氮肥种类对钙质紫色土氨氧化作用及氨氧化微生物群落的影响

Effects of nitrogen fertilizer types on ammonia oxidation and ammonia-oxidizing microbial community in calcareous purple soil

  • 摘要: 微生物驱动的硝化作用是氮循环的关键过程。土壤氨氧化作用是硝化作用的第一步, 也是硝化作用的限速步骤, 施氮是影响土壤氨氧化微生物的重要因素。因此, 明确不同氮肥种类(尿素、硫酸铵和硝酸钾)对土壤氨氧化微生物群落与硝化势的影响, 可以为缓解农田氮素流失和改善氮素循环提供参考。本研究以钙质紫色土为研究对象, 采用盆栽试验, 设置不施氮肥(CK)、施尿素(UR)、施硫酸铵(AS)和施硝酸钾(PN) 4个处理。通过测定不同类型氮肥处理下土壤化学性质、硝化势、土壤氨氧化细菌(AOB)和氨氧化古菌(AOA)的群落结构及α多样性, 明确不同类型氮肥对土壤氨氧化作用的影响。结果表明, 与CK处理相比, AS和UR处理下土壤pH分别显著降低2.52和0.32个单位(P<0.05), AS和UR处理下土壤全氮(TN)和铵态氮(NH4+-N)含量分别显著提升53.6%~83.0%和1 359.5%~1 740.4% (P<0.05); 3种施氮处理下土壤碱解氮(AN)和硝态氮(NO3-N)含量分别显著增加164.9%~233.1%和434.6~1 485.3% (P<0.05); AS处理土壤速效磷(AP)含量显著降低33.7% (P<0.05); AS和UR处理下土壤碳氮比(C/N)分别显著降低40.0%和20.0% (P<0.05); 各处理间土壤有机碳(SOC)含量无显著差异(P>0.05); AS处理土壤硝化势显著降低42.0% (P<0.05), UR和PN处理土壤硝化势分别显著提升292.0%和62.6% (P<0.05)。与CK处理相比, AS和UR处理下AOA amoA基因丰度分别显著提高84.1%和44.4% (P<0.05), AS处理AOB amoA基因丰度显著降低44.0% (P<0.05), UR处理显著提高1 821.3% (P<0.05)。冗余分析显示: 土壤pH和NH4+-N含量为AOA群落结构的主要影响因子, C/N、土壤有机碳(SOC)和碱解氮(AN)为AOB群落结构的主要影响因子(P<0.05)。逐步回归分析显示: NH4+-N和AN为AOA amoA基因丰度的主要影响因子(P<0.001), 速效磷(AP)和AN为AOB amoA基因丰度的主要影响因子(P<0.001)。偏最小二乘法分析显示: AOB amoA基因丰度、SOC、AP、AN和pH对土壤硝化势具有显著影响(P<0.05)。综上, 施用硫酸铵会显著降低土壤硝化势, 而施用尿素会增加土壤硝化势, 且AOB群落为钙质紫色土中氨氧化作用的主要驱动者, 施用硫酸铵主要通过增加AN含量, 降低AP含量和AOB amoA基因丰度, 降低硝化势; 而施用尿素主要通过增加AN含量和AOB amoA基因丰度, 最终增加硝化势。

     

    Abstract: Microorganism-driven nitrification is a key process in the nitrogen cycle. Soil ammonia oxidation is the first rate-limiting step in nitrification, and nitrogen application can affect soil ammonia-oxidizing microorganisms. The effects of different types of nitrogen fertilizers (urea, ammonium sulfate, and potassium nitrate) on soil ammonia-oxidizing microorganisms community and nitrification potential are still debated and can be a crucial reference for alleviating nitrogen loss and improving nitrogen cycle in farmland. In this study, four treatments i.e. no nitrogen fertilizer applied (CK), application of ammonium sulfate (AS), application of urea (UR), and application of potassium nitrate (PN) were established in a pot experiment using calcareous purple soil. Their effects on soil ammonia oxidation were investigated by measuring soil chemical factors, nitrification potential, and community structure and α diversity of soil ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA). Our results indicated that, compared to CK treatment, AS and UR treatments significantly reduced soil pH by 2.52 and 0.32 (P<0.05), and significantly reduced carbon-nitrogen ratio by 40.0% and 20.0% (P<0.05), respectively, while significantly increased total nitrogen (TN) and ammonium nitrogen (NH4+-N) contents by 53.6%−83.0% and 1 359.5%−1 740.4% (P<0.05), respectively. Compared to CK treatment, Soil alkaline hydrolyzed nitrogen (AN) and nitrate nitrogen (NO3-N) contents were significantly increased by 164.9%−233.1% and 434.6%−1 485.3% (P<0.05) under all three nitrogen fertilization treatments, while AS treatment significantly reduced soil available phosphorus (AP) content by 33.7% (P<0.05). The differences in soil organic carbon (SOC) under different treatments were not significant. The lowest nitrification potential was observed under AS treatment, which was reduced by 42% than that under CK treatment, while nitrification potential was significantly increased by 292.0% and 62.6% (P<0.05) under UR and PN treatments, respectively. Moreover, compared to CK treatment, the amoA gene abundance of AOA under AS and UR treatments significantly increased by 84.1% and 44.4% (P<0.05), respectively; the amoA gene abundance of AOB under AS treatment significantly reduced by 44.0% (P<0.05), and UR treatment significantly increased by 1 821.3% (P<0.05). Redundancy analysis showed that pH and NH4+-N were the main factors influencing the AOA community structure, whereas AOB community structure was mostly influenced by C/N, SOC, and AN. Stepwise regression analysis showed that NH4+-N and AN were the main factors influencing amoA gene abundance in AOA, while AP and AN were the main factors influencing amoA gene abundance in AOB. Partial least squares analysis showed that the amoA gene abundance of AOB, SOC, AP, AN, and pH had significant effects on soil nitrification potential (P<0.05). Our findings suggest that the application of ammonium sulfate significantly reduces the nitrification potential by increasing the AN content and reducing the AP content and amoA gene abundance of AOB, whereas urea application increases the nitrification potential by increasing AN content and amoA gene abundance of AOB. The AOB community was the primary driver of soil ammonia oxidation in the calcareous purple soil, and different nitrogen fertilizers exhibited different effects on the ammonia-oxidizing microbial community and nitrification potential. Ammonium sulfate application mainly reduced the nitrification potential by increasing AN content, reducing AP content, and the amoA gene abundance of AOB, whereas urea mainly increased the AN content and amoA gene abundance of AOB, leading to increased nitrification potential.

     

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