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Using Fe(II)/Fe(III) as catalyst to drive a novel anammox process with no need of anammox bacteria

厌氧氨氧化菌 化学 反硝化 X射线光电子能谱 催化作用 细菌 无机化学 核化学 氮气 化学工程 反硝化细菌 生物化学 有机化学 遗传学 生物 工程类
作者
Yafei Yang,Cancan Xiao,Qing Yu,Zhiqiang Zhao,Yaobin Zhang
出处
期刊:Water Research [Elsevier BV]
卷期号:189: 116626-116626 被引量:110
标识
DOI:10.1016/j.watres.2020.116626
摘要

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 NO2−-induced Fe(II) oxidation and subsequent NH4+-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 NO2− addition, indicating that Fe(II) was anaerobically oxidized to Fe(III). With depletion of NO2−, the Fe(II) content began to increase which was a result of Feammox. Consequently, 96.0% NH4+-N of the NO2−-added reactor was removed during 18 days operation, while NH4+-N content remained essentially unchanged in the control in which NO2− 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 NO2−. During the treatment, anammox bacteria was not detected, but the relative abundance of Geobacter of the NO2−-added group increased by 13 folds. Isotope experiment in 15NH4+-containing reactors found that much more 30N2 and 29N2 in the 14NO2−-added group were produced than those in the control (without 14NO2−), confirming that 14NO2− induced Fe(II) oxidation to participate in Feammox for 15NH4+ removal. Also, NO2− could be produced from partial denitrification of NO3−, meaning that NO3− as a more common species might substitute NO2− to trigger this new anammox process.
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