辽河口芦苇湿地土壤氨氧化菌的时空变化

采用传统的最大或然数法(MPN)和不依赖于培养的变性梯度凝胶电泳技术(DGGE),对辽河口芦苇湿地土壤中AOB的丰度、多样性进行了解析,并试图探究AOB同土壤可溶性盐分等环境因素之间的关系.结果表明:芦苇湿地土壤中AOB多样性指数时空分布存在较大差异,同一月份中不同站点之间群落结构相似性较大,AOB细菌数量与土壤可溶性盐分之间存在显著负相关关系(P<0.05),与土壤总氮和有机质含量之间存在极显著性正相关关系(P<0.01),表明盐分、总氮和有机质含量是辽河口湿地AOB数量时空分布的重要影响因素.     

Distribution characteristics of ammonia-oxidizing bacteria in the Typha latifolia constructed wetlands using fluorescent in situ hybridization(FISH)

A molecular biology method, fluorescent in situ hybridization（FISH）, in which the pre-treatment was improved in allusion to the media of the constructed wetlands（CW）, e.g. the soil and the grit, was used to investigate the vertical distribution characteristics of ammonia-oxidizing bacteria（AOB） quantity and the relation with oxidation-reduction potential（ORP） in the Typha latifolia constructed wetlands under three different Ioadings in summer from May to September. Results showed that the quantity of the AOB decreased in the Typha latifolia CW with the increase of vertical depth. However, the AOB quantity was 2-4 times the quantity of the control in the root area. Additionally, ORP in the rhizosphere was found to be higher than other areas, which showed that Typha latifolia CW was in an aerobic state in summer when using simulated non-point sewage at the rural area of Taihu Lake in China and small town combined sewage.     

我国北方四类土壤中氨氧化古菌和氨氧化细菌的活性及对氨氧化的贡献

氨氧化古菌(ammonia-oxidizing archaea,AOA)与氨氧化细菌(ammonia-oxidizing bacteria,AOB)是目前已知的两类好氧氨氧化微生物,广泛分布于各类生态系统中.采用双氰胺(dicyandiamide;DCD)和1-辛炔(1-octyne)抑制剂的方法对我国北方湿地、草原、农田、沙漠4类生态系统的土壤中AOA和AOB的氨氧化速率(ammonia oxidation rate,AR)分别进行定量测定,剖析AOA、AOB对不同土壤中氨氧化的贡献.结果表明:在氨氮含量较高的湿地土壤((32.58±1.38)mg·kg~(-1))中氨氧化速率由AOB主导(ARAOB占AR的86.19%),而在氨氮含量较低的草原土壤((10.40±0.69)mg·kg~(-1))、农田土壤((5.09±0.25)mg·kg~(-1))中氨氧化速率则由AOA主导(ARAOA分别占AR的65.50%、62.20%).氨氮含量是影响AOA、AOB相对活性的主要限制性因素.湿地土壤中氨氧化速率最高,为3.22 mg·kg~(-1)·d~(-1)(以N计),其次是草原土壤和农田土壤,其AR分别为1.11、1.00 mg·kg~(-1)·d~(-1),沙漠土壤中未检测到氨氧化速率.对氨氧化古菌、细菌的amoA基因进行定量分析的结果表明:在氨氮含量最高的湿地土壤和最低的沙漠土壤((1.27±0.05)mg·kg~(-1))中AOA丰度高于AOB丰度,在草原、农田土壤中AOB丰度高于AOA丰度.amoA基因生物多样性分析表明,377个古菌amoA序列以85%相似度可以划分为19个独立操作单元(operational taxonomic unit,OTU),具有较高的生物多样性,其Shannon指数为1.51~1.73.直接通过氨氧化微生物amoA基因丰度来推测AOA、AOB的活性具有一定的缺陷,而依靠AOA、AOB分别的氨氧化速率能够准确地衡量其在不同生态系统中对氨氮去除的相对贡献,对于理解不同生态系统中氨氮去除过程和效应有着重要的意义.     

