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, 设置不施肥(CK)、尿素(UR)、硫酸铵(AS)和硝酸钾(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1359.5%~1740.4% (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434.6~1485.3% (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处理硝化势显著提升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AOB amoA基因丰度显著提高1821.3% (P<0.05)。冗余分析显示: 土壤pH和NH4+-N为AOA群落结构的主要影响因子, C/N、SOC和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, 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: Nitrification driven by microorganisms is a key process in the nitrogen cycle. Soil ammonia oxidation is the first and rate-limiting step of nitrification, and nitrogen application can affect soil ammonia-oxidizing microorganisms. The effects of different nitrogen fertilizer types (urea, ammonium sulfate and potassium nitrate) on soil ammonia-oxidizing microbial community and nitrification potential are still in default of empirical evidence and should be identified to provide reference for alleviating farmland nitrogen loss and improving nitrogen cycle. In this study, calcareous purple soil was used as the research object, and four treatments of no fertilizer (CK), urea (UR), ammonium sulfate (AS) and potassium nitrate (PN) were set up by pot experiment. The effects of different types of nitrogen fertilizers on soil ammonia oxidation were clarified by measuring soil chemical factors, nitrification potential, community structure and 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, and reduced C/N ratio by 40.0% and 20.0% (P<0.05), but significantly increased total nitrogen (TN) and ammonium nitrogen (NH4+-N) content by 53.6%~83.0% and 1359.5%~1740.4% respectively (P<0.05); soil alkaline hydrolysis nitrogen (AN) and nitrate nitrogen (NO3--N) content were significantly increased by 164.9%~233.1% and 434.6~1485.3% among three N fertilization treatments (P<0.05); soil available phosphorus (AP) content was significantly reduced by 33.7% merely in AS treatment compared to the other three treatment groups (P<0.05); there was no obvious differs in soil organic carbon (SOC) content among different treatments (P>0.05); the lowest nitrification potential was found in AS treatment than those in the other three treatment groups, reduced by 42% relative to CK treatment, while nitrification potential was significantly increased by 292.0% and 62.6% respectively in UR and PN treatments (P<0.05). Moreover, AS and UR treatments significantly increased the amoA gene abundance of AOA by 84.1% and 44.4%, AS treatment significantly reduced the amoA gene abundance of AOB by 44.0%, and UR treatment significantly increased the amoA gene abundance of AOB by 1821.3% (P<0.05) compared to CK treatment, respectively. Redundancy analysis showed that pH and NH4+-N were the main influencing factors of AOA community structure, while C/N, SOC and AN were the main influencing factors of AOB community structure (P<0.05). Stepwise regression analysis showed that were NH4+-N and AN were the main influencing factors of the amoA gene abundance of AOA, while AP and AN were the main influencing factors of the amoA gene abundance of AOB (P<0.001). 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 AN content and reducing AP content and the amoA genes abundance of AOB, while urea application increases the nitrification potential by increasing AN content and the amoA genes abundance of AOB. AOB community is the main driver of soil ammonia oxidation in calcareous purple soil. In calcareous purple soil, the application of different nitrogen fertilizers had different effects on ammonia-oxidizing microbial community and nitrification potential. Among them, the application of ammonium sulfate mainly reduced nitrification potential by increasing AN content, reducing AP content and the amoA gene abundance of AOB, while the application of urea mainly increased AN content and the amoA gene abundance of AOB , and finally increased the nitrification potential.

     

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