日光温室黄瓜根际与非根际土壤氨氧化微生物对施氮的 响应及其影响因子研究
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(内蒙古农业大学,内蒙古 呼和浩特 010019)

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张迎(2000-),在读硕士研究生,主要从事温室土壤修复研究。E-mail:zhangying701213@163.com。

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内蒙古自治区自然科学基金(2019MA03061);呼和浩特市基础研究与应用基础研究科技计划项目(2025- 规- 基-10)。


Response of ammonia-oxidizing microorganisms in rhizosphere and non-rhizosphere soil of cucumbers in solar greenhouse to nitrogen application and influencing factors
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(Inner Mongolia Agricultural University,Hohhot Inner Mongolia 010019)

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    摘要:

    氨氧化微生物[氨氧化古菌(AOA)和氨氧化细菌(AOB)]是土壤硝化作用的重要参与者。探讨驱动日光温室黄瓜根系土壤氮循环的关键氨氧化微生物及其主要影响因子,明确关键氨氧化微生物在黄瓜根系的具体分布,为后续富集关键氨氧化微生物提供研究基础。本试验利用高通量测序的方法,探究施氮处理下土壤因子与黄瓜根系不同位置土壤中AOA、AOB 多样性和群落结构的相关性。结果表明,从多样性角度看,黄瓜根际和非根际土壤中的关键氨氧化微生物均为AOB。在黄瓜根际土壤中,AOB 丰富度和多样性的主要影响因子是pH,AOA 和AOB 群落组成差异性的主要诱因是NO3--N 积累;在黄瓜非根际土壤中,AOB 丰富度和多样性及群落组成改变的主要影响因子是NH4+-N。从群落结构角度看,黄瓜根际土壤中的关键氨氧化微生物为AOA 的奇古菌门(Thaumarchaeota)和亚硝化球菌属(Nitrosophaera)及AOB 的亚硝化螺菌属(Nitrosospira),黄瓜非根际土壤中的关键氨氧化微生物为AOB 的亚硝化螺菌属。在黄瓜根际土壤中,AOA 奇古菌门和亚硝化球菌属的主要影响因素为NH4+-N 浓度降低,AOB 亚硝化螺菌属的主要影响因素为NO3N 浓度增加;在黄瓜非根际土壤中,AOB亚硝化螺菌属的主要影响因素为NH4+-N 积累。综上,AOA 和AOB 共同主导黄瓜根际土壤中的氨氧化作用,其主要影响因子为pH、NH4+-N 和NO3--N;同时AOB 又主导黄瓜非根际土壤中的氨氧化作用,其主要影响因子为NH4+-N。

    Abstract:

    Ammonia-oxidizing microorganisms[ammonia-oxidizing archaea(AOA)and ammonia-oxidizing bacteria(AOB)]are important players in soil nitrification. In this study,the key microorganisms driving soil nitrogen cycling and their main influencing factors in solar greenhouse cucumber were investigated,and the specific distribution of dominant ammoniaoxidizing microorganisms in the root system of cucumber was clarified,in order to provide a research basis for enriching the dominant ammonia-oxidizing microorganisms. In this experiment,high-throughput sequencing was utilized to investigated the correlation between environmental factors and the diversity and community structure of AOA and AOB in the soil of cucumber root system under nitrogen treatment. The results showed that the key ammonia-oxidizing microorganisms were AOB both in cucumber rhizosphere and non-rhizosphere soils from the perspective of diversity. In cucumber rhizosphere soil,the main influencing factor for the abundance and diversity of AOB was pH,and the main inducer for the difference in the community composition of AOA and AOB was the accumulation of NO3--N,and in cucumber non-rhizosphere soil,the main influencing factor for the abundance and diversity of AOB and the change in the community composition of AOB was NH4+-N. From the perspective of community structure,the key ammonia-oxidizing microorganisms in the cucumber rhizosphere soil were Thaumarchaeota and Nitrosophaera of AOA and Nitrosospira of AOB,and the key ammonia-oxidizing microorganisms in the cucumber non-rhizosphere soil were Nitrosospira of AOB. In cucumber rhizosphere soil,the main influencing factor for Thaumarchaeota and Nitrosophaera of AOA was a decrease in NH4+-N concentration,and that for Nitrosospira of AOB was an increase in NO3--N concentration; in cucumber non-rhizosphere soil,the main influencing factor for Nitrosospira of AOB was the accumulation of NH4+-N. In summary,AOA and AOB jointly dominated ammonia oxidation in cucumber rhizosphere soil,with the main influencing factors being pH,NH4+-N and NO3--N. Meanwhile,AOB dominated ammonia oxidation in cucumber non-rhizosphere soil,with the main influencing factors being NH4+-N.

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张迎,王艳霞,王嘉,宋阳,孙婧,李晓静.日光温室黄瓜根际与非根际土壤氨氧化微生物对施氮的 响应及其影响因子研究[J].中国土壤与肥料123,2026,(6):54-67

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  • 收稿日期:2025-07-23
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  • 录用日期:2025-12-29
  • 在线发布日期: 2026-08-18
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