利用RFLP分析DO对附积床系统中AOB群落结构的影响

为了解析DO浓度对附积床反应器脱氮系统中COD、NH4+-N、TN去除效率的影响,以及对氨氧化菌群(AOB)结构及多样性的影响,分析了DO分别为1.0~2.0,2.0~3.0,3.0~4.0mg/L时COD、NH4+-N、TN去除效率,并采用针对AOB功能基因氨单加氧酶(amoA)的限制性内切酶片段长度多态性技术(RFLP)分析了三组DO浓度下反应器中AOB的群落结构及多样性.结果表明,不同DO条件下,系统均取得较高的COD和NH4+-N的去除效果, NH4+-N的去除效率随着DO的增加而提高.不同DO浓度下反应器生物膜上AOB菌群多样性丰富,且与DO对AOB菌群的多样性影响较小相比,DO对AOB的菌群结构及种类的影响较大.     

艾比湖湿地盐节木根际土壤氨氧化微生物多样性和丰度及其与环境因子的相关性分析

氨氧化反应是硝化作用的关键步骤,参与这一反应的微生物是氨氧化细菌(AOB)和氨氧化古菌(AOA).对新疆艾比湖湿地盐节木根际和非根际土壤的氨氧化微生物进行群落结构和丰度分析,并探究其与土壤理化因子的相关性.同时,以氨单加氧酶基因(amo A)为分子标记,构建克隆文库和测序并与q-PCR法结合研究AOA、AOB的群落结构和丰度,利用Pearson相关分析法探究其与环境因子的相关性.结果表明,根际土壤中AOB的多样性高于AOA,amo A基因序列多属于土壤/水体沉积物分支,AOB克隆文库中的所有序列均属于亚硝化单胞菌属(Nitrosomonas).根际土壤中AOA amo A和AOB amo A的数量分别为2.09×104和2.91×105copies·g~(-1),AOB/AOA的比值为13.9;非根际土壤中AOA amo A和AOB amo A的数量分别为3.85×104和4.76×105copies·g~(-1),AOB/AOA的比值为12.36.相关分析显示,氨氧化微生物的群落结构和丰度与电导率(EC)、有机质(OM)、速效氮(AN)、氨氮(NH_4~+-N)和总氮(TN)等环境因子显著相关.这些结果表明,根际土壤中AOB的群落多样性高于AOA,根际和非根际土壤中AOB的丰度均高于AOA,说明在艾比湖湿地AOB是氨氧化微生物的优势种群,且EC、OM、AN、NH_4~+-N和TN可能会影响氨氧化微生物的群落结构和丰度.     

菜地氨氧化微生物驱动的N2O和NO对有机无机肥配施的响应

氨氧化细菌（AOB）和氨氧化古菌（AOA）是驱动土壤氨氧化过程的"引擎".氨氧化过程在土壤氧化亚氮（N₂O）和一氧化氮（NO）排放过程中扮演着重要角色.有机无机肥配施是实现化肥零增长和作物稳产增产的重要途径，但在有机无机肥配施下，菜地土壤AOB和AOA对氨氧化过程的相对贡献仍不清楚.本研究采用选择性抑制的方法（辛炔和乙炔）区分有机肥添加近3年后（2016年10月—2019年5月）AOB和AOA在氨氧化过程中对碱性菜地土壤N₂O和NO产生的相对贡献.试验共设5种施肥处理：不施氮肥（CK）、单施尿素（N）、单施有机肥（M）、50%尿素+50%有机肥（M1N1）和80%尿素+20%有机肥（M1N4）.结果表明，有机无机肥配施（M1N1和M1N4）可显著增加土壤电导率、有机碳和全氮含量.培养试验发现，与N处理相比，M和M1N1处理分别使N₂O排放量增加100.7%和38.8%，NO排放量增加77.9%和42.8%，AOB基因丰度增加16.6%和10.2%，同时，AOB对N₂O排放的相对贡献增加6.5%.相反，M1N4处理分别使N₂O和NO排放量降低19.3%和4.8%，AOB基因丰度降低37.5%，同时，AOB对N₂O及NO排放的相对贡献分别降低7.8%和7.4%.相关分析表明，土壤N₂O和NO累积排放量与土壤AOB基因丰度呈显著正相关（p<0.05），与土壤AOA基因丰度无显著相关性.有机无机肥配施下AOB是氨氧化过程的主要驱动者，适当比例的有机无机肥配施（即M1N4）措施可在一定程度上减弱AOB对碱性菜地土壤N₂O及NO排放的相对贡献.     

农业废物好氧堆肥中氨氧化细菌的群落结构

应用聚合酶链式反应-变性梯度凝胶电泳（PCR-DGGE）技术对农业废物好氧堆肥过程中氨氧化细菌（ammonia-oxidizingbacteria,AOB）种群结构随时间的变化情况进行了研究,结果表明,AOB群落的Shannon-Weaver指数初始值为2.58,堆肥结束时为2.02,多样性整体呈下降趋势.通过对部分优...     

