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土壤中提取的细菌产生一氧化氮、一氧化二氮和氮气及其受亚硝酸根离子和氧气浓度的调节作用

Production of NO, N2O and N2 by extracted soil bacteria, regulation by NO2(-) and O2 concentrations.

作者信息

Morley Nicholas, Baggs Elizabeth M, Dörsch Peter, Bakken Lars

机构信息

School of Biological Sciences, Plant and Soil Science, University of Aberdeen, Aberdeen, UK.

出版信息

FEMS Microbiol Ecol. 2008 Jul;65(1):102-12. doi: 10.1111/j.1574-6941.2008.00495.x. Epub 2008 May 6.

Abstract

The oxygen control of denitrification and its emission of NO/N2O/N2 was investigated by incubation of Nycodenz-extracted soil bacteria in an incubation robot which monitors O2, NO, N2O and N2 concentrations (in He+O2 atmosphere). Two consecutive incubations were undertaken to determine (1) the regulation of denitrification by O2 and NO2(-) during respiratory O2 depletion and (2) the effects of re-exposure to O2 of cultures with fully expressed denitrification proteome. Early denitrification was only detected (as NO and N2O) at <or=80 microM O2 in treatments with NO2(-), and the rates were three orders of magnitude lower than the rates observed after oxygen depletion (with N2 as the primary product). When re-exposed to O2, the cultures continued to denitrify (8-55% of the rates during the foregoing anoxic phase), but its main product was N2O. The N2O reductase activity recovered as oxygen was being depleted. The results suggest that expression of the denitrifying proteome may result in significant subsequent aerobic denitrification, and this has profound implications for the understanding and modelling of denitrification and N2O emission. Short anoxic spells caused by transient flooding during rainfall, could lead to subsequent unbalanced aerobic denitrification, in which N2O is a major end product.

摘要

通过在一个监测氧气、一氧化氮、氧化亚氮和氮气浓度(在氦气 + 氧气气氛中)的培养机器人中对 Nycodenz 提取的土壤细菌进行培养,研究了反硝化作用的氧气控制及其一氧化氮/氧化亚氮/氮气的排放。进行了连续两次培养,以确定(1)在呼吸性氧气消耗期间氧气和亚硝酸根对反硝化作用的调节,以及(2)对具有完全表达的反硝化蛋白质组的培养物重新暴露于氧气的影响。在有亚硝酸根的处理中,仅在氧气浓度≤80 微摩尔时检测到早期反硝化作用(以一氧化氮和氧化亚氮形式),其速率比氧气耗尽后观察到的速率(以氮气为主要产物)低三个数量级。当重新暴露于氧气时,培养物继续进行反硝化作用(为前述缺氧阶段速率的 8 - 55%),但其主要产物是氧化亚氮。随着氧气耗尽,氧化亚氮还原酶活性恢复。结果表明,反硝化蛋白质组的表达可能导致随后显著的好氧反硝化作用,这对理解和模拟反硝化作用及氧化亚氮排放具有深远意义。降雨期间短暂洪水引起的短暂缺氧期,可能导致随后不平衡的好氧反硝化作用,其中氧化亚氮是主要终产物。

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