水稻根际联合固氮细菌的研究

从我国南方水稻根部分离到3株氧化型革兰氏阴性细菌,编号为A1601,A1701和A1702。经15N示踪实验证明,它们均有较高的固氮能力。在无氮培养基中加入少量稻根浸出液进行培养后,可使固氮酶活性明显提高。根据菌株的形态和生理生化等特征鉴定,3株菌均为产孽菌属的细菌,分别为争论产碱菌(Alcaligenes paradoxus A1601),反硝化产碱蔺木糖氧化亚种(Alcaligenes denitrificans subsp.xylosoxydons A1701)和反硝化产碱菌反硝化亚种(Alcaligenes denitridicans subsp.denitrificans A1702)。这是继粪产碱菌(Alcaligenesfaecalis)之后,发现的产碱菌属中另外3株未见报道的固氮细菌。     

喹啉废水反硝化反应器中优势菌的代谢功能分析

采用纯培养技术对一个降解喹啉的反硝化反应器筛选到的26株优势菌株进行反硝化能力以及好氧降解喹啉能力研究,其中的反硝化菌还测定了反硝化条件下的喹啉降解能力。结果发现Bacillus、Staphylococcus、Pseudomonas、Brucella、Delftia等5个属的10株菌具有反硝化能力,Rhodococcus属的9株细菌能够好氧降解喹啉,揭示了反硝化喹啉降解反应器中主要细菌类型的代谢特性,发现在缺氧反硝化反应器中存在多样的代谢类型的细菌。     

好氧反硝化聚磷菌的筛选及菌群构建优化

【背景】近年来,随着海水养殖规模的扩大,养殖产品产生的排泄物与残留的饲料大量积累,导致养殖水域的氮磷元素含量上升,水体富营养化加剧并对环境造成危害。【目的】从红树林人工湿地中筛选出好氧反硝化聚磷菌株并研究各菌株的最佳除氮除磷效率,随后通过响应面法构建菌群,进一步强化菌株去除污染物的能力。【方法】将前期筛选出的5株耐盐异养硝化-好氧反硝化菌通过异染颗粒染色和聚-β-羟基丁酸(poly-β-hydroxybutyricacid,PHB)染色进行好氧反硝化聚磷菌的筛选,通过单因素试验明确各菌株的最佳除氮除磷条件,并利用Design-Expert软件和Box-Benhnken响应面法进行配比试验。【结果】经过筛选获得3株耐盐好氧反硝化聚磷菌,分别为肺无色杆菌(Achromobacter pulmonis) strain E43、氧化木糖无色杆菌(Achromobacterxylosoxidans)strainJ1和食油假单胞菌(Pseudomonasoleovorans)strain F2,发现菌株E43具有聚磷功能,确定了耐盐好氧反硝化聚磷菌群的最优降解投加比例为E43:J1:F2=1:1:...     

SBR和MBR反应器中好氧反硝化菌的筛选与分析

好氧反硝化菌是土壤、沉积物、活性污泥等介质中广泛存在的一类微生物。研究以相同种泥扩大培养的SBR(序批式活性污泥反应器)和MBR(膜生物反应器)中活性污泥为研究对象,采用平板分离法分别从运行6个月的SBR和MBR反应器中分离得到9株和11株好氧反硝化菌。经好氧反硝化性能测定发现,20株细菌中有16株总氮去除率在50%以上,且NO_2~--N累积量均在0.5 mg/L以下。经系统进化分析表明,在门分类级别中,采用同一种泥的2个反应器中好氧反硝化菌表现出极大的一致性,20株好氧反硝化菌全部属于变形菌门(Proteobacteria)。但是,进一步分析发现不同反应器中好氧反硝化菌表现出较大的属、种间的差异。其中,SBR反应器9株好氧反硝化菌分属于4个属,6个物种;而从MBR反应器获得的11株细菌分属于2个属,6个物种;仅1个物种(Pseudomonas toyotomiensis)在2个反应器均有发现。     

好氧反硝化菌的研究进展

综述了好氧反硝化菌的种类和特性、好氧反硝化菌的反硝化作用机制和影响因素.好氧反硝化菌主要包括假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)、副球菌属(Para-coccus)和芽孢杆菌属(Bacillus)等,属好氧或兼性好氧异养微生物.好氧反硝化菌能在好氧条件下进行反硝化,其主要产物是N2O,并可将铵态氮直接转化成气态产物.催化好氧反硝化菌反硝化作用的硝酸盐还原酶是周质酶而不是膜结合酶.溶解氧和C/N往往是影响好氧反硝化菌反硝化作用的主要因素.介绍了间歇曝气法、选择性培养基法等好氧反硝化菌的主要分离筛选方法.概述了好氧反硝化菌在水产养殖、废水生物处理、降解有机污染物以及对土壤氮素损失的影响方面的研究进展.     

