Key Laboratory of Industrial Ecology and Environmental Engineering (Ministry of Education, China), School of Environmental Science and Technology, Dalian University of Technology, Dalian 116024, China; School of Ecology and Environment, Zhengzhou University, Zhengzhou 450001, China.
Key Laboratory of Industrial Ecology and Environmental Engineering (Ministry of Education, China), School of Environmental Science and Technology, Dalian University of Technology, Dalian 116024, China.
Water Res. 2021 Feb 1;189:116626. doi: 10.1016/j.watres.2020.116626. Epub 2020 Nov 12.
A novel 'anammox' in the absence of anammox bacteria was confirmed to occur in an anaerobic sludge slurry system, in which Fe(II)/Fe(III) cycle driven by NO-induced Fe(II) oxidation and subsequent NH-induced Fe(III) reduction (Feammox) pushed the nitrogen removal. Results showed that Fe(II) contents significantly (p<0.05) decreased and Fe(III) accordingly increased with NO addition, indicating that Fe(II) was anaerobically oxidized to Fe(III). With depletion of NO, the Fe(II) content began to increase which was a result of Feammox. Consequently, 96.0% NH-N of the NO-added reactor was removed during 18 days operation, while NH-N content remained essentially unchanged in the control in which NO was not added. X-ray diffraction (XRD) and X-ray Photoelectron Spectroscopy (XPS) analysis indicated that FeOOH was produced from chemical Fe(II) oxidation with NO. During the treatment, anammox bacteria was not detected, but the relative abundance of Geobacter of the NO-added group increased by 13 folds. Isotope experiment in NH-containing reactors found that much more N and N in the NO-added group were produced than those in the control (without NO), confirming that NO induced Fe(II) oxidation to participate in Feammox for NH removal. Also, NO could be produced from partial denitrification of NO, meaning that NO as a more common species might substitute NO to trigger this new anammox process.
在不存在厌氧氨氧化菌的情况下,确认在厌氧污泥浆系统中发生了一种新型的“厌氧氨氧化”反应,该反应由 NO 诱导的 Fe(II)氧化和随后的 NH 诱导的 Fe(III)还原(Feammox)驱动的 Fe(II)/Fe(III)循环推动了氮的去除。结果表明,随着 NO 的添加,Fe(II)含量显著(p<0.05)下降,Fe(III)相应增加,表明 Fe(II)被厌氧氧化为 Fe(III)。随着 NO 的消耗,Fe(II)含量开始增加,这是 Feammox 的结果。因此,在 18 天的运行中,添加 NO 的反应器中 96.0%的 NH-N 被去除,而在未添加 NO 的对照反应器中,NH-N 含量基本保持不变。X 射线衍射(XRD)和 X 射线光电子能谱(XPS)分析表明,FeOOH 是由 Fe(II)与 NO 的化学氧化产生的。在处理过程中,未检测到厌氧氨氧化菌,但添加 NO 的组中 Geobacter 的相对丰度增加了 13 倍。含 NH 的反应器中的同位素实验发现,添加 NO 的组中产生的 N 和 N 比对照组(无 NO)多得多,证实了 NO 诱导的 Fe(II)氧化参与了 Feammox 反应,用于 NH 的去除。此外,NO 可以由部分反硝化 NO 产生,这意味着 NO 作为一种更常见的物质可能替代 NO 来触发这种新的厌氧氨氧化过程。