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Responses of ammonia-oxidizing archaeal and betaproteobacterial populations to wastewater salinity in a full-scale municipal wastewater treatment plant

机译:大型市政污水处理厂中氨氧化古细菌和β变形细菌种群对废水盐度的响应

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The diversity and abundance of ammonia-oxidizing Betaproteobacteria and archaea were investigated in a full-scale municipal wastewater treatment plant where the wastewater conductivity level varied considerably (due to seawater salinity intrusion) during this study between 2004 and 2007. Based on the quantitative polymerase chain reaction of ammonia monooxygenase subunit A (amoA) genes, an increase in the ammonia oxidizing bacteria amoA gene copies occurred with a decrease in the wastewater salinity level. A corresponding decrease in the average ammonia-oxidizing archaea to bacteria ratio, from 1.22 (2004 and 2005), 0.17 (2006), and then to 0.07 (2007), was observed. Phylogenetic analyses on amoA gene sequences indicated that Nitrosomonas marina-like ammonia oxidizing bacteria and Thaumarcheota i.la (marina group) ammonia-oxidizing archaea were dominant when the wastewater salinity level fluctuated at high values with an average of 4.83 practical salinity unit (psu), while Nitrosomonas urea-like ammonia oxidizing bacteria and Thaumarcheota 1.1b (soil group) ammonia-oxidizing archaea became dominant when the wastewater salinity decreased to a more stable lower level with an average of 1.93 psu. Based on the amoA gene-based terminal restriction fragment length polymorphism analyses, results from this study demonstrated that the observed shift in ammonia oxidizing bacteria and archaea populations is likely caused by a change of the wastewater salinity level.
机译:在2004年至2007年的这项研究中,对一家大型市政污水处理厂进行了氨氧化贝塔氏杆菌和古细菌的多样性和丰度研究,该厂的废水电导率水平变化很大(由于海水盐度的入侵)。基于定量聚合酶链氨单加氧酶亚基A(amoA)基因发生反应后,氨氧化细菌amoA基因拷贝增加,而废水盐度水平降低。观察到平均氨氧化古细菌与细菌的比率相应降低,从1.22(2004和2005),0.17(2006),然后降至0.07(2007)。对amoA基因序列的系统进化分析表明,当废水盐度水平高波动且平均为4.83实用盐度单位(psu)时,亚硝基亚滨亚硝基甲烷(Nitrosomonas marina)类氨氧化细菌和Thaumarcheota i.la(marina组)氨氧化古细菌占主导地位。当废水的盐度降低到更稳定的较低水平,平均为1.93 psu时,亚硝基亚脲类尿素类氨氧化细菌和Thaumarcheota 1.1b(土壤类)氨氧化古菌占主导地位。基于基于amoA基因的末端限制性片段长度多态性分析,这项研究的结果表明,观察到的氨氧化细菌和古细菌种群的变化很可能是由废水盐度水平的变化引起的。

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