反硝化除磷菌筛选及其特性研究

【目的】研究反硝化除磷菌特性。【方法】通过微生物筛选和生物学特性研究方法,从对虾养殖池塘中筛选出多株可在有氧条件下同时具有反硝化除磷功能的菌种。【结果】菌株LY-1可在18 h内将初始量为10 mg/L的亚硝酸盐氮降低至0.04 mg/L,PO43?-P降低至0.05 mg/L。在DO浓度为5.0?5.9 mg/L时,该菌反硝化除磷率近100%。试验选取具有反硝化除磷功能的枯草芽孢杆菌为阳性对照菌,大肠杆菌为阴性对照菌,比较研究了菌株LY-1在不同pH、温度、盐度、PO43?-P浓度、亚硝酸盐浓度时反硝化除磷的强弱,在pH为5?9范围时,该菌亚硝酸盐氮去除率近99%,PO43?-P去除率86%;温度为30°C时,该菌反硝化除磷率近100%;盐度为5‰?15‰、PO43?-P浓度为10 mg/L、亚硝酸盐氮浓度为20 mg/L时,该菌亚硝酸盐氮和PO43?-P去除率均可达99%。【结论】菌株LY-1反硝化除磷性能显著高于对照菌(P<0.05)。通过菌株LY-1形态学观察、生理生化及16S rRNA基因序列分析,初步鉴定为蜡样芽孢杆菌(Bacillus cereus)。     

油藏本源反硝化功能菌的产气作用(N2O)及对原油物性的影响

利用叠皿夹层培养法从新疆油田采出水中筛选到8株反硝化菌株T1、D1、D44、D46、D15、S1、S2、S6,经16S rDNA序列测定鉴定分析,这8株菌分别与施氏假单胞菌(T1、D1、D44)、恶臭假单胞菌(D46、D15)和铜绿假单胞菌(S1、S2、S6)相似,相似度均达到100%。通过室内批次培养试验,评价了这8株菌利用不同碳源的反硝化产气作用(N₂O)及对原油物性的影响。结果表明: 在以蔗糖为碳源时,产气量最大,以甘油为碳源时,产N₂O气浓度最高;菌株反硝化代谢过程导致原油体积膨胀和粘度降低,膨胀率与N₂O气体浓度呈显著正相关,相关系数为0.983,但与产气体积无相关性;铜绿假单胞菌株S1、S2、S6在以甘油为唯一碳源时产生少量表面活性剂(530～730 mg·L^-1),可降低表面张力并具有乳化原油的作用,但其产气量较少,对原油的膨胀与降粘作用低于其他反硝化菌株。研究提示,在筛选采油功能菌时,菌株反硝化产N₂O气体的能力应给予足够重视。     

滇池可培养好氧反硝化细菌多样性及其脱氮特性

【目的】氮污染已成为当今水体污染的一个重要因素,为了解滇池可培养好氧反硝化细菌的多样性,获得高效好氧反硝化细菌资源,为污染水体或浅层地下水的生物修复提供材料。【方法】采用富集培养方法从滇池沉积物和水体样品中分离好氧反硝化细菌,对好氧反硝化细菌的16S r RNA基因序列进行系统发育分析,并筛选其中的高效好氧反硝化细菌。【结果】分离出260株好氧反硝化菌,经16S rRNA基因序列分析,260株菌分属于2门13科14属的59个种。假单胞菌属(Pseudomonas)为优势细菌属,其次是不动杆菌属(Acinetobacter)、气单胞菌属(Aeromonas)和代尔夫特菌属(Delftia)。筛选到12株高效好氧反硝化细菌菌株,其中8株属于假单胞菌(Pseudomonas spp.),4株为不动杆菌(Acinetobacter spp.)。定量分析发现菌株N15-6-1的反硝化效果较好。对菌株N15-6-1的脱氮条件优化结果显示,在以蔗糖为碳源,温度为30–35℃、C/N=12、静止培养时,反硝化能力较强,其在48 h内硝态氮的去除率达到98.81%,总氮的去除率达96.27%。【结论】滇池存在着较丰富的可培养好氧反硝化细菌,好氧反硝化细菌的分离丰富了好氧反硝化菌的种类,其中的高效脱氮菌株为污染水体或浅层地下水的生物修复提供了初步的候选菌株。     

