长期外源有机物料添加对土壤无机碳库的影响

Effects of long-term addition of exogenous organic materials on soil inorganic carbon pool

  • 摘要: 长期外源有机物料添加对农田土壤无机碳库的具体影响尚不清楚。本研究基于华北农田16年的长期定位试验, 开展了6个施肥处理对照(CK)、单施氮肥(N)、单施化肥(NPK)、氮肥配施有机肥(MN)、化肥配施有机肥(MNPK)和化肥配施秸秆(SNPK)对土壤碳库分布及其相关理化性质影响的研究, 并运用主成分分析法探讨了外源有机物料添加对土壤碳库变化的影响机制。研究结果表明: 与CK相比, 长期外源有机物料添加使0~20 cm土层的土壤有机碳(SOC)含量平均提高45%; MNPK处理使40~50 cm土层的土壤无机碳(SIC)含量提高21%, 而SNPK处理使50~60 cm土层的SIC含量降低28%; 土壤pH值和水分条件是SIC变化的关键因素, 同时SOC含量、有机物料投入量、土壤母质等因子共同影响该过程; 秸秆分解产生的有机酸和CO2以及促进本底SOC矿化产生CO2, 进而导致土壤pH显著下降, 这是SNPK处理导致深层SIC显著损失的主要原因。综上, 化肥配施有机肥有利于土壤有机碳和无机碳的积累, 而化肥配施秸秆则可能导致深层无机碳的损失, 这不仅为揭示外源有机物料添加后土壤碳库的转化机制提供理论依据, 而且对评估SIC在土壤碳储存中的关键作用具有重要意义。

     

    Abstract: The specific effects of long-term addition of exogenous organic materials on soil inorganic carbon pool in farmland is still unclear. Our study was conducted to figure out the effects of different fertilization on soil carbon pool distribution and related physicochemical properties based on a 16-year long-term experiment in North China. Six treatments were set up as follows: control (CK), nitrogen fertilizer (N), chemical fertilizer (NPK), nitrogen fertilizer combined with organic fertilizer (MN), chemical fertilizer combined with organic fertilizer (MNPK), and chemical fertilizer combined with straw (SNPK). In this study, the effects of different fertilization treatments on soil organic carbon (SOC), soil inorganic carbon (SIC) content and other key soil physicochemical properties were analyzed in detail. Principal component analysis was used to investigate the mechanism of exogenous organic material addition on soil carbon pool change. The results showed that the soil organic carbon (SOC) content in 0-20 cm soil layer was increased by 45% on average by long-term addition of exogenous organic materials compared with CK. MNPK treatment increased the soil inorganic carbon (SIC) content by 21% in the 40-50 cm soil layer, while SNPK treatment reduced the SIC content by 28% in the 50-60 cm soil layer. Soil pH value and water condition are the key factors of SIC change, and SOC content, organic materials input, soil parent material and other factors affect the process. The decomposition of straw produces organic acids and CO2, and promotes the mineralization of background SOC to produce CO2, which leads to a significant decrease in soil pH. This is the main reason for the significant loss of SIC in deep layer of SNPK. In conclusion, fertilizer combined with organic fertilizer is conducive to the accumulation of soil organic carbon and inorganic carbon, while fertilizer combined with straw may lead to the loss of inorganic carbon in deep soil. This not only provides a theoretical basis for revealing the transformation mechanism of soil carbon pool after the addition of foreign organic materials, but also has important significance for evaluating the key role of SIC in soil carbon storage.

     

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