Qu Xian, He Pin-Jing, Mazéas Laurent, Bouchez Théodore
State Key Laboratory of Pollution Control and Resource Reuse, Key laboratory of Yangtze River Water Environment, College of Environmental Science and Engineering, Tongji University, Shanghai 200092, China.
Huan Jing Ke Xue. 2008 Nov;29(11):3252-7.
The methanogenic pathway during anaerobic digestion of household waste was investigated by stable carbon isotopic signature analysis, and testified by the analysis of gas production, leachate characteristics and microbial fluorescence in situ hybridization (FISH) methods. Furthemore, the difference of methanogenic pathway between mesophilic and thermophilic anaerobic digestion was also discussed. Results showed that under mesophilic conditions, the isotopic stable carbon signature of CH4 (delta13 CH4) initially decreased to -69.5 per thousand, indicating that CH4 was produced from CO2 and H2 by hydrogenotrophic methanogens. When active CH4 production phase started, the delta13 CH4 values quickly increased to -23.8 per thousand, which indicated more and more CH4 were formed by aceticlastic methanogens, dominantly the family of Methanosarcinaceae, shown by the FISH results. The delta13 CH4 values decreased successively and ultimately remained at -55 per thousand, indicating that the fraction of aceticlastic methanogenesis finally decreased to a steady level comparative with CO2-derived methanogenesis at the steady slow methane production phase. Under thermophilic conditions, the delta13 CH4 values remained at a level about -70 per thousand, showing that methane were solely produced from CO2 reduction, and acetate syntrophic oxidation happened during the active methane production phase.
通过稳定碳同位素特征分析研究了生活垃圾厌氧消化过程中的产甲烷途径,并通过产气分析、渗滤液特性分析和微生物荧光原位杂交(FISH)方法进行了验证。此外,还讨论了中温厌氧消化和高温厌氧消化产甲烷途径的差异。结果表明,在中温条件下,CH4的同位素稳定碳特征(δ13CH4)最初降至-69.5‰,表明CH4是由氢营养型产甲烷菌利用CO2和H2产生的。当活跃的CH4产生阶段开始时,δ13CH4值迅速升至-23.8‰,这表明越来越多的CH4是由乙酸裂解产甲烷菌形成的,主要是甲烷八叠球菌科,FISH结果显示了这一点。δ13CH4值相继下降,最终保持在-55‰,表明在稳定的缓慢甲烷产生阶段,乙酸裂解产甲烷的比例最终降至与CO2衍生产甲烷相当的稳定水平。在高温条件下,δ13CH4值保持在约-70‰的水平,表明甲烷仅由CO2还原产生,并且在活跃的甲烷产生阶段发生了乙酸共生氧化。