• ISSN 1008-505X
  • CN 11-3996/S

有机肥替代化肥氮并配施生物炭有效提高砂质潮土氮磷库的容量和供应强度

Manure substitution combined with biochar enhances nitrogen and phosphorus pools capacity and supply intensity in sandy fluvo-aquic soil

  • 摘要:
    目的 砂质潮土结构性差,矿化作用强,保水保肥能力弱等障碍突出,探究生物炭、有机肥及其配施对其不同深度土壤氮素、磷素组分及转化的影响,可为其障碍消减、地力提升提供理论和技术支撑。
    方法 于2021年10月在河南省新乡县朗公庙镇设置小麦-玉米轮作定位试验,冬小麦季设置常规化肥(CK)以及在此基础上一次性施用生物炭(T1,15 t/hm2)、每年施用生物炭(T2,12 t/hm2);有机肥替代化肥氮20% (J1)、40% (J2);J1和J2每年配施生物炭12 t/hm2(TJ1、TJ2)7个处理。于2024年6月(3年后)冬小麦收获期采集0—20 cm (表层)、20—40 cm (中层)、40—60 cm (下层)土壤,分析无机氮及酸解有机氮组分含量(酸解铵态氮、酸解氨基酸态氮、酸解氨基糖态氮、酸解未知态氮、非酸解氮),活性磷(H2O-P、NaHCO3-Pi、NaHCO3-Po)、中等活性磷(NaOH-Pi、NaOH-Po)、稳定态磷(HCl-P、Residual-P)含量,氮、磷素转化相关胞外酶活性。
    结果 T1处理各土层酸解有机氮组分含量较CK处理无明显差异,而T2相较CK提高了表层β-乙酰氨基葡萄糖苷酶活性,显著提高表、中层全氮含量33.3%~52.0%,增加了表层土壤中酸解氨基酸态氮,并促进了表层土壤中稳定态磷积累。相比CK处理,J1和J2处理显著提高了表层β-乙酰氨基葡萄糖苷酶和磷酸酶活性,提升了0—60 cm土层全氮含量和有效态氮、磷含量,显著提高了表层土壤酸解氨基酸态氮含量、中层土壤酸解铵态氮含量,提高表层活性磷含量31.1%~89.9%、中层29.6%~117.7%以及中等活性磷含量51.0%~114.2%。相较T2、J1和J2处理,JT1和JT2处理施进一步提高了各土层氮、磷转化酶活性,尤其是显著提高表层无机氮和活性磷含量,增加表层酸解未知态氮比例,减少下层无机氮积累,TJ1还显著增加中层土壤活性及中等活性磷含量。
    结论 有机肥施用显著提升0—40 cm土层全氮含量,提高了其中活性较强的酸解铵态氮与酸解氨基酸态氮组分占比,进而增强了氮、磷转化胞外酶活性,促进了砂质潮土表层和中层土壤磷素的活化。在此基础上,每年配施生物炭12 t/hm2进一步促进氮素向酸解未知态氮转化,同时加强对易分解有机氮和活性磷库的固持,呈现提高表层活性磷含量,稳定中、下层土壤磷库的效应,有效减少氮磷养分的淋溶损失。因此,砂质潮土地区以20%~40%有机肥替代常规化肥氮施用量,同时配合施用生物炭是提升砂质潮土氮磷库容量及供应强度的可行措施。

     

    Abstract:
    Objectives Sandy fluvo-aquic soil has prominent obstacles such as poor structure, intense mineralization, and weak water and fertilizer retention. Exploring the effects of biochar, manure and their combined application on soil nitrogen and phosphorus components and transformation at different depths can provide theoretical and technical support for its obstacle reduction and soil fertility improvement.
    Methods In October 2021, a wheat-maize rotation experiment was set up in Langgongmiao Town, Xinxiang County, Henan Province. The winter wheat season was set up seven treatments: conventional chemical fertilizer (CK), and on this basis, one-time biochar application (T1, 15 t/hm2), annual biochar (T2, 12 t/hm2), manure instead of chemical fertilizer nitrogen 20% (J1), manure instead of chemical fertilizer nitrogen 40% (J2), J1 combined with biochar (TJ1, 12 t/hm2) and J2 combined with biochar (TJ2, 12 t/hm2). Soil samples were collected at 0–20 cm (topsoil), 20–40 cm (middle soil) and 40–60 cm (deep soil) during the winter wheat harvest period in June 2024. The contents of soil inorganic nitrogen and acid-hydrolyzed organic nitrogen components (acid-hydrolyzed ammonium nitrogen, acid-hydrolyzed amino acid nitrogen, acid-hydrolyzed amino sugar nitrogen, acid-hydrolyzed unknown nitrogen, non-acid-hydrolyzed nitrogen), labile phosphorus (H2O-P, NaHCO3-Pi, NaHCO3-Po), moderately labile phosphorus (NaOH-Pi, NaOH-Po), and stable phosphorus (HCl-P, Residual-P), as well as extracellular enzyme activities related to nitrogen and phosphorus transformations were analyzed.
    Results The content of acid-hydrolyzable organic nitrogen fractions in each soil layer under T1 showed no significant difference compared with CK. In contrast, T2 increased the activity of β-acetyl-glucosaminidase in the topsoil, significantly increased the total nitrogen content in the topsoil and middle soil by 33.3%−52.0%, enhanced acid-hydrolyzable amino acid nitrogen in the topsoil, and promoted the accumulation of stable phosphorus content in the topsoil. Compared with CK, J1 and J2 treatment significantly increased β-acetyl-glucosaminidase and phosphatase activites in the topsoil, elevated total N across the 0–60 cm soil layer, and increased available N and P contents. J1 and J2 treatments also significantly increased acid-hydrolyzable amino acid nitrogen in the topsoil, and acid-hydrolyzable ammonium nitrogen in the middle soil layer, and raised labile phosphorus content by 31.1%−89.9% in the topsoil and by 29.6%−117.7% in the middle soil, as well as moderately labile phosphorus content by 51.0%−114.2% in the middle soil. Compared with T2, J1 or J2 treatment, TJ1 and TJ2 treatment further increased the activities of N and P transforming enzymes across all soil layers, particularly significantly increased the content of inorganic N and labile P in topsoil, increased the proportion of acid-hydrolyzed unknown nitrogen in the topsoil, and reduced the accumulation of inorganic nitrogen in the deep soil. TJ1 also significantly increased the content of labile and moderately labile phosphorus in the middle soil.
    Conclusions The application of manure significantly increased the total N content in the 0–40 cm soil layer, raised the proportions of highly active acid-hydrolyzable ammonium N and acid-hydrolyzable amino acid N fractions, thereby enhancing the activities of extracellular enzymes involved in N and P transformation, and promoting the activation of phosphorus in the surface and middle layers of sandy fluvo-aquic soil. On this basis, the annual combined application of biochar at 12 t/hm2 further facilitates the transformation of N to acid-hydrolyzable unknown form, while strengthening the retention of easily decomposable organic nitrogen and active phosphorus pools. This presents the effects of increasing the active phosphorus content in the surface layer and stabilizing the phosphorus pools in the middle and lower soil layers, effectively reducing the leaching loss of nitrogen and phosphorus nutrients. Therefore, in sandy fluvo-aquic soil regions, replacing 20%−40% of the conventional chemical fertilizer nitrogen application rate with manure, combined with the application of biochar, is a feasible measure to improve the capacity and supply intensity of nitrogen and phosphorus pools in sandy fluvo-aquic soil.

     

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