好氧反硝化微生物多样性及其反硝化功能初步研究

为研究污水厂/养殖池中好氧反硝化微生物的多样性及菌株反硝化能力,本研究采集了位于福建省厦门市和漳州市的污水处理厂、排污口、污水池、对虾养殖池的污水和污泥样品进行好氧反硝化微生物的富集、分离、鉴定和功能筛选。分别以NaNO3、NaNO2作为唯一氮源共分离纯化获得128株单菌。其中以NaNO3为唯一氮源分离得到63株,以NaNO2为唯一氮源分离得到65株。16SrRNA基因序列分析表明,128株单菌分属于γ-变形菌纲(Gammaproteobacteria,58.6%)、芽胞杆菌纲(Bacilli,6.4%)、放线菌纲(Actinobacteria,11.7%)、α-变形菌纲(Alphaproteobacteria,8.6%)、纤维菌纲(Cytophagia,2.3%)、鞘脂杆菌纲(Sphingobacteria,0.8%)和黄杆菌纲(Flavobacteria,1.6%)7个纲中的38个属。其中盐单胞菌属(Halomonas,29.7%)和芽胞杆菌属(Bacillus,12.5%)为优势菌属,并且广泛存在于各个样品中。反硝化功能初筛结果表明,35株菌能在72h内将20mg·L-1 NO-3-N/NO-2-N完全去除;复筛结果表明,21株菌能在72h内将100 mg·L-1 NO-3-N/NO-2-N完全去除,并且盐单胞菌属、卓贝尔氏菌属(Zobellella)、斯塔普氏菌属(Stappia)及节杆菌属(Arthrobactor)反硝化效果较好,其中斯塔普氏属是首次报道具有好氧反硝化功能。本研究结果表明,污水场/养殖池等环境中可培养反硝化细菌多样性丰富,同时高效反硝化菌的获得也为含氮废水的生物处理提供了良好的菌种资源。     

1株滩涂沉积物反硝化细菌的鉴定及其性能研究

利用富集培养法从江苏沿海滩涂沉积物中分离筛选获得1株具有反硝化性能的细菌,命名为MD5。通过形态学观察、糖发酵及16S r DNA序列分析对其进行了分类鉴定、系统发育地位及反硝化性能等方面的研究。结果表明,该菌株能在厌氧条件下利用硝酸钠进行反硝化反应,在初始硝酸盐质量浓度为1 500 mg/L、30℃培养条件下,144 h后培养基中硝酸盐脱除率可达90.1%;在好氧培养条件下,该菌株可使能力测试管中硝酸盐质量浓度下降89.3%。菌株MD5的形态学、糖发酵结果与盐单胞菌一致,且基因序列与盐单胞属(Halomonas)细菌Halomonas sp.IW11-1(AB305262.1)的序列同源性达到99%,表明菌株MD5为1株盐单胞属细菌。本研究分离得到的菌株MD5在厌氧和好氧条件下均具有较强的反硝化能力,对海洋沉积物脱氮具有一定的意义。     

Chemolithotrophic sulfur bacteria in sediments,mats, and stromatolites of western Australian saline lakes

Samples of stromatolites, microbial mats, and sediments from four saline lakes (approximate seasonal salinity ranges 20–220%o) in Western Australia were used to establish enrichments for elective cultures of aerobic and anaerobic denitrifying chemolithoautotrophs that could grow with thiosulfate as sole energy source. Organisms of these types were obtained from all sources tested. Twenty‐four pure cultures were isolated, all of which were gram‐negative, rod‐shaped bacteria exhibiting a considerable diversity of metabolic capability. Isolation of these obligate and facultative sulfur‐oxidizing chemolithotrophs from the stromatolite and mat habitats indicates the possibility that these rod‐shaped bacteria contribute to the oxidative phase of the sulfur cycle in these habitats, in addition to oxidation by phototrophs or Beggiatoa. Only four of the pure cultures could grow without salt, but all 24 showed significant halophily, some tolerating 3 M NaCl. Three novel isolates of NaCl‐dependent, thiosulfate‐oxidizing, aerobic and denitrifying obligate chemolithotrophs are described. In addition, a facultatively heterotrophic halophilic strain growing either methylotrophically on methylamine or chemolithotrophically on thiosulfate aerobically or with anaerobic denitrification was found.     

Anaerobic and aerobic degradation of pyridine by a newly isolated denitrifying bacterium.

