首页> 外文期刊>applied and environmental microbiology >Use of Molecular and Isotopic Techniques To Monitor the Response of Autotrophic Ammonia-Oxidizing Populations of the β Subdivision of the Class Proteobacteria in Arable Soils to Nitrogen Fertilizer
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Use of Molecular and Isotopic Techniques To Monitor the Response of Autotrophic Ammonia-Oxidizing Populations of the β Subdivision of the Class Proteobacteria in Arable Soils to Nitrogen Fertilizer

机译:利用分子和同位素技术监测耕地土壤中变形菌类β自养氨氧化种群对氮肥的响应

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摘要

This study examined the effects of NH4NO3fertilizer on the size and activity of nitrifying, autotrophic, ammonia-oxidizing populations of the β subdivision of the classProteobacteria in arable soils. Plots under different long-term fertilizer regimes were sampled before and after NH4NO3 additions, and the rates of nitrification were determined by 15N isotopic pool dilution assays. Ammonia-oxidizing populations in the plots were quantified by competitive PCR assays based on the amoA and ribosomal 16S genes. Prior to fertilizer addition, ammonium concentrations and nitrification rates in the plots were comparatively low; ammonia-oxidizing populations were present at 104 to 105 gene copies g of soil−1. Three days after the application of fertilizer, nitrification rates had risen considerably but the size of the ammonia-oxidizing population was unchanged. Six weeks after fertilizer treatment, ammonium concentrations and nitrification rates had fallen while the ammonia-oxidizing populations in plots receiving fertilizer had increased. The rapidity of the rise in nitrification rates observed after 3 days suggests that it results from phenotypic changes in the ammonia-oxidizing bacterial population. Associated increases in population sizes were only observed after 6 weeks and did not correlate directly with nitrifying activity. Phylogenetic analyses of PCR products from one of the plots revealed a population dominated byNitrosospira-type organisms, similar to those prevalent in other soils.
机译:本研究考察了NH4NO3肥料对耕地中变形菌门β细分的硝化、自养、氨氧化种群的大小和活性的影响。对添加NH4NO3前后不同长期施肥状态下的样地进行采样,采用15N同位素库稀释法测定硝化速率。通过基于amoA和核糖体16S基因的竞争性PCR测定,对样地中的氨氧化群体进行定量。在添加肥料之前,地块中的铵浓度和硝化速率相对较低;氨氧化种群存在于土壤的104-105个基因拷贝g-1处。施肥三天后,硝化率大幅上升,但氨氧化种群的规模没有变化。施肥处理六周后,铵浓度和硝化速率下降,而施肥地块的氨氧化种群增加。3天后观察到的硝化速率上升的迅速表明,这是氨氧化细菌种群表型变化的结果。仅在 6 周后观察到种群规模的相关增加,并且与硝化活性没有直接关系。对其中一个地块的PCR产物的系统发育分析显示,该种群以亚硝基螺旋体型生物为主,与其他土壤中普遍存在的生物相似。

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