• ISSN 1008-505X
  • CN 11-3996/S

长期不同有机无机肥配施对旱地冬小麦土壤磷组分及产量的影响

Effects of long-term organic-inorganic fertilization regimes on soil phosphorus fractions and grain yield of dryland winter wheat

  • 摘要:
    目的 通过长期定位试验,探究施氮量与有机肥配施对黄土高原旱地冬小麦土壤磷(P)组分转化及有效磷(AP)供给的影响及其与产量形成的耦合关系,为旱地麦田氮磷协同高效管理及有机无机肥配施优化提供理论依据。
    方法 于2014年秋播至2024年收获,在黄土高原旱地冬小麦长期定位试验区开展施肥试验,采用二因素裂区设计,主处理为施氮水平(N0、N75、N150、N225和N300),副处理为有机肥施用(M0和M1),共10个处理,重复3次。2024年收获后采集0—20 cm土层土样,采用Hedley磷分级法测定土壤无机磷和有机磷组分含量,并结合回归分析和Pearson相关性分析探讨土壤磷组分与有效磷及产量形成的关系。
    结果 1)与单施化肥(M0)相比,有机无机肥配施(M1)下冬小麦平均增产15.6%。M1N150处理下产量最高为6500.9 kg/hm2,比M0N0提高64.5%。2)与单施化肥(M0)相比,有机无机肥配施(M1)提高了土壤活性磷组分(H2O-Pi、NaHCO3-Pi和NaHCO3-Po)、中等活性磷组分(NaOH-Pi)、稳定性磷组分(Residual-P)及AP含量,其中AP平均提高311.5%。有机无机肥配施对活性磷库的促进作用大于对稳定磷库的影响,与AP显著增加的趋势一致。在不同施氮量下,活性无机磷与AP整体呈先增加后趋稳的趋势,而稳定性磷库变化幅度较小。不同处理间籽粒产量与AP及活性无机磷含量呈一致的变化趋势,且均表现为显著正相关。3)相关性分析表明,AP与活性无机磷组分(H2O-Pi、NaHCO3-Pi、NaOH-Pi)均呈极显著正相关(P<0.001),表明活性无机磷是维持土壤AP供给的关键磷库。2015—2024年的连续数据进一步显示,产量与AP呈显著正相关;两因素方差分析显示,氮肥与有机肥配施对H2O-Pi、NaOH-Pi和全磷存在显著交互效应(P<0.05)。
    结论 基于2014—2024年长期定位试验,冬小麦产量随施氮量增加呈先增加后趋于稳定的趋势;有机无机肥配施在中等施氮水平下的增产及磷库优化效应更为突出,其中M1N150处理的综合效应最佳。长期施氮与有机无机肥配施促进了土壤不同活性水平磷库间的再分配,提高了活性无机磷(H2O-Pi、NaHCO3-Pi)及中等活性磷(NaOH-Pi和NaOH-Po)的供磷潜力。总体上,产量提升与AP累积主要受活性无机磷驱动,活性无机磷是维持土壤供磷能力的关键磷库。

     

    Abstract:
    Objectives To investigate the effects of long-term N application rates and manure addition on phosphorus (P) fraction transformations in calcareous soils under rainfed winter wheat on the Loess Plateau, and to elucidate their effects on available phosphorus (AP) supply and its relationship with grain yield formation, thereby providing a scientific basis for synergistic N-P management and optimized integrated organic-inorganic fertilization in dryland wheat systems.
    Methods A long-term fertilization experiment was conducted in a rainfed winter wheat field on the Loess Plateau from autumn sowing in 2014 to harvest in 2024. A two-factor split-plot design was employed, with N application rate as the main-plot factor (N0, N75, N150, N225, and N300) and manure application as the subplot factor (M0 and M1), resulting in 10 treatments with three replicates. After the 2024 harvest, soil samples were collected from the 0–20 cm soil layer. Inorganic and organic P fractions were determined using the Hedley sequential fractionation method. Regression analysis and Pearson correlation analysis were used to evaluate the relationships among P fractions, AP, and grain yield.
    Results 1) Compared with chemical fertilizer alone, the combined application of organic and inorganic fertilizers increased winter wheat grain yield by an average of 15.6%. The M1N150 treatment produced the highest yield (6500.9 kg/hm2), which was 64.5% higher than M0N0. 2) Relative to M0, the combined application of organic and inorganic fertilizers (M1) increased labile P fractions (H2O-Pi, NaHCO3-Pi, and NaHCO3-Po), moderately labile P fractions (NaOH-Pi), stable P fractions (Residual-P), and Olsen-P (AP), with AP increasing by an average of 311.5%. The increase in the labile pool exceeded that of the stable pool, consistent with the overall rise in AP. Across different N rates, labile inorganic P and AP generally increased and then plateaued, whereas the stable pools changed only slightly. Grain yield changed mirrored the increases in AP and labile inorganic P. 3) Correlation analysis showed that AP was extremely significantly and positively correlated (P<0.001) with labile inorganic P fractions (H2O-Pi, NaHCO3-Pi, and NaOH-Pi) , indicating that labile inorganic P was the key pool sustaining AP supply. Data from 2015–2024 further showed a significant positive relationship between grain yield and AP. Two-way ANOVA indicated significant interaction effects between N application and manure addition on H2O-Pi, NaOH-Pi and total phosphorus (P<0.05).
    Conclusions Based on the 2014–2024 long-term field experiment, winter wheat grain yield increased with increasing N input and then plateaued; manure addition showed more pronounced yield gains and P-pool optimization under the moderate N rate, with M1N150 performing the best overall. Long-term N application combined with manure application promoted the redistribution of soil P among pools of different lability, enhanced the P-supplying potential of labile inorganic P (H2O-Pi and NaHCO3-Pi) and moderately labile P (NaOH-Pi and NaOH-Po), and optimized the distribution of soil P among pools of different lability. Overall, yield improvement and available phosphorus (AP) accumulation were mainly driven by labile inorganic P, identifying it as the key P pool supporting crop production.

     

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