铁矿区内重金属对土壤氨氧化微生物群落组成的影响

以密云水库上游某铁矿区为研究对象,采用荧光定量PCR和变性梯度凝胶电泳(DGGE)分析了矿区内不同采样点的土壤中氨氧化微生物的数量和群落结构的变化,结果表明,土样中氨氧化细菌(AOB)和氨氧化古菌(AOA)的数量变化范围分别为3.01×107~1.08×109copies/g干土和8.65×107~2.69×109copies/g干土.重金属含量与氨氧化微生物数量的相关性分析以及氨氧化微生物群落结构的冗余分析结果表明,该矿区内重金属污染改变了土壤中的氨氧化微生物的数量和结构.Cu污染对AOA的数量起到了显著抑制作用(r= -0.653*, P<0.05),但是对AOB则没有明显作用;Zn污染对尾矿库区域土壤的AOA/AOB比值影响显著(r= -0.606*, P<0.05);Cd污染改变了AOB的种群分布,降低了AOB的多样性水平.土壤中Cr长期干扰并没有改变氨氧化微生物的数量和结构,但是明显得抑制了氨氧化速率,表明重金属污染在一定程度上也影响了土壤生态系统的氮循环.     

罗红霉素短期冲击对活性污泥中氨氧化微生物丰度和多样性的影响

本研究基于amo A基因,结合实时荧光定量PCR(quantitative real-time PCR,q PCR)和高通量测序技术研究罗红霉素(roxithromycin,ROX)短期冲击对活性污泥中氨氧化古菌(ammonia-oxidizing archaea,AOA)和氨氧化细菌(ammonia-oxidizing bacteria,AOB)丰度和多样性的影响.本研究共设置10种ROX浓度,不同浓度的ROX对氨氧化作用的影响差异明显,环境浓度(0.3~30μg·L~(-1))与中等浓度(300μg·L~(-1)和3000μg·L~(-1))的ROX并未对氨氧化作用产生影响;较高浓度(5 000~12 000μg·L~(-1))的ROX对氨氧化作用产生明显的抑制作用.环境浓度和中等浓度的ROX刺激了AOA增长,而较高浓度的ROX导致AOA的丰度下降.此外,除了环境中的痕量浓度(0.3μg·L~(-1)),其余浓度的ROX均导致AOB丰度下降,且下降趋势比AOA显著,说明AOA对ROX的耐受性高于AOB.高通量测序结果表明,在ROX的选择压下,AOA的OTUs多样性减少,AOB的OTUs多样性增加;但3个样品中最主要的AOA Candidatus Nitrososphaera gargensis的相对丰度随ROX浓度增加而增多,最主要的AOB Nitrosomonas eutropha的相对丰度随ROX浓度增加而减少,这同样说明了AOA对ROX的耐受性高于AOB.冗余分析结果表明:AOA Ca.Nitrososphaera gargensis、Candidatus Nitrosoarchaeum koreensis和AOB Nitrosomonas oligotropha、Nitrosomonas watsonii、Nitrosomonas halophilus均与ROX浓度呈正相关.     

AOB与AnAOB在不同生物填料上挂膜效果的研究

针对厌氧氨氧化工艺运行过程中污泥流失严重与启动时间长等问题,本研究通过对多种市售生物填料的挂膜实验,筛选适合好氧氨氧化菌与厌氧氨氧化菌挂膜的生物填料.结果表明,当活性污泥中的好氧氨氧化菌菌属为Nitrosomonas时,AQ1聚氨酯立方体填料最适合其挂膜,挂膜成熟时好氧氨氧化速率可以达到（0.81±0.08）mg N/（L·h）,挂膜生物量为（0.87±0.14）mg VSS.而更适合厌氧氨氧化菌（Candidatus Kuenenia）挂膜的生物填料为K3环形填料,材质为聚乙烯或者聚丙烯.当厌氧氨氧化菌挂膜成熟时,其厌氧氨氧化速率可以达到（3.27±0.10）mg N/（L·h）,挂膜生物量为（2.74±0.40）mg VSS.厌氧氨氧化菌在K3型填料上的挂膜要优于好氧氨氧化菌,其原因是厌氧氨氧化菌分泌的胞外聚合物含量要高于好氧氨氧化菌,而胞外聚合物是形成生物膜的重要因素.     

