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    不同森林类型土壤有机碳特征及固碳潜力分析

    Analysis of soil organic carbon characteristics and carbon sequestration potential of different forest types

    • 摘要: 研究不同森林类型土壤有机碳分布特征及其影响因素,对提升森林碳汇及水土保持功能具有重要意义。笔者对不同森林类型土壤有机碳及活性有机碳组分分布进行观测分析。选取鹫峰国家森林公园侧柏林、油松林、栓皮栎林和油松栓皮栎混交林4种森林类型0~60 cm土层土壤为研究对象,解析森林类型对土壤固碳的影响,并利用冗余分析确定土壤有机碳变化的关键因子。结果表明:1)除20~40 cm土层外,4种森林类型对各土层的土壤有机碳质量分数均有显著影响,且油松栓皮栎混交林和栓皮栎林的土壤有机碳质量分数明显高于侧柏林和油松林(P < 0.05);2)不同森林类型对土壤活性有机碳质量分数的影响主要体现在土壤表层,且油松栓皮栎混交林和栓皮栎林活性有机碳质量分数高于侧柏林和油松林;3)土壤全氮是影响侧柏林、栓皮栎林和油松栓皮栎混交林土壤有机碳及活性有机碳分布的主要影响因子,土壤速效钾和速效磷是影响油松林土壤有机碳及活性有机碳分布的主要影响因子。油松栓皮栎混交林和栓皮栎林具有较强的固碳能力。结果可为研究区水土保持固碳增汇提供参考。

       

      Abstract:
      Background Studying the distribution patterns and factors that influence soil organic carbon is of great significance for enhancing forest carbon sink and soil and water conservation functions. Authors observed and analyzed the distribution of soil organic carbon and active organic carbon fractions in various forest types.
      Methods Soil in 0–60 cm layer for four forest types in Jiufeng National Forest Park, namely Platycladus orientalis forest, Pinus tabuliformis forest, Quercus variabilis forest and Pinus tabuliformis & Quercus variabilis forest, were selected to analyze the effects of forest types on soil carbon sequestration, and to determine the key factors of soil organic carbon changes using redundancy analysis.
      Results 1) Except for the 20–40 cm soil layer, the four forest types had a significant effect on the soil organic carbon mass fraction of each soil layer, and the soil organic carbon contents of the P. tabuliformis & Q. variabilis forest and Q. variabilis forest was significantly higher than that of P. orientalis forest and P. tabuliformis forest (P < 0.05). 2) The impact of different forest types on the active organic carbon contents was mainly manifested in the soil surface, and the active organic carbon content of the P. tabuliformis & Q. variabilis forest and Q. variabilis forest was higher than that of P. orientalis forest and P. tabuliformis forest. 3) Soil total nitrogen was the main factor affecting the distribution of soil organic carbon and active organic carbon in P. orientalis forest, Q. variabilis forest and P. tabuliformis & Q. variabilis forest. Soil available phosphorus and available potassium were the main factors affecting the distribution of soil organic carbon and active organic carbon in the P. tabuliformis forest.
      Conclusions The P. tabuliformis & Q. variabilis forest and Q. variabilis forest have strong carbon sequestration capacity, this may provide the support of carbon sequestration and soil and water conservation in the study area.

       

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