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连续四年施用生物炭对农业酸性和碱性土壤氨氧化微生物种群和群落结构的影响。

Population and community structure shifts of ammonia oxidizers after four-year successive biochar application to agricultural acidic and alkaline soils.

机构信息

State Key Laboratory of Soil and Sustainable Agriculture, Changshu National Agro-Ecosystem Observation and Research Station, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China; Institute of Environment, Resource, Soil and Fertilizer, Zhejiang Academy of Agricultural Sciences, 198 Shiqiao Road, Hangzhou 310021, China.

State Key Laboratory of Soil and Sustainable Agriculture, Changshu National Agro-Ecosystem Observation and Research Station, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.

出版信息

Sci Total Environ. 2018 Apr 1;619-620:1105-1115. doi: 10.1016/j.scitotenv.2017.11.029. Epub 2017 Nov 29.

Abstract

Long-term studies that advance our mechanistic understanding of biochar (BC)‑nitrogen (N) interactions in agricultural soils are lacking. In this study, soil potential nitrification rates (PNR), the abundance and composition of ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) communities following 4-year of BC application were investigated using the shaken-slurry procedure and molecular sequencing techniques for an acidic Oxisol (QU) and an alkaline Cambisol (YU). Soils were obtained from an outdoor soil column experiment with straw-BC application rates of 0 (BC0), 2.25 (BC2.25) and 11.3 (BC11.3) Mgha per cropping season for eight consecutive wheat/millet seasons. Quantitative polymerase chain reaction (qPCR) and 454 high-throughput pyrosequencing techniques were performed to quantify and sequence amoA gene copies and composition of AOA and AOB. Results showed that QU had lower PNR and a higher ratio of amoA gene copies of AOA to AOB than YU, PNR of QU with BC application was significantly associated with the amoA gene of AOB. Similar to previous short-term findings, BC application enhanced QU soil nitrification, which may be explained by the significant increase in AOB abundance and a shift in AOB community structure from Nitrosospira cluster 2 toward cluster 3, along with the disappearance of some obligate acidophile AOA groups, leading to the appearance of ammonia-oxidizers from neutral-alkaline soils in BC-amended acid soils. Canonical correspondence analysis (CCA) showed that soil pH was the most important factor driving shifts in ammonia-oxidizers composition. Although BC application did not have significant effects on PNR in YU, BC11.3 decreased AOA and AOB gene copies and influenced the relative abundance of community structure. Our findings represent the first investigation of long-term BC effects on AOA and AOB communities in agricultural soils using 454 high-throughput pyrosequencing, showing that BC application can alter soil characteristics and influence ammonia oxidizer community composition, abundance, especially in acid soils.

摘要

长期研究推进了我们对生物炭(BC)-氮(N)在农业土壤中相互作用的机理理解,但仍有所欠缺。本研究采用摇瓶法和分子测序技术,调查了经过 4 年 BC 施用后土壤潜在硝化速率(PNR)、氨氧化古菌(AOA)和氨氧化细菌(AOB)群落的丰度和组成。供试土壤取自一个室外土柱实验,在连续 8 个小麦/谷子轮作季中,秸秆-BC 施用量分别为 0(BC0)、2.25(BC2.25)和 11.3(BC11.3)Mg ha-1。进行了定量聚合酶链反应(qPCR)和 454 高通量焦磷酸测序技术,以定量和测序 amoA 基因拷贝和 AOA 和 AOB 的组成。结果表明,QU 的 PNR 较低,AOA 的 amoA 基因拷贝与 AOB 的比值高于 YU,BC 处理后 QU 的 PNR 与 AOB 的 amoA 基因显著相关。与之前的短期研究结果相似,BC 处理增强了 QU 土壤硝化作用,这可能是由于 AOB 丰度的显著增加和 AOB 群落结构从硝化螺旋菌属 2 群向 3 群的转变,同时一些专性嗜酸 AOA 类群消失,导致在添加 BC 的酸性土壤中出现了来自中性-碱性土壤的氨氧化菌。典范对应分析(CCA)表明,土壤 pH 是驱动氨氧化菌组成变化的最重要因素。尽管 BC 处理对 YU 的 PNR 没有显著影响,但 BC11.3 降低了 AOA 和 AOB 的基因拷贝数,并影响了群落结构的相对丰度。本研究首次采用 454 高通量焦磷酸测序技术调查了长期 BC 处理对农业土壤中 AOA 和 AOB 群落的影响,结果表明,BC 处理可以改变土壤特性并影响氨氧化菌群落组成和丰度,尤其是在酸性土壤中。

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