Ammonium-dependent regulation of aerobic methane-consuming bacteria in landfill cover soil by leachate irrigation

The impacts of landfill leachate irrigation on methane oxidation activities and methane-consuming bacteria populations were studied by incubation of landfill cover soils with leachate and (NH₄)₂SO₄ solution at different ammonium concentrations. The community structures and abundances of methane-oxidizing bacteria (MOB) and ammonia-oxidizing bacteria (AOB) were examined by PCRDGGE and real-time PCR. Compared with the pure (NH₄)₂SO₄ solution, leachate addition was found to have a positive effect on methane oxidation activity. In terms of the irrigation amount, ammonium in leachate was responsible for the actual inhibition of leachate. The extent of inhibitory effect mainly depended on its ammonium concentration. The suppression of the predominant methaneconsuming bacteria, type I MOB, was responsible for the decreased methane oxidation activity by ammonium inhibition. Methaneconsuming bacteria responded diversely in abundance to ammonium. The abundance of type I MOB decreased by fivefold; type II MOB showed stimulation response of fivefold magnification upon the first addition but lessened to be lower than the original level after the second addition; the amount of AOB was stimulated to increase for 20-30 times gradually. Accumulated nitrate from nitrification strengthened the ammonium inhibition on type I and type II MOB, as a result, repetitive irrigation was unfavorable for methane oxidation.     

污水处理工艺对氨氧化菌及细菌群落的影响

采用针对氨氧化菌(AOB)功能基因氨单加氧酶(amoA)的末端限制性片段长度多态性技术(T-RFLP)、克隆测序等方法,研究了北京市2个污水处理厂的4个污水处理系统中AOB的群落结构,同时采用针对16S rRNA基因的T-RFLP技术分析了总细菌的群落结构.T-RFLP指纹图谱分析表明,4个污水处理系统中AOB的优势限制性片段(T-RF)均为291bp和354bp,细菌的优势T-RF为115,117,166,455,465, 468,471,482,800,893bp等.说明污水处理工艺对系统中AOB及细菌的群落结构影响很小.对功能基因amoA的系统发育分析表明,4个污水处理系统中优势AOB均属于Nitrosomonas europaea cluster和Nitrosomonas oligotropha culster.     

Functional relationship between ammonia-oxidizing bacteria and ammonia-oxidizing archaea populations in the secondary treatment system of a full-scale municipal wastewater treatment plant

The abundance of ammonia-oxidizing bacteria and archaea and their amoA genes from the aerobic activated sludge tanks, recycled sludge and anaerobic digesters of a full-scale wastewater treatment plant (WWTP) was determined. Polymerase chain reaction and denaturing gradient gel electrophoresis were used to generate diversity profiles, which showed that each population had a consistent profile although the abundance of individual members varied. In the aerobic tanks, the ammonia-oxidizing bacterial (AOB) population was more than 350 times more abundant than the ammonia-oxidizing archaeal (AOA) population, however in the digesters, the AOA population was more than 10 times more abundant. Measuring the activity of the amoA gene expression of the two populations using RT-PCR also showed that the AOA amoA gene was more active in the digesters than in the activated sludge tanks. Using batch reactors and ddPCR, amoA activity could be measured and it was found that when the AOB amoA activity was inhibited in the anoxic reactors, the expression of the AOA amoA gene increased fourfold. This suggests that these two populations may have a cooperative relationship for the oxidation of ammonia.     

不同氮水平下间作对玉米土壤硝化势和氨氧化微生物数量的影响

利用荧光定量PCR(real-time quantitative PCR,Q-PCR)技术,结合氨氧化细菌(ammonia oxidizing bacteria,AOB)和氨氧化古菌(ammonia oxidizing archaea,AOA)丰度和土壤理化性质的测定,探索了不同氮水平下间作对玉米土壤硝化势(PNF)的影响.试验设置玉米单作和与马铃薯间作两个种植模式,4个施氮水平(不施氮N0、1/2常规施氮N1、常规施氮N2和3/2常规施氮N3)的随机区组试验.结果表明,从不施氮到常规施氮,土壤硝化势和AOA、AOB数量均随施氮量增加而逐渐增加,而高氮(N3)时与N2没有显著差异;间作对土壤硝化势、AOA与AOB数量的影响与施氮量和作物生育期有关,低氮投入(N1)间作有利于增加土壤氨氧化微生物数量和硝化作用.施肥是硝化势增加的主要驱动因子,相关性分析结果表明,土壤含水量是影响PNF的主要环境因子;PNF与土壤中AOA、AOB amoA基因丰度成显著的正相关.尽管玉米马铃薯间作降低了土壤中AOA、AOB amoA基因丰度,却使得间作土壤中AOB占据氨氧化微生物数量上的优势.以上结果表明,施氮和间作均影响了土壤硝化作用和氨氧化微生物AOA和AOB数量的变化,这些变化会影响土壤环境质量.     