New denitrifying bacteria that could degrade pyridine under both aerobic and anaerobic conditions were isolated from industrial wastewater. The successful enrichment and isolation of these strains required selenite as a trace element. These isolates appeared to be closely related to Azoarcus species according to the results of 16S rRNA sequence analysis. An isolated strain, pF6, metabolized pyridine through the same pathway under both aerobic and anaerobic conditions. Since pyridine induced NAD-linked glutarate-dialdehyde dehydrogenase and isocitratase activities, it is likely that the mechanism of pyridine degradation in strain pF6 involves N-C-2 ring cleavage. Strain pF6 could degrade pyridine in the presence of nitrate, nitrite, and nitrous oxide as electron acceptors. In a batch culture with 6 mM nitrate, degradation of pyridine and denitrification were not sensitively affected by the redox potential, which gradually decreased from 150 to -200 mV. In a batch culture with the nitrate concentration higher than 6 mM, nitrite transiently accumulated during denitrification significantly inhibited cell growth and pyridine degradation. Growth yield on pyridine decreased slightly under denitrifying conditions from that under aerobic conditions. Furthermore, when the pyridine concentration used was above 12 mM, the specific growth rate under denitrifying conditions was higher than that under aerobic conditions. Considering these characteristics, a newly isolated denitrifying bacterium, strain pF6, has advantages over strictly aerobic bacteria in field applications.     

好氧反硝化细菌碳氮代谢特点及途径的研究进展

好氧反硝化作用的发现打破了反硝化只能在严格厌氧条件下进行的传统认知,为生物脱氮提供了一条新的途径,已成为近些年的研究热点。碳源可为好氧反硝化过程提供能量和电子供体,其代谢难易程度直接影响着好氧反硝化细菌的脱氮效率,因此有必要明确碳源在好氧反硝化脱氮过程中的代谢机理。基于此,本文阐述了好氧反硝化细菌的种类及其对硝态氮与亚硝态氮的代谢途径;系统分析了不同好氧反硝化细菌对碳氮源代谢的差异与代谢机理;综合分析了碳代谢差异对好氧反硝化脱氮过程的影响,并对未来的研究方向进行了展望,旨在深入理解好氧反硝化细菌同时去除碳氮的机理,为提高废水生物脱氮除碳效率提供理论依据。     

好氧反硝化生物脱氮技术的研究进展

好氧反硝化生物脱氮技术自提出以来,凭借能实现同步硝化反硝化、节省基建投资及运行费用等诸多优点,受到国内外环境领域学者的广泛关注。本文首先总结了近年来好氧反硝化菌种的筛选分离情况,以及环境因子对好氧反硝化菌脱氮效能的影响,包括溶解氧(dissolved oxygen,DO)、碳氮比(C/N)、温度等。然后深入探讨了好氧反硝化生物脱氮技术的原理,好氧反硝化过程中的关键功能基因及酶,同时介绍了分子生物技术在好氧反硝化研究过程中的应用,以及好氧反硝化生物脱氮技术在实际应用方面的研究现状。最后,基于目前的研究瓶颈问题,对未来好氧反硝化生物脱氮技术的研究方向提出了科学展望。     

The denitrification potential and density of denitrifying bacteria in the bottom sediments of Matupi Harbor (Papua New Guinea)

The denitrification potential and density of denitrifying bacteria were determined in suboxidized sediments of Matupi Harbor (Papua New Guinea). The sediments were characterized by low denitrification potentials, not exceeding 0.8 nM/(g h). The maximum density of denitrifying bacteria was recorded in the upper sediment horizons and was 10⁴ cells/g of wet ground.     

Denitrification under various aeration conditions in Comamonas sp., strain SGLY2

Abstract A number of bacteria were isolated from different anoxic reactors. Those having denitrifying potential were tested for their ability to denitrify under aerobic conditions. The activity of their denitrifying enzymes varied from partial inactivation by oxygen (strains NO2B9 and TCET1) to oxygen-independent activity in a strain named SGLY2 which was tentatively identified as Comamonas sp. The effect of different aeration conditions on growth and on denitrification of SGLY2 was studied more extensively. This strain was able to consume oxygen and nitrate simultaneously with the production of nitrogen and without build-up of nitrite. The dissimilatory nitrate-reductase of nitrate-adapted cells was found to be more active in the presence of oxygen than in micro-aerobic or strictly anaerobic conditions.     

