Zhang Xuan, Kong Jiao-Yan, Xia Fang-Fang, Su Yao, He Ruo
Department of Environmental Engineering, Zhejiang University, Hangzhou 310058, China.
Department of Environmental Engineering, Zhejiang University, Hangzhou 310058, China.
Syst Appl Microbiol. 2014 Jun;37(4):296-304. doi: 10.1016/j.syapm.2014.03.003. Epub 2014 May 1.
The influence of NH4(+) on microbial CH4 oxidation is still poorly understood in landfill cover soils. In this study, effects of NH4(+) addition on the activity and community structure of methanotrophs were investigated in waste biocover soil (WBS) treated by a series of NH4(+)-N contents (0, 100, 300, 600 and 1200mgkg(-1)). The results showed that the addition of NH4(+)-N ranging from 100 to 300mgkg(-1) could stimulate CH4 oxidation in the WBS samples at the first stage of activity, while the addition of an NH4(+)-N content of 600mgkg(-1) had an inhibitory effect on CH4 oxidation in the first 4 days. The decrease of CH4 oxidation rate observed in the last stage of activity could be caused by nitrogen limitation and/or exopolymeric substance accumulation. Type I methanotrophs Methylocaldum and Methylobacter, and type II methanotrophs (Methylocystis and Methylosinus) were abundant in the WBS samples. Of these, Methylocaldum was the main methanotroph in the original WBS. With incubation, a higher abundance of Methylobacter was observed in the treatments with NH4(+)-N contents greater than 300mgkg(-1), which suggested that NH4(+)-N addition might lead to the dominance of Methylobacter in the WBS samples. Compared to type I methanotrophs, the abundance of type II methanotrophs Methylocystis and/or Methylosinus was lower in the original WBS sample. An increase in the abundance of Methylocystis and/or Methylosinus occurred in the last stage of activity, and was likely due to a nitrogen limitation condition. Redundancy analysis showed that NH4(+)-N and the C/N ratio had a significant influence on the methanotrophic community in the WBS sample.
在垃圾填埋场覆盖土壤中,铵离子(NH4(+))对微生物甲烷氧化的影响仍知之甚少。在本研究中,通过一系列铵态氮含量(0、100、300、600和1200mgkg(-1))处理的废弃生物覆盖土壤(WBS),研究了添加铵离子对甲烷氧化菌活性和群落结构的影响。结果表明,在活性第一阶段,添加100至300mgkg(-1)的铵态氮可刺激WBS样品中的甲烷氧化,而添加600mgkg(-1)的铵态氮含量在最初4天对甲烷氧化有抑制作用。在活性最后阶段观察到的甲烷氧化率下降可能是由氮限制和/或胞外聚合物积累引起的。I型甲烷氧化菌甲基暖菌属(Methylocaldum)和甲基杆菌属(Methylobacter)以及II型甲烷氧化菌(甲基孢囊菌属(Methylocystis)和甲基弯曲菌属(Methylosinus))在WBS样品中含量丰富。其中,甲基暖菌属是原始WBS中的主要甲烷氧化菌。随着培养,在铵态氮含量大于300mgkg(-1)的处理中观察到甲基杆菌属丰度更高,这表明添加铵态氮可能导致甲基杆菌属在WBS样品中占主导地位。与I型甲烷氧化菌相比,原始WBS样品中II型甲烷氧化菌甲基孢囊菌属和/或甲基弯曲菌属的丰度较低。在活性最后阶段,甲基孢囊菌属和/或甲基弯曲菌属的丰度增加,这可能是由于氮限制条件所致。冗余分析表明,铵态氮和碳氮比对WBS样品中的甲烷氧化菌群落有显著影响。