土地利用变化对土壤硝化及氨氧化细菌区系的影响

以西藏高原相邻的原始森林、天然草原和农田土壤为研究对象,分别采用室内培养法和nested PCR-DGGE技术,对比研究了这3个生态系统的土壤硝化势、硝态氮浓度以及土壤氨氧化细菌（AOB）菌群区系.结果表明,农田土壤的硝化势和硝态氮（NO 3--N）浓度显著高于相邻的草原和森林土壤,硝化势分别是森林和草原土壤的9倍和11倍,NO 3--N是农田土壤无机氮（Nmin）的主要成分,占无机氮的70%～90%.铵态氮（NH 4＋-N）则是森林和草原土壤中主要的无机氮形态.原始森林和天然草原间的硝化势和硝态氮浓度没有显著差异.原始森林的土壤AOB菌群数量、多样性及均匀度最低.天然草原生态系统转换为农田后,土壤AOB菌群的多样性和均匀度显著降低,但是农田土壤的AOB菌群结构仍与其前身草原生态系统有较高的相似性.原始森林的AOB菌群数量、多样性及均匀度最低直接导致了其硝化势最低;农田土壤的硝化势和硝态氮浓度最高意味着农田生态系统中优势AOB的活性最高.以上结果表明,土地利用变化导致土壤氮素内循环及其关键微生物AOB的多样性与活性均发生显著变化,这些变化会影响土壤环境质量以及生态系统的持续与稳定.     

Isolation and characterization of facultative mixotrophic ammonia-oxidizing bacteria from constructed wetlands

Autotrophic ammonia-oxidizing bacteria (AOB) have been widely studied in constructed wetlands systems, while mixotrophic AOB have been less thoroughly examined. Heterotrophic bacteria were isolated from wastewater and rhizospheres of macrophytes of constructed wetlands, and then cultivated in a mixotrophic medium containing ammonium and acetic acid. A molecular characterization was accomplished using ITS-PCR amplification, and phylogenetic analysis based on 16S rRNA gene sequences. Results showed the presence of 35 bacteria, among 400 initially heterotrophic isolates, that were able to remove ammonia. These 35 isolates were classified into 10 genetically different groups based on ITS pattern. Then, a collection of 10 isolates were selected because of their relatively high ammonia removal efficiencies (ARE ≥ 80%) and their phylogenetic diversity. In conditions of mixotrophy, these strains were shown to be able to grow (increase of optical density OD₆₆₀ during incubation with assimilation of nitrogen into cellular biomass) and to oxidize ammonia (important ammonia oxidation efficiencies, AOE between 79% and 87%). Among these facultative mixotrophic AOB, four isolates were genetically related to Firmicutes (Bacillus and Exiguobacterium), three isolates were affiliated to Actinobacteria (Arthrobacter) and three other isolates were associated with Proteobacteria (Pseudomonas, Ochrobactrum and Bordetella).     

