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Potential methane production and molecular characterization of bacterial and archaeal communities in a horizontal subsurface flow constructed wetland under cold and warm seasons

机译:寒冷和温暖季节下水平地下流动人工湿地中潜在的甲烷生产以及细菌和古细菌群落的分子特征

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Organic matter removal in a horizontal subsurface flow constructed wetland (HSSF) treating wastewater is associated with the presence of bacteria and archaea. These organisms perform anaerobic microbial processes such as methanogenesis, which can lead to methane emissions. The aim of this study was to evaluate methane production and characterize the bacterial and archaeal communities found in HSSFs treating secondary urban wastewater during cold and warm seasons. The pilot system used in this study corresponds to four HSSFs, two planted with Phragmites australis (HSSF-Phr) and two planted with Schoenoplectus californicus (HSSF-Sch), the monitoring was carried out for 1335 days. Removal efficiencies for organic matter (biological and chemical oxygen demand) and total and volatile suspended solids were evaluated in each HSSF. Moreover, biomass from each HSSF was sampled during warm and cold season, and methane productions determined by Specific Methanogenic Activity assays((maximum)) (SMA(m)). In the same samples, the quantification and identification of bacteria and archaea were performed. The results showed that the degradation of organic matter (53-67% BOD5 and 51-62% COD) and suspended solids (85-93%) was not influenced by seasonal conditions or plant species. Potential methane production from HSSF-Sch was between 20 and 51% higher than from HSSF-Phr. Moreover, potential methane production during warm season was 3.4-42% higher than during cold season. The quantification of microorganisms in HSSFs, determined greater development of bacteria (38%) and archaea (50-57%) during the warm season. In addition, the species Schoenoplectus californicus has a larger number of bacteria (4-48%) and archaea (34-43%) than Phragmites australis. The identification of microorganisms evidenced the sequences associated with bacteria belong mainly to Firmicutes (42%), Proteobacteria (33%) and Bacteroidetes (25%). The archaea were represented primarily by Methanosarcinales, specifically Methanosaeta (75%) and Methanosarcina (16%). The community structure of the methanogenic archaea in HSSFs did not change throughout the seasons or plant species. (C) 2018 Elsevier B.V. All rights reserved.
机译:在水平地下流人工湿地(HSSF)中处理废水中的有机物去除与细菌和古细菌的存在有关。这些生物执行厌氧性微生物过程,例如甲烷生成,这会导致甲烷排放。这项研究的目的是评估甲烷的产生,并表征在寒冷和温暖季节处理城市二级废水的HSSF中发现的细菌和古细菌群落。在本研究中使用的试验系统对应于四个HSSF,其中两个种植了芦苇(HSSF-Phr),两个种植了加州分枝杆菌(HSSF-Sch),监测进行了1335天。在每个HSSF中评估了有机物(生物和化学需氧量)以及总悬浮物和挥发性悬浮物的去除效率。此外,在温暖和寒冷的季节对每个HSSF的生物质进行采样,并通过比甲烷生成活性测定法((最大))(SMA(m))确定甲烷的产生。在相同的样品中,对细菌和古细菌进行了定量和鉴定。结果表明,有机物(53-67%BOD5和51-62%COD)和悬浮固体(85-93%)的降解不受季节条件或植物种类的影响。 HSSF-Sch潜在的甲烷生产量比HSSF-Phr高20-51%。此外,温暖季节的潜在甲烷产量比寒冷季节高3.4-42%。 HSSFs中微生物的定量确定了温暖季节细菌(38%)和古细菌(50-57%)的发育更大。此外,与南方芦苇相比,Schoenoplectus californicus菌具有更多的细菌(4-48%)和古细菌(34-43%)。对微生物的鉴定证明与细菌相关的序列主要属于Firmicutes(42%),Proteobacteria(33%)和Bacteroidetes(25%)。古细菌主要由甲烷八叠球菌(Methanosarcinales)代表,特别是甲烷八叠球菌(Methanosaetaeta(75%)和甲烷八叠球菌(Methanosarcina)(16%)。 HSSFs中产甲烷古菌的群落结构在整个季节或植物物种中都没有改变。 (C)2018 Elsevier B.V.保留所有权利。

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