首页|氨氧化微生物对硝化潜势和N2O生成的贡献

氨氧化微生物对硝化潜势和N2O生成的贡献

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采用逆转录实时荧光定量PCR技术,分析了春季东海表层沉积物中氨氧化微生物amoA基因表达水平的空间分布特征;并通过培养实验,探究了沉积物中活性氨氧化细菌(ammonia-oxidizing bacteria,AOB)及氨氧化古菌(ammonia-oxidizing archaea,AOA)对硝化潜势和N2O生成的相对贡献。结果显示,表层沉积物中AOA amoA基因表达水平(4。49×102~2。17×106copies/g)显著高于AOB(6。60×101~7。65×105copies/g),二者的amoA基因表达水平均表现出近岸低(AOA:8。92×105copies/g;AOB:2。06×103copies/g)、远岸高(AOA:1。05× 106copies/g;AOB:4。06×104copies/g)的空间分布特征;近岸沉积物的硝化潜势高于远岸;从近岸到远岸,硝化过程由AOA主导逐渐转变为AOB主导。在N2O生成过程中,NH4+的添加能显著促进N2O的生成;相对于AOA,AOB在N2O生成过程中发挥着更加重要的作用。
Contribution of ammonia-oxidizing microorganisms to nitrification potential and N2O production
This study utilized reverse transcription quantitative real-time PCR to investigate the spatial distribution of amoA gene expression levels among ammonia-oxidizing microorganisms in the surface sediments of the East China Sea during spring.Cultivation experiments were performed to assess the relative contributions of ammonia-oxidizing bacteria(AOB)and ammonia-oxidizing archaea(AOA)to the nitrification potential and N2O production in the surface sediments.The results revealed that the expression level of AOA amoA gene was significantly higher than that of AOB(AOA:4.49× 102~2.17×106copies/g;AOB:6.60×101~7.65×105copies/g),with both showing a spatial distribution pattern of lower levels in nearshore areas(AOA:8.92×105copies/g;AOB:2.06×103copies/g)and higher in offshore areas(AOA:1.05×106copies/g;AOB:4.06×104copies/g).Nitrification potential was found to be higher in nearshore sediments than in offshore sediments,with the nitrification process gradually shifting from AOA dominance in nearshore areas to AOB dominance in offshore areas.In the N2O production process,the addition of NH4+significantly enhanced N2O production,with AOB playing a more critical role than AOA in this process.

East China Seasedimentammonia-oxidizing microorganismspotential nitrification rateN2O

王大玲、杨雨虹、贺惠、米铁柱、甄毓

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中国海洋大学环境科学与工程学院,海洋环境与生态教育部重点实验室,山东青岛 266100

青岛海洋科技中心,海洋生态与环境科学功能实验室,山东青岛 266071

中国海洋大学海洋生命学院,山东青岛 266003

中国海洋大学深海圈层与地球系统前沿科学中心,山东青岛 266100

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东海 沉积物 氨氧化微生物 潜在硝化速率 N2O

2024

中国环境科学
中国环境科学学会

中国环境科学

CSTPCDCHSSCD北大核心
影响因子:2.174
ISSN:1000-6923
年,卷(期):2024.44(12)