School of Environment, Beijing Normal University / State Key Joint Laboratory of Environmental Simulation and Pollution Control / Key Laboratory of Water and Sediment Sciences of Ministry of Education, Beijing, 100875, China.
School of Environment, Beijing Normal University / State Key Joint Laboratory of Environmental Simulation and Pollution Control / Key Laboratory of Water and Sediment Sciences of Ministry of Education, Beijing, 100875, China.
Chemosphere. 2019 Nov;235:40-48. doi: 10.1016/j.chemosphere.2019.06.161. Epub 2019 Jun 21.
Anammox is a newly discovered nitrogen transformation process. However, its role in nitrogen removal in fresh water is far from understood. Here, we hypothesized that anammox could occur on suspended sediment in oxic river water. To test this hypothesis, simulation experiments with a nitrogen stable (N) isotopic tracer technique were conducted to study the occurrence of anammox on suspended sediment (SPS) in oxic river water, and the effects of the SPS particle size, including <20 μm, 20-63 μm, 63-100 μm, 100-200 μm, and <200 μm (original SPS) size fractions, were investigated. The results showed that anammox occurred in oxic water with SPS due to the existence of low oxygen microsites around/on SPS, and the anammox rate was even higher than the denitrification rate. The anammox rate increased with the SPS concentration, and it was negatively correlated with the particle size and was positively correlated with the organic carbon content of SPS (p < 0.05). The N produced by anammox in a system containing 1.0 g L SPS with a particle size below 20 μm was 0.27 mg-N/m·d, which was 5.3 times higher than that produced with a particle size of 100-200 μm. The anammox rate was significantly positively correlated with the anammox bacterial abundance (p < 0.01), and Ca. Brocadia was the dominant species. This study suggests that the SPS in oxic water may be a 'hotspot' for the anammox process and that its role in nitrogen removal should be considered in future studies.
厌氧氨氧化是一种新发现的氮转化过程。然而,其在淡水脱氮中的作用还远未被理解。在这里,我们假设厌氧氨氧化可以在好氧河水中的悬浮泥沙上发生。为了验证这一假设,采用氮稳定同位素示踪技术进行模拟实验,研究好氧河水中悬浮泥沙(SPS)上厌氧氨氧化的发生情况,以及 SPS 粒径(包括<20μm、20-63μm、63-100μm、100-200μm 和<200μm(原始 SPS)粒径)的影响。结果表明,由于 SPS 周围/上存在低氧微区,因此厌氧氨氧化发生在好氧水中,并且厌氧氨氧化速率甚至高于反硝化速率。厌氧氨氧化速率随 SPS 浓度的增加而增加,与粒径呈负相关,与 SPS 有机碳含量呈正相关(p<0.05)。在含有 1.0 g/L 粒径小于 20μm 的 SPS 的系统中,由厌氧氨氧化产生的 N 为 0.27 mg-N/m·d,是粒径为 100-200μm 时的 5.3 倍。厌氧氨氧化速率与厌氧氨氧化菌丰度呈显著正相关(p<0.01),优势种为 Ca. Brocadia。本研究表明,好氧水中的 SPS 可能是厌氧氨氧化过程的“热点”,在未来的研究中应考虑其在氮去除中的作用。