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刺激氨氧化菌(AOB)活性可提高人工湿地(CW)中的氨氧化速率。

Stimulating ammonia oxidizing bacteria (AOB) activity drives the ammonium oxidation rate in a constructed wetland (CW).

机构信息

Key Laboratory of Drinking Water Science and Technology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, China; University of Chinese Academy of Sciences, Beijing 100049, China.

Key Laboratory of Drinking Water Science and Technology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, China.

出版信息

Sci Total Environ. 2018 May 15;624:87-95. doi: 10.1016/j.scitotenv.2017.12.084. Epub 2017 Dec 14.

Abstract

An integrated approach to document high ammonium oxidation rate in Guanjinggang constructed wetland (GJG-CW) was performed and the results showed that the substantial ammonium oxidation rate could be obtained by enhancing Ammonia Oxidizing Bacteria (AOB) activity rather than Ammonia Oxidizing Archaea (AOA) activity. In the plant-bed/ditch system, ditch center and plant-bed fringe were two active zones for NH-N removal with ammonium oxidation rate peaking at 2.98±0.04 and 2.15±0.02mgNkgd, respectively. The enhanced AOB activity were achieved by increasing water level fluctuations, extending hydraulic retention time (HRT) and stimulating substrate availability, which subsequently enhanced NH-N removal by 34.06% in GJG-CW. However, the high AOB activity was not correlated with high AOB abundance, but was instead mostly determined by specific AOB taxa, particularly Nitrosomonas, which dominated in the active AOB. The increased cell-specific AOA activity and high AOA diversity were also achieved using those engineering measures. Although the AOA activity decreased overall with extended HRT and increased NH-N contents in GJG-CW, AOA still played a major role on ammonium oxidation in plant-bed soil. The study illustrated that artificially enhancing AOB activity and certain species in anthropogenically polluted water ecosystems would be an effective strategy to improve NH-N removal.

摘要

采用综合方法研究了关景岗人工湿地(GJG-CW)中的高铵氧化速率,结果表明,通过增强氨氧化细菌(AOB)活性而不是氨氧化古菌(AOA)活性可以获得较大的铵氧化速率。在植物床/沟渠系统中,沟渠中心和植物床边缘是 NH-N 去除的两个活性区,铵氧化速率峰值分别为 2.98±0.04 和 2.15±0.02mgNkgd。通过增加水位波动、延长水力停留时间(HRT)和刺激基质可用性来提高 AOB 活性,进而使 GJG-CW 中的 NH-N 去除率提高了 34.06%。然而,高 AOB 活性与高 AOB 丰度没有相关性,而是主要由特定的 AOB 分类群决定,特别是在活性 AOB 中占主导地位的硝化单胞菌。通过这些工程措施,还可以实现细胞特异性 AOA 活性的增加和 AOA 多样性的提高。尽管随着 GJG-CW 中 HRT 的延长和 NH-N 含量的增加,AOA 活性总体上呈下降趋势,但 AOA 仍然在植物床土壤中的铵氧化中起主要作用。该研究表明,人为增强人为污染水生态系统中的 AOB 活性和某些物种将是提高 NH-N 去除率的有效策略。

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