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生物有机肥-米豆轮作土壤氮素转化对作物氮素利用的影响机制

The impact mechanism of soil nitrogen transformation on crop nitrogen utilization in bio organic fertilizer maize soybean rotation

  • 摘要: 为解决东北黑土区玉米-大豆轮作长期依赖化肥导致的氮素利用率低下问题,探究生物有机肥替代氮肥对轮作系统土壤氮素转化与作物氮素利用的影响,设置生物有机肥(OB类)、灭活生物有机肥(O类)、枯草芽孢杆菌菌粉(B类)按10%、20%、30%梯度替代氮肥,测定作物产量、各器官氮素含量与氮肥利用率,以及各生育期土壤氮素组分(全氮、有机氮、无机氮、铵态氮、硝态氮、微生物量氮)、脲酶与蛋白酶活性、土壤净矿化速率与硝化速率、大豆根瘤数量与固氮相关酶活性等指标,采用方差分析、冗余分析、相关性分析与结构方程模型解析氮素转化路径。结果表明:1)生物有机肥替代20%比例氮肥(OB2处理)为最优处理,大豆产量提升25.97%,氮素利用率由11.11%提高至44.77%;后茬玉米产量提升25.60%,氮素利用率由32.37%提高至64.37%。但各指标未随替代比例增加而线性上升,存在最优投入阈值。OB2处理显著增强了土壤氮转化活性,大豆与玉米成熟期土壤净矿化速率、硝化速率较CK分别提高12.16%、20.95%和8.49%、28.48%,表现出跨季增效能力;大豆成熟期土壤无机氮含量提高19.12%,有机氮含量提高24.69%。同时,OB2处理显著促进大豆根瘤发育,根瘤数量、干重、固氮酶活性较CK分别提高70.02%、84.19%和26.25%。冗余分析表明,生育关键期土壤氮转化与无机氮含量显著正相关,成熟期则与微生物量氮库紧密关联(P≤0.005);结构方程模型显示,氮素主要经由“土壤氮矿化与硝化速率—铵态氮与有机氮—作物全氮—产量”路径实现向籽粒的高效转运,关键路径系数为0.656、0.996、0.767和0.307。上述机制证实了生物有机肥可通过培育高效根瘤系统、提升土壤氮库容量与调控微生物过程,最终通过影响土壤氮素转化,实现轮作系统氮素利用效率与产量的同步提升。

     

    Abstract:
    To address the low nitrogen use efficiency caused by long-term dependence on chemical nitrogen fertilizer in maize-soybean rotation systems in the black soil region of Northeast China, a two-year field experiment was conducted during 2023-2024 at the Xiangyang demonstration base of Northeast Agricultural University, Harbin, to clarify how partial substitution of nitrogen fertilizer with bio-organic fertilizer regulated soil nitrogen transformation and crop nitrogen utilization across the rotation. A randomized block design with three replicates was adopted, in which bio-organic fertilizer containing humus and Bacillus subtilis (OB), sterilized bio-organic fertilizer (O), or Bacillus subtilis inoculant alone (B) replaced 10%, 20%, or 30% of the synthetic nitrogen fertilizer, with an unfertilized treatment as the control. Soybean (Dongnong 252) and maize (Dongnong 2004) were grown in rotation under rain-fed conditions. At harvest, crop yield, nitrogen concentration and accumulation in individual organs were determined, and nitrogen use efficiency, agronomic efficiency, yield response index, and yield sustainability were calculated. Topsoil samples (0-20 cm) were collected at key growth stages of both crops: microbial biomass nitrogen was determined by the chloroform fumigation-extraction method, inorganic nitrogen fractions were measured with a continuous flow analyzer, net nitrogen mineralization and nitrification rates were estimated by laboratory incubation, and urease and protease activities were assayed colorimetrically. Soybean nodule number and dry weight were recorded, nitrogenase activity was measured by the acetylene reduction assay, and superoxide dismutase, peroxidase, and leghemoglobin contents were determined to evaluate symbiotic nitrogen fixation capacity. One-way analysis of variance followed by the least significant difference test, redundancy analysis, correlation and interaction analysis, and structural equation modeling were integrated to dissect the pathways linking soil nitrogen transformation to crop nitrogen use and yield formation.
    The results showed that substituting 20% of the nitrogen fertilizer with bio-organic fertilizer (OB2) was the optimal treatment. Compared with the control, soybean yield increased by 25.97% and nitrogen use efficiency rose from 11.11% to 44.77%; in the following maize season, yield increased by 25.60% and nitrogen use efficiency rose from 32.37% to 64.37%. However, none of these indicators increased linearly with the substitution rate, indicating an optimal input threshold. The OB2 treatment significantly and persistently enhanced soil nitrogen transformation activity: the soil net mineralization rate increased by 12.16% and 8.49%, and the nitrification rate by 20.70% and 29.12%, at the maturity stages of soybean and maize, respectively, demonstrating a clear carry-over effect across seasons. At soybean maturity, soil inorganic nitrogen content increased by 19.12% and organic nitrogen by 24.69%. Meanwhile, OB2 markedly promoted soybean nodulation and nitrogen fixation, with nodule number, nodule dry weight, and nitrogenase activity increasing by 70.02%, 84.19%, and 26.25%, respectively. Redundancy analysis indicated that during the nutrient-demanding stages, soil nitrogen transformation was most significantly and positively associated with inorganic nitrogen content, whereas at maturity it was closely linked to the microbial biomass nitrogen pool (P ≤ 0.005). Structural equation modeling further revealed that nitrogen was efficiently transferred to grains mainly through a cascade in which elevated soil mineralization and nitrification rates raised ammonium and organic nitrogen availability, then crop total nitrogen accumulation, and finally grain yield, with key standardized path coefficients of 0.656, 0.996, 0.767, and 0.307. These findings demonstrated that bio-organic fertilizer, through the synergistic action of humus and functional Bacillus subtilis, fostered an efficient nodule system, enlarged the soil nitrogen pool, and regulated microbial transformation processes, thereby synchronously improving nitrogen use efficiency and yield in the maize-soybean rotation system. These results highlight the central role of soil nitrogen transformation in coordinating crop nitrogen supply within rotation systems, providing a theoretical basis and quantitative support for precise bio-organic fertilizer application in cold-region black soils.

     

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