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温度和高乙酸盐浓度对湖泊沉积物泥浆中甲烷生成的影响。

Influence of temperature and high acetate concentrations on methanogenesis in lake sediment slurries.

作者信息

Nozhevnikova Alla N, Nekrasova Valeria, Ammann Adrian, Zehnder Alexander J B, Wehrli Bernhard, Holliger Christof

机构信息

Institute of Microbiology Russian Academy of Sciences, Moscow, Russia.

出版信息

FEMS Microbiol Ecol. 2007 Dec;62(3):336-44. doi: 10.1111/j.1574-6941.2007.00389.x. Epub 2007 Oct 19.

Abstract

Methanogenesis from main methane precursors H(2)/CO(2) and acetate was investigated in a temperature range of 2-70 degrees C using sediments from Lake Baldegg, Switzerland. Psychrophilic, psychrotrophic, mesophilic, and thermophilic methanogenic microbial communities were enriched by incubations for 1-3 months of nonamended sediment slurries at 5, 15, 30, and 50 degrees C. Isotope experiments with slurries amended with (14)C-labeled bicarbonate and (14)C-2-acetate showed that in the psychrophilic community (enriched at 5 degrees C), about 95% of methane originated from acetate, in contrast to the thermophilic community (50 degrees C) where up to 98% of methane was formed from bicarbonate. In the mesophilic community (30 degrees C), acetate was the precursor of about 80% of the methane produced. When the hydrogen-carbon dioxide mixture (H(2)/CO(2)) was used as a substrate, it was directly converted to methane under thermophilic conditions (70 and 50 degrees C). Under mesophilic conditions (30 degrees C), both pathways, hydrogenotrophic and acetoclastic, were observed. At low temperatures (5 and 15 degrees C), H(2)/CO(2) was converted into methane by a two-step process; first acetate was formed, followed by methane production from acetate. When slurries were incubated at high partial pressures of H(2)/CO(2), the high concentrations of acetate produced of more than 20 mM inhibited acetoclastic methanogenesis at a temperature below 15 degrees C. However, slow adaptation of the psychrophilic microbial community to high acetate concentrations was observed.

摘要

利用瑞士Baldegg湖的沉积物,在2至70摄氏度的温度范围内研究了主要甲烷前体H₂/CO₂和乙酸盐的产甲烷过程。通过在5、15、30和50摄氏度下对未改良的沉积物浆液进行1至3个月的培养,富集了嗜冷、嗜温、中温和嗜热的产甲烷微生物群落。用¹⁴C标记的碳酸氢盐和¹⁴C-2-乙酸盐改良浆液的同位素实验表明,在嗜冷群落(在5摄氏度下富集)中,约95%的甲烷来自乙酸盐,而在嗜热群落(50摄氏度)中,高达98%的甲烷由碳酸氢盐形成。在中温群落(30摄氏度)中,乙酸盐是约80%产生的甲烷的前体。当使用氢气-二氧化碳混合物(H₂/CO₂)作为底物时,在嗜热条件下(70和50摄氏度)它直接转化为甲烷。在中温条件下(30摄氏度),观察到了氢营养型和乙酸裂解型两种途径。在低温(5和15摄氏度)下,H₂/CO₂通过两步过程转化为甲烷;首先形成乙酸盐,然后由乙酸盐产生甲烷。当浆液在高H₂/CO₂分压下培养时,产生的高浓度乙酸盐超过20 mM,在低于15摄氏度的温度下抑制了乙酸裂解型产甲烷过程。然而,观察到嗜冷微生物群落对高乙酸盐浓度的缓慢适应。

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