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高起点磷施肥通过促进农田土壤中微生物功能互作对土壤磷转化的影响。

High starter phosphorus fertilization facilitates soil phosphorus turnover by promoting microbial functional interaction in an arable soil.

机构信息

Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; University of the Chinese Academy of Sciences, Beijing 100049, China.

Key Laboratory of Subtropical Soil Science and Plant Nutrition of Zhejiang Province, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China.

出版信息

J Environ Sci (China). 2020 Aug;94:179-185. doi: 10.1016/j.jes.2020.03.040. Epub 2020 May 4.

DOI:10.1016/j.jes.2020.03.040
PMID:32563482
Abstract

Microbial phosphorus (P) turnover is critical in C utilization efficiency in agroecosystems. It is therefore necessary to understand the P mobilization processes occurring during P fertilization in order to ensure both crop yield and environmental quality. Here, we established a controlled pot experiment containing soil amended with three different levels of starter P fertilizer and collected soil samples after 30, 60, and 90 days of incubation. Quantitative microbial element cycling (QMEC) smart chip technology and 16S rRNA gene sequencing were used to investigate functional gene structures involved in carbon, nitrogen and P cycling and the bacterial community composition of the collected samples. Although P fertilization did not significantly affect the structure of the soil microbial community, some rare microbiota were changed in particular phosphorus-solubilizing bacteria were enriched at the high P fertilization level, suggesting that the rare taxa make an important contribution to P turnover. P fertilization also altered the functional gene structure, and high P concentrations enhanced the functional gene diversity and abundance. Partial redundancy analysis further revealed that changes in rare taxa and functional genes of soil microorganisms drive the alteration of soil P pools. These findings extend our understanding of the microbial mechanisms of P turnover.

摘要

微生物磷(P)转化对于农业生态系统中 C 利用效率至关重要。因此,有必要了解 P 施肥过程中发生的 P 动员过程,以确保作物产量和环境质量。在这里,我们建立了一个含有三种不同水平起始 P 肥料的控制盆式实验,并在培养 30、60 和 90 天后收集土壤样本。采用定量微生物元素循环(QMEC)智能芯片技术和 16S rRNA 基因测序技术,研究了参与碳、氮和 P 循环的功能基因结构以及收集样本的细菌群落组成。虽然 P 施肥并没有显著影响土壤微生物群落的结构,但一些稀有微生物群在特定磷溶解细菌在高 P 施肥水平下富集,这表明稀有分类群对 P 转化有重要贡献。P 施肥还改变了功能基因结构,高 P 浓度增强了功能基因的多样性和丰度。偏冗余分析进一步表明,土壤微生物中稀有分类群和功能基因的变化驱动了土壤 P 库的变化。这些发现扩展了我们对 P 转化微生物机制的理解。

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