reached 20.33 g·kg1, with an increase of 38.21% compared to pre-planting. After 12 years, the CK configuration mode had the lowest SOC content at 8.45 g·kg1. There were no significant differences in SOC contents among Configurations I, II, and III. The SOC content in Configuration III was the lowest (9.34 g·kg1) before planting, but became the highest among all configurations after 12 years (13.25 g·kg1). After afforestation, soil total nitrogen (TN), total phosphorus (TP), total potassium (TK), alkali-hydrolyzable nitrogen (AN), and available phosphorus (AP) contents showed a trend of decrease-increase-decrease, while available potassium (AK) content showed a trend of decrease followed by an increase. Compared to pre-planting, all soil nutrient contents decreased after 12 years, with no significant difference among the configurations. However, the CK configuration mode had lower nutrient contents compared with Configurations I, II, and III for all nutrients, except for TP content in CK, which was slightly higher than that in Configuration III. The average TP content in this experiment was 0.21 g·kg1, far below the national average (0.56 g·kg1).
      Conclusion During the vegetation restoration process on nearly barren mountains, the conifer-broadleaf mixed mode (Configuration III) has better recovery effects, and the multi-species mixed configurations are more effective than the two-species mixed mode.

       

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