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Methane Oxidation by Nitrosococcus oceanus and Nitrosomonas europaea

机译:海洋亚硝基球菌和欧洲亚硝基甲烷的甲烷氧化

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摘要

Chemolithotrophic ammonium-oxidizing and nitrite-oxidizing bacteria including Nitrosomonas europaea, Nitrosococcus oceanus, Nitrobacter sp., Nitiospina gracilis, and Nitrococcus mobilis were examined as to their ability to oxidize methane in the absence of ammonium or nitrite. All ammonium oxidizers tested had the ability to oxidize significant amounts of methane to CO2 and incorporate various amounts into cellular components. None of the nitrite-oxidizing bacteria were capable of methane oxidation. The methane-oxidizing capabilities of Nitrosococcus oceanus and Nitrosomonas europaea were examined with respect to ammonium and methane concentrations, nitrogen source, and pH. The addition of ammonium stimulated both CO2 production and cellular incorporation of methane-carbon by both organisms. Less than 0.1 mM CH4 in solution inhibited the oxidation of ammonium by Nitrosococcus oceanus by 87%. Methane concentrations up to 1.0 mM had no inhibitory effects on ammonium oxidation by Nitrosomonas europaea. In the absence of NH4-N, Nitrosococcus oceanus achieved a maximum methane oxidation rate of 2.20 × 10−2 μmol of CH4 h−1 mg (dry weight) of cells−1, which remained constant as the methane concentration was increased. In the presence of NH4-N (10 ppm [10 μg/ml]), its maximum rate was 26.4 × 10−2 μmol of CH4 h−1 mg (dry weight) of cells−1 at a methane concentration of 1.19 × 10−2 mM. Increasing the methane concentration above this level decreased CO2 production, whereas cellular incorporation of methane-carbon continued to increase. Nitrosomonas europaea showed a linear response throughout the test range, with an activity of 196.0 × 10−2 μmol of CH4 h−1 mg (dry weight) of cells −1 at a methane concentration of 1.38 × 10−1 mM. Both nitrite and nitrate stimulated the oxidation of methane. The pH range was similar to that for ammonium oxidation, but the points of maximum activity were at lower values for the oxidation of methane.
机译:在没有铵盐或亚硝酸盐的情况下,检查了化营养性铵氧化和亚硝酸盐氧化的细菌,包括欧洲硝化单胞菌,海洋硝化球菌,硝化细菌,细叶小球藻和运动型硝化球菌的甲烷氧化能力。测试的所有铵氧化剂均具有将大量甲烷氧化为CO2并将各种数量的氮氧化物掺入细胞成分的能力。亚硝酸盐氧化细菌均不能甲烷氧化。关于铵和甲烷浓度,氮源和pH值,检查了海洋亚球菌和欧洲亚硝基甲烷的甲烷氧化能力。铵的加入既刺激了二氧化碳的产生,又刺激了两种生物通过细胞吸收甲烷-碳。溶液中少于0.1 mM的CH4抑制了海洋硝基球菌对铵的氧化作用达87%。甲烷浓度最高为1.0 mM时,对欧洲亚硝化单胞菌的铵氧化没有抑制作用。在没有NH4-N的情况下,海洋硝基球菌的最大甲烷氧化速率为2.20×10 -2 μmolCH4 h -1 mg(干重)细胞< sup> -1 ,随着甲烷浓度的增加而保持恒定。在NH4-N(10 ppm [10μg/ ml])的存在下,其最大比率为26.4×10 -2 μmolCH4 h -1 mg(干燥甲烷浓度为1.19×10 -2 mM的细胞 -1 的重量。将甲烷浓度增加到该水平以上会降低CO2的产生,而细胞内甲烷-碳的掺入持续增加。欧洲硝化单胞菌在整个测试范围内均表现出线性响应,其活度为196.0×10 −2 μmolCH4 h -1 mg(干重)细胞甲烷浓度为1.38×10 -1 mM时为-1 。亚硝酸盐和硝酸盐都刺激甲烷的氧化。 pH范围类似于铵氧化的pH范围,但甲烷氧化的最大活性值较低。

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