辽河口湿地沉积物硝化细菌及硝化作用研究

2009年6月和8月,采用现场培养和实验室模拟培养相结合的方法对辽河口湿地表层沉积物硝化细菌数量、硝化速率及影响因素进行了研究.结果表明,辽河口湿地表层沉积物氨氧化细菌(ammonia-oxidizing bacteria,AOB)数量6月在0.54×104～5.69×104个.g-1之间,平均值为(2.21±2.32)×104个.g-1,8月在1.90×104～7.90×104个.g-1之间,平均值为(3.61±2.87)×104个.g-1;沉积物潜在硝化速率6月在9.72～16.45 mmol.(m2.h)-1之间,平均值为(12.54±3.14)mmol.(m2.h)-1,8月在14.66～24.62 mmol.(m2.h)-1之间,平均值为(18.71±4.21)mmol.(m2.h)-1;净硝化作用速率6月(S1站)为0.41 mmol.(m2.h)-1,8月在0.20～0.53 mmol.(m2.h)-1之间,平均值为(0.35±0.16)mmol.(m2.h)-1.潜在硝化速率显著高于净硝化速率,AOB数量、净硝化作用速率和潜在硝化作用速率均表现为8月高于6月,芦苇根际效应对硝化作用有促进作用.通过SPSS 13.0软件统计分析,表明影响辽河口湿地表层沉积物硝化作用的主要环境因子有上覆水NH 4+-N浓度和沉积物pH、有机质、总氮(TN)、总磷(TP)、NH 4+-N含量以及AOB数量(p0.05),其中上覆水NH 4+-N浓度和沉积物总磷(TP)、NH 4+-N含量对硝化作用影响较大,是辽河口湿地硝化作用影响的关键因素.根据研究结果估算辽河口湿地沉积物硝化作用每天可以将1.14×105kg的NH 4+-N转化为NO 3--N,对河口湿地氮的循环具有重要意义.     

Community analysis of ammonia-oxidizing bacteria in activated sludge of eight wastewater treatment systems

We investigated the communities of ammonia-oxidizing bacteria(AOB) in activated sludge collected from eight wastewater treatment systems using polymerase chain reaction(PCR) followed by terminal restriction fragment length polymorphism(T-RFLP),cloning,and sequencing of the α-subunit of the ammonia monooxygenase gene(amoA).The T-RFLP fingerprint analyses showed that different wastewater treatment systems harbored distinct AOB communities.However,there was no remarkable difference among the AOB TRFLP profiles from different parts of the same system.The T-RFLP fingerprints showed that a full-scale wastewater treatment plant(WWTP) contained a larger number of dominant AOB species than a pilot-scale reactor.The source of influent affected the AOB community,and the WWTPs treating domestic wastewater contained a higher AOB diversity than those receiving mixed domestic and industrial wastewater.However,the AOB community structure was little affected by the treatment process in this study.Phylogenetic analysis of the cloned amoA genes clearly indicated that all the dominant AOB in the systems was closely related to Nitrosomonas spp.not to Nitrosospira spp.Members of the Nitrosomonas oligotropha and Nitrosomonas communis clusters were found in all samples,while members of Nitrosomonas europaea cluster occurred in some systems.     

AOB去除炔雌醇的共代谢与硝基化协同作用

采用氨氧化菌Nitrosomonas europaea降解17α-乙炔雌二醇（EE2）,考察降解过程中氨氮的作用以及EE2的降解机制.结果表明,N.europaea降解EE2属于共代谢过程,氨氮是共代谢发生的必要条件.氨氧化过程产生的亚硝氮会在酸性条件下将EE2硝基化,反应符合一级动力学模型,降解速率常数与亚硝酸根、H⁺及游离亚硝酸浓度成正相关.通过控制pH值大于7.5抑制硝基化反应,证实了N.europaea对EE2的生物降解作用,生物降解反应符合一级动力学模型且降解速率常数为0.0069h^-1.当N.europaea氨氧化反应导致pH值低于7.5时,EE2的去除存在生物降解和硝基化的协同作用,EE2去除符合一级动力学模型且降解速率常数为0.0093h^-1.同时还发现一种未曾报道过的EE2生物降解产物M613,对于其雌激素效应和毒性还需进一步探究.     

AOB去除炔雌醇的共代谢与硝基化协同作用

采用氨氧化菌Nitrosomonas europaea降解17α-乙炔雌二醇（EE2）,考察降解过程中氨氮的作用以及EE2的降解机制.结果表明,N.europaea降解EE2属于共代谢过程,氨氮是共代谢发生的必要条件.氨氧化过程产生的亚硝氮会在酸性条件下将EE2硝基化,反应符合一级动力学模型,降解速率常数与亚硝酸根、H⁺及游离亚硝酸浓度成正相关.通过控制pH值大于7.5抑制硝基化反应,证实了N.europaea对EE2的生物降解作用,生物降解反应符合一级动力学模型且降解速率常数为0.0069h^-1.当N.europaea氨氧化反应导致pH值低于7.5时,EE2的去除存在生物降解和硝基化的协同作用,EE2去除符合一级动力学模型且降解速率常数为0.0093h^-1.同时还发现一种未曾报道过的EE2生物降解产物M613,对于其雌激素效应和毒性还需进一步探究.