Response of denitrification rate associated with wetting and drying cycles in a littoral wetland area of Lake Biwa,Japan

To clarify the relationship between denitrification activity and dry–wet levels in the littoral wetland sediments of Lake Biwa, Japan, denitrification rates and their regulating parameters (degree of dryness, redox potential, nitrate concentration) were measured on different moisture sediments. Redox potential in sediments was higher in the exposed region in contact with atmosphere than the flooded region covered with water. The nitrate concentration in interstitial waters was undetectable in the flooded region. On the other hand, concentration in the exposed region increased with increase in the degree of sediment dryness. The denitrification rate ranged from <0.001 to 0.88 μg N cm⁻³ h⁻¹ in the exposed region and increased with the increase in the degree of dryness. In the flooded region, on the other hand, no detectable rate (<0.001 μg N cm⁻³ h⁻¹) was observed. This indicates that the rates in the exposed region were mainly influenced by nitrate concentration in the interstitial waters accumulated by desiccation of sediments, whereas rates in the flooded region were strongly limited by no accumulation of nitrate in the anaerobic conditions. The potential denitrification rate, under the application condition of nitrate, ranged from 0.13 to 0.26 μg N cm⁻³ h⁻¹ in the flooded region and from 0.77 to 1.5 μg N cm⁻³ h⁻¹ in the exposed region. The potential rates in the flooded region had a tendency to be lower than those in the exposed region, implying that the number of denitrifying bacteria in the flooded region was low due to inactivation of aerobic respiration and denitrification in the denitrifying bacteria community. Kinetic parameters, maximum rate (V _max) and half-saturation constant (K _s) for denitrification were calculated on the experimental procedures of the wetting–drying cycles of sediments. Both parameters decreased by the wetting treatment and increased by the drying treatment. The fluctuation of V _max values with wetting–drying cycles indicated that the number of denitrifying bacteria was influenced by aerobic respiration and denitrification in the denitrifying bacteria community similar to the potential rates, and denitrifying enzyme was induced by the nitrate supplied by nitrification accelerated through the drying process. On the other hand, the fluctuation of K _s values implied that members of denitrifying bacteria were shifted to members of high nitrate affinity by wetting treatment and of low nitrate affinity by drying treatment.     

Structure and activity of lacustrine sediment bacteria involved in nutrient and iron cycles

Knowledge of the bacterial community structure in sediments is essential to better design restoration strategies for eutrophied lakes. In this regard, the aim of this study was to quantify the abundance and activity of bacteria involved in nutrient and iron cycling in sediments from four Azorean lakes with distinct trophic states (Verde, Azul, Furnas and Fogo). Inferred from quantitative PCR, bacteria performing anaerobic ammonia oxidation were the most abundant in the eutrophic lakes Verde, Azul and Furnas (4.5-16.6%), followed by nitrifying bacteria (0.8-13.0%), denitrifying bacteria (DNB) (0.5-6.8%), iron-reducing bacteria (0.2-1.4%) and phosphorus-accumulating organisms (<0.3%). In contrast, DNB dominated sediments from the oligo-mesotrophic lake Fogo (8.8%). Activity assays suggested that bacteria performing ammonia oxidation (aerobic and anaerobic), nitrite oxidation, heterothrophic nitrate reduction, iron reduction and biological phosphorus storage/release were present and active in all Azorean lake sediments. The present work also suggested that the activity of DNB might contribute to the release of phosphorus from sediments.     

Distribution of putative denitrifying methane oxidizing bacteria in sediment of a freshwater lake, Lake Biwa

Methane oxidation coupled to denitrification is mediated by 'Candidatus Methylomirabilis oxyfera', which belongs to the candidate phylum NC10. The distribution of putative denitrifying methane-oxidizing bacteria related to "M. oxyfera" was investigated in a freshwater lake, Lake Biwa, Japan. In the surface layer of the sediment from a profundal site, a phylotype closely related to "M. oxyfera" was most frequently detected among NC10 bacteria in PCR analysis of the 16S rRNA gene. In the sediment, sequences related to "M. oxyfera" were also detected in a pmoA gene library. The presence of NC10 bacteria was also confirmed by catalyzed reporter deposition fluorescence in situ hybridization (CARD-FISH). Denaturing gradient gel electrophoresis (DGGE) and quantitative real-time PCR indicated that the abundance of the "M. oxyfera"-related phylotype was higher in the upper layers of the profundal sediment. The horizontal distribution of the putative methanotrophs in lake sediment was also analyzed by DGGE, which revealed that their occurrence was restricted to deep water areas. These results agreed with those in a previous study of another freshwater lake, and suggested that the upper layer of the profundal sediments is the main habitat for denitrifying methanotrophs.