Center for Microbial Ecology and Technology (CMET), Ghent University, Coupure Links 653, 9000, Gent, Belgium.
BIOMATH, Department of Mathematical Modelling, Statistics and Bioinformatics, Ghent University, Coupure Links 653, 9000, Gent, Belgium.
Water Res. 2019 Jun 1;156:34-45. doi: 10.1016/j.watres.2019.03.008. Epub 2019 Mar 14.
Nitrification and denitrification, the key biological processes for thermophilic nitrogen removal, have separately been established in bioreactors at 50 °C. A well-characterized set of kinetic parameters is essential to integrate these processes while safeguarding the autotrophs performing nitrification. Knowledge on thermophilic nitrifying kinetics is restricted to isolated or highly enriched batch cultures, which do not represent bioreactor conditions. This study characterized the stoichiometry and kinetics of two thermophilic (50 °C) nitrifying communities. The most abundant ammonia oxidizing archaea (AOA) were related to the Nitrososphaera genus, clustering relatively far from known species Nitrososphaera gargensis (95.5% 16S rRNA gene sequence identity). The most abundant nitrite oxidizing bacteria (NOB) were related to Nitrospira calida (97% 16S rRNA gene sequence identity). The nitrification biomass yield was 0.20-0.24 g VSS g N, resulting mainly from a high AOA yield (0.16-0.20 g VSS g N), which was reflected in a high AOA abundance in the community (57-76%) compared to NOB (5-11%). Batch-wise determination of decay rates (AOA: 0.23-0.29 d; NOB: 0.32-0.43 d) rendered an overestimation compared to in situ estimations of overall decay rate (0.026-0.078 d). Possibly, the inactivation rate rather than the actual decay rate was determined in batch experiments. Maximum growth rates of AOA and NOB were 0.12-0.15 d and 0.13-0.33 d respectively. NOB were susceptible to nitrite, opening up opportunities for shortcut nitrogen removal. However, NOB had a similar growth rate and oxygen affinity (0.15-0.55 mg O L) as AOA and were resilient towards free ammonia (IC > 16 mg NH-N L). This might complicate NOB outselection using common practices to establish shortcut nitrogen removal (SRT control; aeration control; free ammonia shocks). Overall, the obtained insights can assist in integrating thermophilic conversions and facilitate single-sludge nitrification/denitrification.
硝化和反硝化是 50°C 下实现嗜热脱氮的关键生物过程,已在生物反应器中分别建立。一套特征明确的动力学参数对于整合这些过程至关重要,同时还需保障进行硝化作用的自养生物。关于嗜热硝化动力学的知识仅限于分离或高度富集的间歇培养物,而这些培养物并不能代表生物反应器的条件。本研究对两种嗜热(50°C)硝化群落的计量学和动力学进行了描述。最丰富的氨氧化古菌(AOA)与 Nitrososphaera 属有关,与已知的 Nitrososphaera gargensis 种(95.5% 16S rRNA 基因序列同一性)聚类关系较远。最丰富的亚硝酸盐氧化细菌(NOB)与 Nitrospira calida 有关(97% 16S rRNA 基因序列同一性)。硝化生物量产率为 0.20-0.24 g VSS g N,主要归因于 AOA 的高产率(0.16-0.20 g VSS g N),这反映了群落中 AOA 的丰度较高(57-76%),而 NOB 的丰度较低(5-11%)。通过分批测定衰减率(AOA:0.23-0.29 d;NOB:0.32-0.43 d)与原位测定的整体衰减率(0.026-0.078 d)相比,存在高估。可能在分批实验中确定的是失活率,而不是实际的衰减率。AOA 和 NOB 的最大生长速率分别为 0.12-0.15 d 和 0.13-0.33 d。NOB 易受亚硝酸盐的影响,为短程脱氮提供了机会。然而,NOB 的生长速率和氧气亲和力(0.15-0.55mg O L)与 AOA 相似,并且对游离氨具有很强的抵抗力(IC>16mg NH-N L)。这可能会使通过常见实践(SRT 控制;曝气控制;游离氨冲击)淘汰 NOB 变得复杂。总的来说,获得的见解可以帮助整合嗜热转化,并促进单污泥硝化/反硝化。