曾婷婷, 王路明, 杨康, 胡春胜, 李晓欣, 董文旭. 长期外源有机物料添加对土壤无机碳库的影响*[J]. 中国生态农业学报(中英文). DOI: 10.12357/cjea.20240295
引用本文: 曾婷婷, 王路明, 杨康, 胡春胜, 李晓欣, 董文旭. 长期外源有机物料添加对土壤无机碳库的影响*[J]. 中国生态农业学报(中英文). DOI: 10.12357/cjea.20240295

长期外源有机物料添加对土壤无机碳库的影响*

  • 摘要: 为深入探究长期外源有机物料添加对农田土壤无机碳库的具体影响,本研究基于华北农田16年的长期定位试验,开展了不同施肥处理对土壤碳库分布及其相关理化性质影响的研究。试验设置了6个处理,包括对照(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),化肥配施秸秆(SNPK)。本研究详细分析了不同施肥处理对土壤有机碳(SOC)、无机碳(SIC)含量及其他关键土壤理化性质的影响,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:长期外源有机物料添加显著提高了0-20 cm土层的SOC含量;与CK相比,MNPK在0-60土层中使SIC含量增加了7.0%,而SNPK则降低了7.6%;在50-60 cm土层SNPK使SIC损失27.9%;秸秆分解产生有机酸和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深层SIC显著损失的主要原因。研究成果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,而且对于评估SIC在土壤碳储存中的关键作用具有重要意义。

     

    Abstract: In order to further explore the specific effects of long-term addition of exogenous organic materials on soil inorganic carbon pool in farmland, this study carried out a study on the effects of different fertilization treatments on soil carbon pool distribution and related physicochemical properties based on a 16-year long-term positioning experiment in farmland in North China. Six treatments were set up, including 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), inorganic carbon (SIC) content and other key soil physicochemical properties were analyzed in detail, and the mechanism of exogenous organic material addition on soil carbon pool change was discussed by principal component analysis. The results showed that the long-term addition of exogenous organic materials significantly increased SOC content in 0-20 cm soil layer. Compared with CK, MNPK increased SIC content by 7.0% in 0-60 soil layer, while SNPK decreased by 7.6%. In 50-60 cm soil layer, SNPK caused 27.9% loss of SIC. 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, which may be the main reason for the significant loss of SIC in the deep layer of SNPK. The research results not only provide theoretical basis for revealing the transformation mechanism of soil carbon pool after the addition of foreign organic materials, but also have important significance for evaluating the key role of SIC in soil carbon storage.

     

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