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高固体厌氧消化器中脱水污泥条件下微生物群落对氨氮胁迫的代谢适应

Metabolic adaptation of microbial communities to ammonium stress in a high solid anaerobic digester with dewatered sludge.

机构信息

State Key Laboratory of Pollution Control and Resource Reuse, College of Environmental Science and Engineering, Tongji University, 1239 Siping Road, Shanghai 200092, PR China.

出版信息

Sci Rep. 2016 Jun 17;6:28193. doi: 10.1038/srep28193.

Abstract

A high solid digester with dewatered sludge was operated for 110 days to ascertain the interactions between bacterial and archaeal communities under ammonium stress, as well as the corresponding changes in bio-degradation mechanisms. The volatile solids reduction (95% confidence intervals in mean) changed from 31.6 ± 0.9% in the stable period (day 40-55) to 21.3 ± 1.5% in the last period (day 71-110) when ammonium concentration was elevated to be within 5,000-6,000 mgN/L. Biogas yield dropped accordingly from 11.9 ± 0.3 to 10.4 ± 0.2 L/d and carbon dioxide increased simultaneously from 35.2% to 44.8%. Anaerobranca better adapted to the ammonium stress, while the initially dominant protein-degrading microbes-Tepidimicrobium and Proteiniborus were suppressed, probably responsible for the increase of protein content in digestate. Meanwhile, Methanosarcina, as the dominant Archaea, was resistant to ammonium stress with the constant relative abundance of more than 92% during the whole operation. Nonmetric Multidimensional Scaling (NMDS) analysis was thus conducted which indicated that the gradually increased TAN dictated the bacterial clusters. The dominant Methanosarcina and the increased carbon dioxide content under ammonium stress suggested that, rather than the commonly acknowledged syntrophic acetate oxidation (SAO) with hydrogenotrophic methanogenesis, only SAO pathway was enhanced during the initial 'ammonium inhibition'.

摘要

采用高固体消化器对脱水污泥进行了 110 天的运行,以确定在铵胁迫下细菌和古菌群落的相互作用,以及生物降解机制的相应变化。挥发性固体减少率(平均值的 95%置信区间)从稳定期(第 40-55 天)的 31.6±0.9%变为最后一期(第 71-110 天)的 21.3±1.5%,此时铵浓度升高至 5000-6000mgN/L。沼气产量相应从 11.9±0.3L/d 下降到 10.4±0.2L/d,同时二氧化碳从 35.2%增加到 44.8%。Anaerobranca 更能适应铵胁迫,而最初占主导地位的蛋白降解微生物-Tepidimicrobium 和 Proteiniborus 受到抑制,这可能是消化物中蛋白含量增加的原因。同时,Methanosarcina 作为主要的古菌,对铵胁迫具有抗性,整个运行过程中相对丰度始终保持在 92%以上。非度量多维尺度分析(NMDS)表明,逐渐增加的 TAN 决定了细菌聚类。优势的 Methanosarcina 和铵胁迫下二氧化碳含量的增加表明,在最初的“铵抑制”阶段,只有 SAO 途径得到了增强,而不是通常认为的产乙酸菌氧化(SAO)与氢营养型甲烷生成。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8650/4911566/cc79f987a56d/srep28193-f1.jpg

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