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首页> 外文期刊>Journal of applied microbiology >Denitrification by indigenous microbial populations of river water measured using membrane inlet mass spectrometry
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Denitrification by indigenous microbial populations of river water measured using membrane inlet mass spectrometry

机译:使用膜入口质谱仪测量的河水中土著微生物种群的反硝化作用

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摘要

The major process that reduces nitrate levels in soils and water is denitrification, which converts nitrate and nitrite into gaseous forms of nitrogen, which are then released into the atmosphere. This study used membrane inlet mass spectrometry (MIMS) to investigate denitrification in river water bacterial isolates supplied with nitrate and succinate as an energy source as well as in the total population by provision of different carbon compounds to untreated river water samples. substantial variation was observed in the gases detected with nitrogen, nitrous oxide and nitric oxide all being produced by one or more of the isolates. The indigenous river population as a whole was found to respond very differently to the addition of different carbon sources. Peak nitrogen levels differed by nearly 1 mmol l~(-1) and nitrous oxide by approximately 0.5mmol l~(-1) depending on which carbon source was supplied. Nitric oxide was only detected when glycerol was supplied as the carbon source. These results demonstrate the complex interactions involved in nitrogen cycling and suggest that with careful management it may be possible to stimulate particular consortia of micro-organisms to reduce more nitrate to harmless nitrogen rather than nitrous oxide, a known greenhouse gas.
机译:降低土壤和水中硝酸盐含量的主要过程是反硝化作用,这会将硝酸盐和亚硝酸盐转化为气态氮,然后释放到大气中。这项研究使用膜入口质谱(MIMS)来研究以硝酸盐和琥珀酸盐为能源的河水细菌分离物中的反硝化作用,以及通过向未经处理的河水样品中提供不同的碳化合物来研究总人口中的反硝化作用。在由一种或多种分离物产生的氮,一氧化二氮和一氧化氮检测到的气体中,观察到了明显的变化。整个土著河流人口对增加不同碳源的反应截然不同。取决于提供的碳源,峰值氮水平相差近1 mmol l〜(-1),一氧化二氮相差约0.5 mmol l〜(-1)。仅在以甘油作为碳源时才检测到一氧化氮。这些结果证明了氮循环中涉及的复杂相互作用,并表明通过精心管理,有可能刺激特定的微生物群落以将更多的硝酸盐还原为无害的氮,而不是已知的温室气体一氧化二氮。

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