长期不同施肥模式对农田黑土微生物群落构建的影响

    Changes in Community Assembly of Microbiomes in Black Soil under Distinct Scenarios of Long-term Field Fertilization

    • 摘要: 高强度集约化农业管理模式影响土壤微生物区系及其功能。围绕我国典型黑土生态环境重点野外科学观测试验站36年的长期不同施肥管理土壤:不施肥(CK)、单施化肥(NPK)、单施有机肥(OM)和有机-无机肥配施(MNPK),研究了土壤肥力和微生物呼吸,并通过高通量测序技术和微生物群落构建模型探讨了长期不同施肥模式对土壤功能微生物演替的环境驱动机制。结果表明:长期施肥提升了土壤肥力,如土壤有机碳、全氮、有效磷含量以及微生物活性。不同施肥管理模式土壤微生物呼吸活性存在显著差异,由大到小依次为MNPK、OM、NPK和CK。与CK(以C计,186.9 μg·g-1)相比,MNPK处理土壤微生物呼吸(以C计,228.7 μg·g-1)增幅高达22.4%。差异物种分析(LEfSe)表明,NPK和MNPK处理具有相似的指示物种,主要为Dyella marensisBacillus megateriumHerbaspirillum sp.,OM处理则主要包括Bacillus acidicelerBacillus megaterium。长期施肥刺激了氨氧化细菌(Nitrosospira)生长,NPK处理氨氧化细菌丰度增加3.61倍,而黑土中氨氧化古菌和亚硝酸盐氧化细菌的优势类群分别为NitrososphaeraNitrospira。微生物共存网络分析表明,MNPK处理土壤微生物的关联度最为紧密,其正向网络关联度占比高达99.6%,显著高于NPK处理的78.4%和OM处理的97.4%。β NTI分析表明,长期施肥导致微生物类群定向富集而强化了群落组装的确定性过程,且MNPK处理确定性过程占比最高。结构方程模型(SEMs)进一步分析表明,长期施肥模式土壤肥力提升与微生物区系活性呈显著正相关,其解释度>90%。上述结果表明,长期施肥显著刺激功能菌生长,改变土壤微生物区系,提升土壤肥力,且MNPK处理对土壤肥力及其功能稳定性的提升,明显优于NPK和OM处理。研究结果可为确立更为完善的农田黑土施肥管理制度提供科学依据。

       

      Abstract: Intensive agricultural management is influential to soil microbiome and its functions. Based on a 36-year fertilization experiment at the Ministry of Agriculture Key Field Observation Station of Harbin Black Soil Ecological Environment, effects of four fertilization managements (CK: no fertilizer; NPK: mineral fertilizer; OM: organic fertilizer; MNPK: mineral NPK plus organic fertilizer) on soil fertility and microbial respiration were quantitively studied, and microbial community assembly mechanisms were analyzed using the high-throughput sequencing and community assembly models. Results show that long-term fertilization improved soil fertility, such as soil organic carbon, total nitrogen, available phosphorus and microbial activity. Soil microbial respiration was increased in the order of CK < NPK < OM < MNPK. Compared with CK (calculated in carbon, 186.9 μg·g-1), soil microbial respiration in MNPK (calculated in carbon, 228.7 μg·g-1) was increased by 22.4%. Linear discriminant analysis effect size (LEfSe) indicates that NPK and MNPK treatments had similar keystones including Dyella marensis, Bacillus megaterium and Herbaspirillum sp., while OM was predominated by Bacillus acidiceler and Bacillus megaterium. As compared with CK, long-term fertilization stimulated the growth of ammonia oxidizing bacteria (AOB) with the Nitrosospira-like AOB increased by 3.61 times in NPK treatment. The dominant phylotypes of ammonia oxidizing archaea (AOA) and nitrite oxidizing bacteria (NOB) were Nitrososphaera and Nitrospira, respectively. The co-occurrence network analysis revealed that soil microbial community in MNPK had the most closely links, with the proportion of positive links reached 99.6% versus 78.4% in NPK and 97.4% in OM. The analysis of β NTI indicates that long-term fertilization strengthened the deterministic processes of microbial community assembly, with the strongest determinism occurred in MNPK. Structural equation models (SEMs) further suggest strongly positive correlations between soil fertility improvement and microbial respiration (explaining > 90% of variation) among fertilization managements. This study demonstrates that long-term fertilization significantly stimulated the growth of functional microbiomes, altered community structure and improved soil fertility. Compared with NPK and OM, MNPK treatment was more efficient in enhancing soil fertility and stability of microbial community. As a whole, these results provide scientific basis for optimizing the efficient fertilization managements in black soils.

       

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