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Unraveling the active microbial populations involved in nitrogen utilization in a vertical subsurface flow constructed wetland treating urban wastewater

机译:在垂直地下流动建造的湿地处理城市废水中揭示施氮中涉及氮利用的活性微生物群

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摘要

The dynamics of the active microbial populations involved in nitrogen transformation in a vertical subsurface flow constructed wetland (VF) treating urban wastewater was assessed. The wetland (1.5 m2) operated under average loads of 130 g COD m- 2 d- 1 and 17 g TN m- 2 d- 1 in Period I, and 80 g COD m- 2 d- 1 and 19 g TN m- 2 d- 1 in Period II. The hydraulic loading rate (HLR) was 375 mm d- 1 and C/N ratio was 2 in both periods. Samples for microbial characterization were collected from the filter medium (top and bottom layers) of the wetland, water influent and effluent at the end of Periods I (Jun–Oct) and II (Nov–Jan). The combination of qPCR and high-throughput sequencing (NGS, MiSeq) assessment at DNA and RNA level of 16S rRNA genes and nitrogen-based functional genes (amoA and nosZ-clade I) revealed that nitrification was associated both with ammonia-oxidizing bacteria (AOB) (Nitrosospira) and ammonia-oxidizing archaea (AOA) (Nitrososphaeraceae), and nitrite-oxidizing bacteria (NOB) such as Nitrobacter. Considering the active abundance (based in amoA transcripts), the AOA population revealed to be more stable than AOB in both periods and depths of the wetland, being less affected by the organic loading rate (OLR). Although denitrifying bacteria (nosZ copies and transcripts) were actively detected in all depths, the denitrification process was low (removal of 2 g TN m- 2 d- 1 for both periods) concomitant with NOx-N accumulation in the effluent. Overall, AOA, AOB and denitrifying bacteria (nosZ) were observed to be more active in bottom than in top layer at lower OLR (Period II). A proper design of OLR and HLR seems to be crucial to control the activity of microbial biofilms in VF wetlands on the basis of oxygen, organic-carbon and NOx-N forms, to improve their capacity for total nitrogen removal.
机译:评估了治疗城市废水的垂直地下流动构建的湿地(VF)中涉及氮转化的活性微生物种群的动态。湿地(1.5平方米)在10g COD m-2 d-1和17g tn m-2 d-1的平均载荷下操作,80g COD m-2 d-1和19 g tn m- 2 D-1期间II。液压加载速率(HLR)为375mm D-1,C / N比在两个时段中为2。从湿地的过滤介质(顶层和底层)收集用于湿地的过滤介质(顶层和底层)的样品,在I(JUN-OCT)和II(11月至1月)中,水流入和流出物。 DNA的QPCR和高通量测序(NGS,MISEQ)评估的组合和16S rRNA基因的RNA水平和氮基官能基因(AmoA和NoSz-Clade I)显示硝化与氨氧化细菌( AOB)(Nitrosospira)和氨氧化古痤疮(AOA)(硝基鏻)和亚硝酸盐氧化细菌(NOB),如硝基杆菌。考虑到活性丰度(基于AMOA转录物),AOA群体显示出比湿地的周期和深度在湿地的时间更稳定,受到有机加载速率(OLR)的影响。虽然在所有深度中主动检测到亚硝基细菌(鼻子拷贝和转录物),但脱硝处理较低(除去2g Tn m-2 d-1,两个时段)伴随到流出物中的NOx-n积累。总而言之,观察到AOA,AOB和反硝化细菌(NOSZ)底部比下层在较低OLR的顶层中更活跃(时期II)。在氧气,有机碳和NOx-N形式控制VF湿地中微生物生物膜的活性至关重要,似乎是至关重要的,以提高它们的总氮去除能力。

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