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    马尾松阔叶化改造土壤团聚体稳定性对胶结剂的响应

    Response of soil aggregate stability to cements in the broad-leaved transformation of Pinus massoniana forests

    • 摘要: 阔叶化改造是实现针叶人工林土壤结构恢复的管理办法。为明晰阔叶化改造如何调节土壤胶结剂以增强团聚体稳定性,以马尾松人工林纯林(PM)及其与伯乐(PM×BS)、连香(PM×CJ)、深山含笑(PM×MM)混交林为研究对象,通过湿筛法和平均质量直径(MWD)、几何平均直径(GMD)和>0.25 mm粒径团聚体质量百分比(R0.25)评估团聚体稳定性,并分析胶结剂(团聚体有机碳(SAOC),游离态铁铝氧化物(Fed/Ald)、非晶形铁铝氧化物(Feo/Alo)、络合态铁铝氧化物(Fep/Alp))对团聚体稳定性的贡献。结果表明:1)0~20 cm土层,PM×CJ和PM×MM > 1 mm团聚体含量较PM增幅在8.76%~112.58%,且MWD、GMD和R0.25均显著提升;在20~40 cm土层,针-阔混交林均显著提高 > 1 mm团聚体含量且PM×CJ的MWD、GMD和R0.25较PM显著提高;2)针-阔混交林显著提高0~20 cm土层各粒径SAOC含量(PM×MM林最高);各林分中三种形态铁铝氧化物含量均为Fed/Ald最高,仅PM×BS 0~40 cm各粒径团聚体Fed含量低于PM;3)0~20 cm土层Fed、SOC和Feo与>1 mm团聚体均极显著正相关(P<0.01),以Fed对MWD的正向显著贡献最高;Ald对20~40 cm土层团聚体稳定性增强起主导作用,并与1~0.5 mm团聚体极显著正相关(P<0.01)。4)Fed、Feo、Ald和SOC含量受pH显著调节(呈显著(P<0.05)或极显著(P<0.01)负相关)。阔叶化改造主要通过提升土壤不同形态Fe/Al氧化物含量以实现土壤团聚体稳定性的改良,研究结果可为马尾松人工林的土壤修复及可持续经营提供数据支撑。

       

      Abstract: Background The introduction of broad-leaved species into coniferous plantations is a practical approach for restoring soil structure. However, how this broad-leaved transformation regulates cementing agents to enhance soil aggregate stability remains unclear. Methods This study investigated pure Pinus massoniana plantations. (PM) and their mixed forests with Bretschneidera sinensis (PM×BS), Cercidiphyllum japonicum (PM×CJ), and Michelia maudiae (PM×MM). The effects of broad-leaved transformation on soil aggregate stability and cementing agents were examined. The cementing agents included soil aggregate organic carbon (SAOC) and iron/aluminum oxides in free (Fed/Ald), amorphous (Feo/Alo), and complexed (Fep/Alp) forms. Results 1) In the 0-20 cm soil layer, the content of >1 mm aggregates in PM×CJ and PM×MM increased by 8.76%-112.58% compared to PM, with significant increases in MWD, GMD, and R0.25. In the 20-40 cm soil layer, mixed forests significantly increased the content of >1 mm aggregates, and PM×CJ showed significant improvements in MWD, GMD, and R0.25 compared to PM. 2) Coniferous-broadleaf mixed forests significantly increased the SAOC content across all particle sizes in the 0-20 cm soil layer (with PM×MM exhibiting the highest values). Among all forest types, the content of iron and aluminum oxides was highest for Fed and Ald. Only in PM×BS, the Fed content in all aggregate sizes within the 0-40 cm layer was lower than in PM. 3) In the 0-20 cm soil layer, Fed, SOC, and Feo showed highly significant positive correlations with >1 mm aggregates (P < 0.01), with Fed contributing the most significantly to the positive enhancement of MWD. In the 20-40 cm soil layer, Ald played a dominant role in enhancing aggregate stability and exhibited a highly significant positive correlation with 1-0.5 mm aggregates (P < 0.01). 4) The contents of Fed, Feo, Ald, and SOC were significantly regulated by pH, showing significant (P < 0.05) or highly significant (P < 0.01) negative correlations. Conclusion The broadleaf transformation primarily enhances the stability of soil aggregates by increasing the contents of various forms of Fe/Al oxides in the soil. The research findings provide data support for soil restoration and sustainable management of P. massoniana plantations.

       

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